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- W2362239782 abstract "Linhe-Jining faulted zone in the Daqingshan area,Inner Mongolia,is an important faulted zone in the north margin of North China craton.The faulted zone consists mainly of ductile shear belt,ductile-brittle shear belt and nappe structures.The nappe structures in the area are formed in the late Cretaceous and may be divided into 4 deformable zones,namely,imbricated thrust nappe structure zone,closed folded-thrust faulted deformable zone,wide-gentle folded-faulted turned folded zone and decollement folded-faulted spreaded folded zone.The deformation of the faulted zones changes from ductile shear to brittle shear,indicating the different formation depths of the faulted zones.The intensity of the fault motions is gradually weakened from south to north.In the area there are distributed metallic deposits mainly of gold-polymetallic and nonmetallic deposits dominately of coal and marble.The gold-polymetallic deposits are mostly related with the ductile shear zone,the faulted structures were the channels for the ore-forming materials and provided the speces for the formation of metallic deposits.The research results also pointed out the perspect and direction of ore-prospecting in the area." @default.
- W2362239782 created "2016-06-24" @default.
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- W2362239782 date "2008-01-01" @default.
- W2362239782 modified "2023-09-23" @default.
- W2362239782 title "Tectonics and mineralization in Daqingshan region,Inner Mongolia" @default.
- W2362239782 hasPublicationYear "2008" @default.
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