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The transition between shortening and extensional regimes in central Mexico recorded in the tourmaline veins of the Comanja Granite
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文摘
The Eocene exhumation of the Comanja Granite evidences the upwelling of southern Mesa Central of Mexico. We document the age and structures formed during the transition Laramide Orogeny-Basin and Range, in Central México. State of stress during the transition Laramide Orogeny-Basin and Range in central Mexico.

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