西安地裂缝构造成因机制及地震勘查思路探讨
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摘要
西安地裂缝所引起的地面沉降及对地面构造物的破坏在国内外尚属罕见,深入研究其成因机制,探索有效的勘查方法,对西安经济持续发展及地学研究具重要意义。浅层地震是探测西安地裂缝最有效的地球物理勘探方法之一,西安地区地震地质条件较好,但表层风积湿陷性黄土分布广泛,地下水位较深是地震勘查的难点。利用浅层高分辨地震查明的临潼-长安断裂和地裂缝深部构造发育特征,并结合区域地质条件对西安地裂缝构造成因机制及地震勘查思路进行探讨,资料可靠,值得参考。
In Xi′an city,the surface subsidence and building damage caused by ground fissure are rare at home and abroad.Deep study on their tectonic genesis mechanism and explore an effective method of surveying are important for regional economic sustainable development and geology study.The shallow seismic exploration is one of the most effective geophysical prospecting methods to Xi′an ground fissure.In Xi′an area,the seismic geologic conditions are fine,but widely distributed shallow aeolian collapsible loess and deep ground water level bring more difficulties for seismic exploration.Tectonic development features of Lintong-Changan fault and ground fissures in Xi′an are obtained by shallow high resolution seismic exploration,combined with regional geological condition,its genesis mechanism and thought of seismic exploration are also discussed.The reliable data is worth referring.
引文
1张家明,等.西安地裂缝研究.西安:西北大学出版社,1990
    2李永善,等.西安地裂及渭河盆地活断层研究.北京:地震出版社,1992
    3冯西杰,等.临潼-长安断裂错距及其分布特征.地震地质,2006,(4):579~588
    4苗康运,等.临潼-长安断裂构造发育特征——基于浅层地震探测结果分析.煤田地质与勘探,2008,(5)

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