黑龙江东部滚突岭地区斜长角闪岩的原岩性质与变质作用演化

杨岩; 郑常青; 徐学纯; 韩玉宝; 郭柏源

doi:10.3799/dqkx.2018.563

Volume 43 Issue 9

Sep. 2018

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Article Navigation > Earth Science > 2018 > 43(9): 3285-3301

Yang Yan, Zheng Changqing, Xu Xuechun, Han Yubao, Guo Boyuan, 2018. Protolith Property and Metamorphic Evolution of Amphibolites in Guntuling Area, Eastern Heilongjiang. Earth Science, 43(9): 3285-3301. doi: 10.3799/dqkx.2018.563

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Yang Yan, Zheng Changqing, Xu Xuechun, Han Yubao, Guo Boyuan, 2018. Protolith Property and Metamorphic Evolution of Amphibolites in Guntuling Area, Eastern Heilongjiang. Earth Science, 43(9): 3285-3301. doi: 10.3799/dqkx.2018.563

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Protolith Property and Metamorphic Evolution of Amphibolites in Guntuling Area, Eastern Heilongjiang

doi: 10.3799/dqkx.2018.563

1.
College of Earth Sciences, Jilin University; Key Laboratory of Mineral Resources Evaluation of Northeast Asia, Ministry of Land and Resources of China, Changchun 130061, China
2.
No. 217 Geological Team of Shanxi Geological Exploration Bureau of Shanxi Province, Datong 037008, China
3.
Zhuhai College, Jilin University, Zhuhai 519040, China

Received Date: 2017-12-11
Publish Date: 2018-09-15

Abstract

Abstract

The Heilongjiang complex which mainly outcrops to the east of Mudanjiang fault, is distributed in band trending north-south along the western margin of Jiamusi massif. However, there are few reports about the mineral composition and evolution of the metamorphism of the Heilongjiang complex, and the previous studies are mostly concentrated in the typical Heilongjiang complex with metamorphic degree of greenschist facies to blueschist facies. Therefore, geochemical characteristics and metamorphic evolution of amphibolite are studied in this paper. Amphibolites consist mainly of garnet-zoisite-bearing amphibolite and garnet-biotite-amphibole-bearing schist outcopped in Guntuling area, eastern Heilongjiang. Garnet-zoisite-bearing amphibolite is characterized by the enrichment of K and Ti, distinctly depleted Hf, and low ratio of Ta/Yb at (0.09-0.16). Furthermore, LREE has weakly negative anomalies relative to HREE, chondrite-normalized REE diagram shows a flat pattern and has no obvious abnormality, which is similar to the features of MORB. Garnet-biotite-amphibole-bearing schist is characterized by the enrichment of K, Th and Ti; furthermore, LREE has weakly enrichments relative to HREE in the chondrite-normalized REE pattern and has no obvious abnormality, which is almost consistent with OIB. Geochemistry and metamorphic evolution of amphibolites show that majority of them are oceanic tholeiite originated from the environment of the mid-ocean ridge, and minority of them are calc-alkaline basalt originated from the environment of intraplate (continental margin) or oceanic island. The amphibolites have undergone three successive stages:the progressive metamorphic phase of the high greenschist facies (T=400-500℃, P=400-500 MPa), peak metamorphic stage of low amphibolite facies (T=550-640℃, P=590-630 MPa) and near isobaric cooling stage of high-greenschist facies (T=530-560℃, P=530-560 MPa). It records a clockwise P-T path from early increased temperature and pressure to late isothermal depressurization. It is inferred that the metamorphism of amphibolite is probably associated with the collision between the Jiamusi Massif and the Songnen Massif.
- amphibolite,
- geochemistry,
- metamorphic evolution,
- P-T paths,
- Heilongjiang complex

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沈阳化工大学材料科学与工程学院沈阳 110142

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Protolith Property and Metamorphic Evolution of Amphibolites in Guntuling Area, Eastern Heilongjiang

doi: 10.3799/dqkx.2018.563

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