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
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摘要
在野外考察过程中,于新疆乌恰地区早侏罗世康苏组沼泽相砂岩层中,发现并识别出软沉积物液化变形层,变形包括负载构造,球-枕构造及卷曲变形构造。通过模拟试验的对比研究认为,该软沉积物变形机制与液化作用有关,触发沉积物液化的动力是古地震,并且根据地震震级与液化最大震中距的关系,推测出造成早侏罗世软沉积物变形的里氏地震震级为6早侏罗世的古地震活动表明,控制盆地形成与分布的塔拉斯-费尔干纳断裂带在早侏罗世时期发生了强烈的右旋走滑运动。侏罗纪以来断裂带的地震活动制约着乌恰盆地中的油气运移和聚集。
During the field work,soft-sediment deformation structures in lower Jurassic Kangsu Formation lacustrine deposits were recognized in the northern part of Wuqia,western Xinjiang Uygur Autonomous Region.Deformation structures are represented by load cast,ball-and-pillow structure and convolute lamination.The mechanism of deformation is related to liquefaction and or fluidization triggered by a paleoseismic event by comparing with the simulation test.According to the correlation between the earthquake magnitude and the maximum epicentral distance of liquefaction,the magnitude producing the lower Jurassic soft-sediment deformation can be predicted as 6
During the field work,soft-sediment deformation structures in lower Jurassic Kangsu Formation lacustrine deposits were recognized in the northern part of Wuqia,western Xinjiang Uygur Autonomous Region.Deformation structures are represented by load cast,ball-and-pillow structure and convolute lamination.The mechanism of deformation is related to liquefaction and or fluidization triggered by a paleoseismic event by comparing with the simulation test.According to the correlation between the earthquake magnitude and the maximum epicentral distance of liquefaction,the magnitude producing the lower Jurassic soft-sediment deformation can be predicted as 6
引文
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魏垂高,张世奇,姜在兴,等.2007.塔里木盆地志留系震积岩特征及其意义.地质学报,81(6):827～833.
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张琴,朱筱敏,张军,等.2003.酒西盆地青南凹陷柳沟庄-窟窿山地区下白垩统震积岩的发现及意义.地质学报,77(2):158～162.
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Ettensohn F R,Rast N,Kulp M A.2000.Locating possibleepicentral areas for paleoearthquakes,middle Ordivicianlexington limestone,Central Kentucky[abs].GeologicalSocitey of America Abstract with Programs,32:A215.
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Li Tiejun,Luo Xiaorong.2005.The Jurassic petroleum systeminthe Kashi depression of theTarimbasin.Petroleum Geology andExperiment,27(1):39～43(in Chinese with English abstract).
Liu Ying,Xie Junpei.1984.Sand Soil Seismic Vibrate Liquefaction.Beijing:Seismology Publishing House(in Chinese with Englishabstract).
Lowes D R.1976.Subaqueousliquefied andfluidizedflows andtheirdeposits.Sedimentology,23(3):285～308.
Luo Jinhai,Zhou Xinyuan,Qiu Bin,et al.2004.Controls of Talas-Ferghana fault on Kashi Sag,Northwestern Tarim Basin.Xinjiang Petroleum Geology,25(6):584～587(in Chinese withEnglish abstract).
Mariotti G,Corda L,Brandano M,et al.2002.Indicators ofpaleoseismicity in the lower to middle Miocene GuadagnaloFormation,central Apennines,Italy.In:Ettenschn F R,RastN,Brett C E,eds.Ancient Seismites:Boulder Colorado.Geological Society of America special paper,359:87～98.
Matsuda J-i.2000.Seismic deformation structure of the past-2300aBP muddy sediments in Kawachi lowland plain,Osaka,Japan.Sedimentary Geology,135:99～116.
Moretti M.2000.Soft-sediment deformation structures interpretedas seismites in middle-late Pleistocene aeolian deposits(Apulian forland,Southern Italy).Sed.Geol.,135(1～4):169～179.
Moretti M,Pieri P,Tropeano M.2002.Late Pleistocene soft-sediment deformation structures interpreted as seismites inparalic deposits in the city of Bari(Apulian foreland southernItaly).In:Ettensohn F R,Rast N,Brett C E,eds.AncientSeismites:Boulder,Colorado.Geological Society of AmericaSpecial Paper,359:75～85.
Nemcok M,Schamel S,Gayer R.2005.Thrust Belts.CambridgeUniversity Press,221～254.
Obermeier S F.1996.Use of liquefaction-inducedfeatures for paleo-seismic analysis——An overview of how seismic liquefactionfeatures can be distinguished fromother features and howtheirregional distribution and properties of source sediment can beused to infer the location and strength of Holocene paleo-earthquakes.Eng.Geol.,44(1～4):1～74.
Qiao Xiufu,Song Tianrui,Gao Linzhi,et al.1994.Seismicsequence in carbonate rocks by vibration liquefaction.ActaGeologica Sinica(English Edition),7(3):243～265.
Qiao Xiufu,Song Tianrui,Li Haibing,et al.1996.Geneticstratigraphy of the Sinian and Lower Cambrian Strata in SouthLiaoning Province.Beijing:Science Press,1～174(inChinese).
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