Metamorphism and P-T Evolution of High-Pressure Granulites from the Fuping Complex, North China Craton

Metamorphism and P-T Evolution of High-Pressure Granulites from the Fuping Complex, North China Craton

Granulite facies rocks provide important keys to evaluating collisional metamorphism in orogenic belts. The mafic granulites of Baoding in the Fuping Complex of the North China Craton occur within the Trans-North China Orogen (TNCO), a major Paleoproterozoic collisional orogen. Here, we present resu...

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Bibliographic Details
Main Authors: Zijing Zhang, Changqing Zheng, Chenyue Liang, M. Santosh, Junjie Hao, Lishuai Dong, Jianjun Hou, Feifei Hou, Meihui Li
Format: Article
Language:English
Published: MDPI AG 2024-01-01
Series:Minerals
Subjects:
Fuping Complex
high-pressure granulite
clockwise P-T path
Trans-North China Orogen
Online Access:https://www.mdpi.com/2075-163X/14/2/138

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https://www.mdpi.com/2075-163X/14/2/138

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