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- W2347808518 abstract "Studying on micro-disseminated gold deposits structure in the west in Pingle downwarping region,surveying in the field and analyzing the correlative data,the author found the existence of a stretching structure system,which formed by the metamorphic core complex,the solid-state rheological structure community,the superficial bedding sliding and decoupling normal fault,the late gravity slip structure system.Around the metamorphic core complex is a ductile shear zone composed by many orbicular tilted outside granite mylonite zone,the mineral lineation shows that the ductile shearing proceeded along the two ridged wings near north-south.The most outstanding performance of bedding solid rheological community is near horizontal ductile shear zone in the shallow metamorphic rock.The superficial normal bedding sliding and decoupling fault slide mostly along the existing interface or the limp stratum from north to south,and is divided into three structure belts by hinder spreading,middle sliding forward gradually and front extrusion.Late slip gravity system,which is made of many sliders,formed mainly at the northern foot in the Wugong Mountain.Isotope age of metamorphic core complex from Orleans University in France shows that the structure developed during late Variscan to Indo-Sinian,the involved stratum indicates that finished at end of the Himalayan or Yanshan period." @default.
- W2347808518 created "2016-06-24" @default.
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- W2347808518 date "2009-01-01" @default.
- W2347808518 modified "2023-09-25" @default.
- W2347808518 title "Analysis on Extensional Tectonics System in the West of Pingle Downwarping Region" @default.
- W2347808518 hasPublicationYear "2009" @default.
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