鄂尔多斯地块北缘动力背景和现今地震活动特征
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摘要
鄂尔多斯地块的动力背景是青藏高原东北缘NE向推挤作用的结果。1970年以来,鄂尔多斯地块北缘现今地震活动表明,中强地震活动具有幕式活动特征,从1970~2015年共经历了4幕活动;块体西北缘与东北缘的中强地震具有迁移对跳活动特征,1970年以来共经历了4组对跳;震例统计结果揭示,地块北缘6.0级左右地震前,块体中等地震经历长时间平静具有普适特征;2005-03以来,块体所在的阴山地震带再次进入中等地震超长平静时段。其幕式活动特征、迁移特征、时间平静特征可作为区域范围强震的预测指标。
The research results show that dynamic background of the Ordos block is the Tibetan plateau compression from an East-West direction.The seismic activity of the Ordos block northern margin since 1970 shows that the moderate seismicity is characterized by episodic activities;moderate earthquakes of Ordos block experienced 4 curtains from 1970 to 2015,strong earthquakes of the northwestern and northeastern margins of the Ordos block has migrating characteristics,a total of 4 curtains since 1970,(before the magnitude 6 earthquake in the northern margin of the block).The moderate earthquake of the entire block has been quiet a long time according to the statistical results of earthquake examples,while moderate seismic is in a long quiet stage in Yinshan seismic zone since March 2005.The curtain activity and migrating characteristics,as well as the time calm characteristics,can be used as a prediction index for strong earthquakes in the region.
The research results show that dynamic background of the Ordos block is the Tibetan plateau compression from an East-West direction.The seismic activity of the Ordos block northern margin since 1970 shows that the moderate seismicity is characterized by episodic activities;moderate earthquakes of Ordos block experienced 4 curtains from 1970 to 2015,strong earthquakes of the northwestern and northeastern margins of the Ordos block has migrating characteristics,a total of 4 curtains since 1970,(before the magnitude 6 earthquake in the northern margin of the block).The moderate earthquake of the entire block has been quiet a long time according to the statistical results of earthquake examples,while moderate seismic is in a long quiet stage in Yinshan seismic zone since March 2005.The curtain activity and migrating characteristics,as well as the time calm characteristics,can be used as a prediction index for strong earthquakes in the region.
引文
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[14]邓启东,程绍平,闵伟,等.鄂尔多斯地块新生代构造活动和动力学的讨论[J].地质力学学报,1999,5(3):13-20(Deng Qidong,Cheng Shaoping,Min Wei,et al.Discussion on the Cenozoic Tectonic Activities and Dynamics of the Ordos Block[J].Journal of Geomechanics,1999,5(3):13-20)
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[17]陈小斌,臧绍先,魏荣强.稳定的鄂尔多斯地块在整体运动吗?[J].地球物理学报,2011,54(7):1 750-1 757(Chen Xiaobin,Zang Shaoxian,Wei Rongqiang.Is the Stable Ordos Block Migrating as an Entire Block?[J].Chinese J Geophys,2011,54(7):1 750-1 757)
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[19]盛书中,万永革,黄骥超,等.应用综合震源机制解法推断鄂尔多斯地块周缘现今地壳应力场的初步结果[J].地球物理学报,2015,58(2):436-452(Sheng Shuzhong,Wan Yongge,Huang Jichao,et al.Present Tectonic Stress Field in the Circum-Ordos Region Deduced from Composite Focal Mechanism Method[J].Chinese J Geophys,2015,58(2):436-452)
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