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- W2385756357 abstract "Through the comprehensive study on the exploration data of the deposits in the northern part of Xiangshan uranium ore field,the overthrust structure is recognized deeply.The overthrust structure strikes EW on the whole and the direction of movement is from south to north.The main detachment surface occurred between Sinian(Z) metamorphic rocks and Jurassic(J3d1)layers.Sinian metamorphic basement is overthrust on the top of Lower Daguding member of Upper Jurassic Group.The nappe system consists of front faults,backthrust fault,the main detachment zone(main structure),and nappe structural window.The nappe had moved 3～4.5 km and it mainly formed during Late Jurassic,i.e.Late Yanshan." @default.
- W2385756357 created "2016-06-24" @default.
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- W2385756357 date "2011-01-01" @default.
- W2385756357 modified "2023-09-25" @default.
- W2385756357 title "The overthrust structural systems and their dynamics in Xiangshan uranium ore field in central Jiangxi Province" @default.
- W2385756357 hasPublicationYear "2011" @default.
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