First partial melting inversion model for a rift-related origin of the Sierra de Chichinautzin volcanic field, central Mexican volcanic belt

Velasco-Tapia, F
Verma, SP

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Publication date

January 2001

DOI

10.1080/00206810109465048

Publisher

Universidad Nacional Autónoma de México (UNAM)

ISSN

0020-6814

Journal

International Geology Review

Citation count (estimate)

Abstract

We present the geochemical and isotopic characteristics of Pleistocene to Holocene olivine-bearing mafic rocks from the Sierra de Chichinautzin (SCN) volcanic field, located in the central part of the Mexican Volcanic Belt (MVB). Some have geochemical characteristics of primary magmas, and their MORB-normalized patterns are similar to those displayed by extension-related mafic rocks. The SCN primary magmas show a limited range in Sr-87/Sr-86 (0.70348-0.7039

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First partial melting inversion model for a rift-related origin of the Sierra de Chichinautzin volcanic field, central Mexican volcanic belt

Abstract

Extracted data

First partial melting inversion model for a rift-related origin of the Sierra de Chichinautzin volcanic field, central Mexican volcanic belt

Abstract

Extracted data

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