The space distribution characteristics of structures from topography and landform of the south part of Ordos block and Weihe basin are analyzed.It is considered that three dimensional cross structures are formed by three NW upwarpings of the south part of Ordos block and EW subsidence centers which range obliquely as well as cross uplifts among them in Weihe basin.The space distribution of historical and modern earthquakes in and surrounding the Weihe basin shows that three dimensional cross structures have a strong dominion on seismicity in the basin.
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冯希杰,王平.立交构造与渭河盆地地震活动[J].地震工程学报,2001,23(2):160-163. FENG Xi-jie, WANG Ping. THREE DIMENSIONAL CROSS STRUCTURE AND SEISMICITY OF WEIHE BASIN[J]. China Earthquake Engineering Journal,2001,23(2):160-163.