冀东青龙-双山子地区新太古代高镁安山岩-镁闪长岩锆石U-Pb年代学、地球化学及大地构造意义

常青松; 王惠初; 荣桂林; 初航; 张健

doi:10.3799/dqkx.2018.273

Volume 44 Issue 1

Jan. 2019

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Chang Qingsong, Wang Huichu, Rong Guilin, Chu Hang, Zhang Jian, 2019. Zircon U-Pb Chronology, Geochemistry and Tectonic Significance of Neoarchean High-Mg Andesites and Magnesian Diorites in Qinglong-Shuangshanzi Area, Eastern Hebei. Earth Science, 44(1): 23-36. doi: 10.3799/dqkx.2018.273

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Chang Qingsong, Wang Huichu, Rong Guilin, Chu Hang, Zhang Jian, 2019. Zircon U-Pb Chronology, Geochemistry and Tectonic Significance of Neoarchean High-Mg Andesites and Magnesian Diorites in Qinglong-Shuangshanzi Area, Eastern Hebei. Earth Science, 44(1): 23-36. doi: 10.3799/dqkx.2018.273

Citation:

Chang Qingsong, Wang Huichu, Rong Guilin, Chu Hang, Zhang Jian, 2019. Zircon U-Pb Chronology, Geochemistry and Tectonic Significance of Neoarchean High-Mg Andesites and Magnesian Diorites in Qinglong-Shuangshanzi Area, Eastern Hebei. Earth Science, 44(1): 23-36. doi: 10.3799/dqkx.2018.273

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Zircon U-Pb Chronology, Geochemistry and Tectonic Significance of Neoarchean High-Mg Andesites and Magnesian Diorites in Qinglong-Shuangshanzi Area, Eastern Hebei

doi: 10.3799/dqkx.2018.273

Chang Qingsong^{1,2
,},
Wang Huichu^1,2,
Rong Guilin³,
Chu Hang^{1,2
,
,},
Zhang Jian¹

1.
Tianjin Center of China Geological Survey, Tianjin 300170, China
2.
Pre-Cambrain Geological Research Center of China Geological Survey, Tianjin 300170, China
3.
Hebei Institute of Geological Survey, Shijiazhuang 050081, China

Received Date: 2018-05-13
Publish Date: 2019-01-15

Abstract

Abstract

Eastern Hebei Province is located in the northern margin of the North China Craton, but magmatic genesis and tectonic setting of Neoarchean igneous rocks in the area still remain controversial. Systematic geochronologic and geochemical study of Neoarchean supracrustal and intrusive rocks in Qinglong-Shuangshanzi area, eastern Hebei are presented in this paper. Zircon LA-MC-ICP-MS U-Pb isotopic dating reveals that the meta-andesite erupted at 2 576 Ma, and the intrusive rocks (gabbro-diorites, tonalites and quartz diorites) emplaced in a range of 2 484 Ma to 2 535 Ma. Part of the early-formed meta-andesites shows high-Mg andesite geochemical characteristics, which indicates these rocks were generated from partial melting of mantle wedge peridotite metasomatised by fluids from dehydration of the subducted slab. The magnesian diorites show adakite characteristics, which suggests they have source characteristics of partial melting of mantle wedge peridotite metasomatised by felsic melts of the subducted slab. Both of the high-Mg meta-andesites and adakite like magnesian diorites belong to a suite of island arc assemblages. Combining previous regional studies, it is concluded that Qinglong-Shuangshanzi area was under a tectonic setting of active continental margin during Neoarchean era.
- eastern Hebei,
- high-Mg andesites,
- adakite like rocks,
- magnesian diorites,
- zircon U-Pb chronology,
- geochemistry

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Zircon U-Pb Chronology, Geochemistry and Tectonic Significance of Neoarchean High-Mg Andesites and Magnesian Diorites in Qinglong-Shuangshanzi Area, Eastern Hebei

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