Clockwise P–T–t paths with considerable heating processes during decompression from high-pressure mafic granulites in the Wuhe Complex, southeastern North China Craton

Author:

Kong Xu,Lu Jun-Sheng,Zhai Ming-Guo,Liu Gang,Feng Qiang,Li Yu-Ting

Funder

National Natural Science Foundation of China

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference156 articles.

1. Geochemical characterization and petrogenesis of mafic granulites from the Central Indian Tectonic Zone (CITZ);Alam;Geol. Soc., London, Special Publ.,2016

2. High pressure granulites at the dawn of the Proterozoic;Anderson;Geology,2012

3. BGMRA (Bureau of Geology Mineral Resources of Anhui), 1987. The Regional Geology of Anhui Province Geological Publishing House, Beijing pp. 548−558 (in Chinese with detailed English illustrations).

4. The barometer tremolite + tschermakite + 2 albite = 2 pargasite + 8 quartz: constraints from experimental data at unit silica activity, with application to garnet-free natural assemblages;Bhadra;Am. Mineral.,2007

5. Pressure–temperature–time paths and a tectonic model for the evolution of granulites;Bohlen;J. Geol.,1987

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