华北克拉通中部带云中山石榴斜长角闪岩变质演化及其构造意义

郭敏洁; 钱加慧; 尹常青; 张健; 卢成森

doi:10.3799/dqkx.2021.016

Volume 46 Issue 11

Nov. 2021

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Article Navigation > Earth Science > 2021 > 46(11): 3892-3909

Guo Minjie, Qian Jiahui, Yin Changqing, Zhang Jian, Lu Chengsen, 2021. Metamorphic Evolution and Tectonic Implications of Garnet Amphibolite from Yunzhongshan Terrane in Central North China Craton. Earth Science, 46(11): 3892-3909. doi: 10.3799/dqkx.2021.016

Citation:

Guo Minjie, Qian Jiahui, Yin Changqing, Zhang Jian, Lu Chengsen, 2021. Metamorphic Evolution and Tectonic Implications of Garnet Amphibolite from Yunzhongshan Terrane in Central North China Craton. Earth Science, 46(11): 3892-3909. doi: 10.3799/dqkx.2021.016

Citation:

Guo Minjie, Qian Jiahui, Yin Changqing, Zhang Jian, Lu Chengsen, 2021. Metamorphic Evolution and Tectonic Implications of Garnet Amphibolite from Yunzhongshan Terrane in Central North China Craton. Earth Science, 46(11): 3892-3909. doi: 10.3799/dqkx.2021.016

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Metamorphic Evolution and Tectonic Implications of Garnet Amphibolite from Yunzhongshan Terrane in Central North China Craton

doi: 10.3799/dqkx.2021.016

Guo Minjie^{1, 2
,
,},
Qian Jiahui^{1, 2
,
,
,},
Yin Changqing^{1, 2},
Zhang Jian^{1, 2},
Lu Chengsen^{1, 2}

1.
Guangdong Provincial Key Laboratory of Mineral Resources & Geological Processes, School of Earth Sciences and Engineering, Sun Yat-Sen University, Zhuhai 519082, China
2.
Southern Marine Science and Engineering Guangdong Laboratory, Zhuhai 519082, China

Received Date: 2021-01-02
Available Online: 2021-12-04
Publish Date: 2021-11-30

Abstract

Abstract

The Yunzhongshan terrane is situated in the middle segment of the Trans-North China Orogen, a key position connecting the Lüliang and Wutai-Hengshan terranes. Addressing its metamorphic evolution is of great importance in understanding the tectonic process of the Lüliang-Yunzhongshan-Wutai-Hengshan areas. Detailed studies of petrology, phase modelling and geochronology were carried out on garnet amphibolite from the Yunzhongshan terrane. Both samples exhibit clockwise P-T-t paths, which are characterized by rutile-bearing peak stages with P-T conditions of 0.96±0.11 GPa/720±8.0℃(L1903) and 1.26±0.08 GPa/756±14.0℃(L1906), respectively. The post-peak stages are dominated by decompression, accompanied by transition of rutile by ilmenite, growth of plagioclase (+hornblende) coronae surrounding garnet and transition of hornblende by cummingtonite. The late stages are dominated by cooling, with local metasomatism of garnet by chlorite. By comparing petrographical features and chemical compositions of the two samples, it can be concluded that the partial melting of garnet amphibolite is affected by the bulk-rock compositions. The rock is refractory when it is rich in Fe, Mg and Ti and poor in Si and Na. Zircon U-Pb dating yields metamorphic ages of 1 928-1 806 Ma, interpreted to represent the cooling stage of metamorphism. This is supported by high concentration of HREE in zircon grains and low crystallization temperatures of 520-680℃ calculated by Ti-in-zircon thermometer. Comparison of the overall geological characteristics of the Lüliang-Yunzhongshan-Wutai-Hengshan areas shows that the lithostratigraphic units and metamorphism evolution in the Yunzhongshan terrane are very similar to those in the Wutai-Hengshan terranes, which record the Late Paleoproterozoic collision orogeny.
- North China Craton,
- Yunzhongshan terrane,
- garnet amphibolite,
- P-T-t path,
- tectonic implication,
- petrology

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References(82)

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Metamorphic Evolution and Tectonic Implications of Garnet Amphibolite from Yunzhongshan Terrane in Central North China Craton

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