[1] 陈宇航,姚根顺,吕福亮,鲁银涛,陈亮,唐鹏程,曹全斌. 2017. 东非鲁伍马盆地渐新统深水水道—朵体沉积特征及控制因素. 石油学报, 38(9): 1047-1058. [Chen Y H,Yao G S,Lü F L,Lü Y T,Chen L,Tang P C,Cao Q B.2017. Sedimentary characteristics and controlling factors of Oligocene deep-water channel-lobe in Rovuma Basin of the East Africa. Acta Petrolei Sinica, 38(9): 1047-1058] [2] 黄银涛. 2016. 莺歌海盆地东方区黄流组浅海重力流沉积特征及地质建模. 中国地质大学硕士学位论文. [Huang Y T.2016. Sedimentary characteristics and reservoir modelling of shallow-marine gravity flow deposition from Huangliu Formation in Dongfang area,Yinggehai Basin,northwestern South China Sea. Masteral dissertation of China University of Geosciences] [3] 黄银涛,姚光庆,朱红涛,周锋德. 2016. 莺歌海盆地东方区黄流组重力流砂体的底流改造作用. 石油学报, 37(7): 855-866. [Huang Y T,Yao G Q,Zhu H T,Zhou F D.2016. Reworking of gravity flow sandbody by bottom-current from Huangliu Formation in Dongfang area of Yinggehai Basin,northwestern South China Sea. Acta Petrolei Sinica, 37(7): 855-866] [4] 李华,何幼斌,王振奇. 2011. 深水高弯度水道—堤岸沉积体系形态及特征. 古地理学报, 13(2): 139-149. [Li H,He Y B,Wang Z Q.2011. Morphology and characteristics of deep water high sinuous channel-levee system. Journal of Palaeogeography(Chinese Edition), 13(2): 139-149] [5] 李华,何幼斌,冯斌,郝烃,苏帅亦,张灿,王季欣. 2018. 鄂尔多斯盆地西缘奥陶系拉什仲组深水水道沉积类型及演化. 地球科学, 43(6): 2149-2159. [Li H,He Y B,Feng B,Hao T,Su S Y,Zhang C,Wang J X.2018. Type and evolution of deep-water channel deposits of Ordovician Lashizhong Formation in western margin of Ordos Basin. Earth Science, 43(6): 2149-2159] [6] 李华,何幼斌. 2020. 深水重力流水道沉积研究进展. 古地理学报, 22(1): 161-174. [Li H,He Y B.2020. Research progress on deepwater gravity flow channel deposit. Journal of Palaeogeography(Chinese Edition), 22(1): 161-174] [7] 梁晓伟,鲜本忠,冯胜斌,陈鹏,尤源,吴千然,淡卫东,张文淼. 2021. 鄂尔多斯盆地陇东地区7段重力流砂体构型及其主控因素. 沉积学报. DOI: 10.14027/j.issn.1000-0550.2021.017. [Liang X W,Xian B Z,Feng S B,Chen P,You Y,Wu Q R,Dan W D,Zhang W M.2021. Architecture and main controls of gravity-flow sandbodies in Chang 7 Member,Longdong Area,Ordos Basin. Acta Sedimentologica Sinica. DOI: 10.14027/j.issn.1000-0550.2021.017] [8] 廖计华,吴克强,郭刚,甘华军,孙鸣,蔡露露,朱石磊,刘子玉. 2018. 莺歌海盆地东方区黄流组大型强振幅体沉积内幕及其油气意义. 石油与天然气地质, 39(1): 153-164. [Liao J H,Wu K Q,Guo G,Gan H J,Sun M,Cai L L,Zhu S L,Liu Z Y.2018. Characteristics of the large-scale high-amplitude reflections and its significance in hydrocarbon exploration in the Huangliu Formation of Dongfang area of the Yinggehai Basin,South China Sea. Oil & Gas Geology, 39(1): 153-164] [9] 林煜,吴胜和,王星,赵晓明,凌云,路瑶,张佳佳. 2014. 深水浊积朵叶储层构型模式研究. 天然气地球科学, 25(8): 1197-1204. [Lin Y,Wu S H,Wang X,Zhao X M,Ling Y,Lu Y,Zhang J J.2014. Research on reservoir architecture models of deep-water turbidite lobes. Natural Gas Geoscience, 25(8): 1197-1204] [10] 蔺鹏. 2018. 西非陆坡逆冲构造区海底扇沉积构型研究. 中国石油大学硕士学位论文. [Lin P.2018. Research on the depositional architecture of submarine fan in the thrust zone of continental slope,West Africa. Masteral dissertation of China University of Petroleum] [11] 刘峰,裴健翔,汪洋,高华,潘光超,李洋森. 2015. 古地貌对海底扇沉积过程的控制及与油气富集的关系: 以莺歌海盆地东方区黄流组一段为例. 中国海上油气, 27(4): 37-46. [Liu F,Pei J X,Wang Y,Gao H,Pan G C,Li Y S.2015. Palaeogeomorphologic control on sedimentary process of submarine fans and hydrocarbon accumulation: a case study of Member 1 of Huangliu Formation in DF area,Yinggehai basin. China Offshore Oil and Gas, 27(4): 37-46] [12] 秦国省,吴胜和,郑联勇,喻宸. 2015. 基于沉积过程的三角洲前缘河口坝储层构型精细分析: 以老君庙油田L11小层为例. 岩性油气藏,27(6),55-63. [Qin G S,Wu S H,Zheng L Y,Yu C.2015. Detailed architecture analysis of mouth bar in delta front based on sedimentary process: a case study of L11 layer in Laojunmiao Oilfield. Lithologic Reservoirs,27(6): 55-63] [13] 王华,陈思,甘华军,廖计华,孙鸣. 2015. 浅海背景下大型浊积扇研究进展及堆积机制探讨: 以莺歌海盆地黄流组重力流为例. 地学前缘, 22(1): 21-34. [Wang H,Chen S,Gan H J,Liao J H,Sun M.2015. Accumulation mechanism of large shallow marine turbidite deposites: a case study of gravity flow deposites of the Huangliu Formation in Yinggehai Basin. Earth Science Frontiers, 22(1): 21-34] [14] 王玉,漆智,杨朝强,马华帅,郇金来,任影. 2019. 浅海重力流储层沉积模式新认识. 地质科技情报, 38(4): 16-22. [Wang Y,Qi Z,Yang Z Q,Ma H S,Huan J L,Ren Y.2019. New understanding of sedimentary model of gravity flow reservoir in shallow sea. Geological Science and Technology Information, 38(4): 16-22] [15] 许璐. 2018. 莺歌海盆地东方X区黄流组Ⅰ段浅海海底扇精细表征及主控因素研究. 西安石油大学硕士学位论文. [Xu L.2018. Characterization and main controlling factors of submarine-fan of 1st Member of Huangliu Formation in Dongfang X area,Yinggehai Basin. Masteral Dissertation of Xi'an Shiyou University] [16] 岳绍飞,张辉,覃利娟,杨朝强,漆智,王勇标. 2020. 莺歌海盆地东方区黄流组一段砂质碎屑流沉积模式. 大庆石油地质与开发, 39(4): 9-18. [Yue S F,Zhang H,Qin L J,Yang Z Q,Qi Z,Wang Y B.2020. Sandy debris-flow sedimentary mode in Member 1 of Huangliu Formation in Dongfang area of Yinggehai Basin. Petroleum Geology & Oilfield Development in Daqing, 39(4): 9-18] [17] 张佳佳,吴胜和. 2019. 海底扇朵叶沉积构型研究进展. 中国海上油气, 31(5): 88-106. [Zhang J J,Wu S H.2019. Research progress on the depositional architecture of submarine-fan lobes. China Offshore Oil and Gas, 31(5): 88-106] [18] 张磊夫,李易隆. 2020. 深水浊积朵叶体构型特征: 以爱尔兰克莱尔盆地石炭系露头为例. 石油勘探与开发, 47(5): 925-934. [Zhang L F,Li Y L.2020. Architecture of deepwater turbidite lobes: a case study of Carboniferous turbidite outcrop in the Clare Basin,Ireland. Petroleum Exploration and Development, 47(5): 925-934] [19] 张文彪,段太忠,刘志强,刘彦锋,杨志成,徐睿. 2017. 深水浊积水道沉积构型模式及沉积演化: 以西非M油田为例. 地球科学, 42(2): 273-285. [Zhang W B,Duan T Z,Liu Z Q,Liu Y F,Yang Z C,Xu R.2017. Architecture model and sedimentary evolution of deepwater turbidity channel: a case study of M Oilfield in West Africa. Earth Scinece, 42(2): 273-285] [20] 赵晓明,吴胜和,刘丽. 2012. 尼日尔三角洲盆地Akpo油田新近系深水浊积水道储层构型表征. 石油学报, 33(6): 1049-1058. [Zhao X M,Wu S H,Liu L.2012. Characterization of reservoir architectures for Neogene deepwater turbidity channels of Akpo oilfield,Niger Delta Basin. Acta Petrolei Sinica, 33(6): 1049-1058] [21] 赵晓明,葛家旺,谭程鹏,张文彪,陆文明. 2019. 深海水道储层构型及其对同沉积构造响应机理的研究现状与展望. 中国海上油气, 31(5): 76-87. [Zhao X M,Ge J W,Tan C P,Zhang W B,Lu W M.2019. Research status and prospect of deep sea channel reservoir architecture and its response mechanism to synsedimentary structure. China Offshore Oil and Gas, 31(5): 76-87] [22] 钟泽红,张迎朝,何小胡,徐涛,任建业,刘小燕,凌涛,韩光明. 2015. 莺歌海盆地东方区黄流组层序叠加样式与海底扇内部构型. 海洋地质与第四纪地质, 35(2): 91-99. [Zhong Z H,Zhang Y C,He X H, Xu T,Ren J Y,Liu X Y,Ling T,Han G M.2015. The Sequence stratigraphy of Huangliu Formation and the internal structures of submarine fan in Dongfang area,Yinggehai Basin. Marine Geology & Quaternary Geology, 35(2): 91-99] [23] Celma C,Teloni R,Rustichelli A.2014. Large-scale stratigraphic architecture and sequence analysis of an early Pleistocene submarine canyon fill,Monte Ascensione succession(Peri-Adriatic basin,eastern central Italy).International Journal of Earth Sciences, 103: 843-875. [24] Clark I R,Cartwright J A.2009. Interactions between submarine channel systems and deformation in deepwater fold belts: Examples from the levant basin,eastern mediterranean sea.Marine & Petroleum Geology, 26(8): 1465-1482. [25] Gong C,Steel R J,Wang Y,Lin C,Olariu C.2016a. Grain size and transport regime at shelf edge as fundamental controls on delivery of shelf-edge sands to deepwater. Earth-Science Reviews, 157: 32-60. [26] Gong C,Steel R J,Wang Y,Lin C,Olariu C.2016b. Shelf-margin architecture variability and its role in sediment-budget partitioning into deep-water areas. Earth-Science Reviews, 154: 72-101. [27] Khan Z,Arnott R.2011. Stratal attributes and evolution of asymmetric inner-and outer-bend levee deposits associated with an ancient deepwater channel-levee complex within the Isaac Formation,southern Canada.Marine and Petroleum Geology, 28: 824-842. [28] Kolia V.2007. A review of sinuous channel avulsion patterns in some major deep-sea fans and factors controlling them.Marine and Petroleum Geology, 24: 450-469. [29] Kond A,vishnikov V,Sha L,Mak K,2015.Submarine fan reservoir architecture and heterogeneity influence on hard-to-recover reserves. Achimov Fm.Scientific and Technical Challenges in the Well Drilling Progress,24:12-41. [30] Lamb M A,Anderson K S, Graham, S A.2003. Stratigraphic architecture of a sand-rich,deep-sea depositional system: the stevens sandstone,San Joaquin Basin,California. AAPG Special Publication,13. [31] Liu J P,Xian B Z,Ji Y L,Gong C L,Wang J H,Wang Z,Chen P,Song D L,Wei W Z,Zhang X M,Dou L X.2020. Alternating of aggradation and progradation dominated clinothems and its implications for sediment delivery to deep lake: the Eocene Dongying Depression,Bohai Bay Basin,east China.Marine and Petroleum Geology, 114: 104-197. [32] McArthur A D,Kneller B C,Souza P A,Kuchle J.2016. Characterization of deep-marine channel-levee complex architecture with palynofacies: an outcrop example from the Rosario Formation,Baja California,Mexico.Marine and Petroleum Geology, 73: 157-173. [33] Mutti E,Normark W R.1987. Comparing examples of modern and ancient turbidite systems: problems and concepts.In: Leggett J K,Zuffa G G(eds).Marine Clastic Sedimentology: Concepts and Case Studies.Springer.Netherlands,1-38. [34] Xian B Z,Liu J P,Dong Y L,Lu Z Y,He Y X,Wang J H.2017. Classification and facies sequence model of subaqueous debris flows. Acta Geologica Sinica(English Edition), 91(2): 751-752. [35] Zhang J J,Wu S H,Hu G Y,Fan T E,Yu B,Lin P,Jiang S N,2018. Sea-level control on the submarine fan architecture in a deepwater sequence of the Niger Delta Basin.Marine and Petroleum Geology, 94: 179-197. |