Huanushan - Wufenshan and Huangjianqiu -Xinchang formed positive strike -slip up-warping region, middle belt shown negative down warping, developed Daqishan pull -apart basin.
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。
Based on the negative flower shaped structure and its relative structural movement track in Fangzheng area, this paper suggests that Fangzheng rift is a rifted basin formed by strike slip pull apart.
本文通过对方正地区所发现的负花状构造及其有关构造运动形迹分析的基础上，进一步提出方正断陷是走滑—拉分形成的断陷盆地。
Based on the negative flower shaped structure and its relative structural movement track in Fangzheng area, this paper suggests that Fangzheng rift is a rifted basin formed by strike slip pull apart.
本文通过对方正地区所发现的负花状构造及其有关构造运动形迹分析的基础上，进一步提出方正断陷是走滑—拉分形成的断陷盆地。
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