Melting conditions in the modern Tibetan crust since the Miocene-Reference-Cited by-同舟云学术

Melting conditions in the modern Tibetan crust since the Miocene

Published:2018-08-29 Issue:1 Volume:9 Page:
ISSN:2041-1723
Container-title:Nature Communications
language:en
Short-container-title:Nat Commun

Author:

Chen Jinyu^ORCID,Gaillard Fabrice,Villaros Arnaud,Yang Xiaosong,Laumonier Mickael,Jolivet Laurent,Unsworth Martyn,Hashim Leïla,Scaillet Bruno^ORCID,Richard Guillaume

Funder

EC | European Research Council (ERC)

Agence Nationale de la Recherche (French National Research Agency)

National Natural Science Foundation of China (National Science Foundation of China)

Publisher

Springer Science and Business Media LLC

Subject

General Physics and Astronomy,General Biochemistry, Genetics and Molecular Biology,General Chemistry

Link

http://www.nature.com/articles/s41467-018-05934-7.pdf

Reference70 articles.

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3. Whittington, A. G., Hofmeister, A. M. & Nabelek, P. I. Temperature-dependent thermal diffusivity of the Earth’s crust and implications for magmatism. Nature 458, 319–321 (2009).

4. Nábělek, P. I., Whittington, A. G. & Hofmeister, A. M. Strain heating as a mechanism for partial melting and ultrahigh temperature metamorphism in convergent orogens: Implications of temperature-dependent thermal diffusivity and rheology. J. Geophys. Res. 115, B12417 (2010).

5. Searle, M. Crustal melting, ductile flow, and deformation in mountain belts: cause and effect relationships. Lithosphere 5, 547–554 (2013).

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