李相博,卫平生,刘化清,等. 浅谈沉积物重力流分类与深水沉积模式[J]. 地质论评,2013,59(4):607-614. [Li Xiangbo, Wei Pingsheng, Liu Huaqing, et al. Discussion on the classification of sediment gravity flow and the deep-water sedimentary model[J]. Geological Review, 2013, 59(4): 607-614.]
[2]
张顺,付秀丽,张晨晨. 松辽盆地姚家组—嫩江组地层层序及沉积演化[J]. 沉积与特提斯地质,2011,31(2):34-42.[Zhang Shun, Fu Xiuli, Zhang Chenchen. Stratigraphy sequence and sedimentary evolution of Yaojia Formation-Nenjiang Formation in Songliao Basin[J]. Sedimentary Geology and Tethyan Geology, 2011, 31(2): 34-42.]
[3]
黄清华,谭伟,杨会臣. 松辽盆地白垩纪地层序列与年代地层[J]. 大庆石油地质与开发,1999,18(6):15-17.[Huang Qinghua, Tan Wei, Yang Huichen. Stratigraphic succession and chronostrata of Cretaceous in Songliao Basin[J]. Petroleum Geology and Oilfield Development in Daqing, 1999, 18(6): 15-17.]
[4]
Middleton G V, Hampton M A. Sediment gravity flow: mechanics flow and deposition [C] //Middleton G V, Bouma A H. Tubidites and Deep Water Sedimentation. Pacific Section S.E.P.M., 1973: 1-38.
[5]
林畅松,刘景彦,胡博. 构造活动盆地沉积层序形成过程模拟——以断陷和前陆盆地为例[J]. 沉积学报,2010,28(5):868-874.[Lin Changsong, Liu Jingyan, Hu Bo. Computer simulation on the formation of depositional sequences in tectonic active basin: Case study on rift and foreland basins [J]. Acta Sedimentologica Sinica, 2010, 28(5): 868-874.]
[6]
任建业,林畅松,李思田,等. 二连盆地乌里亚斯太断陷层序地层格架及其幕式充填演化[J]. 沉积学报,1999,17(4):553-559.[Ren Jianye, Lin Changsong, Li Sitian, et al. Sequence stratigraphy framework of Wuliyasitai Faulted Basin in Erlian Basin Group and its episodic filling evolution[J]. Acta Sedimentologica Sinica, 1999, 17 (4): 553-559.]
[7]
冯兴雷,马立祥,谢丛娇,等. 乌里雅斯太凹陷南洼槽下白垩统重力流沉积相模式[J]. 沉积与特提斯地质,2008,28(4):28-35. [Feng Xinglei, Ma Lixiang, Xie Congjiao, et al. Wuliyasitai depression south sag Lower-Cretaceous gravity flow sedimentary facies models[J]. Sedimentary Geology and Tethyan Geology, 2008, 28(4): 28-35.]
[8]
黄传炎,王华,王家豪,等. 板桥凹陷断控重力流沉积特征及沉积模式[J]. 油气地质与采收率,2007,14(6):14-16. [Huang Chuanyan, WangHua, Wang Jiahao, et al. Sedimentary character and sedimentary models of the gravity flow controlled by fault in Banqiao depression[J]. Petroleum Geology and Recovery Efficiency, 2007, 14(6): 14-16.]
[9]
李文厚,周立发,符俊辉,等. 库车坳陷上三叠统的浊流沉积及石油地质意义[J]. 沉积学报,1997,15(2):20-23. [Li Wenhou, Zhou Lifa, Fu Junhui, et al. Turbidity current deposits and their significance on petroleum geology of Upper Triassic in the Kuqa depression[J]. Acta Sedimentologica Sinica, 1997, 15(2): 20-23.]
[10]
冯志强,张顺,解习农,等. 松辽盆地嫩江组大型陆相坳陷湖盆湖底水道的发现及其石油地质意义[J]. 地质学报,2006,80(8):1226-1232. [Feng Zhiqiang, Zhang Shun, Xie Xinong, et al. Discovery of a large-scale lacustrine subaqueous channel in the Nenjiang Formation of the Songliao Basin and its implication on petroleum geology[J]. Acta Geologica Sinica, 2006, 80(8): 1226-1232.]
[11]
王华,姜华,林正良,等. 南堡凹陷东营组同沉积构造活动性与沉积格局的配置关系研究[J]. 地球科学与环境学报,2011,33 (1):70-77. [Wang Hua, Jiang Hua, Lin Zhengliang, et al. Relations between syn-sedimentary tectonic activity and sedimentary framework of Dongying Formation in Nanpu sag[J]. Journal of Earth Sciences and Environment, 2011, 33(1): 70-77.]
[12]
袁珍,李文厚,范萌萌,等. 深水块状砂岩沉积特征及其成因机制探讨: 以鄂尔多斯盆地东南缘上三叠统6油层组为例[J]. 地质科技情报,2011,30(4):43-49. [Yuan Zhen, Li Wenhou, Fan Mengmeng, et al. Genetic mechanism and sedimentary features of deep water massive sandstone: A case study of the Upper Triassic sandstones of Chang 6 Formation in the southeast of Ordos Basin [J]. Geological Science and Technology Information, 2011, 30(4): 43-49.]
[13]
莫午零,吴朝东,张顺. 松辽盆地嫩江组二三段陆相坳陷湖盆大型三角洲前积体形成机制[J]. 石油天然气学报,2012,34(1):1-6.[ Mo Wuling, Wu Chaodong, Zhang Shun. Forming mechanism of continental depression-lacustrine large delta of the 2-3 members of Nenjiang Formation in Songliao Basin[J]. Journal of Oil and Gas Technology, 2012, 34(1): 1-6.]
[14]
John McGaughey, Gervais Perron, et al. Gocad workflows for expert-system decision making[R]. Geoscience Ltd., 29th Golad-meeting, 2009:5-7.
[15]
Lowe D R. Sediment gravity flows: their classification, and some problems of applications to natural flows and deposits[C]//Doyle L J, Pilkey O H. Geology of Continental Slopes (Society of Economic Paleontologists and Mineralogists Special Publication No. 27). EPM Society for Sedimentary, 1979: 75-82.
[16]
Shanmugan G. High-density turbidity current: are they sandy debris flows?[J]. Journal of Sedimentary Research, 1996, 66(1): 2-10.
[17]
Shanmugan 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(2): 285-342.
[18]
刘宪斌,万晓樵,林金逞,等. 陆相浊流沉积体系与油气[J]. 地球学报,2003,2(1):61-66. [Liu Xianbin, Wan Xiaoqiao, Lin Jincheng, et al. Continental turbidite deposition system and hydrocarbon[J]. Acta Geoscientia Sinica, 2003, 24(1): 61-66.]
[19]
Bouma A H, Stone C G. Fine-Grained Turbidite Systems[M]// AAPG Memoir. Tulsa: American Association of Petroleum Geologists, 2000: 1-19.
[20]
吴崇筠,李纯菊,刘国华,等. 断陷湖盆中的浊积岩[C]//中国石油学会石油地质委员会. 碎屑岩沉积相研究. 北京:石油工业出版社,1988:1-17. [Wu Chongjun, Li Chunju, Liu Guohua, et al. Turbidite in faulted lacustrine basin[C]//Petroleum Geology Society and Petroleum Geology Committee. Clastic Sedimentary Facies. Beijing: Petroleum Industry Press, 1988: 1-17.]
[21]
李继亮,陈昌明,高文学,等. 我国几个地区浊积岩系的特征[J]. 地质科学,1978(1):26-44. [Li Jiliang, Chen Changming, Gao Wenxue, et al. On the features of turbidite sequences in some regions of China [J]. Scientia Geologica Sinica, 1978(1): 26-44.]
[22]
李培军,侯泉林,李继亮,等. 闽西南地区早三叠世溪口组浊流沉积[J]. 沉积学报,1997,15(4):51-57. [Li Peijun, Hou Quanlin, Li Jiliang, et al. Turbidites in the Lower Triassic Xikou Formation in southwestern Fujian, South China[J]. Acta Sedimentologica Sinica, 1997, 15(4): 51-57.]
[23]
李云,郑荣才,朱国金,等. 沉积物重力流研究进展综述[J]. 地球科学进展,2011,26(2):157-165.[Li Yun, Zheng Rongcai, Zhu Guojin, et al. Reviews on sediment gravity flow[J]. Advances in Earth Science, 2011, 26(2): 157-165.]
[24]
于兴河. 碎屑岩系油气储层沉积学[M]. 北京:石油工业出版社,2002:51-53.[Yu Xinghe. Reservoir Sedimentology of Clastic Rock Systems [M]. Beijing: Petroleum Industry Press, 2002: 51-53.]
[25]
潘树新,郑荣才,卫平生,等. 陆相湖盆块体搬运体的沉积特征、识别标志与形成机制[J]. 岩性油气藏,2004,25(2):9-18.[Pan Shuxin, Zheng Rongcai, Wei Pingsheng, et al. Deposition characteristics, recognition mark and form mechanism of mass transport deposits in terrestrial lake basin[J]. Lithologic Reservoirs, 2004, 25(2): 9-18.]
[26]
刘振武. 松辽盆地北部构造回返期的油气藏[J]. 江苏地质,2005,29(3):143-146.[Liu Zhenwu. Oil-gas accumulation in tectonic inversion in North Songliao Basin[J]. Jiangsu Geology, 2005, 29(3): 143-146.]
[27]
鄢继华,陈世悦,宋国奇,等. 三角洲前缘滑塌浊积岩形成过程初探[J]. 沉积学报,2004,22(4):573-579. [Yan Jihua, Chen Shiyue, Song Guoqi, et al. Preliminary study on the formation of fluxoturbidite in front of delta [J]. Acta Sedimentologica Sinica, 2004, 22(4): 573-579.]
[28]
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):1065-1076. [Zou Caineng, Zhao Zhengzhang, Yang Hua, et al. Genetic mechanism and distribution of sandy debris flows in terrestrial lacustrine basin[J]. Acta Sedimentologica Sinica, 2009, 27(6): 1065-1076.]
[29]
刘正华,杨香华,汪贵峰,等. 歧南凹陷沙河街组重力流水道砂体成岩作用和孔隙演化模式[J]. 沉积学报,2007,25(2):183-191. [Liu Zhenghua, Yang Xianghua, Wang Guifeng, et al. Diagenesis and pore evolution of gravity-flow sandbody in Shahejie Formation, Qi'nan depression[J]. Acta Sedimentologica Sinica, 2007, 25(2): 183-191.]
