京津冀协同发展区活动构造与地壳稳定性

    Activity structure and crustal stability in Beijing-Tianjin-Hebei collaborative development zone

    • 摘要: 京津冀协同发展区是中国东部规划的战略开发区之一,也是华北地区主要的活动构造区,新构造活动强烈,活动断裂发育,地震频发,具有潜在的地质安全隐患问题。基于张家口地区、雄安新区及邻区、北京及关键构造部位调查研究结果,结合已有研究成果,系统分析了京津冀协同发展区主要活动断裂几何学、运动学和动力学特征及其工程地质、地质灾害特征,采用ArcGIS平台的空间分析功能,初步完成了京津冀协同发展区地壳稳定性评价。研究结果表明,京津冀协同发展区发育邢台-河间-唐山、石家庄-通州NNE向构造带和张家口-渤海NWW向区域性活动构造带,其中全新世活动断裂11条,晚更新世活动断裂16条,第四纪断裂23条;冀北及冀东南地区现今构造应力场最大水平主应力方向为近EW向,而太行山东缘南段为NNE向,北段为NW向;NNE向活动断裂带总体表现为顺时针扭动正断活动,倾向SE,NWW向活动断裂带晚更新世以来具有明显的活动性,整体表现为反时针扭动正断活动,倾向SW。京津冀协同发展区地壳稳定性总体较好,不稳定区及次不稳定区主要分布在邢台、唐山、延怀盆地和全新世活动断裂带内,利于重要城镇和重大工程规划建设。研究成果将为京津冀协同发展区宏观发展战略提供地质支撑。

       

      Abstract: Beijing-Tianjin-Hebei Collaborative Development Zone(BTHCDZ)is one of the strategic development zones in eastern China, and is also the active tectonic region in North China.Based on its strong neotectonic activity, many active faults and frequent earthquakes, it is sure that there are potential geological safety hazards.Based on the results of the investigation and research on Zhangjiakou area, Xiong'an New Area and neighboring area, Beijing area and its key tectonic sites, and combined with the comprehensive analysis of the existing research results, the features of the geometry, kinematics and dynamics of the main active fracture and as well as the engineering geology and geohazards are systematicly analyzed in the BTHCDZ.And then the assessment of crustal stability based on the spatial analysis function of ArcGIS platform in the BTHCDZ has been completed.The results show that: There are Xingtai-Hejian-Tangshan and Shijiazhuang-Tongzhou two NNE-trending, and Zhangjiakou-Bohai one NWW-trending activity tectonic belts existed in the BTHCDZ, and within the three belts, there are 11 Holocene fractures, 16 Late Pleistocene fractures and 23 major Quaternary fractures; The direction of the maximum horizontal principal stress of present tectonic stress field in the north and southeast regions of Hebei Province is near EW, while the southern section of the east edge of Taihangshan is NNE direction and the northern section is NW direction; The overall performance of NNE active fault belt is clockwise normal activity with SE tendency, while NWW active fault belt has obvious activity from Late Pleistocene, and the overall performance is anti-clockwise normal activity with SW tendency; The general crustal stability of the BTHCDZ is general good for the planning and construction of important towns and major projects, and the unstable zones and sub-unstable areas are mainly distributed in Xingtai, Tangshan, Yanhuai Basin and the Holocene active fault zone.The research results will provide geological support for the macro-development strategy of the BTHCDZ.

       

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