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- W2352789558 abstract "Fractural structures develop well in the Baozhadundaban-Jingbulake area of Xinjiang. Large-scale Fractural structures more than 20 totallly had long-time worked, which are characterized by polyphase deformation evolution. Territorial faults are not only the boundaries of ancient sedimentary basins, but also the boundaries of different mineralization zones, controlling the forming-ore spaces, movement of mineralization elements and distribution of ore-deposits. Geochemical anomalies show that the positions of structures intersection in different directions are beneficial zones for various elements enrichment, and at the same time territorial faults show the characteristics with controlling ore-formation. The ductile shear zones widely distributed as controlling factors of large and super large deposits, restrict geologies and metallogenic conditions of the ductile shear zones type gold deposits, and show chronotaxy obviously. The ductile shear zones are the beneficial zones to search for Muruntau-type gold deposits." @default.
- W2352789558 created "2016-06-24" @default.
- W2352789558 creator A5068932131 @default.
- W2352789558 date "2008-01-01" @default.
- W2352789558 modified "2023-09-23" @default.
- W2352789558 title "RESEARCH OF STRUCTURAL GEOLOGICAL FEATURE AND ITS CONTROLLING MECHANISM OF BAOZHADUNBUDABAN- JINGBULAKE AREA IN XINJIANG" @default.
- W2352789558 hasPublicationYear "2008" @default.
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