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DOI | 10.1016/j.jsg.2014.10.008 |
The Xuelongshan high strain zone: Cenozoic structural evolution and implications for fault linkages and deformation along the Ailao Shan-Red River shear zone | |
Zhang, Bo; Zhang, Jinjiang; Liu, Jiang; Wang, Yang; Yin, Cunyuan; Guo, Lei; Zhong, Dalai; Lai, Qinzhou; Yue, Yahui | |
通讯作者 | Zhang, B (通讯作者) |
发表日期 | 2014 |
ISSN | 0191-8141 |
起始页码 | 209 |
结束页码 | 233 |
卷号 | 69 |
英文摘要 | New structural, geometric, petrographic, and U-Pb zircon data constrain the kinematics of the Xuelongshan high strain zone, northermost parts of the Ailao Shan-Red River shear zone. In the Xuelongshan range, mylonitic foliation mainly trends NW-SE. On steep foliation and flatted foliation, mineral stretching lineation is various, from gentle to steep, and ductile shear senses indicate a left-lateral, top-to-the-northwest shear movement on the eastern limb, and a left lateral, top-to-the-southeast shear on the western limb of the range. These dome-related ductile geometries and kinematics, namely D1 deformation, represent regional high-temperature metamorphism due to crustal thickening. The superimposed sinistral strike-slip shearing of D2 deformation occurred locally along the earlier domal fabrics. Metamorphism, migmatization, and the emplacement of leucogranitic veins associated with partial melting were syntectonic with the regional-scale upright antiform. LA-ICP-MS U-Pb dating of zircons reveals the late Permian-Triassic and Oligocene thermal events. The latter event (ca. 33-26 Ma or possibly earlier) from the leucogranitic veins corresponds to the regional metamorphism during crustal thickening along the Xuelongshan. These data indicate that the Jiali-Xuelongshan-Diancangshan-Ailao Shan high strain zones can belong to a system around the Eastern Himalayan Syntaxis (EHS), and that the Xuelongshan zone played a role in linking other segments between the Tibet to Indochina in Cenozoic. (C) 2014 Elsevier Ltd. All rights reserved. |
关键词 | LEFT-LATERAL SHEARZIRCON U-PBDIANCANG SHANCONTINENTAL EXTRUSIONCRUSTAL DEFORMATIONWESTERN YUNNANGNEISS DOMESCHINACONSTRAINTSKINEMATICS |
英文关键词 | Mylonitic gneiss; Kinematic; Antiform; Strike-slip; Cenozoic; Xuelongshan |
语种 | 英语 |
WOS研究方向 | Geology |
WOS类目 | Geosciences, Multidisciplinary |
WOS记录号 | WOS:000347742100014 |
来源期刊 | JOURNAL OF STRUCTURAL GEOLOGY |
来源机构 | 中国科学院青藏高原研究所 |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/258336 |
推荐引用方式 GB/T 7714 | Zhang, Bo,Zhang, Jinjiang,Liu, Jiang,et al. The Xuelongshan high strain zone: Cenozoic structural evolution and implications for fault linkages and deformation along the Ailao Shan-Red River shear zone[J]. 中国科学院青藏高原研究所,2014,69. |
APA | Zhang, Bo.,Zhang, Jinjiang.,Liu, Jiang.,Wang, Yang.,Yin, Cunyuan.,...&Yue, Yahui.(2014).The Xuelongshan high strain zone: Cenozoic structural evolution and implications for fault linkages and deformation along the Ailao Shan-Red River shear zone.JOURNAL OF STRUCTURAL GEOLOGY,69. |
MLA | Zhang, Bo,et al."The Xuelongshan high strain zone: Cenozoic structural evolution and implications for fault linkages and deformation along the Ailao Shan-Red River shear zone".JOURNAL OF STRUCTURAL GEOLOGY 69(2014). |
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