华北克拉通阜平杂岩新太古代-古元古代多期地质事件及其构造性质

杜利林; 杨崇辉; 宋会侠; 王建龙; 段庆松; 黄智强; 程海峰; 耿元生; 任留东

doi:10.3799/dqkx.2020.240

Volume 45 Issue 9

Sep. 2020

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Article Navigation > Earth Science > 2020 > 45(9): 3179-3195

Du Lilin, Yang Chonghui, Song Huixia, Wang Jianlong, Duan Qingsong, Huang Zhiqiang, Cheng Haifeng, Geng Yuansheng, Ren Liudong, 2020. Neoarchean-Paleoproterozoic Multi-Stage Geological Events and Their Tectonic Implications in the Fuping Complex, North China Craton. Earth Science, 45(9): 3179-3195. doi: 10.3799/dqkx.2020.240

Citation:

Du Lilin, Yang Chonghui, Song Huixia, Wang Jianlong, Duan Qingsong, Huang Zhiqiang, Cheng Haifeng, Geng Yuansheng, Ren Liudong, 2020. Neoarchean-Paleoproterozoic Multi-Stage Geological Events and Their Tectonic Implications in the Fuping Complex, North China Craton. Earth Science, 45(9): 3179-3195. doi: 10.3799/dqkx.2020.240

Citation:

Du Lilin, Yang Chonghui, Song Huixia, Wang Jianlong, Duan Qingsong, Huang Zhiqiang, Cheng Haifeng, Geng Yuansheng, Ren Liudong, 2020. Neoarchean-Paleoproterozoic Multi-Stage Geological Events and Their Tectonic Implications in the Fuping Complex, North China Craton. Earth Science, 45(9): 3179-3195. doi: 10.3799/dqkx.2020.240

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Neoarchean-Paleoproterozoic Multi-Stage Geological Events and Their Tectonic Implications in the Fuping Complex, North China Craton

doi: 10.3799/dqkx.2020.240

1.
Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China
2.
Institute of Regional Geological Survey of Hebei Province, Langfang 06500, China

Received Date: 2020-06-27
Publish Date: 2020-09-15

Abstract

Abstract

In this paper, we summarize the evolutionary history on Fuping Complex from the early Neoarchean to late Paleoproterozoic by comprehensive analyses of data collected on its geochemistry, zircon U-Pb dating, isotopic geochemistry and metamorphism. It is found that the protolith of ca. 2.7 Ga gneisses are tonalite with the geochemical features of TTG, and zircons in these gneisses show positive ε_Hf(t) values of 5.44 to 7.50, with single stage model age (T_DM) of 2 745-2 824 Ma, which indicates the intensive crustal growth in early Neoarchean in the Fuping Complex. The late Neoarchean gneisses yield the age of 2 543-2 484 Ma and are mainly composed of tonalite-trondjemite-granodiorite (TTG) besides some monzogranite. TTG gneisses have ε_Nd(t) values ranging from -1.64 to +0.96, with single stage model age (T_DM) of 2.76-3.04 Ga, and zircon ε_Hf(t) of -1.9-+7.91, with single stage model age (T_Hf1) and two stage model age (T_Hf2) of 2 546-2 888 Ma and 2 548-3 119 Ma, respectively. Thus, these TTG are derived from partial melting of the early Neoarchean rocks with some addition of Mesoarchean crust. Gabbro coeval with TTG gneisses displays the features of island arc magma and ca. 2.5 Ga metamorphism in Neoarchean supracrustal rocks, suggesting that the Fuping Complex underwent subduction and arc-continent or continent-continent collision in late Neoarchean. 2.1-2.0 Ga granitoids widely occur in the Fuping Complex with the feartures of A-type granite and the simultaneous volcanic-sedimentary rocks formed intra-continental rift environment in middle Paleoproterozoic. Mafic granulite enclaves in the Fuping Complex yield metamorphic age of 1.89-1.85 Ga and show clockwise P-T paths, which represents closure of intra-continent rifts and cratonization of the North China Craton in late Paleoproterozoic.
- Fuping Complex,
- early Neoarchean to late Paleoproterozoic,
- TTG gneisses,
- A-type granite,
- P-T path,
- cratonization,
- geochemistry

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Neoarchean-Paleoproterozoic Multi-Stage Geological Events and Their Tectonic Implications in the Fuping Complex, North China Craton

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