The Property and Geological Significance of Seismites of Paleogene in Huimin Sag,Shandong Province

YUAN Jing

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Article Navigation > Acta Sedimentologica Sinica > 2004 > 22(1): 41-46

YUAN Jing. The Property and Geological Significance of Seismites of Paleogene in Huimin Sag,Shandong Province[J]. Acta Sedimentologica Sinica, 2004, 22(1): 41-46.

Citation:

YUAN Jing. The Property and Geological Significance of Seismites of Paleogene in Huimin Sag,Shandong Province[J]. Acta Sedimentologica Sinica, 2004, 22(1): 41-46.

The Property and Geological Significance of Seismites of Paleogene in Huimin Sag,Shandong Province

YUAN Jing

College of Earth Resource and Information, University of Petroleum, Dongying Shandong 257061

Received Date: 2003-01-02
Rev Recd Date: 2003-04-15
Publish Date: 2004-03-10

Abstract

This paper discussed the sedimentary property, vertical sequence and geological significance of seismites of Paleogene in Huimin sag, Shandong Province. Seismite is a kind of catastrophic event rock, being the terrane with ancient earthquake records. Huimin sag was a fault lake in Paleogenein Bohaiwan basin. The sandstones and mudstones were the main sedimentary rocks with in the sag. Many typical deformation structures were caused by widespread earthquake in the sag. They were syn sedimentary microfactures (includingfault graded), seismic fissure bed, sandstone vein, water escape structure, "pillow structure", ball structure, convolute lamination, load structure and flame structure, etc. The vertical sequence of seismite of petroclastic rock in Paleogene in Huimin sag, from bottom to top, included 6 units: underlying unshocked layer, fissure layer, microfold layer, pillow structure and partner structure layer, liquefied homogeneous layer and overlying unshocked layer. Thecompletenessof the vertical sequence dependsonthe location of section, seismic level, especially the lithology. It is of important geologicalsignificance to study seismite. Most seismites in Paleogene in Huimin sag developed near the peripheral faults and central fault zone of the sag. The mass appearanceof seismites reflected the intensively active period of basin-controlling boundary faults, andcan be used to interpret the tectonic evolvement of fault basin. The seismites in fault basin can be likely reservoir for their specialtectonic location and structures.
- seismite,
- sedimentary property,
- geologicalsignificance,
- Paleogene Huiminsag

References

[1]	Seilacher A. Fault-graded bed interpreted as seismites.Sedimentology,1969,13(1～2):155～159
[2]	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.科学通报,1988,38(8):609～611[Song Tianrui. Apossible suit of seismo-tsunami sequence in Precambriancarbonate rock stratum in Shisanling in Beijing. Chinese Science Bulletin, 1988, 38(8): 609～611]
[3]	乔秀夫,宋天锐,高林志,等.碳酸盐岩振动液化地震序列.地质学报,1994,68(1):16～32[Qiao Xiufu, Song Tianrui, Gao Linzhi, et al. Seismic sequence in carbonate rocks by vibrational liquefaction. Acta Geological Sinica, 1994, 68(1): 16～34]
[4]	乔秀夫,李海兵,高林志. 华北地台震旦纪-早古生代地震节律. 地学前缘,1997,4(3～4):155～160[ Qiao Xiufu, Li Haibing, Gao Linzhi. Sinian-early Paleozoic seismic rhythms on the north China platform. Earth Science Frontiers, 1997, 4(3～4): 155～160]
[5]	乔秀夫,高林志.华北中新元古代及早中生代地震灾变事件及与Rodinia的关系.科学通报,1999,44(16):1753～1758[Qiao Xiufu, Gao Linzhi. Earthquake events in Neoproterozoic and early Paleozoic and its relationship with supercontinental Rodinia in North China. Chinese Science Bulletin, 1999, 44(16): 1753～1758]
[6]	乔秀夫.中国震积岩的研究与展望.地质论评,1996,42(4):317～320[Qiao Xiufu. Study of seismites of China and its prospects. Geological Review, 1996, 42(4): 317～320]
[7]	梁定益,聂泽同,万晓樵.试论震积岩及震积不整合--以川西、滇西地区为例.现代地质,1991,5(2):138～147[Liang Dingyi, Nie Zetong, Wang Xiaoqiao. Onthe seismitesand seismodiconformity - take the W. Sichuan and W. Yunnan regions as an example. Geoscience, 1991, 5(2): 138～147]
[8]	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.地球科学,1994,19(6):845～850[Liang Dingyi, Nie Zetong, Song Zhimin. A restudy on seismitesand seismo-unconformity:Taking western Sichuan and western Yunnan as an example. Earth Science, 1994, 19(6): 845～850]
[9]	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.现代地质,1995,9(3):1～27[Sun Xiaomeng, Liang Dingyi, Nie Zetong.Seismitesequence in continental margin - Taking seismite in middle region of Jinsha river as an example. Geoscience, 1995, 9(3): 1～27]
[10]	杜远生,张传恒,韩欣.滇西地区中元古代大龙口组震积岩的新发现.沉积学报,1999,24(增刊):28～37[Du Yuansheng, Zhang Chuanheng, Han Xin. New discovery of seismites in Dalongkou group in Mid- Proterozoic in Dianxi. Acta Sedimentologica Sinica, 1996, 14 (Suppl.): 28～37]
[11]	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.沉积学报,1992,10(3):19～24[Wu Xaintao, Yin Guoxun. Discovery and significance of seismites of lake deposition of late Jurassicin Ermei in Sichuan. Acta Sedimentologica Sinica, 1992,10(3): 19～24]
[12]	南凌,崔之久.地震混杂岩(震积岩)的沉积特征和识别.地震地质译丛,1996,18(6):1～9[Nan Ling, Cui Zhijiu. Sedimentary characteristics and recognition of seismites. Seismology and GeologyVersions, 1996, 18(6): 1～9]
[13]	杜远生,韩欣.论震积作用和震积岩.地球科学进展,2000,(4):389～394[Du Yuansheng, Han Xin. Seismo-deposition and seismites. Advance in Earth Sciences, 2000,(4): 389～394]
[14]	Bauerman H.Report on the geology of the country near the forty-ninth parallel of north latitude west of the Rocky Mountains.Geological Survey of Canada Report(1882-83-84,pt.B),1985.1～42
[15]	Ian J Fairchild,Gerhard Einsele, Tianrui Song.Possible seismic origin of molar tooth structures in Neoproterozoic carbonate ramp deposits, north China. Sedimentology,1997,44: 611～636
[16]	Rossetti D F, Goes A M. Deciphering the sedimentologyical imprint of paleoseismic events: an example from the Aptian Codo formation,northern Brazil.Sedimentary Geology,2000,135: 137～156
[17]	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.中国科学(D辑), 2001,31(11):911～918[Qiao Xiufu, Gao linzhi, Peng Yang, et al. Seismic event, sequence and tectonic significance in Canglangpu Stage in Paleo-Tanlu Fault Zone. Science in China(Series D), 2001, 31(11): 911～918]
[18]	Brain R, Pratt. Oceangraphy, bathymetry and syndepositional tectonics of a Precambrianintracratonic basin:integrating sediments,storms,earthquakes and tsunamis in the belt supergroup Helena formation,ca. 1.45 Ga,western north America.Sedimentary Geology,2001,141～142: 371～394
[19]	Roep T B, Events A J. Pillow-beds: a new type of seismites? An examplefrom an Oligocene turbidite fan complex,Alicante. Sedimentology,1992,39: 711～724
[20]	杜远生,张传恒,韩欣.滇西中元古代昆阳群的地震事件沉积及其地质意义.中国科学(D辑),2001,31(4):284～290[Du Yuansheng, Zhang Chuanheng, Han Xin. Earthquake events deposition and geologic significance of Kunyang group in Mid-Proterozoicin Dianxi. Science in China(Series D), 2001, 31(4): 284～290]
[21]	Spallctta C,VailG B.Upper Devonian intraclast parabreccias interpreted as seismites. Marine Geology,1984,55(1～2):133～144
[22]	Rodriguez-Pascua M A, Calvo J P, De Vicente G, et al.Soft-sediment deformation structures interpreted as seismites in lacustrine sediments of the prebetic zone,SE Spain, and their potential use as indicators of earthquake magnitudes during the late Miocene.Sedimentary Geology,2000,135: 117～135
[23]	乔秀夫.中朝板块元古宙板内地震带与盆地格局.地学前缘,2002,9(3):141～149[Qiao Xiufu. Intraplate seismic belt and basin framework of Sino-Korean plate in Proterozoic. Earth Science Frontiers, 2002, 9(3): 141～149]

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The Property and Geological Significance of Seismites of Paleogene in Huimin Sag,Shandong Province

College of Earth Resource and Information, University of Petroleum, Dongying Shandong 257061

Received Date: 2003-01-02

Rev Recd Date: 2003-04-15

Publish Date: 2004-03-10

Key words:

Abstract: This paper discussed the sedimentary property, vertical sequence and geological significance of seismites of Paleogene in Huimin sag, Shandong Province. Seismite is a kind of catastrophic event rock, being the terrane with ancient earthquake records. Huimin sag was a fault lake in Paleogenein Bohaiwan basin. The sandstones and mudstones were the main sedimentary rocks with in the sag. Many typical deformation structures were caused by widespread earthquake in the sag. They were syn sedimentary microfactures (includingfault graded), seismic fissure bed, sandstone vein, water escape structure, "pillow structure", ball structure, convolute lamination, load structure and flame structure, etc. The vertical sequence of seismite of petroclastic rock in Paleogene in Huimin sag, from bottom to top, included 6 units: underlying unshocked layer, fissure layer, microfold layer, pillow structure and partner structure layer, liquefied homogeneous layer and overlying unshocked layer. Thecompletenessof the vertical sequence dependsonthe location of section, seismic level, especially the lithology. It is of important geologicalsignificance to study seismite. Most seismites in Paleogene in Huimin sag developed near the peripheral faults and central fault zone of the sag. The mass appearanceof seismites reflected the intensively active period of basin-controlling boundary faults, andcan be used to interpret the tectonic evolvement of fault basin. The seismites in fault basin can be likely reservoir for their specialtectonic location and structures.

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Reference (23)

[1]	Seilacher A. Fault-graded bed interpreted as seismites.Sedimentology,1969,13(1～2):155～159
[2]	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.科学通报,1988,38(8):609～611[Song Tianrui. Apossible suit of seismo-tsunami sequence in Precambriancarbonate rock stratum in Shisanling in Beijing. Chinese Science Bulletin, 1988, 38(8): 609～611]
[3]	乔秀夫,宋天锐,高林志,等.碳酸盐岩振动液化地震序列.地质学报,1994,68(1):16～32[Qiao Xiufu, Song Tianrui, Gao Linzhi, et al. Seismic sequence in carbonate rocks by vibrational liquefaction. Acta Geological Sinica, 1994, 68(1): 16～34]
[4]	乔秀夫,李海兵,高林志. 华北地台震旦纪-早古生代地震节律. 地学前缘,1997,4(3～4):155～160[ Qiao Xiufu, Li Haibing, Gao Linzhi. Sinian-early Paleozoic seismic rhythms on the north China platform. Earth Science Frontiers, 1997, 4(3～4): 155～160]
[5]	乔秀夫,高林志.华北中新元古代及早中生代地震灾变事件及与Rodinia的关系.科学通报,1999,44(16):1753～1758[Qiao Xiufu, Gao Linzhi. Earthquake events in Neoproterozoic and early Paleozoic and its relationship with supercontinental Rodinia in North China. Chinese Science Bulletin, 1999, 44(16): 1753～1758]
[6]	乔秀夫.中国震积岩的研究与展望.地质论评,1996,42(4):317～320[Qiao Xiufu. Study of seismites of China and its prospects. Geological Review, 1996, 42(4): 317～320]
[7]	梁定益,聂泽同,万晓樵.试论震积岩及震积不整合--以川西、滇西地区为例.现代地质,1991,5(2):138～147[Liang Dingyi, Nie Zetong, Wang Xiaoqiao. Onthe seismitesand seismodiconformity - take the W. Sichuan and W. Yunnan regions as an example. Geoscience, 1991, 5(2): 138～147]
[8]	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.地球科学,1994,19(6):845～850[Liang Dingyi, Nie Zetong, Song Zhimin. A restudy on seismitesand seismo-unconformity:Taking western Sichuan and western Yunnan as an example. Earth Science, 1994, 19(6): 845～850]
[9]	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.现代地质,1995,9(3):1～27[Sun Xiaomeng, Liang Dingyi, Nie Zetong.Seismitesequence in continental margin - Taking seismite in middle region of Jinsha river as an example. Geoscience, 1995, 9(3): 1～27]
[10]	杜远生,张传恒,韩欣.滇西地区中元古代大龙口组震积岩的新发现.沉积学报,1999,24(增刊):28～37[Du Yuansheng, Zhang Chuanheng, Han Xin. New discovery of seismites in Dalongkou group in Mid- Proterozoic in Dianxi. Acta Sedimentologica Sinica, 1996, 14 (Suppl.): 28～37]
[11]	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.沉积学报,1992,10(3):19～24[Wu Xaintao, Yin Guoxun. Discovery and significance of seismites of lake deposition of late Jurassicin Ermei in Sichuan. Acta Sedimentologica Sinica, 1992,10(3): 19～24]
[12]	南凌,崔之久.地震混杂岩(震积岩)的沉积特征和识别.地震地质译丛,1996,18(6):1～9[Nan Ling, Cui Zhijiu. Sedimentary characteristics and recognition of seismites. Seismology and GeologyVersions, 1996, 18(6): 1～9]
[13]	杜远生,韩欣.论震积作用和震积岩.地球科学进展,2000,(4):389～394[Du Yuansheng, Han Xin. Seismo-deposition and seismites. Advance in Earth Sciences, 2000,(4): 389～394]
[14]	Bauerman H.Report on the geology of the country near the forty-ninth parallel of north latitude west of the Rocky Mountains.Geological Survey of Canada Report(1882-83-84,pt.B),1985.1～42
[15]	Ian J Fairchild,Gerhard Einsele, Tianrui Song.Possible seismic origin of molar tooth structures in Neoproterozoic carbonate ramp deposits, north China. Sedimentology,1997,44: 611～636
[16]	Rossetti D F, Goes A M. Deciphering the sedimentologyical imprint of paleoseismic events: an example from the Aptian Codo formation,northern Brazil.Sedimentary Geology,2000,135: 137～156
[17]	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.中国科学(D辑), 2001,31(11):911～918[Qiao Xiufu, Gao linzhi, Peng Yang, et al. Seismic event, sequence and tectonic significance in Canglangpu Stage in Paleo-Tanlu Fault Zone. Science in China(Series D), 2001, 31(11): 911～918]
[18]	Brain R, Pratt. Oceangraphy, bathymetry and syndepositional tectonics of a Precambrianintracratonic basin:integrating sediments,storms,earthquakes and tsunamis in the belt supergroup Helena formation,ca. 1.45 Ga,western north America.Sedimentary Geology,2001,141～142: 371～394
[19]	Roep T B, Events A J. Pillow-beds: a new type of seismites? An examplefrom an Oligocene turbidite fan complex,Alicante. Sedimentology,1992,39: 711～724
[20]	杜远生,张传恒,韩欣.滇西中元古代昆阳群的地震事件沉积及其地质意义.中国科学(D辑),2001,31(4):284～290[Du Yuansheng, Zhang Chuanheng, Han Xin. Earthquake events deposition and geologic significance of Kunyang group in Mid-Proterozoicin Dianxi. Science in China(Series D), 2001, 31(4): 284～290]
[21]	Spallctta C,VailG B.Upper Devonian intraclast parabreccias interpreted as seismites. Marine Geology,1984,55(1～2):133～144
[22]	Rodriguez-Pascua M A, Calvo J P, De Vicente G, et al.Soft-sediment deformation structures interpreted as seismites in lacustrine sediments of the prebetic zone,SE Spain, and their potential use as indicators of earthquake magnitudes during the late Miocene.Sedimentary Geology,2000,135: 117～135
[23]	乔秀夫.中朝板块元古宙板内地震带与盆地格局.地学前缘,2002,9(3):141～149[Qiao Xiufu. Intraplate seismic belt and basin framework of Sino-Korean plate in Proterozoic. Earth Science Frontiers, 2002, 9(3): 141～149]

The Property and Geological Significance of Seismites of Paleogene in Huimin Sag,Shandong Province

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