中国地质(英文)2024,Vol.7Issue(1):80-90,11.DOI:10.31035/cg2023023
Plume-lithosphere interaction in the Comei Large Igneous Province:Evidence from two types of mafic dykes in Gyangze,south Tibet,China
Plume-lithosphere interaction in the Comei Large Igneous Province:Evidence from two types of mafic dykes in Gyangze,south Tibet,China
摘要
关键词
OIB type diabase/Comei Large Igneous Province/Weakly enriched diabase/Plume-lithosphere interaction/Nb-Ta-Ti negative anomaly/Kerguelen plume/Geological survey engineering/Tibet PlateauKey words
OIB type diabase/Comei Large Igneous Province/Weakly enriched diabase/Plume-lithosphere interaction/Nb-Ta-Ti negative anomaly/Kerguelen plume/Geological survey engineering/Tibet Plateau引用本文复制引用
Ya-ying Wang,Ling-sen Zeng,Li-e Gao,Li-long Yan,Ling-hao Zhao,Jia-hao Gao,Ying-long Di,Guang-xu Li,Yi-hong Tian..Plume-lithosphere interaction in the Comei Large Igneous Province:Evidence from two types of mafic dykes in Gyangze,south Tibet,China[J].中国地质(英文),2024,7(1):80-90,11.基金项目
This study was supported by National Science Foundation of China(42102059 and 92055202),the China Geological Survey(DD20221817 and DD20190057),the basic scientific research funding in CAGS(J2204),and the Second Tibetan Plateau Scientific Expedition and Research(2019QZKK0702).Dr.Zeng Yun-chuan and Dr.Guo Chun-li are thanked for their constructive reviews.Editors Hao Zi-guo and Chen Xi-jie are thanked for carefully handling this paper. (42102059 and 92055202)