花牛山—五峰山和黄尖丘—新场两地区形成正性的走滑隆升区，其相应中间地带则显示了负性拉分拗陷作用，发育了大奇山拉分盆地。
Huanushan - Wufenshan and Huangjianqiu -Xinchang formed positive strike -slip up-warping region, middle belt shown negative down warping, developed Daqishan pull -apart basin.
震中拗陷与地震形变带提供了震源区大小的信息。
Epicentral depositions and earthquake deformation zones provide useful information about focal region size.
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