东乌旗罕乌拉韧性剪切带的构造属性及其年代约束

程银行; 滕学建; 李艳锋; 杨俊泉; 刘洋; 彭丽娜; 李影; 李敏

doi:10.3799/dqkx.2014.036

Volume 39 Issue 4

Apr. 2014

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Article Navigation > Earth Science > 2014 > 39(4): 375-386

Cheng Yinhang, Teng Xuejian, Li Yanfeng, Yang Junquan, Liu Yang, Peng Li'na, Li Ying, Li Min, 2014. Chronology Constraint and Tectonic Evolution of Hanwula Early Cretaceous Ductile Shear Belt in Dong Ujimqin, Inner Mongolia. Earth Science, 39(4): 375-386. doi: 10.3799/dqkx.2014.036

Citation:

Cheng Yinhang, Teng Xuejian, Li Yanfeng, Yang Junquan, Liu Yang, Peng Li'na, Li Ying, Li Min, 2014. Chronology Constraint and Tectonic Evolution of Hanwula Early Cretaceous Ductile Shear Belt in Dong Ujimqin, Inner Mongolia. Earth Science, 39(4): 375-386. doi: 10.3799/dqkx.2014.036

Citation:

Cheng Yinhang, Teng Xuejian, Li Yanfeng, Yang Junquan, Liu Yang, Peng Li'na, Li Ying, Li Min, 2014. Chronology Constraint and Tectonic Evolution of Hanwula Early Cretaceous Ductile Shear Belt in Dong Ujimqin, Inner Mongolia. Earth Science, 39(4): 375-386. doi: 10.3799/dqkx.2014.036

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Chronology Constraint and Tectonic Evolution of Hanwula Early Cretaceous Ductile Shear Belt in Dong Ujimqin, Inner Mongolia

doi: 10.3799/dqkx.2014.036

Tianjin Institute of Geology and Mineral Resources, Tianjin 300170, China

Received Date: 2013-09-15
Publish Date: 2014-04-15

Abstract

Abstract

Through field investigation, microscopic analyses of oriented samples and zircon LA-MC-ICPMS U-Pb dating, granitic mylonites of the ducticle shear belt in Hanwula area have been studied, for their kinematic characteristics and ages. In these rocks, main rock-forming minerals (feldspar and quartz) all show the typical characteristics of plastic deformation and dynamic crystallization, with typical fabrics such as "σ", "δ" and "S-C" structures. Averages of 34 coupled attitudes of mineral lineation and shearing foliation are 338°∠24° and 303°∠17°. All the above indicate the left-lateral slip in this belt. The zircon U-Pb dating data suggest that these granitic mylonites are formed in Early Cretaceous with detail ages of 135.9±1.2 Ma to 130.0±0.5 Ma and the ductile shear belt is covered by glutenite of the Lower Cretaceous Damoguaihe Group (Valanginian-Hauterivian). Thus, we consider that Dong Ujimqin area had experienced regional left-lateral extensional structure movement in Early Cretaceous. This study filled the blank of petrology and geochronology study of the ductile shear belt in Hanwula and enhanced the understanding of the Early Cretaceous crust tectonic evolution in Dong Ujimqin.
- Early Cretaceous,
- ductile shear belt,
- granitic mylolite,
- tectonics,
- zircon U-Pb dating,
- geochronology

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Chronology Constraint and Tectonic Evolution of Hanwula Early Cretaceous Ductile Shear Belt in Dong Ujimqin, Inner Mongolia

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