大兴安岭北段扎兰屯地区斜长角闪岩年代学、地球化学和Hf同位素特征及其构造意义

钱程; 汪岩; 陆露; 秦涛; 李林川; 崔天日; 陈会军; 杨柳

doi:10.3799/dqkx.2019.027

Volume 44 Issue 10

Nov. 2019

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Article Navigation > Earth Science > 2019 > 44(10): 3193-3208

Qian Cheng, Wang Yan, Lu Lu, Qin Tao, Li Linchuan, Cui Tianri, Chen Huijun, Yang Liu, 2019. Geochronology, Geochemistry and Hf Isotopic Composition of Amphibolite from Zhalantun Region in Northern Great Xing'an Range and Its Tectonic Significance. Earth Science, 44(10): 3193-3208. doi: 10.3799/dqkx.2019.027

Citation:

Qian Cheng, Wang Yan, Lu Lu, Qin Tao, Li Linchuan, Cui Tianri, Chen Huijun, Yang Liu, 2019. Geochronology, Geochemistry and Hf Isotopic Composition of Amphibolite from Zhalantun Region in Northern Great Xing'an Range and Its Tectonic Significance. Earth Science, 44(10): 3193-3208. doi: 10.3799/dqkx.2019.027

Citation:

Qian Cheng, Wang Yan, Lu Lu, Qin Tao, Li Linchuan, Cui Tianri, Chen Huijun, Yang Liu, 2019. Geochronology, Geochemistry and Hf Isotopic Composition of Amphibolite from Zhalantun Region in Northern Great Xing'an Range and Its Tectonic Significance. Earth Science, 44(10): 3193-3208. doi: 10.3799/dqkx.2019.027

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Geochronology, Geochemistry and Hf Isotopic Composition of Amphibolite from Zhalantun Region in Northern Great Xing'an Range and Its Tectonic Significance

doi: 10.3799/dqkx.2019.027

1.
Shenyang Center of Geological Survey, China Geological Survey, Shenyang 110034, China
2.
College of Paleontology, Shenyang Normal University, Shenyang 110034, China
3.
Key Laboratory of Evolution of Past Life in Northeast Asia, Ministry of Natural Resources, Shenyang 110034, China

Received Date: 2019-02-21
Publish Date: 2019-11-11

Abstract

Abstract

The Late Paleozoic magmatic rocks with ductile deformation occurred in the Zhalantun region located in the middle of the Hegenshan-Heihe tectonic belt, which well record the tectonic evolution history of the Late Paleozoic, but the research degree is low. Through the field investigation, the geochronology and geochemistry of amphibolite lenticles from granitic mylonite in the Toudaogou, southern Zhalantun, are systematically studied, and the petrogenesis and tectonic setting of the amphibolite are discussed. It is found that the protolith of amphibolite is basaltic andesite, yielding an average zircon U-Pb age of 373.0±2.6 Ma which is equivalent to the volcanic rocks of Daminshan Group. The rocks belong to sodium series, which are enriched in light rare earth elements, large ion lithophile elements, but are depleted in high field strength elements. The zircon ε_Hf(t) values of the amphibolite range from +5.39 to +10.06, similar to the features of the Xing'an island arc, suggesting that the protolith of amphibolite may be derived from the melting of a juvenile lower crust originating from depleted mantle which were modified by fluids stemmed from altered ocean crust, and supposedly formed in an fore arc basin above the subduction zone. In the Late Devonian, back-arc basin, inter-arc basin and fore-arc basin ocurred in the southeast region of Erguan-Xing'an block. The amphibolite and its surrounding granitic mylonite experienced multistage metamorphic deformation. The amphibolite yielded a metamorphic age of about 241.5±9.6 Ma, which may be related to the extension of the late evolution of the Tianshan-Xingmeng orogenic belt.
- amphibolite,
- zircon U-Pb geochronology,
- Hf isotopic composition,
- Hegenshan-Heihe suture belt,
- petrology

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References(80)

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Geochronology, Geochemistry and Hf Isotopic Composition of Amphibolite from Zhalantun Region in Northern Great Xing'an Range and Its Tectonic Significance

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