[1]Xue Liangqing,Galloway W E.Fan-delta,braid delta and the classification of delta systems[J].Acta Geological Sinica,1991,65(2):141-153.[薛良清,Galloway W E.扇三角洲、辫状河三角洲与三角洲体系的分类[J].地质学报,1991,65(2):141-153.]
[2]Li Xiangbo,Liu Huaqing,Wan Yanrong,et al.First discovery of sandy debris flow reservoir in Yanchang Formation,Triassic,Ordos Basin[J].Lithologic Reservoirs,2009,21(4):19-21.[李相博,刘化清,完颜容,等.鄂尔多斯盆地三叠系延长组砂质碎屑流储集体的首次发现[J].岩性油气藏,2009,21(4):19-21.]
[3]Li Xiangbo,Fu Jinhua,Chen Qilin,et al.The concept of sandy debris flow and its application in the Yanchang Formation deep water sedimentation of the Ordos Basin[J].Advances in Earth Science,2011,26(3):286-294.[李相博,付金华,陈启林,等.砂质碎屑流概念及其在鄂尔多斯盆地深水沉积研究中的应用[J].地球科学进展,2011,26(3):286-294.]
[4]Li Xiangbo,Liu Huaqing,Chen Qilin.The characteristics of the sandy debris flow of the Triassic Yanchang Formation and it’s exploration significance in the Ordos Basin,China[J].Acta Geologica Sinica,2011,85(5):1187-1202.
[5]Zou Caineng,Zhao Zhengzhang,Yang Hua,et al.Genetic mechanism and distribution of sandy debris flows in terrestrial lacustrine basin[J].Acta Sedimentary Sinica,2009,27(6):1065-1075.[邹才能,赵政璋,杨华,等.陆相湖盆深水砂质碎屑流成因机制与分布特征——以鄂尔多斯盆地为例[J].沉积学报,2009,27(6):1065-1075.]
[6]Yao Jingli,Wang Qi,Zhang Rui,et al.Origin and spatial distribution of carbonate cements in Yanchang Formation (Triassic) sandstones within the lacustrine center of Ordos Basin,NW China[J].Natural Gas Geoscience,2011,22(6):943-950.[姚泾利,王琪,张瑞,等.鄂尔多斯盆地中部延长组砂岩中碳酸盐胶结物成因与分布规律研究[J].天然气地球科学,2011,22(6):943-950.]
[7]Guo Yanru,Liu Huaqing,Li Xiangbo,et al.Method system on studying sequence stratigraphic framework of large sagged lacustrine basin:A case study from Mesozoic Yanchang Formation,Ordos Basin[J].Acta Sedimentologica Sinica,2008,26(3):384-391.[郭彦如,刘化清,李相博,等.大型坳陷湖盆层序地层格架的研究方法体系——以鄂尔多斯盆地中生界延长组为例[J].沉积学报,2008,26(3):384-391.]
[8]Shanmugam G.50 years of the turbidite Paradigm(1950s-1990s):Deep-water processes and facies models:A critical perspective[J].Marine and Petroleum Geology,2000,17:285-342.
[9]Kuenen Ph H,Migliorini C I.Turbidity currents as a cause of graded bedding[J].Journal of Geology,1950,58:91-127.
[10]Dott R H Jr.Dynamics of subaqueous gravity depositional processes[J].AAPG Bulletin,1963,47:104-128.
[11]Weimer P,Slatt R.Introduction to the Petroleum Geology of Deepwater Settings[M].AAPG Studies in Geology 57,SEPM Special Publication,2007:1-419.
[12]Moscardelli L,Wood L.New classification system for mass transport complexes in offshore Trinidad[J].Basin Research,2008,20:73-98.
[13]Lowe D R.Sediment-gravity flows:Their classification,and some problems of applications to natural flows and deposits[M]//Doyle L J,Pilkey O H.Geology of Continental Slopes.Society of Economic Paleontologists and Mineralogists Special Publication,1979,27:75-82.
[14]Lowe D R.Sediment-gravity flows,Ⅱ:Depostional models with special reference to the deposits of high-density turbidity currents[J].Journal of Sedimentary Petrology,1982,52(1):279-297.
[15]Nardin T R,Hein F J,Gorsline D S,et al.A review of mass movement processes,sediment and acoustic characteristics,and contrasts in slope and base-of-slope systems versus canyon-fan-basin floor systems[M]//Doyle L J,Pilkey O H.Geology of Continental Slopes.Economic Paleontologists and Mineralogists Special Publication 27,1979:61-73.
[16]Pierson T C,Costa J E .A rheologic classication of subaerial sediment-water flows[M]// Costa J E,Wieczorek G F.Debris Flows/Avalanches:Process,Recognition,and Mitigation.Geological Society of America Reviews in Engineering Geology VII,1987:1-12.
[17]Tian Zhaoyi,Xu Haipeng,Zeng Siwei.Accumulation geomorphology and sediment characteristics of viscous debris flow[J].Bulletin of Soil and Water Conservation,1985,(1):30-41.[田昭一,徐海鹏,曾思伟.黏性泥石流的堆积地貌及沉积物的特征[J].水土保持通报,1985,(1):30-41.]
[18]He Mingjing,Sun Gennian,Song Yongmei.Study on the formation causes of the geologic landscape relics in the Cuihuashan Mountain National Geo-Park in Xi′ an City,Shaanxi Province[J].Arid Land Geography,2005,28(2):145-149.[贺明静,孙根年,宋咏梅.陕西西安翠华山地质景观遗迹成因探析[J].干旱区地理,2005,28(2):145-149.]
[19]Fang Xiaomin,Shen Mingzhi,Mu Yunzhi.Preliminary exploration on microscopic structure and the forming mechanism of debris flow in Wudu[J].China Science:Serial B,1991,(2):205-215.[方小敏,沈明智,牟昀智.武都泥石流显微构造及其形成机制初探[J].中国科学:B辑,1991,(2):205-215.]
[20]Wang Yuelun,Jia Lanpo.Observation of glacier in Quaternary in Zhoukoudian[J].Acta Geologica Sinica,1952,32(1/2):16-25.[王曰伦,贾兰坡.周口店第四纪冰川现象的观察[J].地质学报,1952,32(1/2):16-25.]
[21]Zhao Guolong,Zhu Hongsen,Li Boyang,et al.Quaternary glacial geology and origin of glacial pothole swarms in Inner Mongolia[J].Regional Geology of China,2001,20(2):200-205.[赵国龙,朱洪森,李泊洋,等.论内蒙古第四纪冰川和冰臼群的成因[J].中国区域地质,2001,20(2):200-205.]
[22]Li Xiangbo,Liu Huaqing,Zhang Zhongyi,et al.“Argillaceous parcel”structure:A direct evidence of debris flow origin of deep-water massive sandstone of Yanchang Formation,Upper Triassic,the Ordos Basin[J].Acta Sedimentologica Sinica,2014,32(4):611-622.[李相博,刘化清,张忠义,等.深水块状砂岩碎屑流成因的直接证据:“泥包砾”结构——以鄂尔多斯盆地延长组为例[J].沉积学报,2014,32(4):611-622.]
[23]Middleton G V,Hampton M A.Sediment gravity flows:Mechanics of flow and deposition[ M ]∥Middleton G V,Bouma A H.Turbidites and deep-water sedimentation:Short course lecture notes,Part I.California:Los Angeles,1973:1-38.
[24]Wang Deping.The sedimentation and formation mechanism of lacustrine endogenic debris flow[J].Acta Geologica Sinica,1991,65(4):299-317.[王德坪.湖相内成碎屑流的沉积及形成机理[J].地质学报,1991,65(4):299-317.]
[25]Hampton M A.Competence of fine-grained debris flows[J].Journal of Sedimentary Petrology,1975,45:834-844.
[26]Costa J E,Williams G P.Debris Flow Dynamics (Videotape)[R].US Geological Survey Open File Report of 84-0606,1984.
[27]Marr J,Harff P,Shanmugam G,et al.Experiments on Subaqueous Sandy Debris Flows[R].Supplement to EOS Transactions.AGU Fall Meeting,San Francisco,1997,78(46):347.
[28]Mulder T,Alexander J.The physical character of subaqueous sedimentary density flows and their deposits[J].Sedimentology,2001,48:269-299.
[29]Talling P J,Masson D G,Sumner F J,et al.Subaqueous sediment density flows:Depositional processes and deposit types[J].Sedimentology,2012,59:1937-2003.
[30]Yao Jingli,Wang Qi,Zhang Rui,et al.Forming mechanism and their environmental implications of chlorite-coatings in Chang 6 sandstone(Upper Triassic) of Hua-Qing area,Ordos Basin[J].Acta Sedimentologica Sinica,2011,29(1):72-79.[姚泾利,王琪,张瑞.等.鄂尔多斯盆地华庆地区延长组长 6 砂岩绿泥石膜的形成机理及其环境指示意义[J].沉积学报,2011,29(1):72-79.]
[31]Wang Yingmin,Wang Hairong,Qiu Yan,et al.Process of dynamics and its response of deep-water sedimentation[J].Acta Sedimentologica Sinica,2007,25(4):495-504.[王英民,王海荣,邱燕,等.深水沉积的地球动力学机制与响应[J].沉积学报,2007,25(4):495-504.]
[32]Xian Benzhong,Wan Jinfeng,Dong Yanlei,et al.Sedimentary characteristics,origin and model of lacustrine deep-water massive sandstone:An example from Dongying Formation in Nanpu Depression[J].Acta Petrologica Sinica,2013,29(9):3287-3299.[鲜本忠,万锦峰,董艳蕾,等.湖相深水块状砂岩特征、成因及发育模式——以南堡凹陷东营组为例[J].岩石学报,2013,29(9):3287-3299.] |