Английская Википедия:Cordillera Blanca Batholith

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Шаблон:Short description The Cordillera Blanca Batholith (Шаблон:Lang-es) is an extensive group of individual plutons that crop out near or at Cordillera Blanca, Peru. The batholith intrudes the Jurassic Chicama Formation. To the west the Cordillera Blanca Fault makes up the border of the batholith. It has been suggested that the magma that originated the batholith was the product of partial melting of underplated basaltic crust.[1]

References

Шаблон:Reflist

See also

Шаблон:Major South American geological formations


Шаблон:Geology-stub