引文
[1]张功成,米立军,吴时国,等.深水区—南海北部大陆边缘盆地油气勘探新领域[J].石油学报,2007,28(2):15-21.[ZHANGGongcheng,MI Lijun,WU Shiguo,et al.Deepwater area:Thenew prospecting targets of northern continental margin ofSouth China Sea[J].Acta Petrolei Sinica,2007,28(2):15-21.]
[2]Chen P H,Chen Z Y,Zhang Q M.Sequence stratigraphy andcontinental margin development of the northwestern shelf ofthe South China Sea[J].AAPG Bulletin,1993,77:842-862.
[3]姜涛.莺歌海-琼东南盆地区中中新世以来低位扇体形成条件和成藏模式[D].武汉:中国地质大学,2005:22-40.[JIANGTao.Formation of Lowstand Fans and Their Hydrocarbon Ac-cumulation Since Middle Miocene in the Yinggehai and Qiong-dongnan Basins[D].Wuhan:China University of Geoscience,2005:22-40.]
[4]魏魁生,崔旱云,叶淑芬,等.琼东南盆地高精度层序地层学研究[J].地球科学:中国地质大学学报,2001,26(1):59-66.[WEI Kuisheng,CUI Hanyun,YE Shufen,et al.High preci-sion sequence stratigraphy in Qiongdongnan Basin[J].EarthScience:Journal of China University of Geosciences,2001,26(1):59-66.]
[5]姜涛,解习农.细粒浊积体的油气地质意义[J].地质科技情报,2003,22(2):51-55.[JIANG Tao,XIE Xinong.Hydrocarbonvalue of finegrained turbidite systems[J].Geological Scienceand Technology Information,2003,22(2):51-55.]
[6]Kathleen D S,Richard B W,Stephan A G.Evolution and stra-tigraphic architecture of marine slope gully complexes:Monterey Formation(Miocene),Gaviota Beach,California[J].Marine and Petroleum Geology,2009,26(2):269-288.
[7]Ercilla G,Casas D,Estrada F,et al.Morpho-sedimentary fea-tures and recent depositional architectural model of the Cant-abrian continental margin[J].Marine Geology,2008,247:61-83.
[8]Arnold H Bouma,William R Normark,Neal E Barnes.Subma-rine Fans and Related Turbidite Systems[M].New York:Springer-Verlag,1985,343.
[9]Piper,D J W,Savoye B.Processes of late Quaternary turbiditycurrent flow and deposition on the Var deep-sea fan,north-west Mediterranean Sea[J].Sedimentology,1993,40(3):557-582.
[10]王海荣,王英民,邱燕,等.南海北部陆坡的地貌形态及其控制因素[J].海洋学报,2008,30(2):70-79.[WANG Hairong,WANG Yingmin,QIU Yan,et al.Geomorphology and itscontrol of deep-water slope of the margin of the South ChinaSea[J].Acta Oceanologica Sinica,2008,30(2):70-79.]
[11]Gareth M Kwwvil,Jeff Peakall,James L Best.The influenceof scale,slope and channel geometry on the flow dynamics ofsubmarine channels[J].Marine and Petroleum Geology,2007,24:487-503.
[12]Paul Weimer.Sequence stratigraphy of the Mississippi fan(Plio-Pleistocene),Gulf of Mexico[J].Geo-Marine Letters,1989,9:185-272.
[13]Bradford E Prather.Controls on reservoir distribution,archi-tecture and stratigrahic trapping in slope settings[J].Marineand Petroleum Geology,2003,20:529-545.
[14]袁圣强,吴时国,赵宗举,等.南海北部陆坡深水区沉积物输送模式探讨[J].海洋地质与第四纪地质,2010,30(4):39-48.[YUAN Shengqiang,WU Shiguo,ZHAO Zongju,et al.Deepwater sediment transportation models for northern SouthChina Sea slopes[J].Marine Geology and Quaternary Geolo-gy,2010,30(4):39-48.
[15]何云龙,解习农,李俊良,等.琼东南盆地陆坡体系发育特征及其控制因素[J].地质科技情报,2010,29(2):118-122.[HEYunlong,XIE Xinong,LI Junliang,et al.Depositional char-acteristics and controlling factors of continental slope systemin the Qiongdongnan Basin[J].Geological Science and Tech-nology Information,2010,29(2):118-122.
[16]Ben Kneller.The influence of flow parameters on turbiditeslope channel architecture[J].Marine and Petroleum Geolo-gy,2003,20:901-910.
[17]Arnold H Bouma,Harry H Roberts.Northern Gulf ofMexico continental slope[J].Geo-Marine Letters,1990,10:177-181.
[18]王大伟,吴时国,董东东,等.琼东南盆地第四纪块体搬运体系的地震特征[J].海洋地质与第四纪地质,2009,29(3):69-74.[WANG Dawei,WU Shiguo,DONG Dongdong,et al.Seis-mic characteristics of Quaternary mass transport deposits inQiongdongnan Basin[J].Marine Geology and Quaternary Ge-ology,2009,29(3):69-74.]
[19]Lin Changsong,Liu Jingyan,Cai Shixiang,et al.Depositionalarchitecture and developing settings of large-scale incised val-ley and submarine gravity flow system in the Yinggehai andQiongdongnan basins,South China Sea[J].Chinese ScienceBulletin,2001,46(8):690-693.
[20]Lutz Lesshafft,Eckart Meiburg,Ben Kneller,et al.Towardsinverse modeling of turbidity currents:The inverse lock-ex-change problem[J].Computer&Geosciences,2011,37:521-529.
[21]吴时国,秦蕴珊.南海北部陆坡深水沉积体系研究[J].沉积学报,2009,27(5):922-930.[WU Shiguo,QIN Yunshan.Theresearch of deepwater depositional system in the northernSouth China Sea[J].Acta Sedimentologica Sinica,2009,27(5):922-930.]
[22]苏明,李俊良,姜涛,等.琼东南盆地中央峡谷的形态与成因[J].海洋地质与第四纪地质,2009,29(4):85-93.[SU Ming,LI Junliang,JIANG Tao,et al.Morphological features andformation mechanism of central canyon in the QiongdongnanBasin,northern South China Sea[J].Marine Geology andQuaternary Geology,2009,29(4):85-93.]
[23]姚根顺,袁圣强,吴时国,等.琼东南盆地深水区双物源沉积模式及勘探前景[J].石油勘探与开发,2008,35(6):685-691.[YAO Genshun,YUAN Shengqiang,WU Shiguo,et al.Double provenance depositional model and exploration pros-pect in deepwater area of Qiongdongnan Basin[J].PeteroleumExploration and Development,2008,35(6):685-691.]
[24]刘方兰,吴庐山.西沙海槽海域地形地貌特征及成因[J].海洋地质与第四纪地质,2006,26(3):7-14.[LIU Fanglan,WULushan.Topographic and morphologic characteristics andgenesis analysis of Xisha Trough Sea area in the South ChinaSea[J].Marine Geology and Quaternary Geology,2006,26(3):7-14.]
[25]彭大钧,庞雄,陈长民,等.从浅水陆架走向深水陆坡——南海深水扇系统的研究[J].沉积学报,2005,23(1):1-11.[PENG Dajun,PANG Xiong,CHEN Changmin,et al.Fromshallow-water shelf to deep-water slope:the study on deep-water fan systems in South China Sea[J].Acta Sedimento-logica Sinica,2005,23(1):1-11.]
[26]付彦辉,吕福亮,吴时国,等.琼东南盆地陆坡区深水浊积水道的地震相特征[J].热带海洋学报.2009,28(4):87-92.[FUYanhui,LU Fuliang,WU Shiguo,et al.Characteristics ofseismic facies in the deepwater turbidite channel system onthe slope of the Qiongdongnan Basin[J].Journal of TropicalOceanography,2009,28(4):87-92.]
[27]Kuenen Ph H.The difference between sliding and turbidityflow[J].Deep Sea Research,1953,3(2):134-139.
[28]贺可强,安振远.崩滑碎屑流的形成条件与形成类型[J].河北地质学院学报,1996,19(3-4):344-351.[HE Keqiang,AN Zhenyuan.A preliminary analysis on the forming condi-tions and the forming types of debris flow caused by land-slides and falls[J].Journal of Hebei College of Geology,1996,19(3-4):344-351.]
[29]Shanmugam G.Reinterpretation of depositional processes in aclassical flysch sequence(Pennsylvanian Jackford Group),Quachita Mountains,Arkansas and Oklahoma:Reply[J].AAPG Bull,1997a,81:476-491.
[30]李祥辉,王成善,胡修棉.深海相中的砂质碎屑流沉积[J].矿物岩石,2000,20(1):132-133.[LI Xianghui,WANG Cheng-shan,HU Xiumian.Sedimentation of sandy debris-flow indeep-sea environment[J].Mineral Petrol.,2000,20(1):132-133.]
[31]张兴阳,高振中,姚雪根.北大西洋洛克尔海槽东北部内波沉积—深水大型沉积物波成因的再解释[J].沉积学报,1999,17:464-472.[ZHANG Xingyang,GAO Zhenzhong,YAO xuegen.Internal-wave deposits in the north-easternRockall Trough,North Atlantic Ocean-Reinterpretation ofdeep-water sediment waves formation[J].Acta Sedimento-logica Sinica,1999,17:464-472.]
[32]邵磊,李学杰,耿建华,等.南海北部深水底流沉积作用[J].中国科学D辑,2007,37(6):771-777.[SHAO Lei,LI Xue-jie,GENG Jianhua,et al.The deepwater bottom sedimenta-tion effect of northern South China Sea[J].Science in China(Series D),2007,37(6):771-777.]