Melting conditions in the modern Tibetan crust since the Miocene

Abundant granitic rocks exposed in ancient mountain belts suggest that crustal melting plays a major role in orogenic processes. However, complex field relations and superposition of multiple tectonic events make it difficult to determine the role of melting in orogenesis. In contrast, geophysical m...

Descripción completa

Detalles Bibliográficos
Autores principales: Chen, Jinyu, Gaillard, Fabrice, Villaros, Arnaud, Yang, Xiaosong, Laumonier, Mickael, Jolivet, Laurent, Unsworth, Martyn, Hashim, Leïla, Scaillet, Bruno, Richard, Guillaume
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2018
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6115434/
https://www.ncbi.nlm.nih.gov/pubmed/30158586
http://dx.doi.org/10.1038/s41467-018-05934-7

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6115434/
https://www.ncbi.nlm.nih.gov/pubmed/30158586
http://dx.doi.org/10.1038/s41467-018-05934-7

Ejemplares similares