Abstract:Regarding Buyitanwulashan mountain in the northern margin of Quanji block in Qaidam basin as the research object, the matching of several unconformity boundaries developed in Buyitanwulashan area and regional tectonic geological events, and 3 tectonic styles, such as extrusion, strike slip and extension developed in norhtern Chaidamu basin have been studied. Through analysis on geological tectonic environment evolution of Buyitanwulashan area from Cenozoic to Proterozoic, combining with regional geological events and structural styles, it is thought that tectonic chatacteristics of Quanji block can be divided into basement, cover and faulted sedimentary in general.