徐州废黄河断裂带的空间展布与活动性研究
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摘要
文中利用遥感影像分析了徐州废黄河断裂带的空间展布及与邵楼断裂的交切关系,利用重磁资料研究了废黄河断裂带的深部几何结构及与郯庐断裂带西边界的交切关系。二阶布格重力异常小波变换细节图反映出徐州废黄河断裂带的深度为7～8km,而三阶和四阶重力异常细节图反映的深度分别为9～11km和15～18km。研究结果表明,废黄河断裂带向SE延伸至九顶附近,向下的切割深度约为8～9km。NW向的废黄河断裂带截切邵楼断裂致使邵楼断裂构造线自东北向西南由N60°E转至N45°E。废黄河断裂带与郯庐断裂带不相交。废黄河断裂带属于前第四纪断裂,活动性较弱。
Based on the remote sensing images interpretation,the spatial distribution of the Fei Huanghe(the ancient Yellow River)fault zone in Xuzhou area was studied and the intersection relationships between Fei Huanghe Fault and Shaolou Fault,and Tan-lu Fault were discussed in the paper.Besides,we researched the deep-seated geometric structure of Fei Huanghe Fault by studying the gravity-magnetic data,and discussed the intersection relationships with the west boundary of Tan-lu Fault.The cutting depth of Fei Huanghe Fault reflected by second order-wavelet transform detail of the Bouguer gravity anomalies is up to 7～8km.The depth reflected by the third order-wavelet and fourth order-wavelet transform detail of the Bouguer gravity anomalies is up to 9～11km and 15～18km,respectively.The results show that the Fei Huanghe Fault extends to Jiuding in southeast direction.The cutting depth is up to 8～9km.The NW-trending Fei Huanghe Fault cut the NE-trending Shaolou Fault,resulting in the change of the tectonic line of the latter from striking N 60°E to N 45°E.Moreover,the Fei Huanghe Fault didn't cut the Tanlu Fault.It is a pre-Quaternary Fault with weak activity.
Based on the remote sensing images interpretation,the spatial distribution of the Fei Huanghe(the ancient Yellow River)fault zone in Xuzhou area was studied and the intersection relationships between Fei Huanghe Fault and Shaolou Fault,and Tan-lu Fault were discussed in the paper.Besides,we researched the deep-seated geometric structure of Fei Huanghe Fault by studying the gravity-magnetic data,and discussed the intersection relationships with the west boundary of Tan-lu Fault.The cutting depth of Fei Huanghe Fault reflected by second order-wavelet transform detail of the Bouguer gravity anomalies is up to 7～8km.The depth reflected by the third order-wavelet and fourth order-wavelet transform detail of the Bouguer gravity anomalies is up to 9～11km and 15～18km,respectively.The results show that the Fei Huanghe Fault extends to Jiuding in southeast direction.The cutting depth is up to 8～9km.The NW-trending Fei Huanghe Fault cut the NE-trending Shaolou Fault,resulting in the change of the tectonic line of the latter from striking N 60°E to N 45°E.Moreover,the Fei Huanghe Fault didn't cut the Tanlu Fault.It is a pre-Quaternary Fault with weak activity.
引文
①江苏省地质局第五地质大队,1985,江苏省徐州南部基岩地质图。
国家地震局震害防御司.1995.中国历史强震目录[M].北京:地震出版社.Department of Earthquake Disaster Prevention,SSB.1995.Catalogue of Chinese Historical Strong Earthquake[M].Seismological Press,Beijing(in Chinese).
洪顺英,张红英,申旭辉,等.2007.南京市活断层卫星遥感图像的研究[J].遥感应用,4:46—50.HONG Shun-ying,ZHANG Hong-ying,SHEN Xu-hui,et al.2007.The research on remote sensing images of active faultsin Nanjing[J].Remote Sensing Information,4:46—50(in Chinese).
贾晓娟,韩宝平.1996.北西向断裂对徐州市岩溶水的控制作用[J].徐煤科技,1(4):25—26.JIA Xiao-juan,HAN Bao-ping.1996.A study on the controlling effect of NW-trending active fault zone on karst water ofXuzhou area[J].Xuzhou Coal and Technology,1(4):25—26(in Chinese).
姜文亮,张景发,龚丽霞.2007.海南岛北部地区活动断裂的遥感解译研究[J].地震地质,29(4):796—804.JIANG Wen-liang,ZHANG Jing-fa,GONG Li-xia.2007.Interpretation of multi-source remote sensing images of activefault in the north of Hainan Island[J].Seismology and Geology,29(4):796—804(in Chinese).
江苏省地质局区域地质调查队.1978.1:20万徐州幅区域地质调查报告[M].北京:地质出版社.178,709.Regional Geological Survey Team of Jiangsu Province.1978.Report of Regional Geological Survey of Xuzhou Sheet atthe Scale of1/200,000[M].Geological Publishing House,Beijing.178,709(in Chinese).
江苏省地质矿产局.1984.江苏省及上海市区域地质志[M].北京:地质出版社.652.Administration of Geology&Mineral Resources of Jiangsu Province.1984.Regional Geological Records of Jiangsu Prov-ince and Shanghai Municipality[M].Geological Publishing House,Beijing.652(in Chinese).
李成立,谢春临,吕庆田.1998.利用位场功率谱计算地质体顶底深度效果[J].大庆石油地质与开发,17(5):45—54.LI Cheng-li,XIE Chun-lin,LQing-tian.1998.Calculating top and bottom depth effect of geological body by applyingpotential field power spectrum[J].Petroleum Geology&Oilfield Development in Daqing,17(5):45—54(inChinese).
刘建光.1992.徐州地区冲断褶皱带研究[J].煤田地质与勘探,20(3):12—19.LIU Jian-guang.1992.A preliminary study on the thrust and fold belt of the Xuzhou region[J].Coal Geology and Ex-ploration,20(3):12—19(in Chinese).
刘建华,宣晓伟,李兰生.1992.地震预报与徐州市的地震工作设想[J].地震学刊,1(3):61—66.LIU Jian-hua,XUAN Xiao-wei,LI Lan-sheng.1992.Expectation of earthquake prediction and earthquake work ofXuzhou city[J].Journal of Seismology,1(3):61—66(in Chinese).
马公伟.1991.徐宿地区大型深层滑脱构造的讨论[J].江苏地质,1(1):28—31.MA Gong-wei.1991.Prediction of large deep decollement structure in Xuzhou-Suzhou area[J].Jiangsu Geology,1(1):28—31(in Chinese).
施纬,张岳桥,董树文.2003.郯庐断裂带中段第四纪活动及其分段特征[J].地球学报,24(1):11—18.SHI Wei,ZHANG Yue-qiao,DONG Shu-wen.2003.Quaternary activity and segmentation behavior of the middle portionof the Tan-Lu Fault zone[J].Acta Geologica Sinica,24(1):11—18(in Chinese).
舒良树,吴俊奇,刘道忠.1994.徐宿地区推覆构造[J].南京大学学报,30(4):638—647.SHU Liang-shu,WU Jun-qi,LIU Dao-zhong.1994.Thrust tectonics of Xuzhou-Suzhou region,eastern China[J].Jour-nal of Nanjing University,30(4):638—647(in Chinese).
宋文荣.1999.宿迁城北构造地貌特征及其成因分析[J].地震学刊,1(2):45—50.SONG Wen-rong.1999.Structural geomorphological characteristics and genesis analysis of north part in Suqian city[J].Journal of Seismology,1(2):45—50(in Chinese).
眭素文,于长春,熊盛青,等.2007.功率谱可视化深度计算方法及在煤火区的应用[J].物探与化探,31(6):560—563.SUI Su-wen,YU Chang-chun,XIONG Sheng-qing,et al.2007.A visualized depth estimating method by power spectrumand its application to a coal fire area[J].Geophysical&Geo-chemical Exploration,31(6):560—563(in Chi-nese).
王桂梁,姜波,曹代勇,等.1998.徐州—宿州弧形双冲-叠瓦扇逆冲断层系统[J].地质学报,72(3):228—236.WANG Gui-liang,JIANG Bo,CAO Dai-yong,et al.1998.On the Xuzhou-Suzhou arcuate duplex-imbricate fan thrustsystem[J].Acta Geologica Sinica,72(3):228—236(in Chinese).
谢瑞征,朱书俊,丁政.1991.郯庐断裂带江苏段全新世活动问题的商榷[J].地震学刊,1(4):15—18.XIE Rui-zheng,ZHU Shu-jun,DING Zheng.1991.Research on recent activity along Jiangsu segment of Tanlu Faultzone[J].Journal of Seismology,1(4):15—18(in Chinese).
熊盛青,周付洪,姚正煦,等.2001.青藏高原中西部航磁调查[M].北京:地质出版社.51—162.XIONG Sheng-qing,ZHOU Fu-hong,YAO Zheng-xu,et al.2001.Aeromagnetic Investigation of the Middle Western Ar-eas of the Qinghai-Xizang Plateau[M].Geological Publishing House,Beijing.51—162(in Chinese).
徐智敏,孙亚军,刘沂轩.2006.徐州废黄河断裂带对区内岩溶地面塌陷控制作用研究[J].能源技术与管理,1(3):54—55.XU Zhi-min,SUN Ya-jun,LIU Yi-xuan.2006.A study on Fei Huanghe(ancient Yellow River)fault zone dominatingkarst collapse of Xuzhou area[J].Energy Technology and Management,1(3):54—55(in Chinese).
姚大全,刘家灿,李杰,等.2003.新沂—泗县地震危险区地震活动和地震构造[J].华北地震科学,21(2):23—28.YAO Da-quan,LIU Jia-can,LI Jie,et al.2003.Seismic activity and structure in Xinyi-Sixian seismic risk region[J].North China Earthquake Sciences,21(2):23—28(in Chinese).
杨明慧,王嗣敏,郑晓凤,等.2009.华北克拉通南部及邻区航磁异常特征与构造分区[J].地质评论,55(6):862—872.YANG Ming-hui,WANG Si-min,ZHENG Xiao-feng,et al.2009.Aeromagnetic anomalies characteristics and tectonic subareasof southern North China Craton and adjacent regions[J].Geological Review,55(6):862—872(in Chinese).
张景发,陶夏新,田云峰,等.2004.城市周边活断层探测中遥感技术的应用[J].自然灾害学报,13(1):137—145.ZHANG Jing-fa,TAO Xia-xin,TIAN Yun-feng,et al.2004.Application of remote sensing technique to exploration of ac-tive fault around urban areas[J].Journal of Natural Disasters,13(1):137—145(in Chinese).
张鹏,王良书,钟锴,等.2007.郯庐断裂带的分段性研究[J].地质评论,53(5):586—591.ZHANG Peng,WANG Liang-shu,ZHONG Kai,et al.2007.Research on the segmentation of Tancheng-Lujiang Faultzone[J].Geological Review,53(5):586—591(in Chinese).
张微,陈汉林,李启敏,等.2007.高分辨遥感在杭州活断层探测中的应用[J].煤田地质与勘探,35(3):10—14.ZHANG Wei,CHEN Han-lin,LI Qi-min,et al.2007.Application of high resolution remote sensing technique to exploration ofactive fault of Hangzhou and its surroundings[J].Coal Geology&Exploration,35(3):10—14(in Chinese).
国家地震局震害防御司.1995.中国历史强震目录[M].北京:地震出版社.Department of Earthquake Disaster Prevention,SSB.1995.Catalogue of Chinese Historical Strong Earthquake[M].Seismological Press,Beijing(in Chinese).
洪顺英,张红英,申旭辉,等.2007.南京市活断层卫星遥感图像的研究[J].遥感应用,4:46—50.HONG Shun-ying,ZHANG Hong-ying,SHEN Xu-hui,et al.2007.The research on remote sensing images of active faultsin Nanjing[J].Remote Sensing Information,4:46—50(in Chinese).
贾晓娟,韩宝平.1996.北西向断裂对徐州市岩溶水的控制作用[J].徐煤科技,1(4):25—26.JIA Xiao-juan,HAN Bao-ping.1996.A study on the controlling effect of NW-trending active fault zone on karst water ofXuzhou area[J].Xuzhou Coal and Technology,1(4):25—26(in Chinese).
姜文亮,张景发,龚丽霞.2007.海南岛北部地区活动断裂的遥感解译研究[J].地震地质,29(4):796—804.JIANG Wen-liang,ZHANG Jing-fa,GONG Li-xia.2007.Interpretation of multi-source remote sensing images of activefault in the north of Hainan Island[J].Seismology and Geology,29(4):796—804(in Chinese).
江苏省地质局区域地质调查队.1978.1:20万徐州幅区域地质调查报告[M].北京:地质出版社.178,709.Regional Geological Survey Team of Jiangsu Province.1978.Report of Regional Geological Survey of Xuzhou Sheet atthe Scale of1/200,000[M].Geological Publishing House,Beijing.178,709(in Chinese).
江苏省地质矿产局.1984.江苏省及上海市区域地质志[M].北京:地质出版社.652.Administration of Geology&Mineral Resources of Jiangsu Province.1984.Regional Geological Records of Jiangsu Prov-ince and Shanghai Municipality[M].Geological Publishing House,Beijing.652(in Chinese).
李成立,谢春临,吕庆田.1998.利用位场功率谱计算地质体顶底深度效果[J].大庆石油地质与开发,17(5):45—54.LI Cheng-li,XIE Chun-lin,LQing-tian.1998.Calculating top and bottom depth effect of geological body by applyingpotential field power spectrum[J].Petroleum Geology&Oilfield Development in Daqing,17(5):45—54(inChinese).
刘建光.1992.徐州地区冲断褶皱带研究[J].煤田地质与勘探,20(3):12—19.LIU Jian-guang.1992.A preliminary study on the thrust and fold belt of the Xuzhou region[J].Coal Geology and Ex-ploration,20(3):12—19(in Chinese).
刘建华,宣晓伟,李兰生.1992.地震预报与徐州市的地震工作设想[J].地震学刊,1(3):61—66.LIU Jian-hua,XUAN Xiao-wei,LI Lan-sheng.1992.Expectation of earthquake prediction and earthquake work ofXuzhou city[J].Journal of Seismology,1(3):61—66(in Chinese).
马公伟.1991.徐宿地区大型深层滑脱构造的讨论[J].江苏地质,1(1):28—31.MA Gong-wei.1991.Prediction of large deep decollement structure in Xuzhou-Suzhou area[J].Jiangsu Geology,1(1):28—31(in Chinese).
施纬,张岳桥,董树文.2003.郯庐断裂带中段第四纪活动及其分段特征[J].地球学报,24(1):11—18.SHI Wei,ZHANG Yue-qiao,DONG Shu-wen.2003.Quaternary activity and segmentation behavior of the middle portionof the Tan-Lu Fault zone[J].Acta Geologica Sinica,24(1):11—18(in Chinese).
舒良树,吴俊奇,刘道忠.1994.徐宿地区推覆构造[J].南京大学学报,30(4):638—647.SHU Liang-shu,WU Jun-qi,LIU Dao-zhong.1994.Thrust tectonics of Xuzhou-Suzhou region,eastern China[J].Jour-nal of Nanjing University,30(4):638—647(in Chinese).
宋文荣.1999.宿迁城北构造地貌特征及其成因分析[J].地震学刊,1(2):45—50.SONG Wen-rong.1999.Structural geomorphological characteristics and genesis analysis of north part in Suqian city[J].Journal of Seismology,1(2):45—50(in Chinese).
眭素文,于长春,熊盛青,等.2007.功率谱可视化深度计算方法及在煤火区的应用[J].物探与化探,31(6):560—563.SUI Su-wen,YU Chang-chun,XIONG Sheng-qing,et al.2007.A visualized depth estimating method by power spectrumand its application to a coal fire area[J].Geophysical&Geo-chemical Exploration,31(6):560—563(in Chi-nese).
王桂梁,姜波,曹代勇,等.1998.徐州—宿州弧形双冲-叠瓦扇逆冲断层系统[J].地质学报,72(3):228—236.WANG Gui-liang,JIANG Bo,CAO Dai-yong,et al.1998.On the Xuzhou-Suzhou arcuate duplex-imbricate fan thrustsystem[J].Acta Geologica Sinica,72(3):228—236(in Chinese).
谢瑞征,朱书俊,丁政.1991.郯庐断裂带江苏段全新世活动问题的商榷[J].地震学刊,1(4):15—18.XIE Rui-zheng,ZHU Shu-jun,DING Zheng.1991.Research on recent activity along Jiangsu segment of Tanlu Faultzone[J].Journal of Seismology,1(4):15—18(in Chinese).
熊盛青,周付洪,姚正煦,等.2001.青藏高原中西部航磁调查[M].北京:地质出版社.51—162.XIONG Sheng-qing,ZHOU Fu-hong,YAO Zheng-xu,et al.2001.Aeromagnetic Investigation of the Middle Western Ar-eas of the Qinghai-Xizang Plateau[M].Geological Publishing House,Beijing.51—162(in Chinese).
徐智敏,孙亚军,刘沂轩.2006.徐州废黄河断裂带对区内岩溶地面塌陷控制作用研究[J].能源技术与管理,1(3):54—55.XU Zhi-min,SUN Ya-jun,LIU Yi-xuan.2006.A study on Fei Huanghe(ancient Yellow River)fault zone dominatingkarst collapse of Xuzhou area[J].Energy Technology and Management,1(3):54—55(in Chinese).
姚大全,刘家灿,李杰,等.2003.新沂—泗县地震危险区地震活动和地震构造[J].华北地震科学,21(2):23—28.YAO Da-quan,LIU Jia-can,LI Jie,et al.2003.Seismic activity and structure in Xinyi-Sixian seismic risk region[J].North China Earthquake Sciences,21(2):23—28(in Chinese).
杨明慧,王嗣敏,郑晓凤,等.2009.华北克拉通南部及邻区航磁异常特征与构造分区[J].地质评论,55(6):862—872.YANG Ming-hui,WANG Si-min,ZHENG Xiao-feng,et al.2009.Aeromagnetic anomalies characteristics and tectonic subareasof southern North China Craton and adjacent regions[J].Geological Review,55(6):862—872(in Chinese).
张景发,陶夏新,田云峰,等.2004.城市周边活断层探测中遥感技术的应用[J].自然灾害学报,13(1):137—145.ZHANG Jing-fa,TAO Xia-xin,TIAN Yun-feng,et al.2004.Application of remote sensing technique to exploration of ac-tive fault around urban areas[J].Journal of Natural Disasters,13(1):137—145(in Chinese).
张鹏,王良书,钟锴,等.2007.郯庐断裂带的分段性研究[J].地质评论,53(5):586—591.ZHANG Peng,WANG Liang-shu,ZHONG Kai,et al.2007.Research on the segmentation of Tancheng-Lujiang Faultzone[J].Geological Review,53(5):586—591(in Chinese).
张微,陈汉林,李启敏,等.2007.高分辨遥感在杭州活断层探测中的应用[J].煤田地质与勘探,35(3):10—14.ZHANG Wei,CHEN Han-lin,LI Qi-min,et al.2007.Application of high resolution remote sensing technique to exploration ofactive fault of Hangzhou and its surroundings[J].Coal Geology&Exploration,35(3):10—14(in Chinese).
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