大兴安岭中段扎兰屯南部花岗质糜棱岩岩石成因及地质意义

李冬雪; 郑常青; 梁琛岳; 周枭; 杨岩; 宋志伟; 陈龙; 耿志忠; 赵英利

doi:10.3799/dqkx.2021.189

Volume 47 Issue 9

Sep. 2022

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Article Navigation > Earth Science > 2022 > 47(9): 3354-3370

Li Dongxue, Zheng Changqing, Liang Chenyue, Zhou Xiao, Yang Yan, Song Zhiwei, Chen Long, Geng Zhizhong, Zhao Yingli, 2022. Genesis and Geological Significance of Granitic Mylonites in Southern Zhalantun, Central Xing'an Range. Earth Science, 47(9): 3354-3370. doi: 10.3799/dqkx.2021.189

Citation:

Li Dongxue, Zheng Changqing, Liang Chenyue, Zhou Xiao, Yang Yan, Song Zhiwei, Chen Long, Geng Zhizhong, Zhao Yingli, 2022. Genesis and Geological Significance of Granitic Mylonites in Southern Zhalantun, Central Xing'an Range. Earth Science, 47(9): 3354-3370. doi: 10.3799/dqkx.2021.189

Citation:

Li Dongxue, Zheng Changqing, Liang Chenyue, Zhou Xiao, Yang Yan, Song Zhiwei, Chen Long, Geng Zhizhong, Zhao Yingli, 2022. Genesis and Geological Significance of Granitic Mylonites in Southern Zhalantun, Central Xing'an Range. Earth Science, 47(9): 3354-3370. doi: 10.3799/dqkx.2021.189

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Genesis and Geological Significance of Granitic Mylonites in Southern Zhalantun, Central Xing'an Range

doi: 10.3799/dqkx.2021.189

1.
College of Earth Sciences, Jilin University, Changchun 130061, China
2.
Key Laboratory of Mineral Resources Evaluation in Northeast Asia, Ministry of Natural Resources, Jilin University, Changchun 130061, China

Received Date: 2021-10-25
Publish Date: 2022-09-25

Abstract

Abstract

The southern of Zhalantun in the Great Xing'an Range is located between the Xing'an Block (XB) and Songnen Block (SB) in the eastern section of the Central Asian Orogenic Belt (CAOB), which is of great importance for the study on the collision and combination of blocks during the tectonic evolution process. The exposed granitic mylonites were analyzed by geological and geochemical analysis, and zircon U-Pb dating in this paper. LA-ICP-MS zircon U-Pb dating results show that the granitic mylonites are divided into two phases: Phase Ⅰ is the Early Devonian (-398.8 Ma), and Phase Ⅱ is the end of the Late Devonian to the beginning of the Early Carboniferous (351.6-365.7 Ma). The rocks of the two periods are characterized by high SiO₂ (68.20%-77.90%), high alkali (K₂O+Na₂O=6.32%-9.67%) and low magnesium (MgO=0.22%-0.97%), belonging to the aluminous and high potassium calc-alkaline series. The REE distribution pattern is right-leaning [(La/Yb)_N=4.33-10.77], with a slight negative Eu anomaly (δEu=0.03-0.13). All samples were enriched in LILE and depleted in HFSE, which have the characteristics of differentiating Ⅰ-type granites. The two phases of granitic mylonites may be Ⅰ-type-differentiated Ⅰ-type granites formed by island arc magmatism under the background of subduction. Combining regional tectonic evolution and petrochemical research, the early Late Paleozoic granitic magmatism in the northern section of the Great Xing'an Range is related to the collision and combination of the XB and SB. During the Early Devonian-Early Carboniferous, the Zhalantun area was under the subduction environment of the Paleo-Asian Ocean-oriented XB and SB, the collision and closure time of the two blocks here may be the Late Carboniferous.
- granitic mylonite,
- Great Xing'an Range,
- Xing'an Block,
- Central Asian Orogenic Belt,
- geochemistry

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References(103)

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