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Evaluation of the ongoing rifting and subduction processes in the geochemistry of magmas from the western part of the Mexican Volcanic Belt
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文摘

Discriminant diagrams were applied to decipher complex tectonic setting of W-MVB.

Miocene basic rocks indicate a rift and intermediate an arc setting.

Crust beneath W-MVB is highly heterogeneous as evidenced from their REE contents.

Triple-rift system does effect chemistry of W-MVB rocks; the three rifts differ.

Basic and intermediate magmas show petrogenetic process-related tectonic settings.

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