渭河盆地线性体自动提取与风险评估

    • 摘要: 渭河盆地位于鄂尔多斯地块和秦岭造山带之间,是构造运动活跃地带,其内部发育有众多大型活动断裂,也是地震活动高发区。本研究基于边缘检测的线性体自动提取算法,利用ALOS PALSAR DEM数据获取渭河盆地线性体空间分布;将线性体提取结果与研究区地震分布、地质特征进行相关性分析,采用加权信息量分析法建立模型,量化评估渭河盆地发生地震的风险性及区域差异性。得到如下结论:⑴利用12.5米高精度DEM数据提取线性体,能够屏蔽人工线性形迹的影响,较好的反映地表构造分布;⑵研究区地震与线性体的空间分布具有明显相关性,表明该区地震主要受活动断裂控制;⑶结合渭河盆地地质、地球物理数据进行地震风险评估,获得了该区地震风险空间分布特征,可为后续防灾减灾提供参考。

       

      Abstract: The Weihe Basin, located between the Ordos Block and the Qinling Orogenic Belt, is an active zone of tectonic movement with numerous large active lineaments and is also a region of frequent seismic activity. In this study, an automate extraction method based on edge detection algorithm was applied to extract the lineaments of the Weihe Basin using ALOS PALSAR DEM data. We conduct a correlation analysis between the results of lineaments and the seismic distribution, as well as geological features in the study area. Based on existing data, a model using the weighted information entropy analysis method was established to assess the seismic risk and regional variations in the Weihe Basin. The following conclusions were drawn: ⑴ The lineament extracted using DEM data with a resolution of 12.5 meters can effectively eliminate the influence of artificial linear traces and well reflect the distribution of surface structures. ⑵ The spatial distribution of earthquakes and lineaments in the study area exhibits a strong correlation, indicating that seismic activity in this region is primarily controlled by active faults. ⑶ Seismic risk assessment was conducted by the integration of geological and geophysical data in the Weihe Basin, the spatial distribution characteristics of seismic risk in the area were obtained, providing a reference for subsequent disaster prevention and mitigation.

       

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