Anatectic record and P–T path evolution of metapelites from the Wulashan Complex, Khondalite Belt, North China Craton-Reference-Cited by-同舟云学术

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Anatectic record and P–T path evolution of metapelites from the Wulashan Complex, Khondalite Belt, North China Craton

Published:2017-12 Issue: Volume:303 Page:10-29
ISSN:0301-9268
Container-title:Precambrian Research
language:en
Short-container-title:Precambrian Research

Author:

Cai Jia,Liu Fulai,Liu Pinghua,Wang Fang,Liu Chaohui,Shi Jianrong

Funder

National Natural Science Foundation of China

Chinese Geological Survey Bureau

Nation 973 Project of the Chinese Ministry of Science and Technology

Basic Scientific Research Foundations of the Institute of Geology

Chinese Academy of Geological Sciences

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference128 articles.

1. Mechanisms of crustal anatexis: a geochemical study of partially melted metapelitic enclaves and host dacite, SE Spain;Acosta-Vigil;J. Petrol.,2010

2. P-T–t evolution of orogenic belts and the causes of regional metamorphism;Brown;J. Geol. Soc.,1993

3. Retrograde processes in migmatites and granulites revisited;Brown;J. Metamorph. Geol.,2002

4. Crustal melting and melt extraction, ascent and emplacement in orogens: mechanisms and consequences;Brown;J. Geol. Soc.,2007

5. Melt segregation in migmatites;Brown;J. Geophys. Res.,1995

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