四川盆地东南部早三叠世地震事件沉积及其地质意义
|
摘要
四川盆地南部及东南部下三叠统飞仙关组和嘉陵江组中常发育有一系列宏观及微观的软沉积物变形、震积角砾岩块、板状砾屑、层内微断层等特殊的地震成因沉积构造。飞仙关组震积岩在重庆北碚白庙子剖面飞仙关组第一、二段中产出,嘉陵江组震积岩产于四川叙永龙洞湾嘉陵江组第二段及四川兴文、贵州习水等地的相同层位中,其沉积序列明显,反映了古地震从开始至平静的全过程。作者认为,早三叠世时,上扬子板块西缘以川西义敦弧的演化为代表的三江构造带活动强烈,可能与四川盆地早三叠世震积岩的形成有联系,随着三江构造带板块碰撞、洋壳俯冲消减,能在较大区域内引发地震活动、火山喷发。
The seismites emerge in the first and sencond members of Lower Triassic Feixianguan Fm.in Baimiaozi section,Beibei,Chongqing,China and in the second member of Lower Triassic Jialingjiang Fm.in Longdongwan,Xuyong county,the southern Sichuan province,China,as well as in the same stratigraphic sequences in Xingwen county,Sichuan province and Xishui county,Guizhou province. There are some macroscopic and microscopic sedimentary structures of seismic events in the outcrops,drilling cores and thin sections including the following basic types could be observed: Soft-sediment liquefied deformation structures include curled deformation(sliding deformation structure,"sausage structure") and microscopic folds(laminated plastic deformation).In the first member of Feixianguan Fm.at Beibei,Chongqing.Microscopic folds(lamina plastic deformation) are found in the second member of Feixianguan Fm.at Longdongwan,and microscopic folds emerge in laminated thin-layer limestone,presenting slight folds in laminated thin-layer limestone and their low radian with undulation.In addition to study areas,some soft-sediment deformation structures such as convolute beddings,microscopic folds and so on are developed in the first member of Feixianguan Fm.at Jichang,Xuanhan county,Sichuan province,China,and may be related to paleoearthquake activities. The tabular-pebbles with different-size diameters are developed in the lower part of the second member of Feixianguan Fm.,interbedded with laminated thin-layer micritic limestone of normal sequences.The sedimentary characteristics of tabular gravel layers are also comparable with those in the second member of Feixianguan Fm.at Beibei,Chongqing. The gravels are developed with different size,shape and psephicitie in the first member of Feixianguan Fm.in Baimiaozi,Beibei Chongqing,and the second member of Jialingjiang Fm.in Longdongwan,Xuyong,Sichuan province,the shape being irregular mass,nearly spherical or tabular,the size ranging from 0.5 to 25cm,the lithology being grey or grey white thick-bedding massive micrite,some of which have certain psephicities. The intraformational microscopic faults are developed in the first and second member of Feixianguan Fm.at Beibei,Chongqing,they are limited to develop intraformationally,and don't cut through the upper and lower beds with short slip of fault and slow angle of fault plane. Some well-developed microscopic seismites can also be discovered in some thin sections of the second member of Jialingjiang Fm.at Longdongwan,Xuyong county,and Jianshe,Dali,Chengdong,Wenxin county,Sichuan province,Huangmuping,Xishui county,Guizhou province,including the following basic types:microscopic liquefied curled deformation structure;microscopic tabular-pebbles layer;microscopic slip and microscopic flame structure. Seismites developed in the lower Triassic in Sichuan Basin have not only wide transverse distribution,but also are distributed longitudinally.Some seismites with volcanic debris sediments of Early Triassic have been found in other places of Sichuan basin besides research area.The author argues that the Sanjiang tectonic belt represented by the evolution of Yidun arc in the western Sichuan had strong activities at the west margin of the upper Yangtze plate,which may be related to the formation of seismites in the early Triassic.At the west margin of the upper Yangtze plate,the strongest tectonic deformation and metamorphism occurred in the early Triassic emerge between YiDui arc and Qiangtang mass,representing the subduction of the Paleo-Tethys.Magmatic and volcanic activities occur when the paleo-Tethyan oceanic crust subducts eastward along Litangbatang volcanic arc and westward along Jinsha River suture zone.In the early Triassic,seismic activities and volcanic eruption can be triggered in large areas with plate collision and ocean crust subduction.The author speculates that Yidui arc is the major cause of formation of seismites in Sichuan Basin that emerge in the early Triassic.
The seismites emerge in the first and sencond members of Lower Triassic Feixianguan Fm.in Baimiaozi section,Beibei,Chongqing,China and in the second member of Lower Triassic Jialingjiang Fm.in Longdongwan,Xuyong county,the southern Sichuan province,China,as well as in the same stratigraphic sequences in Xingwen county,Sichuan province and Xishui county,Guizhou province. There are some macroscopic and microscopic sedimentary structures of seismic events in the outcrops,drilling cores and thin sections including the following basic types could be observed: Soft-sediment liquefied deformation structures include curled deformation(sliding deformation structure,"sausage structure") and microscopic folds(laminated plastic deformation).In the first member of Feixianguan Fm.at Beibei,Chongqing.Microscopic folds(lamina plastic deformation) are found in the second member of Feixianguan Fm.at Longdongwan,and microscopic folds emerge in laminated thin-layer limestone,presenting slight folds in laminated thin-layer limestone and their low radian with undulation.In addition to study areas,some soft-sediment deformation structures such as convolute beddings,microscopic folds and so on are developed in the first member of Feixianguan Fm.at Jichang,Xuanhan county,Sichuan province,China,and may be related to paleoearthquake activities. The tabular-pebbles with different-size diameters are developed in the lower part of the second member of Feixianguan Fm.,interbedded with laminated thin-layer micritic limestone of normal sequences.The sedimentary characteristics of tabular gravel layers are also comparable with those in the second member of Feixianguan Fm.at Beibei,Chongqing. The gravels are developed with different size,shape and psephicitie in the first member of Feixianguan Fm.in Baimiaozi,Beibei Chongqing,and the second member of Jialingjiang Fm.in Longdongwan,Xuyong,Sichuan province,the shape being irregular mass,nearly spherical or tabular,the size ranging from 0.5 to 25cm,the lithology being grey or grey white thick-bedding massive micrite,some of which have certain psephicities. The intraformational microscopic faults are developed in the first and second member of Feixianguan Fm.at Beibei,Chongqing,they are limited to develop intraformationally,and don't cut through the upper and lower beds with short slip of fault and slow angle of fault plane. Some well-developed microscopic seismites can also be discovered in some thin sections of the second member of Jialingjiang Fm.at Longdongwan,Xuyong county,and Jianshe,Dali,Chengdong,Wenxin county,Sichuan province,Huangmuping,Xishui county,Guizhou province,including the following basic types:microscopic liquefied curled deformation structure;microscopic tabular-pebbles layer;microscopic slip and microscopic flame structure. Seismites developed in the lower Triassic in Sichuan Basin have not only wide transverse distribution,but also are distributed longitudinally.Some seismites with volcanic debris sediments of Early Triassic have been found in other places of Sichuan basin besides research area.The author argues that the Sanjiang tectonic belt represented by the evolution of Yidun arc in the western Sichuan had strong activities at the west margin of the upper Yangtze plate,which may be related to the formation of seismites in the early Triassic.At the west margin of the upper Yangtze plate,the strongest tectonic deformation and metamorphism occurred in the early Triassic emerge between YiDui arc and Qiangtang mass,representing the subduction of the Paleo-Tethys.Magmatic and volcanic activities occur when the paleo-Tethyan oceanic crust subducts eastward along Litangbatang volcanic arc and westward along Jinsha River suture zone.In the early Triassic,seismic activities and volcanic eruption can be triggered in large areas with plate collision and ocean crust subduction.The author speculates that Yidui arc is the major cause of formation of seismites in Sichuan Basin that emerge in the early Triassic.
引文
1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[Nan Ling,Cui Zhijiu.Sedimentarycharacteristics and recognition of seismites[J].Seismology and GeologyVersions,1996,18(6):1-9]
2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[Zhou Xiaodong,Chen Yuejun.The Late Sinianseismic depositional rock characteristics in the southern part of Jilinprovince[J].Jilin Geology,1998,17(4):24-28]
3乔秀夫,高林志.华北中新元古代及早古生代地震灾变事件及与Rodinia的关系[J].科学通报,1999,44(16):1753-1758[Qiao Xi-ufu,Gao Linzhi.Earthquake events in Neoproterozoic and Early Paleo-zoic and its relationship with supercontinental Rodinia in north China[J].Chinese Science Bulletin,1999,44(16):1753-1758]
4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[J].沉积学报,1999,24(增刊):28-37[Du Yuansheng,ZhangChuanheng,Han Xin.New Discovery of seismites in Dalongkou Groupin Mid-Proterozoic in Dianxi[J].Acta Sedimentologica Sinica,1996,24(Supp l.):28-37]
5郭胜哲,张立东,张长捷,等.辽宁太子河流域晚元古宙青白口系震积岩的发现及其意义[J].中国区域地质,1999,18(1):106-109[Guo Shengzhe,Zhang Lidong,Zhang Changjie,et al.Seismitesof the Late Proterozoic Qingbaikou System in the Taizi River Valley ofLiaoning[J].Regional Geology of China,1999,18(1):106-109]
6杜远生,张传恒,韩欣,等.滇中中元古代昆阳群的地震事件沉积及其地质意义[J].中国科学:D辑,2001.31(4):283-289[DuYuansheng,Zhang Chuanheng,Han Xin,et al.Mesoproterozoic seis-mic event deposit and its geological significance in Kunyang Group,Central Yunnan[J].Science in China:Series D,2001,31(4):283-289]
7乔秀夫,宋天锐,李海兵.是地震液化泄水成因,不是“渗流管”构造[J].科学通报,2002,47(14):1118-1120[Qiao Xiufu,Song Tian-rui,Li Haibing.Being generated by earthquake liquefaction,not being“seep tube"structure[J].Chinese Science Bulletin,2002,47(14):1118-1120]
8曹国强,陈世悦,鄢继华,等.济阳坳陷早第三纪地震事件沉积序列[J].地质找矿论丛,2004:19(4):252-256[Cao Guoqiang,Chen Shiyue,Yan Jihua,et al.The Early Tertiary sedimentary se-quence of earthquake events in Jiyang Depression[J].Geology Explo-ration Commention,2004,19(4):252-256]
9严兆彬,郭福生,彭花明,等.浙西寒武系大陈岭组地震事件沉积的初步研究[J].地质学报,2005,79(6):730-736[Yan Zaobin,Guo Fusheng,Peng Huaming,et al.Polot study on sedimentation ofCambrian Dachenling Formation resulting from seismic events in thewest of Zhejiang Province[J].Acta Geologica Sinica,2005,79(6):730-736]
10赵卫卫,查明,杨剑萍.中国震积岩研究综述[J].地层学杂志,2006,30(2):171-176[Zhao Weiwei,Zha Ming,Yang Jianping.An overview of seismite research in China[J].Journal of Stratigra-phy,2006,30(2):171-176]
11梁定益,聂泽同,万晓樵,等.试论震积岩与震积不整合——以川西、滇西地区为例[J].现代地质,1991,5(2):138-146[LiangDingyi,Nie Zetong,Wan Xiaoqiao,et al.On the seismite and seis-mic disconformity:take the western Sichuan and western Yunnan re-gions as an example[J].Geoscience,1991,5(2):138-146]
12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——中国地质大学学报,1994,19(6):845-850[Liang Dingyi,Nie Zetong.Song Zhimin.A re-study on seismite and seismo-unconformity:taking western Sichuanand western Yunnan as an example[J].Earth Science.1994,19(6):845-850]
13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(3):19-26[Wu Xiantao,YinGuoxun.Discovery and significance of seismites of lake deposition ofLate Jurassic in Emei in Sichuan[J].Acta Sedimentologica Sinica,1992,10(3):19-26]
14杨国美.重庆北碚地区下三叠统飞仙关组沉积相的基本特征[J].西南石油学院学报,1987,9(2):1-14[Yan Guomei.Funda-mental characteristics of sedimentary facies of Feixianguan Formationin Lower Triassic System,Beibei Area,Ghongqing City,SichuanProvince[J].Journal of Southwest Petroleum Institute,1987,9(2):1-14]
15蒋武.重庆北碚地区上二叠--下三叠统牙形刺及油气意义[J].西南石油学院学报,1982,4(1):12-24[Jiang Wu.Upper Permi-an-Lower Triassic Conodonts in Chongqing-Beibei Area and their sig-nificance in exploring oil and gas[J].Journal of Southwest PetroleumInstitute,1982,4(1):12-24]
16 Seilacher A.Sedimentary structures tentatively attributed to seismic e-vents[J].Marine Geology,1984,55(1-2):1-12
17 Lowes D R.Subaqueous liquefied and fluidized flows and their depos-its[J].Sedimentology,1976,23(3):285-308
18 Rodriguez-Pascua M A,et al.Soft-sediment deformation structures in-terpreted as seismites in lacustrine sediments of the prebetic zone,SESpain and their potential use as indicators of earthquake magnitudesduring the late Miocene[J].Sedimentary Geology,2000,135:117-135
19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,1988,38(8):609-611[Song Tian-rui.A set of possible earthquake-tsunami sequence in PrecambrianCarbonate,Shisanling,Beijing[J].Chinese Science Bulletin,1988,33(8):609-611]
20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[Qiao Xiufu,Song Tianrui,Gao Linzhi,et al.Seismic sequence in carbonate rocks by vibrational liquefaction[J].Acta Geologica Sinica,1994,68(1):16-32]
21乔秀夫.中国震积岩的研究与展望[J].地质论评,1996,42(4):317-320[Qiao Xiufu.Study of seismites of China and its pros-pects[J].Geological Review,1996,42(4):317-320]
22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[Du Yuansheng,Han Xin.Tsunami and tsunamites[J].Geological Science and Technology Information,2000,19(1):19-22]
23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[Du Yuansheng,Han Xin.Seismo-deposition andseismites[J].Advance on Earth Science,2000,15(4):389-394]
24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[Song Tianrui,Liu Yanxue.Ancient earth-quake records and litho-paleogeography[J].Acta SedimentologicaSinica,2009,27(5):872-879]
25王一刚,文应初,洪海涛,等.四川盆地北部晚二叠世———早三叠世碳酸盐岩斜坡相带沉积特征[J].古地理学报,2009,11(2):143-156[Wang Yigang,Wen Yingchu,Hong Haitao,et al.Carbonate slope fades sedimentary characteristics of the Late Permianto Early Triassic in Northern Sichuan Basin[J].Journal of Palaeo-geography,2009,11(2):143-156]
26杜远生,Shi G R,龚一鸣,等.东澳大利亚南悉尼盆地二叠系与地震沉积有关的软沉积变形构造[J].地质学报,2007,81(4):511-518[Du Yuansheng,Guang R Shi,Gong Yinming,et al.Permi-an soft-sediment deformation structures related to earthquake in theSouthern Sydney Basin,Eastern Australia[J].Acta Geologica Sinica2007,81(4):511-518]
27 Elliot C G,Williams P F.Sediment slump structures:a review of di-agnostic criteria and application to an example from Newfoundland[J].Journal of Structural Geology,1988,(10):171-182
28 Morton R A.Nearshore responses to great storm[C]∥Clifton H E,ed.Sedimentary Consequences of Convulsive Geologic Events[J].Ge-ological Society of America Special Paper 229,1988:222
29 Field M E,Gardner J V,Jennings A E,et al.Earthquake inducedsediment failures on a 0.25 slope,Klamath River Delta,California[J].Geology,1982(10):542-546
30 Vaughan N D,Johnson T C,Meams D L,et al.The impact of hurri-cane Diana on the North Carolina continental shelf[J].Marine Geolo-gy,1987(76):169-176
31 Boss S K,Neumann A C.Impacts of hurricane Andrew on carbonateplatform environments,northern Great Bahama Bank[J].Geology,1993,(21):897-900
32 Shinn E A,Steinen R P,Dill R F,et al.Lime-mud layers in high-energy tidal channels:A record of hurricane deposition[J].Geology,1993(21):603-606
33 Guiraud M,Plaziat J C.Seismites in the fluviatile Bima sandstones:identification of Paleoseisms and discussion of their magnitudes in aCretaceous synsedimentary strike-slip basin(Upper Benue,Nigeria)[J].Tectonophysicis,1993(225):493-522
34 Obermeier S F.Use of liquefaction-induced features for paleo-seismicanalysis-An overview of how seismic liquefaction features can be dis-tinguished from other features and how their regional distribution andproperties of source sediment can be used to infer the location andstrength of Holocene paleo-earthquakes[J].Engineering Geology,1996,44(1-4):1-74
35 Pope M C,Read J F,Bambach R,et al.Late Middle to Late Ordivi-cian seismites of Kentucky,southwest Ohio and Virginia:sedimentaryrecorders of earthquakes in the Appalachian basin[J].GSA Bulletin,1997,109(4):489-503
36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,2007,37(3):336-343[Zhang Chuanheng,Wu Zhenjie,Gao Linzhi,et al.Meso-proterozoic earthquake induced soft-sediment deformation and itsgeological significance in Wumishan Formation,North China[J].Sci-ence in China:Series D,2007,37(3):336-343]
37 Ettensohn F R,Rast N,Kulp M A.Locating possible epicentral areasfor paleoearthquakes,middle Ordovician Lexington Limestone,centralKentucky[J].Geological Society of American Abstract Program,2000,32:A215
38 Moretti M.Soft-sediment deformation structures interpreted as seis-mites in middle-late Pleistocene Aeolian deposits(Apulian foreland,Southern Italy)[J].Sedimentary Geology,2000,135(1-4):167-179
39 John Houston,Dan Hart,Andrew Houston.Neogene sedimentary de-formation in the Chilean forearc and implication for Andean basin de-velopment,seismicity and uplift[J].Journal of the Geological Socie-ty,London,2008,165:291-306
40廖太平胡明主编,重庆天府地区地质考察指南[M].北京:石油工业出版社,2008[Liao Taiping,Hu Ming,ed.Geological FieldTrip Guide in Tianfu Area,Chongqing City[M].Beijing:PetroleumIndustry Press,2008]
41 Brian R Pratt.Storms versus tsunamis:Dynamic interplay of sedimen-tary,diagenetic,and tectonic processes in the Cambrian of Montana[J].Geology,2002,30(5):423-426
42罗冰,谭秀成,刘宏,等.川东地区飞一段震积岩的发现及识别标志[J].沉积学报,2009,27(5):1012-1017[Luo Bing,Tan Xi-ucheng,Liu Hong,et al.Discovery and recognition marks of seismiteof the Fei 1 Member in the eastern Sichuan Basin[J].Acta Sedimen-tologica Sinica,2009,27(5):1012-1017]
43 Shanmugam G.The tsunamite problem[J].Journal of SedimentaryResearch,2006,(76):718-730
44杜远生,彭冰霞,韩欣.广西北海涠洲岛晚更新世火山活动引起的地震同沉积变形构造[J].沉积学报,2005,23(2):203-209[Du Yuesheng,Peng Bingxia,Han Xin.Syn-depositional deforma-tion structures by earthquake related to volcanic activity of the LatePleistocene in Weizhou Island,Beihai City Guangxi[J].Acta Sedim-entologica Sinica,2005,23(2):203-209]
45 Simms M J.Uniquely extensive seismite from the latest Triassic King-dom:Evidence for bolide impact?[J].Geology,2003(31):557 560
46刘志成,张廷山,魏祥峰.四川盆地南部赤水地区下三叠统嘉陵江组遗迹化石及其沉积环境[J].海相油气地质.2009,14(1):46-50[Liu Zhicheng,Zhang Tingshan,Wei Xiangfeng.Ichnofossilsand sedimentary environment of Lower Triassic Jialingjiang Formationin Chishui Area,southern part of Sichuan Basin[J].Marine OriginPetroleum Geology,2009,14(1):46-50]
47李忠权,冉隆辉,陈更生,等.川东高陡构造成因地质模式与含气性分析[J].成都理工学院学报,2002,29(6):605-609[LiZhongquan,Ran Longhui,Ghen Gengsheng,et al.Geologic modeland gaseous analyses about the origin of high-steep structures in east-ern Sichuan Basin[J].Journal of Chengdu University of Technology,2002,29(6):605-609]
48吕宝凤,夏斌.川东南“隔档式构造”的重新认识[J].天然气地球科学,2005,16(3):278-282[LüBaofeng,Xia Bin.New knowl-edge about ejective structure in Southeast Sichuan[J].Nature GasGeoscience,2005,16(3):278-282]
49许志琴,李化启,侯立炜,等.青藏高原东缘龙门—锦屏造山带的崛起———大型拆离断层和挤出机制[J].地质通报,2007,26(10):1262-1276[Xu Zhiqin,Li Huaqi,Hou Liwei,et al.Uplift ofthe Longmen-Jinping Orogenic Belt along the eastern margin of theQinghai-Tibet Plateau:large-scale detachment faulting and extrusionmechanism[J].Geological Bulletin of China,2007,26(10):1262-1276]
50邹光富,侯立玮,尹显科.甘孜—理塘蛇绿混杂岩带特征及其构造意义[J].四川地质学报,1994,14(1):17-24[Zou Guangfu,Hou Liwei,Yin Xianke.Characteristics of Garze-Litang ophiolite me-lange zone and its tectonic implication[J].Acta Geologica Sichuan,1994,14(1):17-24]
51邹光富.甘孜—理塘板块缝合带研究的新进展[J].四川地质学报,1995,15(4):257-263[Zou Guangfu.Advance of the researchon the Garze-Litang plate junction[J].Acta Geologica Sichuan,1995,15(4):257-263]
52姚学良,兰艳.甘孜—理塘蛇绿混杂岩带存在N型洋脊玄武岩[J].四川地质学报,2001,21(3):138-140[Yao Xueliang andLan Yan.N-type oceanic ridge basalt in the Garge-Litang ophiolitemelange zone[J].Acta Geologica Sichuan,2001,21(3):138-140]
53杨宗让.川西松潘-甘孜弧前盆地的形成及演化[J].沉积与特提斯地质,2002,22(3):53-59[Yang Zongrang.The formation and e-volution of the Songpan-Garze fore-arc basin,western Sichuan[J].Sedimentary Geology and Tethyan Geology,2002,22(3):53-59]
54 Franoise Roger,Marc Jolivet,Jacques Malavieille.Tectonic evolu-tion of the Triassic fold belts of Tibet[J].Geoscience,2008,(340):180-189
55魏永峰,罗森林,周幼云,等.甘孜—理塘结合带中段蛇绿岩中石榴硅镁石角闪片岩首次发现及地质意义[J].四川地质学报,2004,24(1):1-3[Wei Yongfeng,Luo Senlin,Zhou Youyun,et al.Discovery of garnet-humite-hornblende schist in ophiolite suite and itsgeological significance in the Garzê-Litang suture zone[J].Acta Geo-logica Sichuan,2004,24(1):1-3]
56王清晨.浅议华南陆块群的沉积大地构造学问题[J].沉积学报,2009,27(5):811-817[Wang Qingchen.Preliminary discussion onsedimentary tectonics of the clustered continents of South China[J].Acta Sedimentologica Sinica,2009,27(5):811-817]
57 Anthony J Reid,Christopher J L,Wilsona,Shun Liu.Structural evi-dence for the Permo-Triassic tectonic evolution of the Yidun Arc,east-ern Tibetan Plateau[J].Journal of Structural Geology,2005,27:119-137
58 Anthony J Reid,Christopher J L Wilson,Shun Liu,et al.Mesozoicplutons of the Yidun Arc,SW China:U/Pb geochronology and Hf iso-topic signature[J].Ore Geology Reviews,2007,31:88-106
59曲晓明,侯增谦,唐绍华.义敦岛弧带弧后区板内岩浆作用的时代及意义[J].岩石矿物学杂志,2003,22(2):131-137[Qu Xi-aoming,Hou Zengqian and Tang Shaohua.Age of intraplate volcan-ism in the back-arc area of Yidun island arc and its significance[J].Acta Petrologica et Mineralogica,2003,22(2):131-137]
60戴宗明,孙传敏.松潘-甘孜造山带义敦岛弧中段三叠纪火山-沉积盆地的演化[J].地质通报,2008,27(6):799-813[Dai Zong-ming,Sun Chuanmin.Evolution of Triassic volcanic-sedimentary ba-sins in the central segment of the Yidun island arc of the Songpan-Garzêorogenic belt,Western Sichuan,China[J].Geological Bulletinof China,2008,27(6):799-813]
61刘飞,陈岳龙,苏本勋,等.松潘—甘孜地区三叠系碎屑沉积岩地球化学特征及其锆石年龄研究[J].地球学报,2006,27(4):289-296[Liu Fei,Chen Yuelong,Su Benxun,et al.Geochemistryand zircon ages of Triassic detrital sedimentary rocks from the Ganze-Songpan block[J].Acta Geoscientica Sinica,2006,27(4):289-296]
2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[Zhou Xiaodong,Chen Yuejun.The Late Sinianseismic depositional rock characteristics in the southern part of Jilinprovince[J].Jilin Geology,1998,17(4):24-28]
3乔秀夫,高林志.华北中新元古代及早古生代地震灾变事件及与Rodinia的关系[J].科学通报,1999,44(16):1753-1758[Qiao Xi-ufu,Gao Linzhi.Earthquake events in Neoproterozoic and Early Paleo-zoic and its relationship with supercontinental Rodinia in north China[J].Chinese Science Bulletin,1999,44(16):1753-1758]
4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[J].沉积学报,1999,24(增刊):28-37[Du Yuansheng,ZhangChuanheng,Han Xin.New Discovery of seismites in Dalongkou Groupin Mid-Proterozoic in Dianxi[J].Acta Sedimentologica Sinica,1996,24(Supp l.):28-37]
5郭胜哲,张立东,张长捷,等.辽宁太子河流域晚元古宙青白口系震积岩的发现及其意义[J].中国区域地质,1999,18(1):106-109[Guo Shengzhe,Zhang Lidong,Zhang Changjie,et al.Seismitesof the Late Proterozoic Qingbaikou System in the Taizi River Valley ofLiaoning[J].Regional Geology of China,1999,18(1):106-109]
6杜远生,张传恒,韩欣,等.滇中中元古代昆阳群的地震事件沉积及其地质意义[J].中国科学:D辑,2001.31(4):283-289[DuYuansheng,Zhang Chuanheng,Han Xin,et al.Mesoproterozoic seis-mic event deposit and its geological significance in Kunyang Group,Central Yunnan[J].Science in China:Series D,2001,31(4):283-289]
7乔秀夫,宋天锐,李海兵.是地震液化泄水成因,不是“渗流管”构造[J].科学通报,2002,47(14):1118-1120[Qiao Xiufu,Song Tian-rui,Li Haibing.Being generated by earthquake liquefaction,not being“seep tube"structure[J].Chinese Science Bulletin,2002,47(14):1118-1120]
8曹国强,陈世悦,鄢继华,等.济阳坳陷早第三纪地震事件沉积序列[J].地质找矿论丛,2004:19(4):252-256[Cao Guoqiang,Chen Shiyue,Yan Jihua,et al.The Early Tertiary sedimentary se-quence of earthquake events in Jiyang Depression[J].Geology Explo-ration Commention,2004,19(4):252-256]
9严兆彬,郭福生,彭花明,等.浙西寒武系大陈岭组地震事件沉积的初步研究[J].地质学报,2005,79(6):730-736[Yan Zaobin,Guo Fusheng,Peng Huaming,et al.Polot study on sedimentation ofCambrian Dachenling Formation resulting from seismic events in thewest of Zhejiang Province[J].Acta Geologica Sinica,2005,79(6):730-736]
10赵卫卫,查明,杨剑萍.中国震积岩研究综述[J].地层学杂志,2006,30(2):171-176[Zhao Weiwei,Zha Ming,Yang Jianping.An overview of seismite research in China[J].Journal of Stratigra-phy,2006,30(2):171-176]
11梁定益,聂泽同,万晓樵,等.试论震积岩与震积不整合——以川西、滇西地区为例[J].现代地质,1991,5(2):138-146[LiangDingyi,Nie Zetong,Wan Xiaoqiao,et al.On the seismite and seis-mic disconformity:take the western Sichuan and western Yunnan re-gions as an example[J].Geoscience,1991,5(2):138-146]
12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——中国地质大学学报,1994,19(6):845-850[Liang Dingyi,Nie Zetong.Song Zhimin.A re-study on seismite and seismo-unconformity:taking western Sichuanand western Yunnan as an example[J].Earth Science.1994,19(6):845-850]
13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(3):19-26[Wu Xiantao,YinGuoxun.Discovery and significance of seismites of lake deposition ofLate Jurassic in Emei in Sichuan[J].Acta Sedimentologica Sinica,1992,10(3):19-26]
14杨国美.重庆北碚地区下三叠统飞仙关组沉积相的基本特征[J].西南石油学院学报,1987,9(2):1-14[Yan Guomei.Funda-mental characteristics of sedimentary facies of Feixianguan Formationin Lower Triassic System,Beibei Area,Ghongqing City,SichuanProvince[J].Journal of Southwest Petroleum Institute,1987,9(2):1-14]
15蒋武.重庆北碚地区上二叠--下三叠统牙形刺及油气意义[J].西南石油学院学报,1982,4(1):12-24[Jiang Wu.Upper Permi-an-Lower Triassic Conodonts in Chongqing-Beibei Area and their sig-nificance in exploring oil and gas[J].Journal of Southwest PetroleumInstitute,1982,4(1):12-24]
16 Seilacher A.Sedimentary structures tentatively attributed to seismic e-vents[J].Marine Geology,1984,55(1-2):1-12
17 Lowes D R.Subaqueous liquefied and fluidized flows and their depos-its[J].Sedimentology,1976,23(3):285-308
18 Rodriguez-Pascua M A,et al.Soft-sediment deformation structures in-terpreted as seismites in lacustrine sediments of the prebetic zone,SESpain and their potential use as indicators of earthquake magnitudesduring the late Miocene[J].Sedimentary Geology,2000,135:117-135
19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,1988,38(8):609-611[Song Tian-rui.A set of possible earthquake-tsunami sequence in PrecambrianCarbonate,Shisanling,Beijing[J].Chinese Science Bulletin,1988,33(8):609-611]
20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[Qiao Xiufu,Song Tianrui,Gao Linzhi,et al.Seismic sequence in carbonate rocks by vibrational liquefaction[J].Acta Geologica Sinica,1994,68(1):16-32]
21乔秀夫.中国震积岩的研究与展望[J].地质论评,1996,42(4):317-320[Qiao Xiufu.Study of seismites of China and its pros-pects[J].Geological Review,1996,42(4):317-320]
22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[Du Yuansheng,Han Xin.Tsunami and tsunamites[J].Geological Science and Technology Information,2000,19(1):19-22]
23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[Du Yuansheng,Han Xin.Seismo-deposition andseismites[J].Advance on Earth Science,2000,15(4):389-394]
24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[Song Tianrui,Liu Yanxue.Ancient earth-quake records and litho-paleogeography[J].Acta SedimentologicaSinica,2009,27(5):872-879]
25王一刚,文应初,洪海涛,等.四川盆地北部晚二叠世———早三叠世碳酸盐岩斜坡相带沉积特征[J].古地理学报,2009,11(2):143-156[Wang Yigang,Wen Yingchu,Hong Haitao,et al.Carbonate slope fades sedimentary characteristics of the Late Permianto Early Triassic in Northern Sichuan Basin[J].Journal of Palaeo-geography,2009,11(2):143-156]
26杜远生,Shi G R,龚一鸣,等.东澳大利亚南悉尼盆地二叠系与地震沉积有关的软沉积变形构造[J].地质学报,2007,81(4):511-518[Du Yuansheng,Guang R Shi,Gong Yinming,et al.Permi-an soft-sediment deformation structures related to earthquake in theSouthern Sydney Basin,Eastern Australia[J].Acta Geologica Sinica2007,81(4):511-518]
27 Elliot C G,Williams P F.Sediment slump structures:a review of di-agnostic criteria and application to an example from Newfoundland[J].Journal of Structural Geology,1988,(10):171-182
28 Morton R A.Nearshore responses to great storm[C]∥Clifton H E,ed.Sedimentary Consequences of Convulsive Geologic Events[J].Ge-ological Society of America Special Paper 229,1988:222
29 Field M E,Gardner J V,Jennings A E,et al.Earthquake inducedsediment failures on a 0.25 slope,Klamath River Delta,California[J].Geology,1982(10):542-546
30 Vaughan N D,Johnson T C,Meams D L,et al.The impact of hurri-cane Diana on the North Carolina continental shelf[J].Marine Geolo-gy,1987(76):169-176
31 Boss S K,Neumann A C.Impacts of hurricane Andrew on carbonateplatform environments,northern Great Bahama Bank[J].Geology,1993,(21):897-900
32 Shinn E A,Steinen R P,Dill R F,et al.Lime-mud layers in high-energy tidal channels:A record of hurricane deposition[J].Geology,1993(21):603-606
33 Guiraud M,Plaziat J C.Seismites in the fluviatile Bima sandstones:identification of Paleoseisms and discussion of their magnitudes in aCretaceous synsedimentary strike-slip basin(Upper Benue,Nigeria)[J].Tectonophysicis,1993(225):493-522
34 Obermeier S F.Use of liquefaction-induced features for paleo-seismicanalysis-An overview of how seismic liquefaction features can be dis-tinguished from other features and how their regional distribution andproperties of source sediment can be used to infer the location andstrength of Holocene paleo-earthquakes[J].Engineering Geology,1996,44(1-4):1-74
35 Pope M C,Read J F,Bambach R,et al.Late Middle to Late Ordivi-cian seismites of Kentucky,southwest Ohio and Virginia:sedimentaryrecorders of earthquakes in the Appalachian basin[J].GSA Bulletin,1997,109(4):489-503
36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,2007,37(3):336-343[Zhang Chuanheng,Wu Zhenjie,Gao Linzhi,et al.Meso-proterozoic earthquake induced soft-sediment deformation and itsgeological significance in Wumishan Formation,North China[J].Sci-ence in China:Series D,2007,37(3):336-343]
37 Ettensohn F R,Rast N,Kulp M A.Locating possible epicentral areasfor paleoearthquakes,middle Ordovician Lexington Limestone,centralKentucky[J].Geological Society of American Abstract Program,2000,32:A215
38 Moretti M.Soft-sediment deformation structures interpreted as seis-mites in middle-late Pleistocene Aeolian deposits(Apulian foreland,Southern Italy)[J].Sedimentary Geology,2000,135(1-4):167-179
39 John Houston,Dan Hart,Andrew Houston.Neogene sedimentary de-formation in the Chilean forearc and implication for Andean basin de-velopment,seismicity and uplift[J].Journal of the Geological Socie-ty,London,2008,165:291-306
40廖太平胡明主编,重庆天府地区地质考察指南[M].北京:石油工业出版社,2008[Liao Taiping,Hu Ming,ed.Geological FieldTrip Guide in Tianfu Area,Chongqing City[M].Beijing:PetroleumIndustry Press,2008]
41 Brian R Pratt.Storms versus tsunamis:Dynamic interplay of sedimen-tary,diagenetic,and tectonic processes in the Cambrian of Montana[J].Geology,2002,30(5):423-426
42罗冰,谭秀成,刘宏,等.川东地区飞一段震积岩的发现及识别标志[J].沉积学报,2009,27(5):1012-1017[Luo Bing,Tan Xi-ucheng,Liu Hong,et al.Discovery and recognition marks of seismiteof the Fei 1 Member in the eastern Sichuan Basin[J].Acta Sedimen-tologica Sinica,2009,27(5):1012-1017]
43 Shanmugam G.The tsunamite problem[J].Journal of SedimentaryResearch,2006,(76):718-730
44杜远生,彭冰霞,韩欣.广西北海涠洲岛晚更新世火山活动引起的地震同沉积变形构造[J].沉积学报,2005,23(2):203-209[Du Yuesheng,Peng Bingxia,Han Xin.Syn-depositional deforma-tion structures by earthquake related to volcanic activity of the LatePleistocene in Weizhou Island,Beihai City Guangxi[J].Acta Sedim-entologica Sinica,2005,23(2):203-209]
45 Simms M J.Uniquely extensive seismite from the latest Triassic King-dom:Evidence for bolide impact?[J].Geology,2003(31):557 560
46刘志成,张廷山,魏祥峰.四川盆地南部赤水地区下三叠统嘉陵江组遗迹化石及其沉积环境[J].海相油气地质.2009,14(1):46-50[Liu Zhicheng,Zhang Tingshan,Wei Xiangfeng.Ichnofossilsand sedimentary environment of Lower Triassic Jialingjiang Formationin Chishui Area,southern part of Sichuan Basin[J].Marine OriginPetroleum Geology,2009,14(1):46-50]
47李忠权,冉隆辉,陈更生,等.川东高陡构造成因地质模式与含气性分析[J].成都理工学院学报,2002,29(6):605-609[LiZhongquan,Ran Longhui,Ghen Gengsheng,et al.Geologic modeland gaseous analyses about the origin of high-steep structures in east-ern Sichuan Basin[J].Journal of Chengdu University of Technology,2002,29(6):605-609]
48吕宝凤,夏斌.川东南“隔档式构造”的重新认识[J].天然气地球科学,2005,16(3):278-282[LüBaofeng,Xia Bin.New knowl-edge about ejective structure in Southeast Sichuan[J].Nature GasGeoscience,2005,16(3):278-282]
49许志琴,李化启,侯立炜,等.青藏高原东缘龙门—锦屏造山带的崛起———大型拆离断层和挤出机制[J].地质通报,2007,26(10):1262-1276[Xu Zhiqin,Li Huaqi,Hou Liwei,et al.Uplift ofthe Longmen-Jinping Orogenic Belt along the eastern margin of theQinghai-Tibet Plateau:large-scale detachment faulting and extrusionmechanism[J].Geological Bulletin of China,2007,26(10):1262-1276]
50邹光富,侯立玮,尹显科.甘孜—理塘蛇绿混杂岩带特征及其构造意义[J].四川地质学报,1994,14(1):17-24[Zou Guangfu,Hou Liwei,Yin Xianke.Characteristics of Garze-Litang ophiolite me-lange zone and its tectonic implication[J].Acta Geologica Sichuan,1994,14(1):17-24]
51邹光富.甘孜—理塘板块缝合带研究的新进展[J].四川地质学报,1995,15(4):257-263[Zou Guangfu.Advance of the researchon the Garze-Litang plate junction[J].Acta Geologica Sichuan,1995,15(4):257-263]
52姚学良,兰艳.甘孜—理塘蛇绿混杂岩带存在N型洋脊玄武岩[J].四川地质学报,2001,21(3):138-140[Yao Xueliang andLan Yan.N-type oceanic ridge basalt in the Garge-Litang ophiolitemelange zone[J].Acta Geologica Sichuan,2001,21(3):138-140]
53杨宗让.川西松潘-甘孜弧前盆地的形成及演化[J].沉积与特提斯地质,2002,22(3):53-59[Yang Zongrang.The formation and e-volution of the Songpan-Garze fore-arc basin,western Sichuan[J].Sedimentary Geology and Tethyan Geology,2002,22(3):53-59]
54 Franoise Roger,Marc Jolivet,Jacques Malavieille.Tectonic evolu-tion of the Triassic fold belts of Tibet[J].Geoscience,2008,(340):180-189
55魏永峰,罗森林,周幼云,等.甘孜—理塘结合带中段蛇绿岩中石榴硅镁石角闪片岩首次发现及地质意义[J].四川地质学报,2004,24(1):1-3[Wei Yongfeng,Luo Senlin,Zhou Youyun,et al.Discovery of garnet-humite-hornblende schist in ophiolite suite and itsgeological significance in the Garzê-Litang suture zone[J].Acta Geo-logica Sichuan,2004,24(1):1-3]
56王清晨.浅议华南陆块群的沉积大地构造学问题[J].沉积学报,2009,27(5):811-817[Wang Qingchen.Preliminary discussion onsedimentary tectonics of the clustered continents of South China[J].Acta Sedimentologica Sinica,2009,27(5):811-817]
57 Anthony J Reid,Christopher J L,Wilsona,Shun Liu.Structural evi-dence for the Permo-Triassic tectonic evolution of the Yidun Arc,east-ern Tibetan Plateau[J].Journal of Structural Geology,2005,27:119-137
58 Anthony J Reid,Christopher J L Wilson,Shun Liu,et al.Mesozoicplutons of the Yidun Arc,SW China:U/Pb geochronology and Hf iso-topic signature[J].Ore Geology Reviews,2007,31:88-106
59曲晓明,侯增谦,唐绍华.义敦岛弧带弧后区板内岩浆作用的时代及意义[J].岩石矿物学杂志,2003,22(2):131-137[Qu Xi-aoming,Hou Zengqian and Tang Shaohua.Age of intraplate volcan-ism in the back-arc area of Yidun island arc and its significance[J].Acta Petrologica et Mineralogica,2003,22(2):131-137]
60戴宗明,孙传敏.松潘-甘孜造山带义敦岛弧中段三叠纪火山-沉积盆地的演化[J].地质通报,2008,27(6):799-813[Dai Zong-ming,Sun Chuanmin.Evolution of Triassic volcanic-sedimentary ba-sins in the central segment of the Yidun island arc of the Songpan-Garzêorogenic belt,Western Sichuan,China[J].Geological Bulletinof China,2008,27(6):799-813]
61刘飞,陈岳龙,苏本勋,等.松潘—甘孜地区三叠系碎屑沉积岩地球化学特征及其锆石年龄研究[J].地球学报,2006,27(4):289-296[Liu Fei,Chen Yuelong,Su Benxun,et al.Geochemistryand zircon ages of Triassic detrital sedimentary rocks from the Ganze-Songpan block[J].Acta Geoscientica Sinica,2006,27(4):289-296]
版权所有：© 2023 中国地质图书馆 中国地质调查局地学文献中心