新疆及邻区地震构造图简介
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摘要
简要介绍了新编新疆及邻区地震构造图的主要内容。本图在1∶1 000 000新疆地震构造图的基础上,修改扩编而成。比例尺为1∶2 500 000,采用李廷栋主编的1∶2 500 000中国西部及邻区地质构造图为底图。编制过程中吸收了大量相关研究成果,查阅相关文献,结合遥感资料的重新判读和解译。建立了图内近300条活动断裂及150条活动褶皱的数据库及相应的档案。图内涉及喜玛拉雅—帕米尔—西昆仑、天山、阿尔泰—西蒙古—萨彦等地震构造带,对这些地震构造带内靠近边境地区的主要地震构造的基本信息做了简要介绍。
This paper introduced briefly the seismotectonic map of Xinjiang and its neighborhood with scale of 1∶2 500 000.It was amended and complemented on the base of newly compiled seismotectonic map of Xinjiang whose scale is 1∶1 000 000,and expensively compiled.The base map of this seismotectonic map is the geological structure map of western China and its neighborhood which was compiled by Li Ting-dong.The abundant new materials from relative research works and referential literatures as well as the analysis on the remote sensing data were used in the compiling work.Data base and documents of nearly 300 active faults and 150 active folds were set up.The basic information of the major active faults in this map,especially those near the border area,were introduced briefly in this paper.
This paper introduced briefly the seismotectonic map of Xinjiang and its neighborhood with scale of 1∶2 500 000.It was amended and complemented on the base of newly compiled seismotectonic map of Xinjiang whose scale is 1∶1 000 000,and expensively compiled.The base map of this seismotectonic map is the geological structure map of western China and its neighborhood which was compiled by Li Ting-dong.The abundant new materials from relative research works and referential literatures as well as the analysis on the remote sensing data were used in the compiling work.Data base and documents of nearly 300 active faults and 150 active folds were set up.The basic information of the major active faults in this map,especially those near the border area,were introduced briefly in this paper.
引文
[1]吴传勇,罗福忠,白美祥,等.新版1:1 000 000新疆地震构造图简介[J].内陆地震,2009,23(2):258-262.
[2]李廷栋,耿树方,范本贤,等.中国西部及邻区1∶2 500 000地质图[M].北京:地质出版社,2006.
[3]李祥根.中国新构造运动概论[M].北京:地震出版社,2003.
[4]Nikonov AA.Aplying of radiocarbon determination to detomic ages of paleoearthquake in South of Centre Asia[J].Geophysics,1981,9:70-79.
[5]尼科诺夫A A.全新世和现代地壳活动[M].北京:地震出版社,1977.
[6]Burtman V S,Molnar P.Deep Subduction benedth the Pamir,Geological Society of America Special Paper 1993,281.
[8]李海兵,Frank Valli,许志琴,等.喀喇昆仑断裂的变形特征及构造演化[J].中国地质,2006,33(2):239-255.
[9]李海兵,司家亮,潘家伟,等.活动断裂的变性特征及其大地震复发周期的估算[J].地质通报,2008,27(12):1 968-1 991.
[10]付碧宏,张松林,谢小平,等.阿尔金断裂带西段-康西瓦断裂的晚第四纪构造地貌特征研究[J].第四纪研究,2006,26(2):228-235.
[11]冯先岳,栾超群,李军,等.1987年4月30日乌恰西6.0级地震[J].内陆地震,1988,2(2):131-141.
[12]АбдрахматовКБ,ЛемзинИН.СовременньыеиЧетвертинныетектоничекиедвцжениялоТаласс-Фергаскомуразлому,Тянъ-Шанъвновейшемэтапегеологическоторазвития[M].“Илим”,Бишкек,1991:66-73.
[13]ИбрагимовРН.СейсмогенныезоныСреднегоТянь-Шаня(НапримереВосточногоУзбетиана)[M].Цзд.《ФАН》УзбекскойССР,Ташкект,1978.
[14]Shen Jun,Wang Yi-peng,Zhao Rui-bing,et al.,Surveying of the deformed terraces and crust shortening rate in the northwestTarim Basin,Chinese Science Bulletin,2001,46(12):1 043-1 046.
[15]邓起东,Molnar P,Brown E T,等.天山南缘北轮台断裂库尔楚段晚第四纪的最新活动和滑动速率[J].内陆地震,2001,15(4):289-298.
[16]加藤碵一.地震と活断層の科学[M].朝倉说?1989.
[17]Molnar P.Faulting associated with large earthquake and the everge rate of deformation central and Eastern Asia[J].J.Geo-phys Res,1984,(89):6 203-6 228.
[18]尹光华.伊犁盆地新构造运动与地震[J].内陆地震,1993,7(2):180-187.
[19]Tapponnier,Molnar.Active tectonics of central Asia[J].J.G.R.,1979,84(B7):3 425-3 458.
[20]沈军,杨小平.博罗科努断裂西北段地震形变带初步研究[J].内陆地震,1998,12(3):248-255.
[21]邓起东,冯先岳,张培震,等.天山活动构造[M].北京:地震出版社,2000.
[22]Buljinnyan I,Bayasgalan A,Borisov B A,et al.Ruptures of major earthqaukes and active deformation in Mongolia and its sur-roundings[J].Geological Society of America,Memoir,1993,(181):62.
[23]沈军,李莹飘,汪一鹏.阿尔泰山活动断裂[J].地学前缘,2003,10(特刊):132-141.
[24]洪顺英,申旭辉,赖木收,等.阿尔泰山东缘主要活动断裂影象特征分析[J].地震地质,2006,28(1):119-127.
[25]新疆维吾尔自治区地震局.富蕴地震断裂带[M].北京:地震出版社,1985.
[26]柏美祥,罗福忠,尹光华,等.新疆可可托海-二台活动断裂带[J].内陆地震,1996,10(4):319-329.
[27]ХилькоСЯ,ФлоренсовНА,КурушинРА,идр.СейсмотектектонинескиелинемантыипалеосейсмиДискацииМогольскогоАлтая[C]//СейсмотектоникаЮжныхрайоныСССР.1978.
[28]尹光华,蒋靖祥,吴国栋.2008年3月21日于田7.4级地震的构造背景[J].干旱区地理,2008,31(4):543-549.
[29]冯先岳.新疆古地震[M].乌鲁木齐:新疆科技卫生出版社,1997.
[2]李廷栋,耿树方,范本贤,等.中国西部及邻区1∶2 500 000地质图[M].北京:地质出版社,2006.
[3]李祥根.中国新构造运动概论[M].北京:地震出版社,2003.
[4]Nikonov AA.Aplying of radiocarbon determination to detomic ages of paleoearthquake in South of Centre Asia[J].Geophysics,1981,9:70-79.
[5]尼科诺夫A A.全新世和现代地壳活动[M].北京:地震出版社,1977.
[6]Burtman V S,Molnar P.Deep Subduction benedth the Pamir,Geological Society of America Special Paper 1993,281.
[8]李海兵,Frank Valli,许志琴,等.喀喇昆仑断裂的变形特征及构造演化[J].中国地质,2006,33(2):239-255.
[9]李海兵,司家亮,潘家伟,等.活动断裂的变性特征及其大地震复发周期的估算[J].地质通报,2008,27(12):1 968-1 991.
[10]付碧宏,张松林,谢小平,等.阿尔金断裂带西段-康西瓦断裂的晚第四纪构造地貌特征研究[J].第四纪研究,2006,26(2):228-235.
[11]冯先岳,栾超群,李军,等.1987年4月30日乌恰西6.0级地震[J].内陆地震,1988,2(2):131-141.
[12]АбдрахматовКБ,ЛемзинИН.СовременньыеиЧетвертинныетектоничекиедвцжениялоТаласс-Фергаскомуразлому,Тянъ-Шанъвновейшемэтапегеологическоторазвития[M].“Илим”,Бишкек,1991:66-73.
[13]ИбрагимовРН.СейсмогенныезоныСреднегоТянь-Шаня(НапримереВосточногоУзбетиана)[M].Цзд.《ФАН》УзбекскойССР,Ташкект,1978.
[14]Shen Jun,Wang Yi-peng,Zhao Rui-bing,et al.,Surveying of the deformed terraces and crust shortening rate in the northwestTarim Basin,Chinese Science Bulletin,2001,46(12):1 043-1 046.
[15]邓起东,Molnar P,Brown E T,等.天山南缘北轮台断裂库尔楚段晚第四纪的最新活动和滑动速率[J].内陆地震,2001,15(4):289-298.
[16]加藤碵一.地震と活断層の科学[M].朝倉说?1989.
[17]Molnar P.Faulting associated with large earthquake and the everge rate of deformation central and Eastern Asia[J].J.Geo-phys Res,1984,(89):6 203-6 228.
[18]尹光华.伊犁盆地新构造运动与地震[J].内陆地震,1993,7(2):180-187.
[19]Tapponnier,Molnar.Active tectonics of central Asia[J].J.G.R.,1979,84(B7):3 425-3 458.
[20]沈军,杨小平.博罗科努断裂西北段地震形变带初步研究[J].内陆地震,1998,12(3):248-255.
[21]邓起东,冯先岳,张培震,等.天山活动构造[M].北京:地震出版社,2000.
[22]Buljinnyan I,Bayasgalan A,Borisov B A,et al.Ruptures of major earthqaukes and active deformation in Mongolia and its sur-roundings[J].Geological Society of America,Memoir,1993,(181):62.
[23]沈军,李莹飘,汪一鹏.阿尔泰山活动断裂[J].地学前缘,2003,10(特刊):132-141.
[24]洪顺英,申旭辉,赖木收,等.阿尔泰山东缘主要活动断裂影象特征分析[J].地震地质,2006,28(1):119-127.
[25]新疆维吾尔自治区地震局.富蕴地震断裂带[M].北京:地震出版社,1985.
[26]柏美祥,罗福忠,尹光华,等.新疆可可托海-二台活动断裂带[J].内陆地震,1996,10(4):319-329.
[27]ХилькоСЯ,ФлоренсовНА,КурушинРА,идр.СейсмотектектонинескиелинемантыипалеосейсмиДискацииМогольскогоАлтая[C]//СейсмотектоникаЮжныхрайоныСССР.1978.
[28]尹光华,蒋靖祥,吴国栋.2008年3月21日于田7.4级地震的构造背景[J].干旱区地理,2008,31(4):543-549.
[29]冯先岳.新疆古地震[M].乌鲁木齐:新疆科技卫生出版社,1997.
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