Registros del 1 al 10 de 14 encontrados |
![](./images/clear.gif) 1.- A north-south transect across the central Mexican volcanic belt at approximately 100 degrees W; spatial distribution, petrological, geochemical, and isotopic characteristics of quaternary volcanism
Oxford University Press; Oxford; GBR; United Kingdom, 2007
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![](./images/clear.gif) 2.- FOR A HIGHLY HETEROGENEOUS SUBDUCTION-MODIFIED MANTLE WEDGE
IUGG; [LOCATION VARIES]; III; INTERNATIONAL, 1999
IUGG 99; ABSTRACTS
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![](./images/clear.gif) 3.- HORNBLENDE PERIDOTITE XENOLITHS FROM CENTRAL MEXICO REVEAL THE HIGHLY OXIDIZED NATURE OF SUBARC UPPER MANTLE
GEOLOGICAL SOCIETY OF AMERICA (GSA); BOULDER, CO; USA; UNITED STATES, 1998
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![](./images/clear.gif) 4.- HYDROUS PHASE EQUILIBRIA OF A MEXICAN HIGH-SILICA ANDESITE; A CANDIDATE FOR A MANTLE ORIGIN?
PERGAMON; OXFORD; III; INTERNATIONAL, 2001
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![](./images/clear.gif) 5.- Impact of the Orozco fracture zone on the central Mexican volcanic belt
Elsevier; Amsterdam; NLD; Netherlands, 2010
Continental margin volcanism; a volume in memory of James F. Luhr
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![](./images/clear.gif) 6.- LOW ALUMINUM ANDESITES NEAR VALLE DE BRAVO, CENTRAL MEXICO
GEOLOGICAL SOCIETY OF AMERICA (GSA); BOULDER, CO; USA; UNITED STATES, 1998
GEOLOGICAL SOCIETY OF AMERICA, 1998 ANNUAL MEETING
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![](./images/clear.gif) 7.- Mantle peridotite xenoliths in andesite lava at El Penon, central Mexican volcanic belt; isotopic and trace element evidence for melting and metasomatism in the mantle wedge beneath an active arc
Elsevier; Amsterdam; NLD; Netherlands, 2007
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![](./images/clear.gif) 8.- MANTLE XENOLITHS HOSTED BY HYDROUS ANDESITES NEAR VALLE DE BRAVO, CENTRAL MEXICO
GEOLOGICAL SOCIETY OF AMERICA (GSA); BOULDER, CO; USA; UNITED STATES, 1997
GEOLOGICAL SOCIETY OF AMERICA, 1997 ANNUAL MEETING
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![](./images/clear.gif) 9.- NEOGENE VOLCANISM AT THE FRONT OF THE CENTRAL MEXICAN VOLCANIC BELT; BASALTIC ANDESITES TO DACITES, WITH CONTEMPORANEOUS SHOSHONITES AND HIGH-TIO (SUB 2) LAVA
GEOLOGICAL SOCIETY OF AMERICA (GSA); BOULDER, CO; USA; UNITED STATES, 2001
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![](./images/clear.gif) 10.- NEOGENE VOLCANISM AT THE FRONT OF THE CENTRAL MEXICAN VOLCANIC BELT; BASALTIC ANDESITES TO DACITES, WITH CONTEMPORANEOUS SHOSHONITES AND HIGH-TIO (SUB 2) LAVA; REPLY
GEOLOGICAL SOCIETY OF AMERICA (GSA); BOULDER, CO; USA; UNITED STATES, 2003
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