Registros del 1 al 9 de 9 encontrados |
![](./images/clear.gif) 1.- A test of whether contrasting magma supply rates (hotter vs. cooler lower crust) influences the differentiation of arc magmas in the Mexican arc
American Geophysical Union; Washington, DC; USA; United States, 2009
AGU 2009 fall meeting
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![](./images/clear.gif) 2.- Eruptive history of Volcan Tepetiltic, Mexico; evidence for remelting of silicic ashflows revealed by 40Ar/39Ar geochronology
American Geophysical Union; Washington, DC; USA; United States, 2004
AGU 2004 fall meeting
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![](./images/clear.gif) 3.- Evidence for degassing-induced crystallization in peripheral andesite and dacite flows along the flanks of Volcan Sanganguey, Mexico
American Geophysical Union; Washington, DC; USA; United States, 2006
AGU 2006 fall meeting
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![](./images/clear.gif) 4.- Evidence from a crystal-poor, zoned (rhyolite-andesite) pyroclastic deposit from Volcan Tepetiltic, western Mexico for rapid generation of silicic melt by partial melting of granitoid and not by segregation from a long-lived crystal-rich mush
American Geophysical Union; Washington, DC; USA; United States, 2007
AGU 2007 fall meeting
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![](./images/clear.gif) 5.- FERRIC-FERROUS RATIOS, H (SUB 2) O CONTENTS AND D/H RATIOS OF PHLOGOPITE AND BIOTITE FROM LAVAS OF DIFFERENT TECTONIC REGIMES
SPRINGER INTERNATIONAL; HEIDELBERG-NEW YORK; III; INTERNATIONAL, 1996
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![](./images/clear.gif) 6.- QUATERNARY MINETTES AND ASSOCIATED VOLCANIC ROCKS OF MASCOTA, WESTERN MEXICO; A CONSEQUENCE OF PLATE EXTENSION ABOVE A SUBDUCTION MODIFIED MANTLE WEDGE
SPRINGER INTERNATIONAL; HEIDELBERG-NEW YORK; III; INTERNATIONAL, 1996
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![](./images/clear.gif) 7.- The andesites of the Tancitaro volcanic field, Michoacan Mexico; evidence for their formation in the lower crust
American Geophysical Union; Washington, DC; USA; United States, 2006
AGU 2006 fall meeting
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![](./images/clear.gif) 8.- The origin of low-Sr rhyolites by multiple episodes of partial melting
American Geophysical Union; Washington, DC; USA; United States, 2008
AGU 2008 fall meeting
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![](./images/clear.gif) 9.- Why do some andesite stratovolcanoes evolve to erupt rhyolite and/or rhyodacite and others do not?
Mineralogical Society; London; GBR; United Kingdom, 2013
Goldschmidt abstracts 2013
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