冀西北怀安杂岩的年代学、地球化学、Nd-Hf-O同位素组成及其地质意义

郝光明; 颉颃强; 刘永顺; 董春艳; 任鹏; 白文倩; 王树庆; 胡晓佳; 万渝生

doi:10.3799/dqkx.2020.188

Volume 45 Issue 9

Sep. 2020

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Article Navigation > Earth Science > 2020 > 45(9): 3353-3371

Hao Guangming, Xie Hangqiang, Liu Yongshun, Dong Chunyan, Ren Peng, Bai Wenqian, Wang Shuqing, Hu Xiaojia, Wan Yusheng, 2020. SHRIMP Zircon U-Pb Ages, Geochemistry, Nd-Hf-O Isotopic Compositions of the Huai'an Complex in the Northwest of Hebei Province and Its Geological Significance. Earth Science, 45(9): 3353-3371. doi: 10.3799/dqkx.2020.188

Citation:

Hao Guangming, Xie Hangqiang, Liu Yongshun, Dong Chunyan, Ren Peng, Bai Wenqian, Wang Shuqing, Hu Xiaojia, Wan Yusheng, 2020. SHRIMP Zircon U-Pb Ages, Geochemistry, Nd-Hf-O Isotopic Compositions of the Huai'an Complex in the Northwest of Hebei Province and Its Geological Significance. Earth Science, 45(9): 3353-3371. doi: 10.3799/dqkx.2020.188

Citation:

Hao Guangming, Xie Hangqiang, Liu Yongshun, Dong Chunyan, Ren Peng, Bai Wenqian, Wang Shuqing, Hu Xiaojia, Wan Yusheng, 2020. SHRIMP Zircon U-Pb Ages, Geochemistry, Nd-Hf-O Isotopic Compositions of the Huai'an Complex in the Northwest of Hebei Province and Its Geological Significance. Earth Science, 45(9): 3353-3371. doi: 10.3799/dqkx.2020.188

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SHRIMP Zircon U-Pb Ages, Geochemistry, Nd-Hf-O Isotopic Compositions of the Huai'an Complex in the Northwest of Hebei Province and Its Geological Significance

doi: 10.3799/dqkx.2020.188

1.
Beijing SHRIMP Center, Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China
2.
Tianjin Center, China Geological Survey, Tianjin 300170, China
3.
School of Earth Science and Resources, Chang'an University, Xi'an 710054, China

Received Date: 2020-04-13
Publish Date: 2020-09-15

Abstract

Abstract

The Huai'an Complex in Northwest Hebei Province consists of meta-supracrustal rocks and metamorphic plutonic rocks. There are still some controversies about some issues such as the formation age of supracrustal rocks, the tectonic setting of Huai'an Complex and the relationship between Huai'an Complex and Khondalite belt. Some representative outcrops of the Huai'an Complex have been studied in detail by field investigation, petrology, zircon SHRIMP U-Pb dating, isotopic and elements geochemistry. All of the 4 samples yielded metamorphic ages of 1.86-1.81 Ga, which further supports the previous view that the Huai'an Complex suffered extensive late Paleoproterozoic metamorphism. The BIF-bearing supracrustal rock assemblage was intruded and enclaved by the meta-gabbro (HB1425) and gneissic tonalite (HB1426), which yielded the formation ages of ca. 2.5 Ga and 2.55 Ga, respectively. It suggests that the supracrustal rocks in this location are older than 2.55 Ga. Leptite (HB1431) and hypersthene garnet biotite plagioclase gneiss (Hy-Grt-Bt-Pl gneiss, HB1435) contain the oldest detrital zircons of 2.46 Ga and 2.51 Ga, respectively, probably together with some Paleoproterozoic zircons, indicating that the supracrustal rocks in the two localities are Paleoproterozoic. These results further confirm the development of two stage supracrustal rock assemblages in the Huai'an Complex. The whole rocks ε_Nd(t), T_DM1 and T_DM2 of the meta-gabbro and gneissic tonalite are +2.19 to +3.06, 2.67 to 2.75 Ga and 2.67 to 2.69 Ga, respectively, indicating no widespread older continental crust material is involved in their source and the Neoarchean is the main period of continental crust growth in the Huai'an area. Some of the ~1.82 Ga metamorphic zircons in metagabbro yielded positive ε_Hf(t) values up to +11.1. The most likely reason for the Hf isotope composition is the mantle addition during the Paleoproterozoic metamorphic event. The zircon O-isotope shows that there may be rocks with low δ¹⁸O in the area, and low δ¹⁸O fluid could modify the O-isotope of zircon during the Paleoproterozoic metamorphism. It is concluded that the Huai'an Complex has the similar double-layered crustal structure to the Khondalite Belt although it is different in the proportion of the late Noearchean and Paleoproterozoic rocks. The Huai'an Complex may represent the deeper crustal level of the Khondalite belt due to stronger exhumation.
- zircon U-Pb dating,
- Nd-Hf-O isotopes,
- Huai'an Complex,
- supracrustal rocks,
- North China Craton,
- geochemistry

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