首页|期刊导航|中国地质(英文)|An integrated north-south paleo-Dadu-Anning River:New insights from bulk major and trace element analyses of the Xigeda Formation

An integrated north-south paleo-Dadu-Anning River:New insights from bulk major and trace element analyses of the Xigeda FormationOACSTPCD

An integrated north-south paleo-Dadu-Anning River:New insights from bulk major and trace element analyses of the Xigeda Formation

Yong Zheng;Hai-bing Li;Jia-wei Pan;Ping Wang;Ya Lai;Zheng Gong

Key Laboratory of Deep-Earth Dynamics,Institute of Geology,Chinese Academy of Geological Sciences,China Geological Survey,Ministry of Natural Resources,Beijing 100037,China||Jiangsu Donghai Continental Deep Hole Crustal Activity National Observaion and Research Station,Lianyungang 222300,China||Southern Marine Science and Engineering Guangdong Laboratory,Guangzhou 511458,ChinaKey Laboratory of Deep-Earth Dynamics,Institute of Geology,Chinese Academy of Geological Sciences,China Geological Survey,Ministry of Natural Resources,Beijing 100037,China||Jiangsu Donghai Continental Deep Hole Crustal Activity National Observaion and Research Station,Lianyungang 222300,China||Southern Marine Science and Engineering Guangdong Laboratory,Guangzhou 511458,ChinaKey Laboratory of Deep-Earth Dynamics,Institute of Geology,Chinese Academy of Geological Sciences,China Geological Survey,Ministry of Natural Resources,Beijing 100037,China||Jiangsu Donghai Continental Deep Hole Crustal Activity National Observaion and Research Station,Lianyungang 222300,China||Southern Marine Science and Engineering Guangdong Laboratory,Guangzhou 511458,ChinaGeophysical Exploration Center,China Earthquake Administration,Zhengzhou 450002,ChinaKey Laboratory of Deep-Earth Dynamics,Institute of Geology,Chinese Academy of Geological Sciences,China Geological Survey,Ministry of Natural Resources,Beijing 100037,China||Jiangsu Donghai Continental Deep Hole Crustal Activity National Observaion and Research Station,Lianyungang 222300,China||Southern Marine Science and Engineering Guangdong Laboratory,Guangzhou 511458,ChinaInstitute of Geophysics,China Earthquake Administration,Beijing 100081,China

Dadu RiverAnninghe faultRiver diversionXigeda FormationTectonic upliftProvenanceSongpan-Ganzi flyschAncient lakeXianshuihe-Xiaojiang fault systemTibetan Plateau

Dadu RiverAnninghe faultRiver diversionXigeda FormationTectonic upliftProvenanceSongpan-Ganzi flyschAncient lakeXianshuihe-Xiaojiang fault systemTibetan Plateau

《中国地质(英文)》 2024 (1)

龙门山的逆冲—推覆和隆升:来自于山前飞来峰的年代制约

91-103,13

This work was financially supported by the Natural Science Foundation of China(419410164207224041830217),Ministry of Science and Technology of China(2019QZKK0901,2021FY100101),Key Special Project for Introduced Talents Team of the Southern Marine Science and Engineering Guangdong Laboratory(GML2019ZD0201),China Geological Survey(DD20221630),and Special Fund of the Institute of Geophysics,China Earthquake Administration(DQJB20B21).

10.31035/cg2023027

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