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辽宁东部寒岭—偏岭断裂带深部地质特征
引用本文:姜岩,薛林福,祝铭,刘文玉.辽宁东部寒岭—偏岭断裂带深部地质特征[J].世界地质,2016,35(2):495-502.
作者姓名:姜岩  薛林福  祝铭  刘文玉
作者单位:吉林大学 地球科学学院,长春 130061
摘    要:通过对4条高精度重力、高精度磁测和MT实测非震地球物理综合剖面的处理解释,结合已有区域地球物理及野外地质研究,对辽宁东部寒岭—偏岭断裂带的特征进行了研究。根据航磁异常上延结果,认为该断裂为左旋走滑断裂,其最大错断距离约53 km。布格重力异常上延结果表明,与寒岭—偏岭断裂带相关的次级断裂切割深度小,主要发育在沉积盖层中。四条非震综合物探剖面处理解释结果表明,寒岭—偏岭断裂带在不同地段的深部地质产状不同,断裂带西段深部倾向为N,视倾角约为65°;断裂带中段深部倾向NW,视倾角约为60°;断裂带北段深部倾向NW或SE,具有摆动特征,视倾角变化较大,约为35°~50°。

关 键 词:寒岭—偏岭断裂带  深部地质特征  非震地球物理剖面  辽宁东部

Deep geological features of Hanling- - Pianling fault zone in eastern Liaoning
JIANG Yan,XUE Lin-Fu,ZHU Ming,LIU Wen-Yu.Deep geological features of Hanling- - Pianling fault zone in eastern Liaoning[J].World Geology,2016,35(2):495-502.
Authors:JIANG Yan  XUE Lin-Fu  ZHU Ming  LIU Wen-Yu
Institution:College of Earth Sciences,Jilin University,Changchun 130061,China
Abstract:On the basis of the comprehensive interpretation of four high- precision gravity,high- precision mag- netic and MT measured non- seismic geophysical profiles,combining with the regional geological data and field geo- logical research,the authors studied the features for the deep Hanling- - Pianling fault zone in eastern Liaoning. Ac- cording to the result of aeromagnetic anomalies upward continuation,it is considered that the fault zone is a sinistral strike- slip fault,and its biggest leap distance is about 53 km. According to Bouguer gravity anomalies upward con- tinuation,there is a shallower cutting depth with Hanling- - Pianling fault zone. It mostly developed in the sedimenta- ry cover. The processing and interpretation results of four integrated geophysical profiles show that the occurrences of Hanling - - Pianling fault are various in different locations,the deep tendency of the western fault is N,the appar- ent dip is about 65°; while the deep fault in the middle tends to NW, its apparent dip is about 60°; the north of the deep fault tends to NW and SE,and the change of apparent dip is large about 35° ~50° according to its swing fea- ture.
Keywords:Hanling-Pianling fault zone  deep geological feature  non- seismic geophysical profile  eastern Liaoning
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