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		<title>Феннер, Кларенс Норман - История изменений</title>
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		<updated>2026-04-10T10:57:56Z</updated>
		<subtitle>История изменений этой страницы в вики</subtitle>
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	<entry>
		<id>https://wiki.web.ru/index.php?title=%D0%A4%D0%B5%D0%BD%D0%BD%D0%B5%D1%80,_%D0%9A%D0%BB%D0%B0%D1%80%D0%B5%D0%BD%D1%81_%D0%9D%D0%BE%D1%80%D0%BC%D0%B0%D0%BD&amp;diff=61189&amp;oldid=prev</id>
		<title>Виктор Слётов в 19:41, 30 июня 2012</title>
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				<updated>2012-06-30T19:41:13Z</updated>
		
		<summary type="html">&lt;p&gt;&lt;/p&gt;

		&lt;table style=&quot;background-color: white; color:black;&quot;&gt;
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		&lt;td colspan='2' style=&quot;background-color: white; color:black;&quot;&gt;← Предыдущая&lt;/td&gt;
		&lt;td colspan='2' style=&quot;background-color: white; color:black;&quot;&gt;Версия 19:41, 30 июня 2012&lt;/td&gt;
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		&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Строка 58:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Строка 58:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;#Pleistocene&amp;nbsp; climate and topography of the Arequipa region,&amp;nbsp; Peru: Geotr.&amp;nbsp; Soc.&amp;nbsp; Amer., Bull.59,895-917 (1948).&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;#Pleistocene&amp;nbsp; climate and topography of the Arequipa region,&amp;nbsp; Peru: Geotr.&amp;nbsp; Soc.&amp;nbsp; Amer., Bull.59,895-917 (1948).&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;#The chemical kinetics of&amp;nbsp; the Katmai&amp;nbsp; explosion:&amp;nbsp; Amer. J.&amp;nbsp; Sci.,248, pt.I,&amp;nbsp; pp.&amp;nbsp; 593-627; pt.II,&amp;nbsp; pp. 697-725 (1950). (Published posthumously.)&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;#The chemical kinetics of&amp;nbsp; the Katmai&amp;nbsp; explosion:&amp;nbsp; Amer. J.&amp;nbsp; Sci.,248, pt.I,&amp;nbsp; pp.&amp;nbsp; 593-627; pt.II,&amp;nbsp; pp. 697-725 (1950). (Published posthumously.)&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;nbsp;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;color: red; font-weight: bold; text-decoration: none;&quot;&gt;&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;nbsp;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;color: red; font-weight: bold; text-decoration: none;&quot;&gt;[[Category:Биографии ученых]]&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
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&lt;/table&gt;</summary>
		<author><name>Виктор Слётов</name></author>	</entry>

	<entry>
		<id>https://wiki.web.ru/index.php?title=%D0%A4%D0%B5%D0%BD%D0%BD%D0%B5%D1%80,_%D0%9A%D0%BB%D0%B0%D1%80%D0%B5%D0%BD%D1%81_%D0%9D%D0%BE%D1%80%D0%BC%D0%B0%D0%BD&amp;diff=23233&amp;oldid=prev</id>
		<title>Pavel в 13:27, 23 января 2009</title>
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				<updated>2009-01-23T13:27:05Z</updated>
		
		<summary type="html">&lt;p&gt;&lt;/p&gt;

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		&lt;td colspan='2' style=&quot;background-color: white; color:black;&quot;&gt;← Предыдущая&lt;/td&gt;
		&lt;td colspan='2' style=&quot;background-color: white; color:black;&quot;&gt;Версия 13:27, 23 января 2009&lt;/td&gt;
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		&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Строка 1:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Строка 1:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;nbsp;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;color: red; font-weight: bold; text-decoration: none;&quot;&gt;[[Изображение:Fenner CN.jpg|thumb|right|К.Н.Феннер]]&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;Феннер Кларенс Норман {{англ|Fenner Clarence Norman}}( родился 19.07.1870, Клифтон, штат Нью-Джерси, умер 24.12.1949, там же), американский геолог-минералог и петрограф. &amp;nbsp;&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;Феннер Кларенс Норман {{англ|Fenner Clarence Norman}}( родился 19.07.1870, Клифтон, штат Нью-Джерси, умер 24.12.1949, там же), американский геолог-минералог и петрограф. &amp;nbsp;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
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&lt;/table&gt;</summary>
		<author><name>Pavel</name></author>	</entry>

	<entry>
		<id>https://wiki.web.ru/index.php?title=%D0%A4%D0%B5%D0%BD%D0%BD%D0%B5%D1%80,_%D0%9A%D0%BB%D0%B0%D1%80%D0%B5%D0%BD%D1%81_%D0%9D%D0%BE%D1%80%D0%BC%D0%B0%D0%BD&amp;diff=23231&amp;oldid=prev</id>
		<title>Pavel в 11:58, 23 января 2009</title>
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				<updated>2009-01-23T11:58:49Z</updated>
		
		<summary type="html">&lt;p&gt;&lt;/p&gt;

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		&lt;td colspan='2' style=&quot;background-color: white; color:black;&quot;&gt;← Предыдущая&lt;/td&gt;
		&lt;td colspan='2' style=&quot;background-color: white; color:black;&quot;&gt;Версия 11:58, 23 января 2009&lt;/td&gt;
		&lt;/tr&gt;
		&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Строка 49:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Строка 49:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;#Tuffs&amp;nbsp; and&amp;nbsp; other&amp;nbsp; volcanic&amp;nbsp; deposits of Katmai&amp;nbsp; and Yellowstone&amp;nbsp; Park: Trans.&amp;nbsp; Am.&amp;nbsp; Geophys. Union,&amp;nbsp; l8th&amp;nbsp; Ann.&amp;nbsp; Meeting, pp.236-239 (1937)&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;#Tuffs&amp;nbsp; and&amp;nbsp; other&amp;nbsp; volcanic&amp;nbsp; deposits of Katmai&amp;nbsp; and Yellowstone&amp;nbsp; Park: Trans.&amp;nbsp; Am.&amp;nbsp; Geophys. Union,&amp;nbsp; l8th&amp;nbsp; Ann.&amp;nbsp; Meeting, pp.236-239 (1937)&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;#Olivine&amp;nbsp; fourchites&amp;nbsp; from&amp;nbsp; Raymond&amp;nbsp; Fosdick&amp;nbsp; Mountains,&amp;nbsp; Antarctica:&amp;nbsp; Geol. Soc.Amer.,Bull.49, 367-400 (1938).&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;#Olivine&amp;nbsp; fourchites&amp;nbsp; from&amp;nbsp; Raymond&amp;nbsp; Fosdick&amp;nbsp; Mountains,&amp;nbsp; Antarctica:&amp;nbsp; Geol. Soc.Amer.,Bull.49, 367-400 (1938).&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;nbsp;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;color: red; font-weight: bold; text-decoration: none;&quot;&gt;#The phenomena&amp;nbsp; of&amp;nbsp; Falling Mountain:&amp;nbsp; Am.&amp;nbsp; J.&amp;nbsp; Sci.&amp;nbsp; (5),35-A,&amp;nbsp; 35-48&amp;nbsp; (193S). Contact&amp;nbsp; relations&amp;nbsp; between rhyolite&amp;nbsp; and&amp;nbsp; basalt&amp;nbsp; on Gardiner&amp;nbsp; River,&amp;nbsp; Yellowstone&amp;nbsp; Park:&amp;nbsp; Geol,.Soc.&amp;nbsp; Amer., Bull.. 49, 1441-1483&amp;nbsp; (1938).&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;nbsp;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;color: red; font-weight: bold; text-decoration: none;&quot;&gt;#Geologia&amp;nbsp; de&amp;nbsp; los&amp;nbsp; Alrededores&amp;nbsp; de&amp;nbsp; Arequipa.&amp;nbsp; Universidad&amp;nbsp; de&amp;nbsp; San&amp;nbsp; Augustin&amp;nbsp; de&amp;nbsp; Arequipa.(Translation&amp;nbsp; by&amp;nbsp; Carlos&amp;nbsp; Nicholson,&amp;nbsp; Professor&amp;nbsp; in&amp;nbsp; the&amp;nbsp; University),&amp;nbsp; pp.&amp;nbsp; 164-206,&amp;nbsp; pl.&amp;nbsp; 25 (1940).&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;nbsp;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;color: red; font-weight: bold; text-decoration: none;&quot;&gt;#The nature of&amp;nbsp; the ore-forming fluid;&amp;nbsp; a discussion:&amp;nbsp; Econ. Geol.,35, 883-904 (1940).&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;nbsp;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;color: red; font-weight: bold; text-decoration: none;&quot;&gt;#Rhyolite&amp;nbsp; basalt complex on Gardiner River,&amp;nbsp; Yellowstone Park, Wyoming;&amp;nbsp; a&amp;nbsp; discussion: Geol.&amp;nbsp; Soc.&amp;nbsp; Amer.,&amp;nbsp; BuIl.55,&amp;nbsp; 1081-1096&amp;nbsp; (1944).&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;nbsp;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;color: red; font-weight: bold; text-decoration: none;&quot;&gt;#Immiscibility&amp;nbsp; of igneous magmas: Am. J.Sci.,246,465-502 (1948).&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;nbsp;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;color: red; font-weight: bold; text-decoration: none;&quot;&gt;#Incandescent&amp;nbsp; tuff&amp;nbsp; flows in&amp;nbsp; Southern Pent: Geol.&amp;nbsp; Soc.&amp;nbsp; Amer., Bull.59,879-893 (1948).&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;nbsp;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;color: red; font-weight: bold; text-decoration: none;&quot;&gt;#Pleistocene&amp;nbsp; climate and topography of the Arequipa region,&amp;nbsp; Peru: Geotr.&amp;nbsp; Soc.&amp;nbsp; Amer., Bull.59,895-917 (1948).&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;nbsp;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;color: red; font-weight: bold; text-decoration: none;&quot;&gt;#The chemical kinetics of&amp;nbsp; the Katmai&amp;nbsp; explosion:&amp;nbsp; Amer. J.&amp;nbsp; Sci.,248, pt.I,&amp;nbsp; pp.&amp;nbsp; 593-627; pt.II,&amp;nbsp; pp. 697-725 (1950). (Published posthumously.)&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
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&lt;/table&gt;</summary>
		<author><name>Pavel</name></author>	</entry>

	<entry>
		<id>https://wiki.web.ru/index.php?title=%D0%A4%D0%B5%D0%BD%D0%BD%D0%B5%D1%80,_%D0%9A%D0%BB%D0%B0%D1%80%D0%B5%D0%BD%D1%81_%D0%9D%D0%BE%D1%80%D0%BC%D0%B0%D0%BD&amp;diff=23230&amp;oldid=prev</id>
		<title>Pavel в 11:56, 23 января 2009</title>
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				<updated>2009-01-23T11:56:05Z</updated>
		
		<summary type="html">&lt;p&gt;&lt;/p&gt;

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		&lt;td colspan='2' style=&quot;background-color: white; color:black;&quot;&gt;← Предыдущая&lt;/td&gt;
		&lt;td colspan='2' style=&quot;background-color: white; color:black;&quot;&gt;Версия 11:56, 23 января 2009&lt;/td&gt;
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		&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Строка 11:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Строка 11:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;#The&amp;nbsp; crystallization&amp;nbsp; of a basaltic magma&amp;nbsp; from&amp;nbsp; the standpoint&amp;nbsp; of physical&amp;nbsp; chemistry:&amp;nbsp; Am. J.Sci.(4), 29,&amp;nbsp; 217-234&amp;nbsp; (1910).&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;#The&amp;nbsp; crystallization&amp;nbsp; of a basaltic magma&amp;nbsp; from&amp;nbsp; the standpoint&amp;nbsp; of physical&amp;nbsp; chemistry:&amp;nbsp; Am. J.Sci.(4), 29,&amp;nbsp; 217-234&amp;nbsp; (1910).&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;#A&amp;nbsp; replacement&amp;nbsp; of&amp;nbsp; rhyolite&amp;nbsp; porphyry&amp;nbsp; by&amp;nbsp; stephanite&amp;nbsp; and&amp;nbsp; chalcopyrite&amp;nbsp; at&amp;nbsp; Leadville,&amp;nbsp; Colorado:&amp;nbsp; Colorado&amp;nbsp; Sch. of Mines&amp;nbsp; Quart.,3l,235-240 (1910).&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;#A&amp;nbsp; replacement&amp;nbsp; of&amp;nbsp; rhyolite&amp;nbsp; porphyry&amp;nbsp; by&amp;nbsp; stephanite&amp;nbsp; and&amp;nbsp; chalcopyrite&amp;nbsp; at&amp;nbsp; Leadville,&amp;nbsp; Colorado:&amp;nbsp; Colorado&amp;nbsp; Sch. of Mines&amp;nbsp; Quart.,3l,235-240 (1910).&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;-&lt;/td&gt;&lt;td style=&quot;background: #ffa; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;#The&amp;nbsp; Watchung&amp;nbsp; basalt&amp;nbsp; and&amp;nbsp; the&amp;nbsp; paragenesis of&amp;nbsp; its&amp;nbsp; zeolites and&amp;nbsp; other&amp;nbsp; secondary&amp;nbsp; minerals:&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;#The&amp;nbsp; Watchung&amp;nbsp; basalt&amp;nbsp; and&amp;nbsp; the&amp;nbsp; paragenesis of&amp;nbsp; its&amp;nbsp; zeolites and&amp;nbsp; other&amp;nbsp; secondary&amp;nbsp; minerals: &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;New &lt;/ins&gt;York Acad.&amp;nbsp; of Sci., 22, 2,&amp;nbsp; pt.&amp;nbsp; 2, 93-187&amp;nbsp; (1910).&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;-&lt;/td&gt;&lt;td style=&quot;background: #ffa; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;Neu&amp;nbsp; &lt;/del&gt;York Acad.&amp;nbsp; of Sci., 22, 2,&amp;nbsp; pt.&amp;nbsp; 2, 93-187&amp;nbsp; (1910).&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;#Study of a contact metamorphic&amp;nbsp; ore deposit. The Dolores Mine&amp;nbsp; at&amp;nbsp; Matehuala, S.L.P., Mexico&amp;nbsp; (with J. B.&amp;nbsp; Spurr and G. H.&amp;nbsp; Garrey): Econ. Geol.,7,444-484&amp;nbsp; (1912).&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;-&lt;/td&gt;&lt;td style=&quot;background: #ffa; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;#Study of a contact metamorphic&amp;nbsp; ore deposit. The Dolores Mine&amp;nbsp; at&amp;nbsp; Matehuala, S.L.P., Mexico&amp;nbsp; (with &amp;nbsp;&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;#Petrographic&amp;nbsp; study&amp;nbsp; of&amp;nbsp; the&amp;nbsp; specimens of&amp;nbsp; loess,&amp;nbsp; terra&amp;nbsp; cocida,&amp;nbsp; and&amp;nbsp; scoria&amp;nbsp; collected&amp;nbsp; by&amp;nbsp; the Hrdlicka-Willis&amp;nbsp; Expedition&amp;nbsp; (with&amp;nbsp; F.&amp;nbsp; E.&amp;nbsp; Wright):&amp;nbsp; Bull.52,&amp;nbsp; Bur.&amp;nbsp; Amer.&amp;nbsp; Ethnology, Smithsonian Institution,&amp;nbsp; pp. 55-98 (1912).&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;-&lt;/td&gt;&lt;td style=&quot;background: #ffa; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;J. B.&amp;nbsp; Spurr and G. H.&amp;nbsp; Garrey): Econ. Geol.,7,444-484&amp;nbsp; (1912).&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;-&lt;/td&gt;&lt;td style=&quot;background: #ffa; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;#Petrographic&amp;nbsp; study&amp;nbsp; of&amp;nbsp; the&amp;nbsp; specimens of&amp;nbsp; loess,&amp;nbsp; terra&amp;nbsp; cocida,&amp;nbsp; and&amp;nbsp; scoria&amp;nbsp; collected&amp;nbsp; by&amp;nbsp; the&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;-&lt;/td&gt;&lt;td style=&quot;background: #ffa; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;Hrdlicka-Willis&amp;nbsp; Expedition&amp;nbsp; (with&amp;nbsp; F.&amp;nbsp; E.&amp;nbsp; Wright):&amp;nbsp; Bull.52,&amp;nbsp; Bur.&amp;nbsp; Amer.&amp;nbsp; Ethnology, Smithsonian Institution,&amp;nbsp; pp. 55-98 (1912).&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;#The&amp;nbsp; various forms of&amp;nbsp; silica and&amp;nbsp; their&amp;nbsp; mutual&amp;nbsp; relations: J.Wash.&amp;nbsp; Acad.Sci.,2, 47l-48O (1912).&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;#The&amp;nbsp; various forms of&amp;nbsp; silica and&amp;nbsp; their&amp;nbsp; mutual&amp;nbsp; relations: J.Wash.&amp;nbsp; Acad.Sci.,2, 47l-48O (1912).&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;#The&amp;nbsp; stability&amp;nbsp; relations of&amp;nbsp; the silica minerals. Am.&amp;nbsp; J.&amp;nbsp; Sci. (4), 36,&amp;nbsp; 331-384 (1913). Die StabilitAtsbeziehungen&amp;nbsp; der&amp;nbsp; Kieselsiiuremineralien:&amp;nbsp; Z.&amp;nbsp; Anorg.&amp;nbsp; Chem.,&amp;nbsp; 85,&amp;nbsp; 133-197 (1914),&amp;nbsp; (translation&amp;nbsp; of&amp;nbsp; the&amp;nbsp; foregoing&amp;nbsp; paper).&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;#The&amp;nbsp; stability&amp;nbsp; relations of&amp;nbsp; the silica minerals. Am.&amp;nbsp; J.&amp;nbsp; Sci. (4), 36,&amp;nbsp; 331-384 (1913). Die StabilitAtsbeziehungen&amp;nbsp; der&amp;nbsp; Kieselsiiuremineralien:&amp;nbsp; Z.&amp;nbsp; Anorg.&amp;nbsp; Chem.,&amp;nbsp; 85,&amp;nbsp; 133-197 (1914),&amp;nbsp; (translation&amp;nbsp; of&amp;nbsp; the&amp;nbsp; foregoing&amp;nbsp; paper).&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Строка 23:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Строка 20:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;#Additional notes&amp;nbsp; on babingtonite&amp;nbsp; from Passaic&amp;nbsp; County, New Jersey:&amp;nbsp; J.Wash.Acad.Sci., 4, 598-605 (1914).&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;#Additional notes&amp;nbsp; on babingtonite&amp;nbsp; from Passaic&amp;nbsp; County, New Jersey:&amp;nbsp; J.Wash.Acad.Sci., 4, 598-605 (1914).&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;#The ternary&amp;nbsp; system&amp;nbsp; H2O-H2SiO3-SiO2&amp;nbsp; (with G.W.Morey): J.Am.Chem.Soc. ,39,1173-1209&amp;nbsp; (1917).&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;#The ternary&amp;nbsp; system&amp;nbsp; H2O-H2SiO3-SiO2&amp;nbsp; (with G.W.Morey): J.Am.Chem.Soc. ,39,1173-1209&amp;nbsp; (1917).&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;-&lt;/td&gt;&lt;td style=&quot;background: #ffa; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;#The effect&amp;nbsp; of certain impurities&amp;nbsp; in causing&amp;nbsp; milkiness in optical glass&amp;nbsp; (with J.B.Ferguson):&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;#The effect&amp;nbsp; of certain impurities&amp;nbsp; in causing&amp;nbsp; milkiness in optical glass&amp;nbsp; (with J.B.Ferguson): J.Amer.Ceram.Soc.,1,468-476 (1918).&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;-&lt;/td&gt;&lt;td style=&quot;background: #ffa; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;J.Amer.Ceram.Soc.,1,468-476 (1918).&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;#The&amp;nbsp; technique&amp;nbsp; of optical&amp;nbsp; glass&amp;nbsp; melting: J.Amer.Ceram. Soc.,2, 102-145&amp;nbsp; (1919).&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;#The&amp;nbsp; technique&amp;nbsp; of optical&amp;nbsp; glass&amp;nbsp; melting: J.Amer.Ceram. Soc.,2, 102-145&amp;nbsp; (1919).&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;#The use of optical pyrometers&amp;nbsp; for control of optical giass&amp;nbsp; furnaces:&amp;nbsp; Bull.Inst.Min.Met.Eng, 1919, 1001-1011&amp;nbsp; ; also&amp;nbsp; Pyrometry&amp;nbsp; Volume,&amp;nbsp; 495-505 (1920).&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;#The use of optical pyrometers&amp;nbsp; for control of optical giass&amp;nbsp; furnaces:&amp;nbsp; Bull.Inst.Min.Met.Eng, 1919, 1001-1011&amp;nbsp; ; also&amp;nbsp; Pyrometry&amp;nbsp; Volume,&amp;nbsp; 495-505 (1920).&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;#The relations&amp;nbsp; between tridymite and cristobalite:&amp;nbsp; J. Soc. Glass Tech.,3,&amp;nbsp; Trans., 116-125 (1919).&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;#The relations&amp;nbsp; between tridymite and cristobalite:&amp;nbsp; J. Soc. Glass Tech.,3,&amp;nbsp; Trans., 116-125 (1919).&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;#The Katmai region,&amp;nbsp; Alaska,&amp;nbsp; and&amp;nbsp; the great&amp;nbsp; eruption&amp;nbsp; of 19l2:&amp;nbsp; J. Geol.,28, 569-606&amp;nbsp; (1920).&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;#The Katmai region,&amp;nbsp; Alaska,&amp;nbsp; and&amp;nbsp; the great&amp;nbsp; eruption&amp;nbsp; of 19l2:&amp;nbsp; J. Geol.,28, 569-606&amp;nbsp; (1920).&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;-&lt;/td&gt;&lt;td style=&quot;background: #ffa; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;#The origin and mode of emplacement&amp;nbsp; of&amp;nbsp; the great tufi&amp;nbsp; deposit&amp;nbsp; in&amp;nbsp; the valley of&amp;nbsp; the Ten Thousand&amp;nbsp; Smokes: &lt;del class=&quot;diffchange diffchange-inline&quot;&gt; &lt;/del&gt;Not.Geogr. Soc. Contributed Technical&amp;nbsp; Paper l, l-74&amp;nbsp; (1923)&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;#The origin and mode of emplacement&amp;nbsp; of&amp;nbsp; the great tufi&amp;nbsp; deposit&amp;nbsp; in&amp;nbsp; the valley of&amp;nbsp; the Ten Thousand&amp;nbsp; Smokes: Not.Geogr. Soc. Contributed Technical&amp;nbsp; Paper l, l-74&amp;nbsp; (1923)&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;#Earth movements&amp;nbsp; accompanying&amp;nbsp; the Katmai eruption:&amp;nbsp; J.&amp;nbsp; Geol.,33,116-139; 193-233(1925).&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;#Earth movements&amp;nbsp; accompanying&amp;nbsp; the Katmai eruption:&amp;nbsp; J.&amp;nbsp; Geol.,33,116-139; 193-233(1925).&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;#Magmatic&amp;nbsp; problems of the Aleutians:&amp;nbsp; Nat. Res. Council,&amp;nbsp; Bull., 44, vol.2, pt.2, 124-727 (1926).&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;#Magmatic&amp;nbsp; problems of the Aleutians:&amp;nbsp; Nat. Res. Council,&amp;nbsp; Bull., 44, vol.2, pt.2, 124-727 (1926).&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;#The Katmai&amp;nbsp; magmatic province: J.Geol.,34,673-772 (1926).&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;#The Katmai&amp;nbsp; magmatic province: J.Geol.,34,673-772 (1926).&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;#An unusual occurrence of albite:&amp;nbsp; Am.&amp;nbsp; Mineral.,11,255-259 (1926).&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;#An unusual occurrence of albite:&amp;nbsp; Am.&amp;nbsp; Mineral.,11,255-259 (1926).&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;-&lt;/td&gt;&lt;td style=&quot;background: #ffa; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;#The&amp;nbsp; analytical&amp;nbsp; determination&amp;nbsp; of uranium,&amp;nbsp; thorium,&amp;nbsp; and lead as a basis&amp;nbsp; for&amp;nbsp; age&amp;nbsp; calculations:&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;#The&amp;nbsp; analytical&amp;nbsp; determination&amp;nbsp; of uranium,&amp;nbsp; thorium,&amp;nbsp; and lead as a basis&amp;nbsp; for&amp;nbsp; age&amp;nbsp; calculations: Am. J.Sci.(5),16, 369-381 (1928).&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;-&lt;/td&gt;&lt;td style=&quot;background: #ffa; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;Am. J.Sci.(5),16, 369-381 (1928).&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;#&lt;/ins&gt;Radioactive&amp;nbsp; &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;minerals from &lt;/ins&gt; Divino&amp;nbsp; de Uba, Brazil:&amp;nbsp; Am.J.Sci.(5),16,382-39I&amp;nbsp; (1928)&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;-&lt;/td&gt;&lt;td style=&quot;background: #ffa; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;Radioactive&amp;nbsp; &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;mineralsfrom &lt;/del&gt; Divino&amp;nbsp; de Uba, Brazil:&amp;nbsp; Am.J.Sci.(5),16,382-39I&amp;nbsp; (1928)&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;#The&amp;nbsp; mass spectrum of&amp;nbsp; lead from&amp;nbsp; Broggerite&amp;nbsp; (with&amp;nbsp; C.S.Piggot): Nature,123,793-794 (1929)&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;#The&amp;nbsp; mass spectrum of&amp;nbsp; lead from&amp;nbsp; Broggerite&amp;nbsp; (with&amp;nbsp; C.S.Piggot): Nature,123,793-794 (1929)&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;#The&amp;nbsp; crystallization&amp;nbsp; of&amp;nbsp; basalts: Am. J.Sci.,18,225-253 (1929)&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;#The&amp;nbsp; crystallization&amp;nbsp; of&amp;nbsp; basalts: Am. J.Sci.,18,225-253 (1929)&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
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		<author><name>Pavel</name></author>	</entry>

	<entry>
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		<title>Pavel в 11:54, 23 января 2009</title>
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				<updated>2009-01-23T11:54:13Z</updated>
		
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		&lt;td colspan='2' style=&quot;background-color: white; color:black;&quot;&gt;Версия 11:54, 23 января 2009&lt;/td&gt;
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		&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Строка 38:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Строка 38:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;Radioactive&amp;nbsp; mineralsfrom&amp;nbsp; Divino&amp;nbsp; de Uba, Brazil:&amp;nbsp; Am.J.Sci.(5),16,382-39I&amp;nbsp; (1928)&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;Radioactive&amp;nbsp; mineralsfrom&amp;nbsp; Divino&amp;nbsp; de Uba, Brazil:&amp;nbsp; Am.J.Sci.(5),16,382-39I&amp;nbsp; (1928)&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;#The&amp;nbsp; mass spectrum of&amp;nbsp; lead from&amp;nbsp; Broggerite&amp;nbsp; (with&amp;nbsp; C.S.Piggot): Nature,123,793-794 (1929)&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;#The&amp;nbsp; mass spectrum of&amp;nbsp; lead from&amp;nbsp; Broggerite&amp;nbsp; (with&amp;nbsp; C.S.Piggot): Nature,123,793-794 (1929)&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;nbsp;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;color: red; font-weight: bold; text-decoration: none;&quot;&gt;#The&amp;nbsp; crystallization&amp;nbsp; of&amp;nbsp; basalts: Am. J.Sci.,18,225-253 (1929)&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;nbsp;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;color: red; font-weight: bold; text-decoration: none;&quot;&gt;#Mount&amp;nbsp; Karmai&amp;nbsp; and Mount&amp;nbsp; Mageik:&amp;nbsp; Z.&amp;nbsp; Vulkanology,13,1-24,16 pl.(1930).&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;nbsp;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;color: red; font-weight: bold; text-decoration: none;&quot;&gt;#The&amp;nbsp; significance&amp;nbsp; of&amp;nbsp; the word 'eutectic':&amp;nbsp; J.Geol.,38,159-165 (1930).&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;nbsp;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;color: red; font-weight: bold; text-decoration: none;&quot;&gt;#The Engels copper deposits, California:&amp;nbsp; Econ.Geol.,25,420-425&amp;nbsp; (1930). (Discussion&amp;nbsp; of&amp;nbsp; the article&amp;nbsp; by&amp;nbsp; A.&amp;nbsp; Knopf&amp;nbsp; and&amp;nbsp; C. A.&amp;nbsp; Anderson.)&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;nbsp;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;color: red; font-weight: bold; text-decoration: none;&quot;&gt;#The&amp;nbsp; residual&amp;nbsp; liquids of crystallizing magmas: Mineral. Mag.,22,539-560 (1931)&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;nbsp;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;color: red; font-weight: bold; text-decoration: none;&quot;&gt;#The&amp;nbsp; age of a monazite crystal&amp;nbsp; from&amp;nbsp; Portland,&amp;nbsp; Connecticut: Am.J.Sci (5),23,327-333 (1932).&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;nbsp;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;color: red; font-weight: bold; text-decoration: none;&quot;&gt;#Pneumatolytic&amp;nbsp; processes&amp;nbsp; in&amp;nbsp; the&amp;nbsp; formation&amp;nbsp; of&amp;nbsp; minerals&amp;nbsp; and&amp;nbsp; ores. In&amp;nbsp; Ore&amp;nbsp; Deposits&amp;nbsp; of&amp;nbsp; the Western States,&amp;nbsp; pp. 58-106: Am.&amp;nbsp; Inst. Min.&amp;nbsp; Met. Eng.,&amp;nbsp; New York&amp;nbsp; (1933)&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;nbsp;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;color: red; font-weight: bold; text-decoration: none;&quot;&gt;#Some magmatic&amp;nbsp; problems : J.W ash. Acad.Sci.,24,113-124&amp;nbsp; (1934)&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;nbsp;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;color: red; font-weight: bold; text-decoration: none;&quot;&gt;#Henry&amp;nbsp; Stephens Washington:(1867-1934) Science,&amp;nbsp; n.s.,79,47-48 (1934)&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;nbsp;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;color: red; font-weight: bold; text-decoration: none;&quot;&gt;#Hydrothermal&amp;nbsp; metamorphism&amp;nbsp; in&amp;nbsp; geyser basins&amp;nbsp; of&amp;nbsp; Yellowstone&amp;nbsp; Park,&amp;nbsp; as shown&amp;nbsp; by&amp;nbsp; deep drilling:&amp;nbsp; Trans.&amp;nbsp; Am.&amp;nbsp; Geophys. Union.&amp;nbsp; I5th&amp;nbsp; Ann.&amp;nbsp; Meeting,&amp;nbsp; pp.240-243 (1934)&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;nbsp;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;color: red; font-weight: bold; text-decoration: none;&quot;&gt;#Life&amp;nbsp; History&amp;nbsp; of&amp;nbsp; the&amp;nbsp; Sudbury nickel&amp;nbsp; irruptive:&amp;nbsp; Geol.Mag.,72,381-382 (1935)&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;nbsp;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;color: red; font-weight: bold; text-decoration: none;&quot;&gt;#Review&amp;nbsp; and&amp;nbsp; discussion of Prof.Paper&amp;nbsp; 179 (U.&amp;nbsp; S. Geol.&amp;nbsp; survey) by&amp;nbsp; C.S.Ross on origin&amp;nbsp; of the&amp;nbsp; copper deposits of&amp;nbsp; the&amp;nbsp; Ducktown&amp;nbsp; type&amp;nbsp; in&amp;nbsp; the&amp;nbsp; Southern&amp;nbsp; Appalachian&amp;nbsp; region:&amp;nbsp; Economic Geol.,30, 928-936 (1935).&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;nbsp;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;color: red; font-weight: bold; text-decoration: none;&quot;&gt;#Bore-hole&amp;nbsp; investigations&amp;nbsp; in Yellowstone&amp;nbsp; Park: J. Geol,.,44,225-315 (1936)&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;nbsp;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;color: red; font-weight: bold; text-decoration: none;&quot;&gt;#A view of magmatic differentiation: J.Geol.,45,158-168 (1937)&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;nbsp;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;color: red; font-weight: bold; text-decoration: none;&quot;&gt;#Tuffs&amp;nbsp; and&amp;nbsp; other&amp;nbsp; volcanic&amp;nbsp; deposits of Katmai&amp;nbsp; and Yellowstone&amp;nbsp; Park: Trans.&amp;nbsp; Am.&amp;nbsp; Geophys. Union,&amp;nbsp; l8th&amp;nbsp; Ann.&amp;nbsp; Meeting, pp.236-239 (1937)&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;nbsp;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;color: red; font-weight: bold; text-decoration: none;&quot;&gt;#Olivine&amp;nbsp; fourchites&amp;nbsp; from&amp;nbsp; Raymond&amp;nbsp; Fosdick&amp;nbsp; Mountains,&amp;nbsp; Antarctica:&amp;nbsp; Geol. Soc.Amer.,Bull.49, 367-400 (1938).&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
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		<author><name>Pavel</name></author>	</entry>

	<entry>
		<id>https://wiki.web.ru/index.php?title=%D0%A4%D0%B5%D0%BD%D0%BD%D0%B5%D1%80,_%D0%9A%D0%BB%D0%B0%D1%80%D0%B5%D0%BD%D1%81_%D0%9D%D0%BE%D1%80%D0%BC%D0%B0%D0%BD&amp;diff=23228&amp;oldid=prev</id>
		<title>Pavel в 11:42, 23 января 2009</title>
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				<updated>2009-01-23T11:42:53Z</updated>
		
		<summary type="html">&lt;p&gt;&lt;/p&gt;

		&lt;table style=&quot;background-color: white; color:black;&quot;&gt;
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		&lt;td colspan='2' style=&quot;background-color: white; color:black;&quot;&gt;← Предыдущая&lt;/td&gt;
		&lt;td colspan='2' style=&quot;background-color: white; color:black;&quot;&gt;Версия 11:42, 23 января 2009&lt;/td&gt;
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		&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Строка 18:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Строка 18:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;Hrdlicka-Willis&amp;nbsp; Expedition&amp;nbsp; (with&amp;nbsp; F.&amp;nbsp; E.&amp;nbsp; Wright):&amp;nbsp; Bull.52,&amp;nbsp; Bur.&amp;nbsp; Amer.&amp;nbsp; Ethnology, Smithsonian Institution,&amp;nbsp; pp. 55-98 (1912).&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;Hrdlicka-Willis&amp;nbsp; Expedition&amp;nbsp; (with&amp;nbsp; F.&amp;nbsp; E.&amp;nbsp; Wright):&amp;nbsp; Bull.52,&amp;nbsp; Bur.&amp;nbsp; Amer.&amp;nbsp; Ethnology, Smithsonian Institution,&amp;nbsp; pp. 55-98 (1912).&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;#The&amp;nbsp; various forms of&amp;nbsp; silica and&amp;nbsp; their&amp;nbsp; mutual&amp;nbsp; relations: J.Wash.&amp;nbsp; Acad.Sci.,2, 47l-48O (1912).&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;#The&amp;nbsp; various forms of&amp;nbsp; silica and&amp;nbsp; their&amp;nbsp; mutual&amp;nbsp; relations: J.Wash.&amp;nbsp; Acad.Sci.,2, 47l-48O (1912).&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;nbsp;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;color: red; font-weight: bold; text-decoration: none;&quot;&gt;#The&amp;nbsp; stability&amp;nbsp; relations of&amp;nbsp; the silica minerals. Am.&amp;nbsp; J.&amp;nbsp; Sci. (4), 36,&amp;nbsp; 331-384 (1913). Die StabilitAtsbeziehungen&amp;nbsp; der&amp;nbsp; Kieselsiiuremineralien:&amp;nbsp; Z.&amp;nbsp; Anorg.&amp;nbsp; Chem.,&amp;nbsp; 85,&amp;nbsp; 133-197 (1914),&amp;nbsp; (translation&amp;nbsp; of&amp;nbsp; the&amp;nbsp; foregoing&amp;nbsp; paper).&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;nbsp;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;color: red; font-weight: bold; text-decoration: none;&quot;&gt;#The&amp;nbsp; mode&amp;nbsp; of&amp;nbsp; formation&amp;nbsp; of&amp;nbsp; certain&amp;nbsp; gneisses&amp;nbsp; in&amp;nbsp; the&amp;nbsp; highlands&amp;nbsp; of&amp;nbsp; New&amp;nbsp; Jersey: J.Geol.,22, 594-612; 694-702 (1914).&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;nbsp;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;color: red; font-weight: bold; text-decoration: none;&quot;&gt;#Babingtonite&amp;nbsp; from Passaic&amp;nbsp; County,&amp;nbsp; New Jersey:&amp;nbsp; J.Wash. Acad. Sci,4, 552-558&amp;nbsp; (1914).&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;nbsp;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;color: red; font-weight: bold; text-decoration: none;&quot;&gt;#Additional notes&amp;nbsp; on babingtonite&amp;nbsp; from Passaic&amp;nbsp; County, New Jersey:&amp;nbsp; J.Wash.Acad.Sci., 4, 598-605 (1914).&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;nbsp;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;color: red; font-weight: bold; text-decoration: none;&quot;&gt;#The ternary&amp;nbsp; system&amp;nbsp; H2O-H2SiO3-SiO2&amp;nbsp; (with G.W.Morey): J.Am.Chem.Soc. ,39,1173-1209&amp;nbsp; (1917).&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;nbsp;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;color: red; font-weight: bold; text-decoration: none;&quot;&gt;#The effect&amp;nbsp; of certain impurities&amp;nbsp; in causing&amp;nbsp; milkiness in optical glass&amp;nbsp; (with J.B.Ferguson):&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;nbsp;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;color: red; font-weight: bold; text-decoration: none;&quot;&gt;J.Amer.Ceram.Soc.,1,468-476 (1918).&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;nbsp;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;color: red; font-weight: bold; text-decoration: none;&quot;&gt;#The&amp;nbsp; technique&amp;nbsp; of optical&amp;nbsp; glass&amp;nbsp; melting: J.Amer.Ceram. Soc.,2, 102-145&amp;nbsp; (1919).&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;nbsp;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;color: red; font-weight: bold; text-decoration: none;&quot;&gt;#The use of optical pyrometers&amp;nbsp; for control of optical giass&amp;nbsp; furnaces:&amp;nbsp; Bull.Inst.Min.Met.Eng, 1919, 1001-1011&amp;nbsp; ; also&amp;nbsp; Pyrometry&amp;nbsp; Volume,&amp;nbsp; 495-505 (1920).&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;nbsp;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;color: red; font-weight: bold; text-decoration: none;&quot;&gt;#The relations&amp;nbsp; between tridymite and cristobalite:&amp;nbsp; J. Soc. Glass Tech.,3,&amp;nbsp; Trans., 116-125 (1919).&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;nbsp;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;color: red; font-weight: bold; text-decoration: none;&quot;&gt;#The Katmai region,&amp;nbsp; Alaska,&amp;nbsp; and&amp;nbsp; the great&amp;nbsp; eruption&amp;nbsp; of 19l2:&amp;nbsp; J. Geol.,28, 569-606&amp;nbsp; (1920).&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;nbsp;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;color: red; font-weight: bold; text-decoration: none;&quot;&gt;#The origin and mode of emplacement&amp;nbsp; of&amp;nbsp; the great tufi&amp;nbsp; deposit&amp;nbsp; in&amp;nbsp; the valley of&amp;nbsp; the Ten Thousand&amp;nbsp; Smokes:&amp;nbsp; Not.Geogr. Soc. Contributed Technical&amp;nbsp; Paper l, l-74&amp;nbsp; (1923)&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;nbsp;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;color: red; font-weight: bold; text-decoration: none;&quot;&gt;#Earth movements&amp;nbsp; accompanying&amp;nbsp; the Katmai eruption:&amp;nbsp; J.&amp;nbsp; Geol.,33,116-139; 193-233(1925).&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;nbsp;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;color: red; font-weight: bold; text-decoration: none;&quot;&gt;#Magmatic&amp;nbsp; problems of the Aleutians:&amp;nbsp; Nat. Res. Council,&amp;nbsp; Bull., 44, vol.2, pt.2, 124-727 (1926).&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;nbsp;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;color: red; font-weight: bold; text-decoration: none;&quot;&gt;#The Katmai&amp;nbsp; magmatic province: J.Geol.,34,673-772 (1926).&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;nbsp;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;color: red; font-weight: bold; text-decoration: none;&quot;&gt;#An unusual occurrence of albite:&amp;nbsp; Am.&amp;nbsp; Mineral.,11,255-259 (1926).&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;nbsp;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;color: red; font-weight: bold; text-decoration: none;&quot;&gt;#The&amp;nbsp; analytical&amp;nbsp; determination&amp;nbsp; of uranium,&amp;nbsp; thorium,&amp;nbsp; and lead as a basis&amp;nbsp; for&amp;nbsp; age&amp;nbsp; calculations:&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;nbsp;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;color: red; font-weight: bold; text-decoration: none;&quot;&gt;Am. J.Sci.(5),16, 369-381 (1928).&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;nbsp;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;color: red; font-weight: bold; text-decoration: none;&quot;&gt;Radioactive&amp;nbsp; mineralsfrom&amp;nbsp; Divino&amp;nbsp; de Uba, Brazil:&amp;nbsp; Am.J.Sci.(5),16,382-39I&amp;nbsp; (1928)&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;nbsp;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;color: red; font-weight: bold; text-decoration: none;&quot;&gt;#The&amp;nbsp; mass spectrum of&amp;nbsp; lead from&amp;nbsp; Broggerite&amp;nbsp; (with&amp;nbsp; C.S.Piggot): Nature,123,793-794 (1929)&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
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&lt;/table&gt;</summary>
		<author><name>Pavel</name></author>	</entry>

	<entry>
		<id>https://wiki.web.ru/index.php?title=%D0%A4%D0%B5%D0%BD%D0%BD%D0%B5%D1%80,_%D0%9A%D0%BB%D0%B0%D1%80%D0%B5%D0%BD%D1%81_%D0%9D%D0%BE%D1%80%D0%BC%D0%B0%D0%BD&amp;diff=23227&amp;oldid=prev</id>
		<title>Pavel в 11:27, 23 января 2009</title>
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				<updated>2009-01-23T11:27:39Z</updated>
		
		<summary type="html">&lt;p&gt;&lt;/p&gt;

		&lt;table style=&quot;background-color: white; color:black;&quot;&gt;
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		&lt;td colspan='2' style=&quot;background-color: white; color:black;&quot;&gt;← Предыдущая&lt;/td&gt;
		&lt;td colspan='2' style=&quot;background-color: white; color:black;&quot;&gt;Версия 11:27, 23 января 2009&lt;/td&gt;
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		&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Строка 4:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Строка 4:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;Основные труды в области минералогии посвящены изучению парагенезиса различных минералов (в частности, цеолитов) в условиях пневматолитового и гидротермального процессов. Дал первую диаграмму состояния кремнекислоты. Изучал процессы современного вулканизма (Катмай на Аляске, Иеллоустонский национальный парк и др.). Проводил петрографические исследования в различных районах Северной и Южной Америки. Образование многих минералов, руд и горных пород объяснял с позиций кристаллизационной дифференциации и ликвации магмы. Разработал (1928) аналитические методы разделения урановых и ториевых минералов и их применения для определения абсолютного возраста горных пород.&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt; &lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;Основные труды в области минералогии посвящены изучению парагенезиса различных минералов (в частности, цеолитов) в условиях пневматолитового и гидротермального процессов. Дал первую диаграмму состояния кремнекислоты. Изучал процессы современного вулканизма (Катмай на Аляске, Иеллоустонский национальный парк и др.). Проводил петрографические исследования в различных районах Северной и Южной Америки. Образование многих минералов, руд и горных пород объяснял с позиций кристаллизационной дифференциации и ликвации магмы. Разработал (1928) аналитические методы разделения урановых и ториевых минералов и их применения для определения абсолютного возраста горных пород.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;nbsp;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;color: red; font-weight: bold; text-decoration: none;&quot;&gt;&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;nbsp;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;color: red; font-weight: bold; text-decoration: none;&quot;&gt;Список трудов:&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;nbsp;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;color: red; font-weight: bold; text-decoration: none;&quot;&gt;#Note&amp;nbsp; on&amp;nbsp; geology&amp;nbsp; of&amp;nbsp; the&amp;nbsp; Monte&amp;nbsp; Cristo&amp;nbsp; district,&amp;nbsp; Snohomish&amp;nbsp; County,&amp;nbsp; Washington:&amp;nbsp; Sch. of Mines Quart., 14, 359-360 (1892).&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;nbsp;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;color: red; font-weight: bold; text-decoration: none;&quot;&gt;#The&amp;nbsp; Old&amp;nbsp; Telegraph&amp;nbsp; Mine,&amp;nbsp; Bingham&amp;nbsp; Canyon,&amp;nbsp; Utah:&amp;nbsp; Sch.&amp;nbsp; of Mines&amp;nbsp; Quart.,&amp;nbsp; 14,&amp;nbsp; 354-358 (1893).&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;nbsp;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;color: red; font-weight: bold; text-decoration: none;&quot;&gt;#Features&amp;nbsp; indicative&amp;nbsp; of physiographic&amp;nbsp; conditions&amp;nbsp; prevailing&amp;nbsp; at&amp;nbsp; the&amp;nbsp; time&amp;nbsp; of&amp;nbsp; trap&amp;nbsp; intrusions&amp;nbsp; in New&amp;nbsp; Jersey: J . Geol, 16, 299-327 (1908)&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;nbsp;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;color: red; font-weight: bold; text-decoration: none;&quot;&gt;#The&amp;nbsp; crystallization&amp;nbsp; of a basaltic magma&amp;nbsp; from&amp;nbsp; the standpoint&amp;nbsp; of physical&amp;nbsp; chemistry:&amp;nbsp; Am. J.Sci.(4), 29,&amp;nbsp; 217-234&amp;nbsp; (1910).&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;nbsp;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;color: red; font-weight: bold; text-decoration: none;&quot;&gt;#A&amp;nbsp; replacement&amp;nbsp; of&amp;nbsp; rhyolite&amp;nbsp; porphyry&amp;nbsp; by&amp;nbsp; stephanite&amp;nbsp; and&amp;nbsp; chalcopyrite&amp;nbsp; at&amp;nbsp; Leadville,&amp;nbsp; Colorado:&amp;nbsp; Colorado&amp;nbsp; Sch. of Mines&amp;nbsp; Quart.,3l,235-240 (1910).&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;nbsp;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;color: red; font-weight: bold; text-decoration: none;&quot;&gt;#The&amp;nbsp; Watchung&amp;nbsp; basalt&amp;nbsp; and&amp;nbsp; the&amp;nbsp; paragenesis of&amp;nbsp; its&amp;nbsp; zeolites and&amp;nbsp; other&amp;nbsp; secondary&amp;nbsp; minerals:&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;nbsp;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;color: red; font-weight: bold; text-decoration: none;&quot;&gt;Neu&amp;nbsp; York Acad.&amp;nbsp; of Sci., 22, 2,&amp;nbsp; pt.&amp;nbsp; 2, 93-187&amp;nbsp; (1910).&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;nbsp;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;color: red; font-weight: bold; text-decoration: none;&quot;&gt;#Study of a contact metamorphic&amp;nbsp; ore deposit. The Dolores Mine&amp;nbsp; at&amp;nbsp; Matehuala, S.L.P., Mexico&amp;nbsp; (with &lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;nbsp;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;color: red; font-weight: bold; text-decoration: none;&quot;&gt;J. B.&amp;nbsp; Spurr and G. H.&amp;nbsp; Garrey): Econ. Geol.,7,444-484&amp;nbsp; (1912).&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;nbsp;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;color: red; font-weight: bold; text-decoration: none;&quot;&gt;#Petrographic&amp;nbsp; study&amp;nbsp; of&amp;nbsp; the&amp;nbsp; specimens of&amp;nbsp; loess,&amp;nbsp; terra&amp;nbsp; cocida,&amp;nbsp; and&amp;nbsp; scoria&amp;nbsp; collected&amp;nbsp; by&amp;nbsp; the&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;nbsp;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;color: red; font-weight: bold; text-decoration: none;&quot;&gt;Hrdlicka-Willis&amp;nbsp; Expedition&amp;nbsp; (with&amp;nbsp; F.&amp;nbsp; E.&amp;nbsp; Wright):&amp;nbsp; Bull.52,&amp;nbsp; Bur.&amp;nbsp; Amer.&amp;nbsp; Ethnology, Smithsonian Institution,&amp;nbsp; pp. 55-98 (1912).&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;nbsp;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;color: red; font-weight: bold; text-decoration: none;&quot;&gt;#The&amp;nbsp; various forms of&amp;nbsp; silica and&amp;nbsp; their&amp;nbsp; mutual&amp;nbsp; relations: J.Wash.&amp;nbsp; Acad.Sci.,2, 47l-48O (1912).&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
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&lt;/table&gt;</summary>
		<author><name>Pavel</name></author>	</entry>

	<entry>
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		<title>Pavel:&amp;#32;Новая: Феннер Кларенс Норман {{англ|Fenner Clarence Norman}}( родился 19.07.1870, Клифтон, штат Нью-Джерси, умер 24.12.1949, там же), ...</title>
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				<updated>2009-01-23T11:20:46Z</updated>
		
		<summary type="html">&lt;p&gt;Новая: Феннер Кларенс Норман {{англ|Fenner Clarence Norman}}( родился 19.07.1870, Клифтон, штат Нью-Джерси, умер 24.12.1949, там же), ...&lt;/p&gt;
&lt;p&gt;&lt;b&gt;Новая страница&lt;/b&gt;&lt;/p&gt;&lt;div&gt;Феннер Кларенс Норман {{англ|Fenner Clarence Norman}}( родился 19.07.1870, Клифтон, штат Нью-Джерси, умер 24.12.1949, там же), американский геолог-минералог и петрограф. &lt;br /&gt;
&lt;br /&gt;
Окончил Колумбийский университет в Нью-Йорке (1892) по специальности горный инженер. После этого работал геологом на месторождениях Канады, Мексики, Южной и Центральной Америки. В 1907 г вернулся в Колумбийский университет, где получил степень мастера в 1909 и степень доктора философии в 1910. В 1910-1938 годах К.Н.Феннер работал в качестве петролога Геофизической лаборатории Института Карнеги (Вашингтон, США). &lt;br /&gt;
&lt;br /&gt;
Основные труды в области минералогии посвящены изучению парагенезиса различных минералов (в частности, цеолитов) в условиях пневматолитового и гидротермального процессов. Дал первую диаграмму состояния кремнекислоты. Изучал процессы современного вулканизма (Катмай на Аляске, Иеллоустонский национальный парк и др.). Проводил петрографические исследования в различных районах Северной и Южной Америки. Образование многих минералов, руд и горных пород объяснял с позиций кристаллизационной дифференциации и ликвации магмы. Разработал (1928) аналитические методы разделения урановых и ториевых минералов и их применения для определения абсолютного возраста горных пород.&lt;/div&gt;</summary>
		<author><name>Pavel</name></author>	</entry>

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