震积岩特征综述及地质意义
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摘要
震积岩是一种灾变事件岩。文章综述了震积岩特征及其地质意义,着重介绍了震积岩的岩石类型、震积序列、鉴别标志及震积岩-海啸岩-震浊积岩的对比鉴别。同时,结合国内学者的研究成果,归纳出由震积岩-海啸岩-震浊积岩-背景沉积组成的6种地震震积序列,并指出震积岩对于构造演化解释、沉积学及石油储层地质方面的研究意义。
Seismite is a type of catastrophic deposits.The characteristics and geological significance of seismites are summarized.The rock types,seismic sequences,distinguishing marks of seismites and the contrasts among seismites,tsunamites and seismoturbidites are introduced.Based on the former research,six seismic sequences are proposed,which are composed of seismites,tsunamites,seismoturbidites and background deposits.Seismites take a significant part in the studies on the interpretation of tectonic evolution,sedimentology and reservoir geology.
Seismite is a type of catastrophic deposits.The characteristics and geological significance of seismites are summarized.The rock types,seismic sequences,distinguishing marks of seismites and the contrasts among seismites,tsunamites and seismoturbidites are introduced.Based on the former research,six seismic sequences are proposed,which are composed of seismites,tsunamites,seismoturbidites and background deposits.Seismites take a significant part in the studies on the interpretation of tectonic evolution,sedimentology and reservoir geology.
引文
[1]Barrett P J.Effects of the 1964 Alaskan earthquake on some shallowwater sediments in Prince William Sound,Southeast Alaska[J].Journal ofSedimentaryResearch,1966,36(4):992-1006.
[2]Seilacher A.Fault-graded beds interpreted as seismites[J].Sedimentology,1969,13(1-2):155-159.
[3]Spalleta C,Vai GB.Upper Devonian intraclast parabreccias interpreted as seismites[J].Marine Geology,1984,55(1-2):133-144.
[4]Seilacher A.Sedimentary structures tentatively attributed to seismic events[J].Marine Geology,1984,55(1-2):1-12.
[5]宋天锐,和政军,丁孝忠.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,1988,33(8):609-611
[6]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):16-34.
[7]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.
[8]付文利,王艳琴,杨光,等.东营凹陷沙三段、沙四段震积岩研究[J].油气地质与采收率,2004,11(2):6-8.
[9]路慎强.济阳坳陷古近系碎屑岩地层中震积岩识别标志研究[J].中国石油大学学报(自然科学版),2006,30(5):8-13.
[10]杜远生,韩欣.论震积作用和震积岩[J].地球科学进展,2000,15(4):389-394.
[11]乔秀夫,高林志,彭阳,等.古郯庐带沧浪铺阶地震事件、层序及构造意义[J].中国科学(D辑),2001,31(11):911-918.
[12]南凌,崔之久.地震混杂岩(震积岩)的沉积特征和识别[J].地震地质译丛,1996,18(6):1-9.
[13]周晓东,陈跃军.吉南地区晚震旦世震积岩特征[J].吉林地质,1998,17(4):24-28.
[14]Kullberg J,Oloriz F,Marques B,et al.Flat-pebble conglomerates:a local marker for Early Jurassic seismicity related to syn-rift tectonics in the Sesimbra area(Lusitanian Basin,Portugal)[J].Sed-imentary Geology,2001,139(1):49-70.
[15]Roep T B,Events A J.Pillow-beds:a new type of seismites?An example from an Oligocene turbidite fan complex Alicante[J].Sedimentology,1992,39:711-724.
[16]DU Yuan-sheng,ZHANG Chuan-heng,HAN Xin,et al.Earthquake event deposits in Mesoproterozoic Kunyang Group in central Yunnan Province and its geological implications[J].Science in China(D-earth science),2001,44(7):600-608.
[17]Knaust D.Pinch-and-swell structures at the Middle/Upper Muschelkalk boundary(Triassic):evidence of earthquake effects(seismimites)in the Germanic Basin[J].International Journal of Earth Sciences,2002,91(2):291-303.
[18]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):138-146.
[19]梁定益,聂泽同,宋志敏.再论震积岩及震积不整合——以川西、滇西地区为例[J].地球科学,1994,19(6):845-850.
[20]杜远生,张传恒,韩欣.滇中地区中元古代大龙口组震积岩的新发现[J].地球科学,1999,24(增刊):28-37.
[21]Mutti E,RicciLucchi F,Seguret M,et al.Seismoturbidites:a new group of resedimented deposits[J].Marine Geology,1984,55(1-2):103-116.
[22]吴贤涛,尹国勋.四川峨眉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):19-26.
[2]Seilacher A.Fault-graded beds interpreted as seismites[J].Sedimentology,1969,13(1-2):155-159.
[3]Spalleta C,Vai GB.Upper Devonian intraclast parabreccias interpreted as seismites[J].Marine Geology,1984,55(1-2):133-144.
[4]Seilacher A.Sedimentary structures tentatively attributed to seismic events[J].Marine Geology,1984,55(1-2):1-12.
[5]宋天锐,和政军,丁孝忠.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,1988,33(8):609-611
[6]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):16-34.
[7]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.
[8]付文利,王艳琴,杨光,等.东营凹陷沙三段、沙四段震积岩研究[J].油气地质与采收率,2004,11(2):6-8.
[9]路慎强.济阳坳陷古近系碎屑岩地层中震积岩识别标志研究[J].中国石油大学学报(自然科学版),2006,30(5):8-13.
[10]杜远生,韩欣.论震积作用和震积岩[J].地球科学进展,2000,15(4):389-394.
[11]乔秀夫,高林志,彭阳,等.古郯庐带沧浪铺阶地震事件、层序及构造意义[J].中国科学(D辑),2001,31(11):911-918.
[12]南凌,崔之久.地震混杂岩(震积岩)的沉积特征和识别[J].地震地质译丛,1996,18(6):1-9.
[13]周晓东,陈跃军.吉南地区晚震旦世震积岩特征[J].吉林地质,1998,17(4):24-28.
[14]Kullberg J,Oloriz F,Marques B,et al.Flat-pebble conglomerates:a local marker for Early Jurassic seismicity related to syn-rift tectonics in the Sesimbra area(Lusitanian Basin,Portugal)[J].Sed-imentary Geology,2001,139(1):49-70.
[15]Roep T B,Events A J.Pillow-beds:a new type of seismites?An example from an Oligocene turbidite fan complex Alicante[J].Sedimentology,1992,39:711-724.
[16]DU Yuan-sheng,ZHANG Chuan-heng,HAN Xin,et al.Earthquake event deposits in Mesoproterozoic Kunyang Group in central Yunnan Province and its geological implications[J].Science in China(D-earth science),2001,44(7):600-608.
[17]Knaust D.Pinch-and-swell structures at the Middle/Upper Muschelkalk boundary(Triassic):evidence of earthquake effects(seismimites)in the Germanic Basin[J].International Journal of Earth Sciences,2002,91(2):291-303.
[18]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):138-146.
[19]梁定益,聂泽同,宋志敏.再论震积岩及震积不整合——以川西、滇西地区为例[J].地球科学,1994,19(6):845-850.
[20]杜远生,张传恒,韩欣.滇中地区中元古代大龙口组震积岩的新发现[J].地球科学,1999,24(增刊):28-37.
[21]Mutti E,RicciLucchi F,Seguret M,et al.Seismoturbidites:a new group of resedimented deposits[J].Marine Geology,1984,55(1-2):103-116.
[22]吴贤涛,尹国勋.四川峨眉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):19-26.
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