High-temperature S-type granitoids (charnockites) in the Jining complex, North China Craton: Restite entrainment and hybridization with mafic magma

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High-temperature S-type granitoids (charnockites) in the Jining complex, North China Craton: Restite entrainment and hybridization with mafic magma

The Liangcheng garnet granitoids are parautochthonous S-type granites that occur within granulite-facies metasediments in the ultrahigh-temperature (UHT) Jining Complex, eastern part of the Khondalite Belt, North China Craton. These garnet granitoids contain mafic microgranular enclaves and are inti...

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Bibliographic Details
Main Authors:	Wang, L., Guo, J., Yin, C., Peng, P., Zhang, J., Spencer, Christopher, Qian, J.
Format:	Journal Article
Published:	Elsevier BV 2018
Online Access:	http://hdl.handle.net/20.500.11937/72715

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