辽东半岛隆昌地区~2 113 Ma变辉长岩地球化学与Hf同位素研究:对胶辽吉造山带构造演化的制约

赵岩; 寇林林; 张朋; 毕中伟; 李东涛; 陈聪

doi:10.3799/dqkx.2019.185

Volume 44 Issue 10

Nov. 2019

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Article Navigation > Earth Science > 2019 > 44(10): 3333-3345

Zhao Yan, Kou Linlin, Zhang Peng, Bi Zhongwei, Li Dongtao, Chen Cong, 2019. Characteristics of Geochemistry and Hf Isotope from Meta-Gabbro in Longchang Area, Liaodong Peninsula: Implications on Evolution of the Jiao-Liao-Ji Paleoproterozoic Orogenic Belt. Earth Science, 44(10): 3333-3345. doi: 10.3799/dqkx.2019.185

Citation:

Zhao Yan, Kou Linlin, Zhang Peng, Bi Zhongwei, Li Dongtao, Chen Cong, 2019. Characteristics of Geochemistry and Hf Isotope from Meta-Gabbro in Longchang Area, Liaodong Peninsula: Implications on Evolution of the Jiao-Liao-Ji Paleoproterozoic Orogenic Belt. Earth Science, 44(10): 3333-3345. doi: 10.3799/dqkx.2019.185

Citation:

Zhao Yan, Kou Linlin, Zhang Peng, Bi Zhongwei, Li Dongtao, Chen Cong, 2019. Characteristics of Geochemistry and Hf Isotope from Meta-Gabbro in Longchang Area, Liaodong Peninsula: Implications on Evolution of the Jiao-Liao-Ji Paleoproterozoic Orogenic Belt. Earth Science, 44(10): 3333-3345. doi: 10.3799/dqkx.2019.185

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Characteristics of Geochemistry and Hf Isotope from Meta-Gabbro in Longchang Area, Liaodong Peninsula: Implications on Evolution of the Jiao-Liao-Ji Paleoproterozoic Orogenic Belt

doi: 10.3799/dqkx.2019.185

Zhao Yan^{1,2
,},
Kou Linlin^1,2,
Zhang Peng^1,2,
Bi Zhongwei^1,2,
Li Dongtao^1,2,
Chen Cong^1,2

1.
Shenyang Center of Geological Survey, China Geological Survey, Shenyang 110034, China
2.
Northeast China Center for Geoscience and Innovation, Shenyang 110034, China

Received Date: 2019-07-29
Publish Date: 2019-11-11

Abstract

Abstract

The meta-gabbro, distributed in the Longchang area, eastern part of the North China craton, yields a zircon U-Pb age of 2 113±15 Ma by LA-ICP-MS. Detailed geochemistry analyses, whole rock Nd isotope and zircon U-Pb and in-situ Hf isotope analyses were made to confine tectonic settings of the Jiao-Liao-Ji orogenic belt and other crucial problems. The gabbro samples studied show calc-alkaline to high potassic alkaline series features with weak alteration and also low content of TiO₂(< 1.31%), moderate content of MgO (6.88%-7.62%), FeO^T(11.91%-14.25%) and K₂O (0.85%-1.23%). The studied samples are characterized with low REE content and show weak REE fractionation and depletion in high field strength elements like P and Hf. The samples also show enrichment in large ion lithophile elements like Rb, Ba and K, and enrichment in Nd isotope content, with ε_Nd(t) values of -1.6 to 2.6. (¹⁷⁶Hf/¹⁷⁷Hf)_i of zircon from the meta-gabbro samples ranging from 0.281 497 to 0.281 612, and the calculated ε_Hf(t) values ranging from 2.2 to 6.3. The calculated Hf modal ages are 2.25 to 2.33 Ga. Several crucial diagrams from meta-gabbro sample analysis results show far distance from MORB or OIB both of which are typical basalts distributed in a rift geological setting. E-MORB with continental crust component mixed in may be the exact origin of the meta-basalts in the Longchang area. It can be concluded that there was ocean crust subduction in~2.1 Ga within the Jiao-Liao-Ji orogenic belt, with possible paleo-arc and the evolution model of the Jiao-Liao-Ji orogenic belt is more like an arc-continental collision model.
- North China craton,
- Jiao-Liao-Ji orogenic belt,
- Longchang area,
- Paleoproterozoic,
- meta-gabbro,
- geochemistry

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References(59)

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Characteristics of Geochemistry and Hf Isotope from Meta-Gabbro in Longchang Area, Liaodong Peninsula: Implications on Evolution of the Jiao-Liao-Ji Paleoproterozoic Orogenic Belt

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