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- W2352974836 abstract "The Baidunzi-Xiaoxigong ductile shear zone,as the southernmost one of the eight ductile shear zones in the Beishan area,Gansu,is situated at the southern border of the southern Beishan area and near the northern border of the Dunhuang massif.It extents in a nearly E-W direction with a length of 160 km and a width of 5—8 km.This shear zone is characterized by subhorizontal dextral shear and formed under the conditions of low-middle to middle-slightly high temperatures and relatively low differential structural stresses(53—106 MPa).The principal strain(Rxz) is 4—20,the shear strain(γ) is 1.41—2.42 and the shear displacement is up to 10—25 km.The ductile shear zone has a marked controlling effect on gold deposits:it controls the distribution of gold deposits(occurrences) on a regional scale and the shape,attitude and size of gold mineralization zones and orebodies on a deposit scale.The features of transpressional ductile deformation determine that gold mineralization is mainly of altered mylonite type and that alteration is featured by metasomatism.Gold mineralization occurred a little later than ductile shear deformation." @default.
- W2352974836 created "2016-06-24" @default.
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- W2352974836 date "2007-01-01" @default.
- W2352974836 modified "2023-09-25" @default.
- W2352974836 title "BAIDUNZI-XIAOXUGONG DUCTILE SHEAR ZONE AND ITS ORE-CONTROLLING EFFECT IN THE SOUTHERN BEISHAN AREA,GANSU" @default.
- W2352974836 hasPublicationYear "2007" @default.
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