中国东南部晚中生代基性岩脉地幔源区的岩性演化历史

雷祝梁; 曾罡; 王小均; 陈立辉

doi:10.3799/dqkx.2019.021

Volume 44 Issue 4

Apr. 2019

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Lei Zhuliang, Zeng Gang, Wang Xiaojun, Chen Lihui, 2019. Mantle Source Lithology of Late Mesozoic Mafic Dikes in Southeastern China. Earth Science, 44(4): 1159-1168. doi: 10.3799/dqkx.2019.021

Citation:

Lei Zhuliang, Zeng Gang, Wang Xiaojun, Chen Lihui, 2019. Mantle Source Lithology of Late Mesozoic Mafic Dikes in Southeastern China. Earth Science, 44(4): 1159-1168. doi: 10.3799/dqkx.2019.021

Lei Zhuliang, Zeng Gang, Wang Xiaojun, Chen Lihui, 2019. Mantle Source Lithology of Late Mesozoic Mafic Dikes in Southeastern China. Earth Science, 44(4): 1159-1168. doi: 10.3799/dqkx.2019.021

Citation:

Lei Zhuliang, Zeng Gang, Wang Xiaojun, Chen Lihui, 2019. Mantle Source Lithology of Late Mesozoic Mafic Dikes in Southeastern China. Earth Science, 44(4): 1159-1168. doi: 10.3799/dqkx.2019.021

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Mantle Source Lithology of Late Mesozoic Mafic Dikes in Southeastern China

doi: 10.3799/dqkx.2019.021

State Key Laboratory for Mineral Deposits Research, School of Earth Sciences and Engineering, Nanjing University, Nanjing 210023, China

Received Date: 2018-12-19
Publish Date: 2019-04-15

Abstract

Abstract

Late Mesozoic magmatism in southeastern China was controlled by the subduction of paleo-Pacific plate, and the mantle beneath the area should also have been affected by such process.Late Mesozoic mafic dikes are widely distributed in southeastern China, especially in the coastal areas, which provide an ideal setting for studying the mantle evolution and subduction process of paleo-Pacific plate. Here it summarizes the chronological and geochemical data of mafic dikes in Hunan, Jiangxi, Zhejiang, Fujian and Guangdong provinces. Source lithologies of these rocks are identified by the compositions of fractionation-corrected primary magmas. The study indicates that the mantle lithologies of these mafic dikes in southeastern China do not show obvious differences in space, but significant changes with time. The source lithologies of mafic dikes during the period of 150-110 Ma are composed of SiO₂-rich pyroxenite and SiO₂-poor pyroxenite, whereas the source lithologies during 110-64 Ma are primarily composed of SiO₂-poor pyroxenite, with minor peridotite. Therefore, it is suggested that the lithological variation of Late Mesozoic mantle beneath southeastern China is controlled by the subduction of paleo-Pacific plate via the variation of the subduction angle.
- mafic dike,
- primary magma,
- source lithology,
- paleo-Pacific plate,
- southeastern China,
- petrology

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References(52)

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Mantle Source Lithology of Late Mesozoic Mafic Dikes in Southeastern China

doi: 10.3799/dqkx.2019.021

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