| DETACHMENT FAULT IN DINGGYE AREA IN THE MIDDLE PART OF THE HIMALAYAN OROGEN |
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| 作者姓名： | LIUDemin LIDewei |
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| 作者单位： | CollegeofEarthSciences,ChinaUniversityofGeosciences,Wuhan,HB430074,China |
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| 基金项目： | 中国区域性抵制勘测项目，the Dinggye area |
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| 摘 要： | Dinggye lies in the middle part of the Himalayan Orogen. A lot of low angle extension detachment faults have been developed in Dinggye area and some of them make up the main body of the South Tibet Detachment System. On the whole, the extension direction of all the detachment faults is perpendicular to the strike of the Himalayan Orogen. Each detachment fault has its distinct characteristics. Mylonite was extensively developed in the detachment faults and can be divided into a variety of types such as siliceous mylonite, felsic mylonite, granite mylonite, protomylonite, crystallization mylonite and so on. On the basis of our field survey works, these detachment faults can be classified according to their locations into three units listed as follows: (1) In the northern part of the study area, the detachment faults occur on large scale and in orbicular shape, and form the middle layer of the metamorphic core complexes. (2) In the southern part of the study area, the detachment faults occur in linear shape that is parallel to the Himalayan Orogen and has a stable attitude, and have undergone two phases of development. In the first phase, the Rouqiechun Group rocks were formed and make up the hanging wall, while in the second phase the Jiachun Group rocks were formed and make up the hanging wall. (3) In the southeastern part of the study area, the detachment faults strike nearly along southeast direction in a stable way and some of these detachment faults were distorted by the late-formed faults and folds. Furthermore, in the southwestern part of the study area, the ductile shear zones are parallel to the detachment faults.
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| 关 键 词： | 中国 喜玛拉雅山 定日地区 断层脱离 延伸结构 断层特性 糜棱岩类型 |
DETACHMENT FAULT IN DINGGYE AREA IN THE MIDDLE PART OF THE HIMALAYAN OROGEN |
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| LIUDemin LIDewei.DETACHMENT FAULT IN DINGGYE AREA IN THE MIDDLE PART OF THE HIMALAYAN OROGEN[J].Geotectonicaet Metallogenia,2003,27(1):70-80. |
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| Authors: | Liu Demin Li Dewei |
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| Abstract: | Dinggye lies in the middle part of the Himalayan Orogen. A lot of low angle extension detachment faults have been developed in Dinggye area and some of them make up the main body of the South Tibet Detachment System. On the whole, the extension direction of all the detachment faults is perpendicular to the strike of the Himalayan Orogen. Each detachment fault has its distinct characteristics. Mylonite was extensively developed in the detachment faults and can be divided into a variety of types such as siliceous mylonite, felsic mylonite, granite mylonite, protomylonite, crystallization mylonite and so on. On the basis of our field survey works, these detachment faults can be classified according to their locations into three units listed as follows: (1) In the northern part of the study area, the detachment faults occur on large scale and in orbicular shape, and form the middle layer of the metamorphic core complexes. (2) In the southern part of the study area, the detachment faults occur in linear shape that is parallel to the Himalayan Orogen and has a stable attitude, and have undergone two phases of development. In the first phase, the Rouqiechun Group rocks were formed and make up the hanging wall, while in the second phase the Jiachun Group rocks were formed and make up the hanging wall. (3) In the southeastem part of the study area, the detachment faults strike nearly along southeast direction in a stable way and some of these detachment faults were distorted by the late-formed faults and folds. Furthermore, in the southwestern part of the study area, the ductile shear zones are parallel to the detachment faults. |
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| Keywords: | detachment fault extension structure Dinggye Area Himalayan Orogen |
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