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

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Date

2012

Authors

Calderon, Mauricio
Fosdick, J.C.
Warren, C.
Massonne, H.-J.
Fanning, Christopher
Fadel Cury, L.
Schwanethal, J.
Fonseca, P.E.
Galaz, G.
Gaytan, D.

Journal Title

Journal ISSN

Volume Title

Publisher

Elsevier

Abstract

The Canal de las Montañas Shear Zone (CMSZ), southern Patagonian Andes (51-52°S), is a low-grade mylonite belt generated from felsic ignimbritic, pelitic and basaltic protoliths of the Late Jurassic-Early Cretaceous Rocas Verdes basin. The different typ

Description

Keywords

Keywords: Geothermobarometry; Metamorphic sole; Patagonian Andes; Rocas Verdes basin; Sarmiento Ophiolitic Complex; Geochronology; Hydraulic structures; Lead; Mica; Shearing; Structural geology; Tectonics; Cretaceous; crystallization; emplacement; felsic rock; fold Geochronology; Geothermobarometry; Metamorphic sole; Patagonian Andes; Rocas Verdes basin; Sarmiento Ophiolitic Complex

Citation

URI

http://hdl.handle.net/1885/52196

Collections

ANU Research Publications

Source

Tectonophysics

Type

Journal article

Book Title

Entity type

Access Statement

License Rights

DOI

10.1016/j.tecto.2011.12.034

Restricted until

2037-12-31

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01_Calderon_The_low-grade_Canal_de_las_2012.pdf (2.92 MB)

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