Cognate Mafic Enclaves Formed by Cumulated Mush Convection in a Granitic Magma Chamber:Evidence from Mineral Chemistry of the Triassic Zhashui Pluton,Qinling OrogenOACSTPCD
Cognate Mafic Enclaves Formed by Cumulated Mush Convection in a Granitic Magma Chamber:Evidence from Mineral Chemistry of the Triassic Zhashui Pluton,Qinling Orogen
ZHANG Hongbing;ZHOU Xuchen;LAI Shaocong;ZHANG Hua;QIN Jiangfeng
State Key Laboratory of Continental Dynamics,Department of Geology,Northwest University,Xi'an 710069,ChinaState Key Laboratory of Continental Dynamics,Department of Geology,Northwest University,Xi'an 710069,ChinaState Key Laboratory of Continental Dynamics,Department of Geology,Northwest University,Xi'an 710069,ChinaState Key Laboratory of Continental Dynamics,Department of Geology,Northwest University,Xi'an 710069,ChinaState Key Laboratory of Continental Dynamics,Department of Geology,Northwest University,Xi'an 710069,China
mafic enclavesgranitic chambermafic cumulateconvectionQinling orogen
mafic enclavesgranitic chambermafic cumulateconvectionQinling orogen
《地质学报（英文版）》 2024 (6)
1479-1488,10
Constructive reviews by two anonymous reviewers greatly improved the paper,and are gratefully acknowledged.This work was supported by the National Natural Science Foundation of China(Grant Nos.42372071,41421002),the Foundation for the Author of National Excellent Doctoral Dissertation of China(Grant No.201324)and a research grant of the State Key Laboratory of Continental Dynamics(Grant No.SKLCD-04).
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