The clastic rocks widespread in the Triassic Xikang Group in western Sichuan consist dominantly of turbiditic flysch for摘要三叠系西康群碎屑岩主体为一套浊积岩复理石建造。
MIDDLE JURASSIC TO EARLY CRETACEOUS FLYSCH TRACE FOSSILS FROM NGARI REGION, TIBET西藏阿里(狮泉河—多玛)地区中侏罗—早白垩世复理石相遗迹化石