正断型隐伏生长断层上断点埋深的研究——以银川隐伏断层钻孔联合剖面为例
详细信息 本馆镜像全文    |  推荐本文 | | 获取馆网全文
摘要
断层上断点埋深是隐伏活动断层地震危险性评价中的一个重要参数。在隐伏断层活动性研究中,钻孔探测是重要的探测手段之一(徐锡伟,2002),但由于标志地层发育的局限和钻探分辨能力的局限,识别的断层上断点埋深往往会大于实际埋深。为了减小这种误差,本文以银川隐伏生长断层探测钻孔联合地质剖面资料为基础,提出了一种生长指数法,用以推算隐伏生长断层的上断点埋深。得出的3个钻探场点的断层“理论上断点”埋深分别为:9.09m(新渠稍场点),7.86m(满春场点)和7.25m(板桥场点),小于钻探可识别的上断点埋深。经验证,这应更接近于断层的实际断错情况。
Buried depth of fault up-breakpoint is a important parameter in earthquake risk estimate of buried active fault. In study of the buried fault activity, drilling is one of the important exploration means, but as a result of localization of the marker horizon developed and drilling own resolving power, the depth of up-breakpoint which drilling can identify always deeper than the actual depth of fault up-breakpoint. In order to minish the error, based on the drill exploration composite geological section data in Yinchuan buried growth fault, put forward a sort of growth index means, to reckon depth of up-breakpoint of buried growth fault. From the account we gained the “academic up-breakpoint” depth of the 3 proving grounds in Yinchuan buried fault, the result is as follows: The academic up-breakpoint depth of Xingqushao proving grounds is 9.09m, in Manchun proving grounds, the academic up-breakpoint depth is 7.86m, in Banqiao proving grounds, the academic up-breakpoint depth is 7.25m. All of the results less than depth of the fault up-breakpoint that drilling can identify. By validate, much more close to actual broken complexion of the fault.
引文
柴炽章、孟广魁、杜鹏等,2006,隐伏活动断层的多层次综合探测———以银川隐伏活动断层为例,地震地质,28(4),536~546。
    邓起东,2002,城市活动断裂探测和地震危险性评价问题,地震地质,24(4),601~605。
    邓起东、徐锡伟、张先康等,2003,城市活动断裂探测的方法和技术,地学前缘,10(1),93~104。
    徐锡伟、朱金芳、吴建春等,2002,福州市活断层探测设计,北京:地震出版社。
    Thorsen,C.E.,1963,Age of growthfaultingin southeast Louisana,Trans,Gulf-Coast Ass.Geol.socs,13,103~110.

版权所有:© 2023 中国地质图书馆 中国地质调查局地学文献中心