The low-grade Canal de las Montañas Shear Zone and its role in the tectonic emplacement of the Sarmiento Ophiolitic Complex and Late Cretaceous Patagonian Andes orogeny, Chile-Reference-Cited by-同舟云学术

The low-grade Canal de las Montañas Shear Zone and its role in the tectonic emplacement of the Sarmiento Ophiolitic Complex and Late Cretaceous Patagonian Andes orogeny, Chile

Published:2012-02 Issue: Volume:524-525 Page:165-185
ISSN:0040-1951
Container-title:Tectonophysics
language:en
Short-container-title:Tectonophysics

Author:

Calderón M.,Fosdick J.C.,Warren C.,Massonne H.-J.,Fanning C.M.,Cury L. Fadel,Schwanethal J.,Fonseca P.E.,Galaz G.,Gaytán D.,Hervé F.

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geophysics

Reference85 articles.

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