地震地质

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利用地震反射剖面探测研究安丘-莒县断裂板泉段的浅部构造特征

秦晶晶1,刘保金1,王志才2,酆少英3,邓小娟1,花鑫升1,李倩1   

  1. 1. 中国地震局地球物理勘探中心
    2. 山东省地震局
    3.
  • 收稿日期:2021-03-23 修回日期:2021-06-14 发布日期:2021-09-26
  • 通讯作者: 秦晶晶
  • 基金资助:
    国家重点研发计划

Research on shallow structural characteristics in the Banquan segment of Anqiu-Juxian fault zone based on shallow seismic reflection profiling

  • Received:2021-03-23 Revised:2021-06-14 Published:2021-09-26

摘要: 安丘-莒县断裂是郯庐断裂带内活动性最强的一条断裂,也是1668年郯城81/2级地震的发震断裂。跨板泉盆地和安丘-莒县断裂完成的浅层反射地震剖面清晰地揭示了地层界面形态和断裂浅部特征。研究结果表明:板泉盆地是一个由多条断裂组成的第四纪晚期发育的断陷盆地,且第四纪地层厚度和堑状构造特征明显受到断裂F1和F2的影响和控制;盆地东、西两侧为基底隆起区,第四纪地层厚度小于30m;盆地内部沉积了较厚的新生代地层,呈现西浅东深的倾斜形态,与下伏基岩地层呈不整合接触。浅层地震反射剖面揭示的安丘-莒县断裂,是由2条相向而倾的分支断层组成,在剖面深部合并为1条断裂。安丘-莒县断裂在板泉段总体呈现走向NE、倾向W的正断层性质。从断裂的上断点埋深和第四纪活动特征来看,板泉盆地的西边界白芬子-浮来山断裂活动性相对较弱,为前第四纪断裂;其东边界昌邑-大店断裂和安丘-莒县断裂错断了基岩顶界面,且第四纪以来存在错断迹象,其活动时代均为晚更新世。研究结果可为进一步理解1668年郯城8.5级地震发震断层活动方式、活动时代以及郯庐断裂带板泉段的近地表特征及其活动性提供了地震学依据。

关键词: 郯庐断裂带, 板泉盆地, 安丘-莒县断裂, 昌邑-大店断裂, 断层活动性

Abstract: The Anqiu-Juxian fault is the latest active fault in TanLu fault zone, which is also the seismogenic fault of Tancheng M8.5 earthquake in 1668. The shallow seismic reflection profile,laid across the east branch of Anqiu-Juxian fault and the Banchan basin, clearly revealed the stratigraphic interface morphology and shallow fault characteristics. The results show that Banquan Basin, a graben basin developed in the late Quaternary, is composed of multiple faults, and the thickness of Quaternary strata and graben structure characteristics are obviously affected and controlled by faults F1 and F2.Also, the eastern and western sides of the basin are the basement uplift areas, and the Quaternary strata thickness is less than 30m.There are thick Cenozoic strata deposited in the basin, showing the inclined form of shallow west and deep east, which are in unconformity contact with underlying bedrock strata. The east branch of Anqiu-Juxian fault revealed by the shallow seismic reflection profile is composed of two branch faults dipping in opposite direction, which merge into one fault in the deep section. The Banquan section of Anqiu-Juxian fault generally shows a normal fault characteristics of striking NE and dipping W. According to the buried depth of the upper breakpoints of these fractures and the characteristics of the Quaternary activity, Baifenzi-Fulaishan fault on the western boundary of Banquan basin is relatively weak, which is the pre-Quaternary fault. Changyi-Dadian fault on the eastern boundary of Banquan basin and Anqiu-Juxian fault not only dissected the bedrock top interface, but also showed signs of dissecting since Quaternary, and its active age are the late Pleistocene. The research results can provide seismological evidence for further understanding of activity mode and activity age of the seismogenic fault of the 1668 Tancheng M8.5 earthquake, as well as the near-surface characteristics and activity of the Banquan segment of the Tanlu fault zone.

Key words: TanLu fault zone, Banquan basin, Anqiu-Juxian fault, Changyi-Dadian fault, Fault activity.