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- W2349567992 abstract "As carring out the regional geological survey at the scale of 1∶50 000 in Jinggang Mountains the authors found the nappe structure. The nappe structure is mainly composed of a series of the NNE NE thrust fault zones and the thrust sheets. The strata of the Sinian, Cambrian, Ordovician, Devonian, Carboniferous, Triassic, Jurassic and Cretaceous are all involved in the thrust nappe system. The nappe structure is double thrust structures that are formed as a result of the sedimentary covering or basement strata partly migrating from southeast to northwest early and from east to west later. The formation of the nappe structure in the studied area is involved mainly in the two epochs: early Yanshanian epoch and later Yanshanian epoch early Himalayan epoch. The mineral deposits and coal fields are extensively controlled by the nappe structure in the area, especially the buried coal fields." @default.
- W2349567992 created "2016-06-24" @default.
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- W2349567992 date "2003-01-01" @default.
- W2349567992 modified "2023-09-25" @default.
- W2349567992 title "CHARACTERISTICS OF THE THRUST NAPPE STRUCTRUE IN JINGGANG MOUNTAINS AND ITS MEANING FOR ORE PROSPECTING" @default.
- W2349567992 hasPublicationYear "2003" @default.
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