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Altered volcanic ash layers of the Late Cretaceous San Felipe Formation, Sierra Madre Oriental (Northeastern Mexico): UPb geochronology, provenance and tectonic setting
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文摘

Upper Cretaceous altered ash-beds from Northeastern Mexico have been studied.

According to Usingle bondPb dating in zircon, the deposit occurred between 84.6 and 73.7 Ma.

Geochemistry data indicate a rhyodacitic to rhyolitic composition.

Ash-beds have an affinity to continental arc in transition to extension setting.

The origin of the San Felipe ash beds is probably linked to Laramide Magmatic Arc.

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