多种重磁位场边缘识别方法及在南黄海北部断裂构造识别中的应用研究
许文强1,2(
), 袁炳强3, 刘必良4, 姚长利1,2
), 袁炳强3, 刘必良4, 姚长利1,2
Multiple gravity and magnetic potential field edge detection methods and their application to the boundary of fault structures in northern South Yellow Sea
Wen-Qiang XU1,2(), Bing-Qiang YUAN3, Bi-Liang LIU4, Chang-Li YAO1,2
), Bing-Qiang YUAN3, Bi-Liang LIU4, Chang-Li YAO1,2
图1. 南黄海及邻区大地构造位置[
①—郯-庐断裂; ②—五莲-青岛-荣成断裂; ③—千里岩断裂; ④—嘉山-响水断裂; ⑤—江山-绍兴断裂
Fig.1. Sketch map of the tectonic location of the northern basin of the South Yellow Sea and its adjacent areas[
①—Tancheng-Lujiang fault belt;②—Wulian-Qingdao-Rongcheng fault belt;③—Qianliyan fault belt;④—Jiashan-Xiangshui fault belt;⑤—Jiangshan-Shaoxing fault belt
