闽西南永定大坪辉长岩脉的年代学、地球化学特征及地质意义

王锦荣; 吕新彪; 张建平; 林晓晖; 王继林; 林香

doi:10.3799/dqkx.2019.258

Volume 46 Issue 1

Jan. 2021

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Wang Jinrong, Lü Xinbiao, Zhang Jianping, Lin Xiaohui, Wang Jilin, Lin Xiang, 2021. Geochronology, Geochemistry and Geological Significance of Gabbros from Yongding Daping Area, Southwest Fujian. Earth Science, 46(1): 73-86. doi: 10.3799/dqkx.2019.258

Citation:

Wang Jinrong, Lü Xinbiao, Zhang Jianping, Lin Xiaohui, Wang Jilin, Lin Xiang, 2021. Geochronology, Geochemistry and Geological Significance of Gabbros from Yongding Daping Area, Southwest Fujian. Earth Science, 46(1): 73-86. doi: 10.3799/dqkx.2019.258

Citation:

Wang Jinrong, Lü Xinbiao, Zhang Jianping, Lin Xiaohui, Wang Jilin, Lin Xiang, 2021. Geochronology, Geochemistry and Geological Significance of Gabbros from Yongding Daping Area, Southwest Fujian. Earth Science, 46(1): 73-86. doi: 10.3799/dqkx.2019.258

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Geochronology, Geochemistry and Geological Significance of Gabbros from Yongding Daping Area, Southwest Fujian

doi: 10.3799/dqkx.2019.258

Wang Jinrong^{1, 2
,
,},
Lü Xinbiao^{1
,
,
,},
Zhang Jianping²,
Lin Xiaohui³,
Wang Jilin⁴,
Lin Xiang⁵

1.
Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, China
2.
The Second Geological Institute of China Metallurgical Geology Bureau, Fuzhou 350108, China
3.
The Second Bureau of China Metallurgical Geology Bureau, Fuzhou 350108, China
4.
The Testing Center of Shandong Bureau of China Metallurgical Geology Bureau, Jinan 250014, China
5.
Brigade in Northern Fujian, Fuzhou 350002, China

Received Date: 2019-10-16
Publish Date: 2021-01-15

Abstract

Abstract

The age,petrogenesis and geodynamic background of the igneous rock belt across southern Hunan,southern Jiangxi,northern Guangdong and southwestern Fujian,have been controversial in last decades. In this paper,new gabbro samples from Daping of Yongding area in southwestern Fujian are studied to discuss related problems. Based on field work and microscopic petrographical observation,baddeleyite U-Pb isotope age,whole rock major and trace elements content,and Sr-Nd isotoperatios are acquired. The obtained isotopic dating result is 184.0±6.5 Ma,which indicates that the time of magmatism is in early Jurassic. Whole rock data show that these gabbros are high K₂O and high K₂O+Na₂O,no Nb and Ta positive anomalies,(⁸⁷Sr/⁸⁶Sr)_i value are between 0.708 0 and 0.709 0,ε_Nd(t) value are from -3.6 to -3.0. Geochemistry data prove that gabbro originated from partial melting of enriched lithospheric mantle and had not experienced AFC process. At the same time,there are bimodal volcanic rocks and A-type granites formed in same area,indicating a extension dynamic background in Early Jurassic,enriched lithospheric mantle has EMII characteristics and been heated by the upwelling of as the nosphere mantle,their melts formed Yongding Daping gabbros and Fangkeng Formations basalt respectively.
- Southwestern Fujian,
- Yongding Daping,
- gabbro,
- petrogeochemistry

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References(79)

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Geochronology, Geochemistry and Geological Significance of Gabbros from Yongding Daping Area, Southwest Fujian

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