From Crustal Thickening to Orogen‐Parallel Escape: The 120‐Myr‐Long HT‐LP Evolution Recorded by Titanite in the Paleozoic Famatinian Backarc, NW Argentina-Reference-Cited by-同舟云学术

From Crustal Thickening to Orogen‐Parallel Escape: The 120‐Myr‐Long HT‐LP Evolution Recorded by Titanite in the Paleozoic Famatinian Backarc, NW Argentina

Published:2020-09 Issue:9 Volume:39 Page:
ISSN:0278-7407
Container-title:Tectonics
language:en
Short-container-title:Tectonics

Author:

Farias Pablo¹^ORCID,Weinberg Roberto¹^ORCID,Sola Alfonso²^ORCID,Becchio Raul²³

Affiliation:

1. School of Earth, Atmosphere and Environment Monash University Clayton Victoria Australia

2. Instituto Geonorte Universidad Nacional de Salta, INENCO‐CONICET Salta Argentina

3. LaTe Andes Salta Argentina

Funder

Australian Research Council

Agencia Nacional de Promoción Científica y Tecnológica

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2020TC006184

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