About: James Gilluly

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James Gilluly (June 24, 1896 – December 29, 1980) was an American geologist. Regarding the Cupriferous Porphyry Genesis, Gilluly integrated detailed observations of the Ajo porphyry between 1936 and 1936 with experimental data (Goranson, 1931, Gilluly, 1937). Gilluly concluded that after the Ajo quartz monzonite intruded and crystallized, it was fractured by magmatic bypass solutions (p. 73). Gilluly frequency experimental restrictions to estimate a paleo depth between 1000 and 3000 (m) (average 2000 (m) or 0.5 kbar at lithostatic pressure), consistent with solidus temperatures of 900 °C for granite, containing 4% by weight of water. He realized that the source magmatic content was water, sulfur and halogens, and that the binders can form complexes with metals to produce an aqueous fluid w

Attributes	Values
rdf:type	Thing
rdfs:label	James Gilluly (de) James Gilluly (en)
rdfs:comment	James Gilluly (* 24. Juni 1896 in Seattle; † 29. Dezember 1980) war ein US-amerikanischer Geologe. Gillulys Vaters war irischer und seine Mutter württembergischer Abstammung. Er studierte ab 1915 an der University of Washington, unterbrochen vom Dienst in der US Navy im Ersten Weltkrieg und Jobs in Bergwerken, Stahlhütten und im Hafen zur Finanzierung seines Studiums. Nach dem Universitätsabschluss (1921) ging er 1922 zur United States Geological Survey (USGS). Von dieser wurde er 1931 nach Innsbruck zu Bruno Sander geschickt, um dessen Methoden der Gefügekunde zu erlernen. Gilluly nutzte den Aufenthalt auch zu Studienfahrten in Osteuropa. 1940 wurde er Professor an der University of California, Los Angeles (UCLA). (de) James Gilluly (June 24, 1896 – December 29, 1980) was an American geologist. Regarding the Cupriferous Porphyry Genesis, Gilluly integrated detailed observations of the Ajo porphyry between 1936 and 1936 with experimental data (Goranson, 1931, Gilluly, 1937). Gilluly concluded that after the Ajo quartz monzonite intruded and crystallized, it was fractured by magmatic bypass solutions (p. 73). Gilluly frequency experimental restrictions to estimate a paleo depth between 1000 and 3000 (m) (average 2000 (m) or 0.5 kbar at lithostatic pressure), consistent with solidus temperatures of 900 °C for granite, containing 4% by weight of water. He realized that the source magmatic content was water, sulfur and halogens, and that the binders can form complexes with metals to produce an aqueous fluid w (en)
foaf:depiction
dcterms:subject	1896 births 1980 deaths American people of German descent Johns Hopkins University alumni United States Geological Survey personnel United States Navy personnel of World War I University of California, Los Angeles faculty University of Washington alumni Yale University alumni American people of Irish descent 20th-century American geologists Presidents of the Geological Society of America Scientists from Seattle
Wikipage page ID	59806885 (xsd:integer)
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Link from a Wikipage to another Wikipage	Battle of Leyte Johns Hopkins Blue Jays men's lacrosse United States Geological Survey United States Navy University of California, Los Angeles University of Washington County Galway Geological Society of America Military Geology Unit Denver, Colorado 1896 births 1980 deaths American people of German descent Johns Hopkins University alumni United States Geological Survey personnel United States Navy personnel of World War I University of California, Los Angeles faculty University of Washington alumni Yale University alumni American Geophysical Union East St. Louis List of Penrose Medal winners Guggenheim Fellowship American people of Irish descent 20th-century American geologists Presidents of the Geological Society of America Scientists from Seattle Württemberg Kittitas County, Washington National Academy of Sciences Second Red Scare Military history of the United States during World War II Yale University United States Marines South West Pacific Command Robert Emmett
sameAs	James Gilluly James Gilluly James Gilluly James Gilluly James Gilluly James Gilluly
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has abstract	James Gilluly (* 24. Juni 1896 in Seattle; † 29. Dezember 1980) war ein US-amerikanischer Geologe. Gillulys Vaters war irischer und seine Mutter württembergischer Abstammung. Er studierte ab 1915 an der University of Washington, unterbrochen vom Dienst in der US Navy im Ersten Weltkrieg und Jobs in Bergwerken, Stahlhütten und im Hafen zur Finanzierung seines Studiums. Nach dem Universitätsabschluss (1921) ging er 1922 zur United States Geological Survey (USGS). Von dieser wurde er 1931 nach Innsbruck zu Bruno Sander geschickt, um dessen Methoden der Gefügekunde zu erlernen. Gilluly nutzte den Aufenthalt auch zu Studienfahrten in Osteuropa. 1940 wurde er Professor an der University of California, Los Angeles (UCLA). Im Zweiten Weltkrieg war er wieder bei der USGS in der Prospektion kriegswichtiger Mineralien beschäftigt und war Militärgeologe im Pazifik, wo er Strände für die Landungen insbesondere auf den Philippinen aussuchte. Nach dem Krieg lehrte er weiter an der UCLA, ging aber 1950 in der McCarthy-Ära (er sah den verlangten Eid als Zumutung an und war die administrativen Lasten an der Universität leid) wieder zur USGS, wo er unter anderem Felderkundungen in Nevada unternahm. Sein Lehrbuch der Geologie war in den USA zeitweise ein Standardwerk. Er widmete seine späteren Jahre den Neuauflagen des Buches und reiste dazu weltweit. Er war an der Debatte um den Ursprung der Granite beteiligt und vertrat die Meinung, dass Gebirgsbildung nicht nur auf bestimmte besonders aktive Phasen in der geologischen Vergangenheit beschränkt war, sondern ständig stattfand. 1962 war er der 17. William Smith Lecturer der Geological Society of London, deren Ehrenmitglied er war. Er erhielt 1969 die Walter H. Bucher Medal und 1958 die Penrose-Medaille. 1959 erhielt er die höchste Auszeichnung des US Innenministeriums, die Distinguished Service Medal. 1959 wurde er Ehrendoktor der Princeton University. Er war Mitglied der National Academy of Sciences und der American Academy of Arts and Sciences (1949). 1962 war er Vorstand der Abteilung Geowissenschaften des National Research Council. 1948 war er Präsident der Geological Society of America. (de) James Gilluly (June 24, 1896 – December 29, 1980) was an American geologist. Regarding the Cupriferous Porphyry Genesis, Gilluly integrated detailed observations of the Ajo porphyry between 1936 and 1936 with experimental data (Goranson, 1931, Gilluly, 1937). Gilluly concluded that after the Ajo quartz monzonite intruded and crystallized, it was fractured by magmatic bypass solutions (p. 73). Gilluly frequency experimental restrictions to estimate a paleo depth between 1000 and 3000 (m) (average 2000 (m) or 0.5 kbar at lithostatic pressure), consistent with solidus temperatures of 900 °C for granite, containing 4% by weight of water. He realized that the source magmatic content was water, sulfur and halogens, and that the binders can form complexes with metals to produce an aqueous fluid with larger volumes. On the other hand, one can also count on the fact that volatiles decrease the solubility of water in magma and the vapor pressure of expelled fluid could fracture the wedge-shaped dome made of country rock and solidified magma. This is summarized in the discharges of magmatic fluids corresponding to continuous processes that lead to the accumulation of fluids in intercourse, which maintains an intermittent fracturing., Theinfluence of Geochemical Techniques on the Development of Genetic Models for Porphyry Copper Deposits, published in the Vol. 10 of the Reviews in Economic Geology de la Society of Economic Geologists. (en)
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is Link from a Wikipage to another Wikipage of	San Rafael Group Sinbad Formation Horquilla Formation Joseph Hoover Mackin Entrada Sandstone Geological Society of America Gilluly, James Alfred Woodford List of Guggenheim Fellowships awarded in 1960 List of Penrose Medal winners Henry G. Ferguson Summerville Formation
is Wikipage redirect of	Gilluly, James
is foaf:primaryTopic of	wikipedia-en:James_Gilluly

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