Provenance, age constraints and metamorphism of Ediacaran metasedimentary rocks from the El Triunfo Complex (SE Chiapas, México): evidence for Rodinia breakup and Iapetus active margin-Reference-Cited by-同舟云学术

Provenance, age constraints and metamorphism of Ediacaran metasedimentary rocks from the El Triunfo Complex (SE Chiapas, México): evidence for Rodinia breakup and Iapetus active margin

Published:2016-07-15 Issue:16 Volume:58 Page:2065-2091
ISSN:0020-6814
Container-title:International Geology Review
language:en
Short-container-title:International Geology Review

Author:

González-Guzmán Reneé¹,Weber Bodo¹,Manjarrez-Juárez Román¹,Cisneros de León Alejandro²,Hecht Lutz³,Herguera-García Juan Carlos⁴

Affiliation:

1. Departamento de Geología, Centro de Investigación Científica y de Educación Superior de Ensenada (CICESE), Ensenada, México

2. Instituto de Geología, Universidad Nacional Autónoma de México, Ciudad Universitaria, Coyoacán, México

3. Leibniz-Institut für Evolutions- und Biodiversitätsforschung, Humboldt-Universität Berlin, Berlin, Germany

4. División de Oceanología, CICESE, Ensenada, México

Funder

Consejo Nacional de Ciencia y Tecnología

Publisher

Informa UK Limited

Subject

Geology

Link

https://www.tandfonline.com/doi/pdf/10.1080/00206814.2016.1207208

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4. Active or passive continental margin? Geochemical and Nd isotope constraints of metasediments in the backstop of a pre-Andean accretionary wedge in southernmost Chile (46°30′-48°30′S)

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