内蒙古海勒斯台俯冲增生混杂岩地质特征及发现的意义

林敏; 马昌前; 徐立明; 李玉娟; 杨仲; 汤建荣

doi:10.3799/dqkx.2019.200

Volume 44 Issue 10

Nov. 2019

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Article Navigation > Earth Science > 2019 > 44(10): 3279-3296

Lin Min, Ma Changqian, Xu Liming, Li Yujuan, Yang Zhong, Tang Jianrong, 2019. Geological Characteristics of Subduction-Accretionary Complexes in Hellestein District, Inner Mongolia and Its Discovery Significance. Earth Science, 44(10): 3279-3296. doi: 10.3799/dqkx.2019.200

Citation:

Lin Min, Ma Changqian, Xu Liming, Li Yujuan, Yang Zhong, Tang Jianrong, 2019. Geological Characteristics of Subduction-Accretionary Complexes in Hellestein District, Inner Mongolia and Its Discovery Significance. Earth Science, 44(10): 3279-3296. doi: 10.3799/dqkx.2019.200

Citation:

Lin Min, Ma Changqian, Xu Liming, Li Yujuan, Yang Zhong, Tang Jianrong, 2019. Geological Characteristics of Subduction-Accretionary Complexes in Hellestein District, Inner Mongolia and Its Discovery Significance. Earth Science, 44(10): 3279-3296. doi: 10.3799/dqkx.2019.200

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Geological Characteristics of Subduction-Accretionary Complexes in Hellestein District, Inner Mongolia and Its Discovery Significance

doi: 10.3799/dqkx.2019.200

Lin Min^{1,2
,},
Ma Changqian^{1
,
,},
Xu Liming^1,2,
Li Yujuan²,
Yang Zhong²,
Tang Jianrong²

1.
Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, China
2.
Geological Survey of Fujian Province, Fuzhou 350013, China

Received Date: 2019-08-08
Publish Date: 2019-11-11

Abstract

Abstract

The Hellestein subduction accretive mélange occurs in the middle part of the Hegen Mountain-Heihe suture zone, and its structural style is left thrust shear as a whole. The accretive mélange consists of matrix and rock complex. The main matrix is composed of mylonite, phyllonite, ultramylonite and a small amount of tuff, siltstone and fine sandstone. The tectonic environment is a pre-arc basin and the age is mainly Middle Cambrian. The rock complex includes oceanic island seamount rock block, back-arc oceanic basin oceanic crust fragment, volcanic arc block and rift continental block. The age of the complexes ranges mainly from Middle Cambrian to Middle Ordovician. Based on the deformation degree and contact relationship of subduction accretion complex, and combined with the age of matrix, rock complex and TTG rock series, the age of formation of Hellestein subduction accretion complex is determined as Middle-Late Ordovician. The subduction of this area began in the Early Cambrian and formed a volcanic island arc on the continental margin, then the back-arc basin developed in the Early Ordovician, and the oceanic crust appeared in the back-arc basin of the Middle Ordovician. At the same time, the Middle Cambrian matrix returned to rise in the Middle Ordovician after subduction. In the end, the back-arc oceanic basin soon died due to the continuous regional convergence and compression of plate in the Late Ordovician. The arc land began to collide, leading to bidirectional subduction. During the process of arc-continent collision, the new blocks of the back-arc basin formed in the late stage were mixed into the matrix formed in the early stage.
- Inner Mongolia,
- Hellestein,
- tectonic mélange,
- subduction accretion,
- Early Paleozoic,
- petrology

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References(75)

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