[1] 陈安清,陈洪德,侯明才,等. 2011. 鄂尔多斯盆地中—晚三叠世事件沉积对印支运动Ⅰ幕的指示[J]. 地质学报,85(10):1681-1690.

Chen Anqing, Chen Hongde, Hou Mingcai, et al. 2011. The Middle-Late Triassic event sediments in Ordos Basin: Indicators for episode I of the Indosinian movement[J]. Acta Geologica Sinica, 85(10): 1681-1690.
[2] 陈飞,胡光义,孙立春,等. 2012. 鄂尔多斯盆地富县地区上三叠统延长组砂质碎屑流沉积特征及其油气勘探意义[J]. 沉积学报,30(6):1042-1052.

Chen Fei, Hu Guangyi, Sun Lichun, et al. 2012. Sedimentary characteristics and the significance of petroleum exploration of sandy debris flows of Yanchang Formation of the Upper Triassin, Fuxian area, Ordos Basin[J]. Acta Sedimentologica Sinica, 30(6): 1042-1052.
[3] 杜锦霞. 2015. 松辽盆地北部青山口组重力流特征研究及其地质意义[J]. 沉积学报,33(2):385-393.

Du Jinxia. 2015. Characteristics of gravity flow sediment and its geologic significance in northern Songliao Basin[J]. Acta Sedimentologica Sinica, 2015, 33(2): 385-393.
[4] 冯有良,杨智,张洪,等. 2023. 咸化湖盆细粒重力流沉积特征及其页岩油勘探意义:以准噶尔盆地玛湖凹陷风城组为例[J]. 地质学报,97(3):839-863.

Feng Youliang, Yang Zhi, Zhang Hong, et al. 2023. Fine-grained gravity flow sedimentary features and their petroleum significance within saline lacustrine basins: A case study of the Fengcheng Formation in Mahu Depression, Junggar Basin, China[J]. Acta Geologica Sinica, 97(3): 839-863.
[5] 付国民,赵俊兴,张志升,等. 2010. 鄂尔多斯盆地东南缘三叠系延长组物源及沉积体系特征[J]. 矿物岩石,30(1):99-105.

Fu Guomin, Zhao Junxing, Zhang Zhisheng, et al. 2010. The pro-venance and features of depositional system in the Yanchang Formation of Triassic in southeast area of Ordos Basin[J]. Journal of Mineralogy and Petrology, 30(1): 99-105.
[6] 付金华,罗顺社,牛小兵,等. 2015. 鄂尔多斯盆地陇东地区长7段沟道型重力流沉积特征研究[J]. 矿物岩石地球化学通报,2015,34(1):29-37.

Fu Jinhua, Luo Shunshe, Niu Xiaobing, et al. 2015. Sedimentary characteristics of channel type gravity flow of the member 7 of Yanchang Formation in the Longdong area, Ordos Basin[J]. Bulletin of Mineralogy, Petrology and Geochemistry, 34(1): 29-37.
[7] 高宇慧,佟莹,黄会会,等. 2022. 准噶尔盆地沙湾凹陷西斜坡陆相湖盆重力流沉积特征与油气关系[J]. 新疆地质,40(3):378-381.

Gao Yuhui, Tong Ying, Huang Huihui, et al. 2022. Relationship between gravity flow sedimentary characteristics and oil and gas in continental lake basin on the west slope of Shawan Sag, Junggar Basin[J]. Xinjiang Geology, 40(3): 378-381.
[8] 葛毓柱,钟建华,李勇,等. 2015. 鄂尔多斯盆地富县地区三叠系延长组长8—长6油层组类眼状构造成因探讨[J]. 古地理学报,17(6):797-804.

Ge Yuzhu, Zhong Jianhua, Li Yong, et al. 2015. Genetic discussion about eye-like structure of the Chang 8-6 intervals of Triassic Yanchang Formation in Fuxian area, Ordos Basin[J]. Journal of Palaeogeography, 17(6): 797-804.
[9] 黄军平,杨田,张艳,等. 2023. 湖相细粒沉积岩沉积动力学机制与沉积模式:以鄂尔多斯盆地铜川地区延长组长7油层组露头为例[J]. 沉积学报,41(4):1227-1239.

Huang Junping, Yang Tian, Zhang Yan, et al. 2023. Sedimentary dynamics and deposition model of lacustrine finegrained sedimentary rocks: A case study of the Chang 7 oil member from the Yanchang Formation in the Ordos Basin,Tongchuan area[J]. Acta Sedimentologica Sinica, 41(4): 1227-1239.
[10] 姜超. 2018. 断陷湖盆斜坡带重力流砂体沉积特征及沉积模式:以沾化凹陷渤南洼陷南部斜坡带沙三段为例[J]. 油气地质与采收率,25(1):6-13.

Jiang Chao. 2018. Characteristics and model of gravity flow sand body deposition in the slope zone of rifted lacustrine basin: A case study from the Sha3 member in the south slope zone of Bonan Sag, Zhanhua Depression[J]. Petroleum Geology and Recovery Efficiency, 25(1): 6-13.
[11] 李克永,熊山,牛斌莉,等. 2018. 鄂尔多斯盆地南部上三叠统重力流沉积的主控因素[J]. 西北大学学报(自然科学版),48(4):603-610.

Li Keyong, Xiong Shan, Niu Binli, et al. 2018. The main controlling factors of gravity flow of the Upper Triassic in the southern Ordos Basin[J]. Journal of Northwest University (Natural Science Edition), 48(4): 603-610.
[12] 李相博,付金华,陈启林,等. 2011. 砂质碎屑流概念及其在鄂尔多斯盆地延长组深水沉积研究中的应用[J]. 地球科学进展,26(3):286-294.

Li Xiangbo, Fu Jinhua, Chen Qilin, et al. 2011. 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, 26(3): 286-294.
[13] 李相博,刘化清,陈启林,等. 2010. 大型坳陷湖盆沉积坡折带特征及其对砂体与油气的控制作用:以鄂尔多斯盆地三叠系延长组为例[J]. 沉积学报,28(4):717-729.

Li Xiangbo, Liu Huaqing, Chen Qilin, et al. 2010. Characteristics of slope break belt in large depression lacustrine basin and its controlling effect on sandbody and petroleum: Taking the Triassic Yanchang Formation in the Ordos Basin as an example[J]. Acta Sedimentologica Sinica, 28(4): 717-729.
[14] 李相博,刘化清,完颜容,等. 2009. 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,21(4):19-21.

Li Xiangbo, Liu Huaqing, Rong Wanyan, et al. 2009. First discovery of the sandy debris flow from the Triassic Yanchang Formation, Ordos Basin[J]. Lithologic Reservoirs, 21(4): 19-21.
[15] 李相博,刘化清,张忠义,等. 2014. 深水块状砂岩碎屑流成因的直接证据:“泥包砾”结构:以鄂尔多斯盆地上三叠统延长组研究为例[J]. 沉积学报,32(4):611-622.

Li Xiangbo, Liu Huaqing, Zhang Zhongyi, et al. 2014. “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.
[16] 李晓路,马芳侠,贺永红,等. 2022. 鄂尔多斯盆地东南部长6段重力流沉积类型及成因[J]. 断块油气田,29(1):40-46.

Li Xiaolu, Ma Fangxia, He Yonghong, et al. 2022. Sedimentary types and genesis of gravity flow in Chang 6 member of southeastern Ordos Basin[J]. Fault-Block Oil & Gas Field, 29(1): 40-46.
[17] 梁晓伟,鲜本忠,冯胜斌,等. 2022. 鄂尔多斯盆地陇东地区长7段重力流砂体构型及其主控因素[J]. 沉积学报,40(3):641-652.

Liang Xiaowei, Xian Benzhong, Feng Shengbin, et al. 2022. Architecture and main controls of gravity-flow sandbodies in Chang 7 member, Longdong area, Ordos Basin[J]. Acta Sedimentologica Sinica, 40(3): 641-652.
[18] 廖纪佳,朱筱敏,邓秀芹,等. 2013. 鄂尔多斯盆地陇东地区延长组重力流沉积特征及其模式[J]. 地学前缘,20(2):29-39.

Liao Jijia, Zhu Xiaomin, Deng Xiuqin, et al. 2013. Sedimentary characteristics and model of gravity flow in Triassic Yanchang Formation of Longdong area in Ordos Basin[J]. Earth Science Frontiers, 20(2): 29-39.
[19] 刘芬,朱筱敏,梁建设,等. 2020. 鄂尔多斯盆地延长组深水重力流岩相发育特征及其储集性[J]. 海洋地质前沿,36(6):46-55.

Liu Fen, Zhu Xiaomin, Liang Jianshe, et al. 2020. Lithofacies characteristics of Gravity flow deposits and their impacts on reservoir quality in the Yanchang Formation, Ordos Basin[J]. Marine Ge-ology Frontiers, 36(6): 46-55.
[20] 刘磊,陈洪德,钟怡江,等. 2017. 渤海湾盆地辽东湾坳陷古近系沙一段、沙二段重力流沉积及其油气勘探意义[J]. 古地理学报,19(5):807-818.

Liu Lei, Chen Hongde, Zhong Yijiang, et al. 2017. Gravity-flow deposits in the members 1 and 2 of Paleogene Shahejie Formation and their significance for oil-gas exploration in Liaodong Bay Depression, Bohai Bay Basin[J]. Journal of Palaeogeography, 19(5): 807-818.
[21] 刘招君. 2003. 湖泊水下扇沉积特征及影响因素:以伊通盆地莫里青断陷双阳组为例[J]. 沉积学报,21(1):148-154.

Liu Zhaojun. 2003. Lacus subaqueous fan sedimentary characteristics and influence factors: A case study of Shuangyang Formation in Moliqing fault subsidence of Yitong Basin[J]. Acta Sedimentologica Sinica, 21(1): 148-154.
[22] 吕奇奇,付金华,罗顺社,等. 2022. 坳陷湖盆重力流水道—朵叶复合体沉积特征及模式:以鄂尔多斯盆地西南部三叠系延长组长7段为例[J]. 石油勘探与开发,49(6):1143-1156.

Qiqi Lü, Fu Jinhua, Luo Shunshe, et al. 2022. Sedimentary characteristics and model of gravity flow channel - lobe complex in a depression lake basin: A case study of Chang 7 member of Triassic Yanchang Formation in southwestern Ordos Basin, NW China[J]. Petroleum Exploration and Development, 49(6): 1143-1156.
[23] 潘树新. 2012. 大型坳陷湖盆深水重力流研究:以松辽盆地青山口组为例[D]. 成都:成都理工大学.

Pan Shuxin. 2012. Deep-water gravity deposits in Songliao terrestrial basin[D]. Chengdu: Chengdu University of Technology.
[24] 冉逸轩,周翔. 2020. 鄂尔多斯盆地西南部延长组6段重力流沉积特征及其油气地质意义[J]. 沉积学报,38(3):571-579.

Ran Yixuan, Zhou Xiang. 2020. Sedimentary characteristics and petroleum geological significance of the Chang 6 gravity flow in the southwest Ordos Basin[J]. Acta Sedimentologica Sinica, 38(3): 571-579.
[25] 孙宁亮,钟建华,王书宝,等. 2017. 鄂尔多斯盆地南部三叠系延长组深水重力流沉积特征及其石油地质意义[J]. 古地理学报,19(2):299-314.

Sun Ningliang, Zhong Jianhua, Wang Shubao, et al. 2017. Sedimentary characteristics and petroleum geologic significance of deep-water gravity flow of the Triassic Yanchang Formation in southern Ordos Basin[J]. Journal of Palaeogeography, 19(2): 299-314.
[26] 王德坪. 1991. 湖相内成碎屑流的沉积及形成机理[J]. 地质学报,65(4):299-316.

Wang Deping. 1991. The sedimentation and formation mechanism of lacustrine endogenic debris flow[J]. Acta Geologica Sinica, 65(4): 299-316.
[27] 王颖,王晓州,王英民,等. 2010. 沉积物理模拟实验在确定重力流临界坡度中的应用[J]. 成都理工大学学报(自然科学版),37(4):463-468.

Wang Ying, Wang Xiaozhou, Wang Yingmin, et al. 2010. Determination of the gravity flow critical gradient using sedimentary simulation experiment[J]. Journal of Chengdu University of Technology (Science & Technology Edition), 37(4): 463-468.
[28] 王予帆,尹天豪,丁毅,等. 2022. 二连盆地阿尔凹陷东部陡坡带腾一下亚段重力流沉积特征[J]. 断块油气田,29(4):489-495,538.

Wang Yufan, Yin Tianhao, Ding Yi, et al. 2022. Sedimentary characteristics of gravity flow from Lower submember of the First member of Tengger Formation in the eastern steep slope belt of Aer Sag, Erlian Basin[J]. Fault-Block Oil & Gas Field, 29(4): 489-495, 538.
[29] 鲜本忠,万锦峰,姜在兴,等. 2012. 断陷湖盆洼陷带重力流沉积特征与模式:以南堡凹陷东部东营组为例[J]. 地学前缘,19(1):121-135.

Xian Benzhong, Wan Jinfeng, Jiang Zaixing, et al. 2012. Sedimentary characteristics and model of gravity flow deposition in the depressed belt of rift lacustrine basin: A case study from Dongying Formation in Nanpu Depression[J]. Earth Science Frontiers, 2012, 19(1): 121-135.
[30] 鄢继华,陈世悦,宋国奇,等. 2004. 三角洲前缘滑塌浊积岩形成过程初探[J]. 沉积学报,22(4):573-578.

Yan Jihua, Chen Shiyue, Song Guoqi, et al. 2004. Preliminary study on the formation of fluxoturbidite in front of delta[J]. Acta Sedimentologica Sinica, 2004, 22(4): 573-578.
[31] 杨剑萍,黄雅睿,卢惠东,等. 2021. 东营凹陷营11北地区沙三中亚段重力流触发机制[J]. 中国石油大学学报(自然科学版),45(4):1-11.

Yang Jianping, Huang Yarui, Lu Huidong, et al. 2021. Triggering mechanism of gravity flow sandbodies of middle Es3 member in the north of well Ying 11, Dongying Depression[J]. Journal of China University of Petroleum (Edition of Natural Science), 45(4): 1-11.
[32] 杨仁超,何治亮,邱桂强,等. 2014. 鄂尔多斯盆地南部晚三叠世重力流沉积体系[J]. 石油勘探与开发,41(6):661-670.

Yang Renchao, He Zhiliang, Qiu Guiqiang, et al. 2014. Late Triassic gravity flow depositional systems in the southern Ordos Basin[J]. Petroleum Exploration and Development, 41(6): 661-670.
[33] 杨田,操应长,田景春. 2021. 浅谈陆相湖盆深水重力流沉积研究中的几点认识[J]. 沉积学报,39(1):88-111.

Yang Tian, Cao Yingchang, Tian Jingchun. 2021. Discussion on research of deep-water gravity flow deposition in lacustrine basin[J]. Acta Sedimentologica Sinica, 39(1): 88-111.
[34] 张关龙,陈世悦,鄢继华,等. 2006. 三角洲前缘滑塌浊积体形成过程模拟[J]. 沉积学报,24(1):50-55.

Zhang Guanlong, Chen Shiyue, Yan Jihua, et al. 2006. Simulation of luxoturbidite in front of delta[J]. Acta Sedimentologica Sinica, 24(1): 50-55.
[35] 邹才能,赵政璋,杨华,等. 2009. 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.

Zou Caineng, Zhao Zhengzhang, Yang Hua, et al. 2009. Genetic mechanism and distribution of sandy debris flows in terrestrial lacustrine basin[J]. Acta Sedimentologica Sinica, 27(6): 1065-1075.
[36] Bouma A H. 1962. Sedimentology of some flysch deposits: A graphic approach to facies interpretation[M]. Amsterdam: Elsevier: 1-168.
[37] Johnson D. 1938. The origin of submarine canyons[J]. Journal of Geomorphology, 1: 111-340.
[38] Kuenen P H, Migliorini C I. 1950. Turbidity currents as a cause of graded bedding[J]. The Journal of Geology, 58(2): 91-127.
[39] Passega R. 1964. Grain size representation by CM patterns as a geologic tool[J]. Journal of Sedimentary Research, 34(4): 830-847.
[40] Shanmugam G. 1996. High-density turbidity currents: Are they sandy debris flows?[J]. Journal of Sedimentary Research, 66(1): 2-10.
[41] Shanmugam G. 2002. Ten turbidite myths[J]. Earth-Science Reviews, 58(3/4): 311-341.
[42] Shanmugam G. 2009. Slides, slumps, flows debris, and turbidity currents[M]//Steele J H. Encyclopedia of ocean sciences. 2nd ed. London: Elsevier: 447-467.
[43] Shanmugam G. 2013. New perspectives on deep-water sandstones: Implications[J]. Petroleum Exploration and Development, 40(3): 316-324.
[44] Shanmugam G, Lehtonen L R, Straume T, et al. 1994. Slump and debris-flow dominated upper slope facies in the Cretaceous of the Norwegian and northern North Seas (61-67°N): Implications for sand distribution[J]. AAPG Bulletin, 78(6): 910-937.
[45] Wang R Y, Wang G P, Zhao G, et al. 2023. Geological characteristics and resources potential of shale oil in Chang 7 member of Upper Triassic Yanchang Formation in Fuxian area, southern Ordos Basin, western China[J]. Unconventional Resources, 3: 237-247.