应力事件与浊流沉积的时空关系
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摘要
地球系统科学针对不同的地质、构造、生物和气候现象开展综合研究,分析其内在机理的联系.结合当前国际地学前缘的发展态势,认为应力场和浊流沉积的综合研究将在揭示灾难性地质现象的控制机理、阐明油气资源的成因与分布的同时,为探讨地壳构造变化提供区域性指标.这些指标不仅指示地壳活动的阶段性,还将有助于恢复地幔-地壳-地貌-水流的系统演化历史.特别是深海浊流沉积的综合研究,可望成为“走向深海大洋”、开展深海地学综合研究的另一突破口.
The earth system science targets integrated research on different geological, structural, biological and climatic phenomena and analyzes their interrelationships. Judging from the current trend on international geoscience frontiers, we think an integrated approach for studying stress field and turbidity deposition will help discover the controlling mechanism of catastrophic geological events and illuminate the origin and distribution of oil and gas resources, and it may also provide some regional indices for investigating crustal and structural changes. These indices may not only reveal the stages in regional crustal activity, but also assist in reconstructing the evolutionary history of the mantle, crust, landscape and current systems. An integrated approach toward deep-sea turbidite research may likely become another breakthrough point in our earth system science maneuvers.
The earth system science targets integrated research on different geological, structural, biological and climatic phenomena and analyzes their interrelationships. Judging from the current trend on international geoscience frontiers, we think an integrated approach for studying stress field and turbidity deposition will help discover the controlling mechanism of catastrophic geological events and illuminate the origin and distribution of oil and gas resources, and it may also provide some regional indices for investigating crustal and structural changes. These indices may not only reveal the stages in regional crustal activity, but also assist in reconstructing the evolutionary history of the mantle, crust, landscape and current systems. An integrated approach toward deep-sea turbidite research may likely become another breakthrough point in our earth system science maneuvers.
引文
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[6] Lin J,Stein RS.Stresstriggeringinthrust andsubduction earth-quakes and stress interaction between the southern San Andreas and nearby thrust and strike-slip faults[J].Journal of Geophysi-cal Research,2004,109:B02303,doi:10.1029/2003JB002607.
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[10] 杨树新,陈连旺,谢富仁.中国大陆现今构造应力场的回归分析研究[J].岩土力学,2003,24(增刊):357-360.YANG Shu-xin,CHEN Lian-wang,XIE Fu-ren.Astudy of re-gression analysis and numerical si mulation on modern tec-stress fieldin China mainland[J].Rock and Soil Mechanics,2003,24(Supp):357-360.
[11] I manishi Y,Sato T,Higashi T,et al.A network of supercon-ducting gravi meters detects submicrogal coseismic gravity changes[J].Science,2004,306:476-478.
[12] Adams J.Great earthquakes recorded byturbidites off the Wash-ington-Oregon coast.Assessing earthquake hazards and reducing risk in the Pacific Northwest[J].USGS Professional Paper1560,1996,1:147-158.
[13] Tr啨hu A M,Bohrmann G,Rack F R,et al.Proc.ODPinitial re-ports,ocean drilling program,2003,204[EB/OL].http://www-odp.tamu.edu,2005-04-20.
[14] Floyd J S,Tolstoy M,Mutter J C,et al.Seismotectonics of mid-ocean ridge propagation in Hess Deep[J].Science,2002,298:1765-1768.
[15] Kuenen P H,Migliorini C I.Turbidity currents as a cause of graded bedding[J].Journal of Geology,1950,58:41-127.
[16] Kelling G.Flysch trough to lowstand fan:A history of turbidite architecture,with special reference to Turkish basins[R].[s.l.]:ISPARTA,2001.
[17] Shanmugam G.49years of the turbidite paradigm(1950s-1990s):Deep-water processes and facies models—Acritical perspective[J].Marine and Petroleum Geology,2000,17:285-342.
[18] Walker R G.Deep-water sandstonefacies andancient submarinefans:Modelsfor exploration for stratigraphic traps[J].American Associa-tion of Petroleum Geologists Bulletin,1978,51:821-855.
[19] Lomas S A,Joseph P.Confined turbidite systems[M].London:Special Publication,2004.
[20] 郭成贤.我国深水异地沉积研究三十年[J].古地理学报,2000,2:1-10.GUO Cheng-xian.The thirty-year study of deep-water allogene de-positsin China[J].Journal of Palaeogeography,2000,2:1-10.
[21] 饶孟余,钟建华,赵志根,等.浊流沉积研究综述和展望[J].煤田地质与勘探,2004,32:1-5.RAO Meng-yu,ZHONG Jian-hua,ZHAO Zhi-gen,et al.Overview and prospect on study of turbidity deposits[J].Coal Geology&Ex-ploration,2004,32:1-5.
[22] 李巍然,管玉涛,杨作升,等.冲绳海槽浊流灾害性研究[J].自然灾害学报,1999,8:98-102.LI Wei-ran,GUAN Yu-tao,YANG Zuo-sheng,et al.Study on hazardous characteristics of turbidflowin Okinawa Through[J].Journal of Natural Disasters,1999,8:98-102.
[23] 高红芳,白志琳.南海笔架南盆地沉积和构造研究[J].中国海上油气(地质),2002,16:245-249.GAO Hong-fang,BAI Zhi-lin.Astudy on sedi mentation and tec-tonics in Bijia’nan Basin,South China Sea[J].China Offshore Oil and Gas(Geology),2002,16:245-249.
[24] 吴时国,张光学,郭常升,等.东沙海区天然气水合物形成及分布的地质因素[J].石油学报,2004,25:7-12.WUShi-guo,ZHANG Guang-xue,GUO Chang-sheng,et al.Ge-ological constraint onthe distribution of gas hydrateinthe Dong-sha continental slope of South China Sea[J].Acta PetrolEi Sini-ca,2004,25:7-12.
[25] Shanmugam G.Ten turbidite myths[J].Earth-Science Reviews,2002,58:311-341.
[26] Gani M R.Fromturbid to lucid:Astraightforward approach to sedi ment gravity flows and their deposits[J].The Sedi mentary Record,2004,2(3):4-8.
[27] Bouma A H.Coarse-grained andfine-grainedturbidite systems as end member models:Applicability and dangers[J].Marine and Petroleum Geology,2000,17:137-143.
[28] Bouma A H,Stone C G.Fine-grained turbidite systems[J].AAPG Memoir,2000,72:1-342.
[29] Bruhn C HL.Contrastingtypes of Oligocene/Miocene,giant tur-bidite reservoirs from deep water Campos Basin,Brazil.AAPG Distinguished Lecture Program2001[EB/OL].http://www.aapg.org/education/dist_lect/slides/2001_02/bruhn_abs.html,2005-04-20.
[30] Santos R A,Lopes MR F,Cor偄C A G,et al.Adaptive visualiza-tion of deepwater turbidite systems in Campos Basin using3-D seismic[J].The Leading Edge,2000,19:512-517.
[31] Stow D A,Mayall M.Deep-water sedi mentary systems:New models for the21st century[J].Marine and Petroleum Geology,2000,17:125-135.
[2] 中国科学院地学部“中国地球科学发展战略”研究组.地球科学:世纪之交的回顾与展望[M].济南:山东教育出版社,2002.Chinese Academy of Sciences Division of Geology.Earthscience:Areviewand prospect at the turn of the century[M].Qingdao:Shangdong Education Press,2002.
[3] 汪品先.我国的地球系统科学研究向何处去?[J].地球科学进展,2003,18:837-851.WANG Pin-xian.Earthsystemsciencein China quo vadis?[J].Advance in Earth Sciences,2003,18:837-851.
[4] 天 戈.谁能阻止小行星撞击地球?[M].北京:当代世界出版社,2004.TIAN Ge.Who can stop the earth collisioned by planet?[M].Beijing:Current World Press,2004.
[5] Berger WH,von Rad U.Decadal to millennial cyclicityin varves and turbidites fromthe Arabian Sea:Hypothesis of tidal origin[J].Global and Planetary Change,2002,34:313-325.
[6] Lin J,Stein RS.Stresstriggeringinthrust andsubduction earth-quakes and stress interaction between the southern San Andreas and nearby thrust and strike-slip faults[J].Journal of Geophysi-cal Research,2004,109:B02303,doi:10.1029/2003JB002607.
[7] Reinecker J,Heidbach O,Tingay M,et al.The2004release of the World Stress Map[EB/OL].http://www.world-stress-map.org,2005-04-20.
[8] 谢富仁,崔效锋,赵建涛.全球应力场与构造分析[J].地学前缘,2003,10:22-30.XIE Fu-ren,CUI Xiao-feng,ZHAOJian-tao.Analysis of global tec-tonic stress field[J].Earth Science Frontiers,2003,10:22-30.
[9] 谢富仁,崔效锋,赵建涛,等.中国大陆及邻区现代构造应力场分区[J].地球物理学报,2004,47:654-662.XIE Fu-ren,CUI Xiao-feng,ZHAOJian-tao,et al.Regional divi-sion of the recent tectonic stress fieldin China and adjacent areas[J].Chinese Journal of Geophysics,2004,47:654-662.
[10] 杨树新,陈连旺,谢富仁.中国大陆现今构造应力场的回归分析研究[J].岩土力学,2003,24(增刊):357-360.YANG Shu-xin,CHEN Lian-wang,XIE Fu-ren.Astudy of re-gression analysis and numerical si mulation on modern tec-stress fieldin China mainland[J].Rock and Soil Mechanics,2003,24(Supp):357-360.
[11] I manishi Y,Sato T,Higashi T,et al.A network of supercon-ducting gravi meters detects submicrogal coseismic gravity changes[J].Science,2004,306:476-478.
[12] Adams J.Great earthquakes recorded byturbidites off the Wash-ington-Oregon coast.Assessing earthquake hazards and reducing risk in the Pacific Northwest[J].USGS Professional Paper1560,1996,1:147-158.
[13] Tr啨hu A M,Bohrmann G,Rack F R,et al.Proc.ODPinitial re-ports,ocean drilling program,2003,204[EB/OL].http://www-odp.tamu.edu,2005-04-20.
[14] Floyd J S,Tolstoy M,Mutter J C,et al.Seismotectonics of mid-ocean ridge propagation in Hess Deep[J].Science,2002,298:1765-1768.
[15] Kuenen P H,Migliorini C I.Turbidity currents as a cause of graded bedding[J].Journal of Geology,1950,58:41-127.
[16] Kelling G.Flysch trough to lowstand fan:A history of turbidite architecture,with special reference to Turkish basins[R].[s.l.]:ISPARTA,2001.
[17] Shanmugam G.49years of the turbidite paradigm(1950s-1990s):Deep-water processes and facies models—Acritical perspective[J].Marine and Petroleum Geology,2000,17:285-342.
[18] Walker R G.Deep-water sandstonefacies andancient submarinefans:Modelsfor exploration for stratigraphic traps[J].American Associa-tion of Petroleum Geologists Bulletin,1978,51:821-855.
[19] Lomas S A,Joseph P.Confined turbidite systems[M].London:Special Publication,2004.
[20] 郭成贤.我国深水异地沉积研究三十年[J].古地理学报,2000,2:1-10.GUO Cheng-xian.The thirty-year study of deep-water allogene de-positsin China[J].Journal of Palaeogeography,2000,2:1-10.
[21] 饶孟余,钟建华,赵志根,等.浊流沉积研究综述和展望[J].煤田地质与勘探,2004,32:1-5.RAO Meng-yu,ZHONG Jian-hua,ZHAO Zhi-gen,et al.Overview and prospect on study of turbidity deposits[J].Coal Geology&Ex-ploration,2004,32:1-5.
[22] 李巍然,管玉涛,杨作升,等.冲绳海槽浊流灾害性研究[J].自然灾害学报,1999,8:98-102.LI Wei-ran,GUAN Yu-tao,YANG Zuo-sheng,et al.Study on hazardous characteristics of turbidflowin Okinawa Through[J].Journal of Natural Disasters,1999,8:98-102.
[23] 高红芳,白志琳.南海笔架南盆地沉积和构造研究[J].中国海上油气(地质),2002,16:245-249.GAO Hong-fang,BAI Zhi-lin.Astudy on sedi mentation and tec-tonics in Bijia’nan Basin,South China Sea[J].China Offshore Oil and Gas(Geology),2002,16:245-249.
[24] 吴时国,张光学,郭常升,等.东沙海区天然气水合物形成及分布的地质因素[J].石油学报,2004,25:7-12.WUShi-guo,ZHANG Guang-xue,GUO Chang-sheng,et al.Ge-ological constraint onthe distribution of gas hydrateinthe Dong-sha continental slope of South China Sea[J].Acta PetrolEi Sini-ca,2004,25:7-12.
[25] Shanmugam G.Ten turbidite myths[J].Earth-Science Reviews,2002,58:311-341.
[26] Gani M R.Fromturbid to lucid:Astraightforward approach to sedi ment gravity flows and their deposits[J].The Sedi mentary Record,2004,2(3):4-8.
[27] Bouma A H.Coarse-grained andfine-grainedturbidite systems as end member models:Applicability and dangers[J].Marine and Petroleum Geology,2000,17:137-143.
[28] Bouma A H,Stone C G.Fine-grained turbidite systems[J].AAPG Memoir,2000,72:1-342.
[29] Bruhn C HL.Contrastingtypes of Oligocene/Miocene,giant tur-bidite reservoirs from deep water Campos Basin,Brazil.AAPG Distinguished Lecture Program2001[EB/OL].http://www.aapg.org/education/dist_lect/slides/2001_02/bruhn_abs.html,2005-04-20.
[30] Santos R A,Lopes MR F,Cor偄C A G,et al.Adaptive visualiza-tion of deepwater turbidite systems in Campos Basin using3-D seismic[J].The Leading Edge,2000,19:512-517.
[31] Stow D A,Mayall M.Deep-water sedi mentary systems:New models for the21st century[J].Marine and Petroleum Geology,2000,17:125-135.
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