浙西南松阳地区斜长角闪岩变质作用演化及地质意义

郭腾达; 郑常青; 周喜文; 董云峰; 周枭; 王照元; 宋旸; 石磊

doi:10.3799/dqkx.2019.059

Volume 46 Issue 2

Feb. 2021

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Article Navigation > Earth Science > 2021 > 46(2): 489-503

Guo Tengda, Zheng Changqing, Zhou Xiwen, Dong Yunfeng, Zhou Xiao, Wang Zhaoyuan, Song Yang, Shi Lei, 2021. Metamorphism Evolution and Geological Significance of Amphibolite in Songyang Area of Southwest Zhejiang Province. Earth Science, 46(2): 489-503. doi: 10.3799/dqkx.2019.059

Citation:

Guo Tengda, Zheng Changqing, Zhou Xiwen, Dong Yunfeng, Zhou Xiao, Wang Zhaoyuan, Song Yang, Shi Lei, 2021. Metamorphism Evolution and Geological Significance of Amphibolite in Songyang Area of Southwest Zhejiang Province. Earth Science, 46(2): 489-503. doi: 10.3799/dqkx.2019.059

Citation:

Guo Tengda, Zheng Changqing, Zhou Xiwen, Dong Yunfeng, Zhou Xiao, Wang Zhaoyuan, Song Yang, Shi Lei, 2021. Metamorphism Evolution and Geological Significance of Amphibolite in Songyang Area of Southwest Zhejiang Province. Earth Science, 46(2): 489-503. doi: 10.3799/dqkx.2019.059

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Metamorphism Evolution and Geological Significance of Amphibolite in Songyang Area of Southwest Zhejiang Province

doi: 10.3799/dqkx.2019.059

Guo Tengda^{1, 2
,
,},
Zheng Changqing^{1, 2
,
,
,},
Zhou Xiwen³,
Dong Yunfeng^{1, 2},
Zhou Xiao^{1, 2},
Wang Zhaoyuan^{1, 2},
Song Yang^{1, 2},
Shi Lei^{1, 2}

1.
College of Earth Sciences, Jilin University, Changchun 130061, China
2.
MNR Key Laboratory of Mineral Resources Evaluation in Northeast Asia, Jilin University, Changchun 130061, China
3.
Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China

Received Date: 2019-06-22
Publish Date: 2021-02-15

Abstract

Abstract

Amphibolite of the Badu complex in the Songyang area of Southwest Zhejiang Province is one of the major metamorphic rocks consisting of Precambrian metamorphic basement, However, its protolith and metamorphic evolution remain unclear. In this study, on the basis of the investigation of petrography, mineral chemistry and whole-rock major and trace element analyses, it is found that the protolith for amphilbolite belongs to high Fe tholeiite, which likely formed in an island-arc setting. The prograde metamorphic information is preserved in the garnet core, showing that peak metamorphic stage (M1) consists of garnet (rim)+edenite+plagioclase (An=40-43) +clinopyroxene+biotite+ilmenite and decompression metamorphic stage (M2) is characterized by the assemblage of actinolite + chlorite + sphene±biotite±ilmenite. By means of phase equilibrium simulation and traditional thermobarometer, it gets P-T conditions of 800-850 MPa and 710-740℃ for M1, ~480 MPa and~440℃ for M2, respectively. These P and T conditions confine a typical clockwise P-T path. Through regional comparison, the amphibolite in Badu complex may have undergone Indosinian metamorphism and the amalgamation of the Indochina with South China and North China blocks.
- Badu complex,
- amphibolite,
- island arc basalt,
- metamorphism evolution,
- Southwest Zhejiang Province,
- petrology

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References(81)

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Metamorphism Evolution and Geological Significance of Amphibolite in Songyang Area of Southwest Zhejiang Province

doi: 10.3799/dqkx.2019.059

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