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- W2354135323 abstract "The Quegetagedu ductile deformation belts are located in the east part of Tianshan region. From a structural point of view, the belts belong to the Huai-nan continental marginal activity group in the Kazakhstan-Junggar slab. The deformation belts are formed by Late Carboniferous rocks, mainly mylonitization volcanic rocks and volcanic clastic sedimentary rocks. Within the belts, the schistosity has a steep dip to the south is well developed. The penetration-stretching lineation is distributed extensively on the surface of the schistosity, and the structural kinetic metamorphism schist is formed. The magnetic susceptibility anisotropic medium of the kinetic deformation metamorphism is P or = 1.10 (above). The magnetism foliation is well developed, and the highest value of F reaches 1.23. The flash ratio of the magnetic susceptibility ellipsoid is E1, and the shape factor of the magnetic ellipsoid is T0. According to the anglicizing results by X-ray from a group of rocks, the orientation is occured clearly in the structural rocks, chlorite and sericite. Comparing to the other regions, the Qugetage ductility deformation belts belong to the giant ductility belt of upper-middle Tainshan Quogemintashi-Huangshan, and in the part of the northern marginal transit belt. It has very similar condition and environment of mineralization to nearby Xiaorequanzi and Tuwu Cu-deposits." @default.
- W2354135323 created "2016-06-24" @default.
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- W2354135323 date "2004-01-01" @default.
- W2354135323 modified "2023-09-24" @default.
- W2354135323 title "IDENTIFICATION AND UNDERSTANDING OF DUCTILITY DEFORMATION BELTS IN QUEGETAGEDI REGION, EAST TIANSHAN" @default.
- W2354135323 hasPublicationYear "2004" @default.
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