地质学报（英文版）2024，Vol.98Issue(6)：1479-1488,10.DOI:10.1111/1755-6724.15194
Cognate Mafic Enclaves Formed by Cumulated Mush Convection in a Granitic Magma Chamber:Evidence from Mineral Chemistry of the Triassic Zhashui Pluton,Qinling Orogen
Cognate Mafic Enclaves Formed by Cumulated Mush Convection in a Granitic Magma Chamber:Evidence from Mineral Chemistry of the Triassic Zhashui Pluton,Qinling Orogen
摘要
关键词
mafic enclaves/granitic chamber/mafic cumulate/convection/Qinling orogenKey words
mafic enclaves/granitic chamber/mafic cumulate/convection/Qinling orogen引用本文复制引用
ZHANG Hongbing,ZHOU Xuchen,LAI Shaocong,ZHANG Hua,QIN Jiangfeng..Cognate Mafic Enclaves Formed by Cumulated Mush Convection in a Granitic Magma Chamber:Evidence from Mineral Chemistry of the Triassic Zhashui Pluton,Qinling Orogen[J].地质学报（英文版）,2024,98(6):1479-1488,10.基金项目
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). （Grant Nos.42372071,41421002）
