Based on drilling-wells and seismic data, it was proved that there are strike-slip tectonics in Santanghu basin in the following two basic forms: simplified strike-slip faults and positive flower strike-slip faults.
Based on drilling-wells and seismic data, it was proved that there are strike-slip tectonics in Santanghu basin in the following two basic forms: simplified strike-slip faults and positive flower strike-slip faults.
摘要通过对钻井岩心资料系统观察以及地震资料的全面检查，证实新疆三塘湖盆地内存在走滑构造，表现为简单走滑（逆－平移）断层和正花状走滑断层两种基本形式。