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- W2350902599 abstract "The Dapinggou ductile-brittle deformation belt outcrops among the brown-red K-feldspar gneiss of the Late Archaeozoic Dagelabulake Group,being nearby the northern side of the northern Altun fault and about 50km far away from Xorkol part of the Altun strike-slip fault.The belt dips to Southern at a high-angle of 65～85°with an EW-trending.Each second-order ductile-brittle deformation belt trends EW to NWW trending wavy,with a hundreds meter length and tens meter width.There develops lineation and foliation in the belt and an obvious intragranular deformation of minerals,such as quartz and K-feldspar.Synkinematic recrystallized sericite well develops inner deformed rocks.The mechanical property of the belt is ductile-brittle shear-compressional deformation. There developed kinds of mylonite,specially,the K-feldspar porphyroid-bearing sericite quartz mylonite is common sight in the belt. Analysis of petro-fabrics shows that the quartz is mainly deformed along its basal or basal-near glide system,witch indicates that the deformation temperature is about 250～350℃.Finite strain measurement shows that the strain ellipsoid axis ratio(Rxz)is 2.9～4.8. The differential stress value is measured about 59～61 MPa and the sense of movement is right-lateral thrusting with a NNW-trending maximum compressive stress.Combining to the geotectonic evolution,the authors consider that the Dapinggou ductile-brittle deformation belt developed under the geotectonic setting of collision of plates in the early Paleozoic,indicated the deformation feature of basement rock under the collision process." @default.
- W2350902599 created "2016-06-24" @default.
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- W2350902599 date "2008-01-01" @default.
- W2350902599 modified "2023-09-25" @default.
- W2350902599 title "Study on the Dapinggou ductile-brittle deformation belt in northern Altum margin area,NW China." @default.
- W2350902599 hasPublicationYear "2008" @default.
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