天镇-怀安地区变质基性岩墙群：华北克拉通古元古代末期碰撞-伸展构造体制转换标志

张家辉; 王惠初; 郭敬辉; 田辉; 任云伟; 常青松; 施建荣; 相振群

doi:10.3799/dqkx.2020.125

Volume 45 Issue 9

Sep. 2020

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Article Navigation > Earth Science > 2020 > 45(9): 3239-3257

Zhang Jiahui, Wang Huichu, Guo Jinghui, Tian Hui, Ren Yunwei, Chang Qingsong, Shi Jianrong, Xiang Zhenqun, 2020. Metamorphic Mafic Dykes from Tianzhen-Huai'an Area: Transformation Criteria of the Late Paleoproterozoic Collision to Extension in the North China Craton. Earth Science, 45(9): 3239-3257. doi: 10.3799/dqkx.2020.125

Citation:

Zhang Jiahui, Wang Huichu, Guo Jinghui, Tian Hui, Ren Yunwei, Chang Qingsong, Shi Jianrong, Xiang Zhenqun, 2020. Metamorphic Mafic Dykes from Tianzhen-Huai'an Area: Transformation Criteria of the Late Paleoproterozoic Collision to Extension in the North China Craton. Earth Science, 45(9): 3239-3257. doi: 10.3799/dqkx.2020.125

Citation:

Zhang Jiahui, Wang Huichu, Guo Jinghui, Tian Hui, Ren Yunwei, Chang Qingsong, Shi Jianrong, Xiang Zhenqun, 2020. Metamorphic Mafic Dykes from Tianzhen-Huai'an Area: Transformation Criteria of the Late Paleoproterozoic Collision to Extension in the North China Craton. Earth Science, 45(9): 3239-3257. doi: 10.3799/dqkx.2020.125

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Metamorphic Mafic Dykes from Tianzhen-Huai'an Area: Transformation Criteria of the Late Paleoproterozoic Collision to Extension in the North China Craton

doi: 10.3799/dqkx.2020.125

Zhang Jiahui^{1, 2, 3
,
,},
Wang Huichu^{1, 2},
Guo Jinghui³,
Tian Hui^{1, 2},
Ren Yunwei^{1, 2},
Chang Qingsong^{1, 2},
Shi Jianrong^{1, 2},
Xiang Zhenqun^{1, 2}

1.
Tianjin Center, China Geological Survey, Tianjin 300170, China
2.
Pre-Cambrain Geological Research Center, China Geological Survey, Tianjin 300170, China
3.
State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China

Received Date: 2020-04-01
Publish Date: 2020-09-15

Abstract

Abstract

Paleoproterozoic is an important orogenic tectonic evolution stage during the formation of the North China Craton. The mafic dyke swarms formed during this period provide important information to understanding the tectonic-magmatic process of rifting-subduction-collision-exhumation of the orogeny. This study reports the metamorphic mafic dykes (two-pyroxene granulite) widely distributed in the Neoarchean-Paleoproterozoic metamorphic base in the Tianzhen-Huai'an area. These dykes occur consistently with regional main tectonic foliation in the field and are mainly composed of clinopyroxene+orthopyroxene+plagioclase+amphibole. The metamorphic age of the mafic dyke is 1 820-1 834 Ma obtained by LA-MC-ICPMS zircon U-Pb isotope dating, which is consistent with the granulite facies metamorphic event in the study area. Based on the analyses of regional mafic dyke age data, we consider that the emplacement age is around 1.95-1.91 Ga. This study documents two types of metamorphic mafic dykes: high Mg low Ti type and low Mg high Ti type. They have experienced different degrees of fractional crystallization of olivine, clinopyroxene and plagioclase. Both types of mafic dykes show negative anomalies in high-field-strength elements (such as Nb, Ta, Ti, Zr, and Hf). According to the zircon Hf isotopic and the geochemical features, we suggest that the mafic dykes originated from a lithospheric mantle metasomatized by subduction fluids, or/and they were contaminated by the crust. Two episodes of metamorphosed mafic dykes are identified in the North China Craton: 2.16-2.04 Ga and 1.97-1.83 Ga. The early stage represents an intra-plate rifting process that occurred on the basis of the initial Craton; in contrast, the later period records transformation from subduction-collision to extensional setting, that is the collisional orogenic tectonic regime changed from horizontal compression to vertical uplift, and the tectonic transition time is roughly around 1.95-1.91 Ga.
- mafic dyke,
- Paleoproterozoic,
- orogeny,
- geochemistry,
- North China Craton

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