海相地层中地震遗迹宏观特征与鉴别
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摘要
笔者根据不同地质时期多个地区宏观地震遗迹特征,综合编汇出一个较完整的地震遗迹序列,包括地震层、海震层两个序列,进一步划分出6个岩石类型,并对各种地震遗迹标志与成因作简要介绍。
According to the macro-characteristics on seismic traces in different geological period and several areas,a relative completed sequence has been compiled in this paper.The sequence includes two sub-sequences;they are seismic bed and marine seismic bed and then further divided into six rock types.Many photos have been presented to explain the origin and distinguish marks about seismic traces on the marine strata.
According to the macro-characteristics on seismic traces in different geological period and several areas,a relative completed sequence has been compiled in this paper.The sequence includes two sub-sequences;they are seismic bed and marine seismic bed and then further divided into six rock types.Many photos have been presented to explain the origin and distinguish marks about seismic traces on the marine strata.
引文
[1]乔秀夫,宋天锐,高林志,等.地层中地震记录(古地震)[M].北京:地质出版社,2006:1-26.
[2]宋天锐,刘燕学.古地震记录与岩相古地理[J].沉积学报,2009,27(5):872-879.
[3]杜远生,张传恒,韩欣,等.滇中中元古代昆阳郡的地震事件沉积及其地质意义[J].中国科学(D辑),2001,11(4):283-289.
[4]梁定益,聂泽同,万晓樵,等.试论震积岩及震积不整合—以川西、滇西地区为例[J].现代地质,1991,5(2):138-147.
[5]梁定益,聂泽同,宋志敏.再论震积岩与震积不整合—以川西、滇西地区为例[J].地球科学,1994,19(6):845-850.
[6]梁定益,聂泽同,宋志敏.扬子西缘东吴伸展运动[J].地球科学,1994,19(4):443-453.
[7]梁定益,宋志敏,赵崇贺,等.河北白石山中元古代地震遗迹的发现[J].地质通报,2002,21(10):625-631.
[8]乔秀夫,李海兵.枕、球枕构造:地层中的古地震记录[J].地质论评,2008,54(6):721-730.
[9]万天丰.地震预报、设防与预警问题[J].自然杂志,2009,31(3):132-135.
[10]杨仕维,李建明.震积岩特征综述与地质意义[J].岩性油气藏,2008,20(1):89-94.
[11]乔秀夫,宋天锐,高林志,等.碳酸盐岩振动液化地震序列[J].地质学报,1994,68(1):16-32.
[12]SPALLETTA C,VAI G B.Upper Devonianintraclast parabrec-cias interpreted as seismites[J].Mar Geal,1984,55:133-144.
[13]SEILACHER A.Fault-graded beds interpreted as Seis mites[J].Sedi mentology,13:155-159.
[14]SEILACHER A.Sedi mentary structures tentatively affributedto seis mic events[J].Marine Geology,1984,55(1-2):1-12.
[15]吴贤诗,尹国勋.四川峨嵋晚侏罗世湖泊沉积中震积岩的发现及其意义[J].沉积学报,1992,10(1):19-24.
[16]梁定益,聂泽同,宋志敏,等.北京房山世界地质公园中元古界雾迷山组地震—海啸序列及地质特征—以野三坡园区为例[J].地质通报,2008,28(1):30-37.
[17]龚一鸣.风暴岩、震积岩、海啸岩—几个名词含义的商榷[J].地质论评,1998,36(5):481-482.
[18]宋天锐.北京十三陵前寒武纪碳酸盐岩地层中的一套可能的地震—海啸序列[J].科学通报,1988,(8):609-611.
[19]杜远生,韩欣.论海啸作用与海啸岩[J].地质科技情报,2000,19(1):19-22.
[20]KASTENS K M,CITA MB.Tsunami-induced sedi met trans-port in the abyssal Mediterranean Sea[J].Geol Soc Am Bull,1981,92:845-857.
[21]张传恒,武振杰,高林志,等.华北中元古界雾迷山组地震驱动的软沉积物变形构造及其地质意义[J].中国科学,D辑:地球科学,2007,37(1):6-8.
[22]ROSSETTI D F,GOES A M.Deciphering the sedi menlogycali mprint of paleoseis mic events:an example fromthe AptianCodc For mation[J].Northern Brazil Sed Geol,2000,135(1-4):137-156.
[23]LUCCHI F R.,VALMORI E.Basin-wideturbidites in a Mio-cene,over-supplied deep-sea plain:a geometrical analysis[J].Sedi mentology,1980,27:240-270.
[24]MUFFI E,LUCCHI F R,Seguret M.Zanzucchi,Seis mofur-bidites:a new group of resedi mented deposits[J].Mar Geol,1984,55:103-116.
[25]孙晓猛,梁定益,聂泽同.大陆边缘震积岩序列—以金沙江中段震积岩为例[J].现代地质,1995,9(3):271-278.
[26]南凌,崔之久.地震混杂岩(震积岩)的沉积特征与识别[J].地震地质译丛,1996,18(6):1-9.
[27]杜远生,韩欣.论震积作用与震积岩[J].地球科学进展,2000,15(4):389-394.
[28]KASTENS K M,CITA MB.Tsunami-inducedsedi ment trans-ports in the abyssal Mediterranean Sea[J].Geol Soc AmBull,1981,92:845-847.
[29]周志广,梁定益,刘文灿,等.藏南晚白垩世宗卓组巨型混杂岩堆积的特征及其地裂—地震成因论证[J].地质论评,2006,52(3):315-321.
[30]KUENEN P.Experi ments in geology[J].Trans Geol SocGlasgow,1958,23:1-28.
[31]ROEP T B,EVENTS A T.Pillow-beds:a new tupe of seis-mites?An example from an Oligocene turbidite fan complexAlicante[J].Sedi mentology,1992,39:711-724.
[32]乔秀夫,李海兵,王思恩,等.新疆境内塔拉斯—费尔干纳断裂早侏罗世走滑的古地震证据[J].地质学报,2008,82(6):721-730.
[2]宋天锐,刘燕学.古地震记录与岩相古地理[J].沉积学报,2009,27(5):872-879.
[3]杜远生,张传恒,韩欣,等.滇中中元古代昆阳郡的地震事件沉积及其地质意义[J].中国科学(D辑),2001,11(4):283-289.
[4]梁定益,聂泽同,万晓樵,等.试论震积岩及震积不整合—以川西、滇西地区为例[J].现代地质,1991,5(2):138-147.
[5]梁定益,聂泽同,宋志敏.再论震积岩与震积不整合—以川西、滇西地区为例[J].地球科学,1994,19(6):845-850.
[6]梁定益,聂泽同,宋志敏.扬子西缘东吴伸展运动[J].地球科学,1994,19(4):443-453.
[7]梁定益,宋志敏,赵崇贺,等.河北白石山中元古代地震遗迹的发现[J].地质通报,2002,21(10):625-631.
[8]乔秀夫,李海兵.枕、球枕构造:地层中的古地震记录[J].地质论评,2008,54(6):721-730.
[9]万天丰.地震预报、设防与预警问题[J].自然杂志,2009,31(3):132-135.
[10]杨仕维,李建明.震积岩特征综述与地质意义[J].岩性油气藏,2008,20(1):89-94.
[11]乔秀夫,宋天锐,高林志,等.碳酸盐岩振动液化地震序列[J].地质学报,1994,68(1):16-32.
[12]SPALLETTA C,VAI G B.Upper Devonianintraclast parabrec-cias interpreted as seismites[J].Mar Geal,1984,55:133-144.
[13]SEILACHER A.Fault-graded beds interpreted as Seis mites[J].Sedi mentology,13:155-159.
[14]SEILACHER A.Sedi mentary structures tentatively affributedto seis mic events[J].Marine Geology,1984,55(1-2):1-12.
[15]吴贤诗,尹国勋.四川峨嵋晚侏罗世湖泊沉积中震积岩的发现及其意义[J].沉积学报,1992,10(1):19-24.
[16]梁定益,聂泽同,宋志敏,等.北京房山世界地质公园中元古界雾迷山组地震—海啸序列及地质特征—以野三坡园区为例[J].地质通报,2008,28(1):30-37.
[17]龚一鸣.风暴岩、震积岩、海啸岩—几个名词含义的商榷[J].地质论评,1998,36(5):481-482.
[18]宋天锐.北京十三陵前寒武纪碳酸盐岩地层中的一套可能的地震—海啸序列[J].科学通报,1988,(8):609-611.
[19]杜远生,韩欣.论海啸作用与海啸岩[J].地质科技情报,2000,19(1):19-22.
[20]KASTENS K M,CITA MB.Tsunami-induced sedi met trans-port in the abyssal Mediterranean Sea[J].Geol Soc Am Bull,1981,92:845-857.
[21]张传恒,武振杰,高林志,等.华北中元古界雾迷山组地震驱动的软沉积物变形构造及其地质意义[J].中国科学,D辑:地球科学,2007,37(1):6-8.
[22]ROSSETTI D F,GOES A M.Deciphering the sedi menlogycali mprint of paleoseis mic events:an example fromthe AptianCodc For mation[J].Northern Brazil Sed Geol,2000,135(1-4):137-156.
[23]LUCCHI F R.,VALMORI E.Basin-wideturbidites in a Mio-cene,over-supplied deep-sea plain:a geometrical analysis[J].Sedi mentology,1980,27:240-270.
[24]MUFFI E,LUCCHI F R,Seguret M.Zanzucchi,Seis mofur-bidites:a new group of resedi mented deposits[J].Mar Geol,1984,55:103-116.
[25]孙晓猛,梁定益,聂泽同.大陆边缘震积岩序列—以金沙江中段震积岩为例[J].现代地质,1995,9(3):271-278.
[26]南凌,崔之久.地震混杂岩(震积岩)的沉积特征与识别[J].地震地质译丛,1996,18(6):1-9.
[27]杜远生,韩欣.论震积作用与震积岩[J].地球科学进展,2000,15(4):389-394.
[28]KASTENS K M,CITA MB.Tsunami-inducedsedi ment trans-ports in the abyssal Mediterranean Sea[J].Geol Soc AmBull,1981,92:845-847.
[29]周志广,梁定益,刘文灿,等.藏南晚白垩世宗卓组巨型混杂岩堆积的特征及其地裂—地震成因论证[J].地质论评,2006,52(3):315-321.
[30]KUENEN P.Experi ments in geology[J].Trans Geol SocGlasgow,1958,23:1-28.
[31]ROEP T B,EVENTS A T.Pillow-beds:a new tupe of seis-mites?An example from an Oligocene turbidite fan complexAlicante[J].Sedi mentology,1992,39:711-724.
[32]乔秀夫,李海兵,王思恩,等.新疆境内塔拉斯—费尔干纳断裂早侏罗世走滑的古地震证据[J].地质学报,2008,82(6):721-730.
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