辽东半岛古元古代北辽河群浪子山组巴罗式变质带分布、变质特征及其构造意义

文飞; 田忠华; 刘平华; 向华

doi:10.3799/dqkx.2020.086

Volume 45 Issue 9

Sep. 2020

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Article Navigation > Earth Science > 2020 > 45(9): 3403-3419

Wen Fei, Tian Zhonghua, Liu Pinghua, Xiang Hua, 2020. A Case Study of Barrovian Metamorphic Zone of Langzishan Formation of Northern Liaohe Group, Liaodong Peninsula. Earth Science, 45(9): 3403-3419. doi: 10.3799/dqkx.2020.086

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Wen Fei, Tian Zhonghua, Liu Pinghua, Xiang Hua, 2020. A Case Study of Barrovian Metamorphic Zone of Langzishan Formation of Northern Liaohe Group, Liaodong Peninsula. Earth Science, 45(9): 3403-3419. doi: 10.3799/dqkx.2020.086

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A Case Study of Barrovian Metamorphic Zone of Langzishan Formation of Northern Liaohe Group, Liaodong Peninsula

doi: 10.3799/dqkx.2020.086

Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China

Received Date: 2020-03-27
Publish Date: 2020-09-15

Abstract

Abstract

Barrovian-type progressive metamorphism could lead to a new understanding of crustal thickening and orogenesis. We conduct a detailed field survey and indoor researches about the Barrovian metamorphic zone of the Lianshanguan-Qijiabao of the Benxi area, to understand better of field distribution and metamorphic characteristics of Barrovian metamorphic zone which is located at the Langzishan Formation of the North Liaohe Group in Liaodong Peninsula. The Barrovian metamorphic zone in the Langzishan Formation is divided into biotite zone, garnet zone, staurolite zone, kyanite zone from south to north, according to detailed field mapping. The analysis of petrography suggests kyanite-staurolite-garnet mica-schist of kyanite zone has three stages mineral assemblages:(1) Progressive metamorphic mineral assemblages (M₁) are Pl+Qz+Ms+Bt+Ctd+Chl±Grt; (2) metamorphic peak (M₂) is characterized by Ky+St+Grt+Bt+Ms+Qz+Pl+Ilm; (3) retrograde metamorphic stage mainly has trichoid sillimanite (M_3-1) and chlorite and sericite around rims and cracks of porphyroblasts (M_3-2). Phase equilibrium modeling shows metamorphic P-T of progressive metamorphic stage and peak stage of kyanite-staurolite-garnet mica-schist are respectively ~440 ℃/~3.7 kbar, ~670 ℃/~7.9 kbar, and the rock has a typical clockwise P-T path. The results of U-Pb geochronology of metamorphic zircons indicate kyanite-staurolite-garnet mica-schist has experienced peak metamorphism at ~1.96 Ga; these ages of U-Pb detrital zircons are scattered among 2 631-2 020 Ma, indicating the clastic sediments may be from an ancient Archean basement of ~2.5 Ga and magmatic rocks of 2.2-2.1 Ga. Combined with previous research data, the clockwise P-T-t path and thrusting nappe structure recorded by the Barrovian metamorphic zone of the Langzishan Formation represent Jiao-Liao-Ji belt has experienced crustal thickening produced by orogenesis around 1.96 Ga.
- Barrovian metamorphic zone,
- Langzishan Formation of Liaohe Group,
- P-T-t path,
- crustal thickening,
- petrology

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