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研究区位于雅布藏布江缝合带南侧,喜马拉雅地块北缘,以札达一拉孜一邛多江断裂为界,北部为浪卡子—曲松构造亚带(亦称北构造亚带),南部为康马—隆子构造亚带(亦称南构造亚带),地处喜马拉雅地块拉轨岗日被动陆缘盆地、洛扎断裂东南端。区内出露的地层主要有早侏罗世日当组、早-中侏罗世陆热组、中侏罗世遮拉组、晚侏罗世维美组以及早白垩世拉康组。第四纪地层出露较
The study area is located on the south side of the Yabuzangbu suture zone and on the northern margin of the Himalayas massif. It is bounded by the Zhada-Lazi-Jiujiang fault and the northern part of the Langka-Qunsong tectonic subtropical zone ), The southern Kangma - Long Tzu structural belt (also known as the South Tectonic Belt), located in the Himalayan block pull Kong Gang passive continental margin basin, South end of the Luoza fault. The strata exposed in the area mainly include Early Jurassic Dayang Formation, Early-Middle Jurassic Geothermal Formation, Middle Jurassic Shurel Formation, Late Jurassic Vimetix Formation and Early Cretaceous Lacan Formation. Quaternary strata exposed more