Sxotf is recognized in the northern qaidam based on the analysis of structures of area . this oblique trusting fault zone with northwestern - southeastern trending consists of fault gouge , fault breccia and fault cleavage . fault hanging wall consists of sertengshan - xitieshan napple , which is distribution in dextral en echelon . fault footwall consists of youcangshan formation in neogene 本文在對(duì)賽什騰? ?錫鐵山斜沖斷裂詳細(xì)地段構(gòu)造解析的基礎(chǔ)上,結(jié)合盆地的沉積特征、地球物理資料等對(duì)該斜沖斷裂的幾何學(xué)、運(yùn)動(dòng)學(xué)及形成時(shí)代進(jìn)行了研究,論文著重探討了賽什騰? ?錫鐵山斜沖斷裂的地質(zhì)意義。