[1] Deptuck M E, Sylvester Z, Pirmez C, et al. Migration-aggradation history and 3-D seismic geomorphology of submarine channels in the Pleistocene Benin-major canyon, western Niger Delta slope[J]. Marine and Petroleum Geology, 2007, 24（6/7/8/9）： 406-433.
[2] 刘军,庞雄,颜承志,等. 南海北部陆坡白云深水区深水沉积结构要素[J]. 吉林大学学报（地球科学版）,2011,41（4）：992-998.

Liu Jun, Pang Xiong, Yan Chengzhi, et al. Deepwater depositional elements in Baiyun deepwater area of the northern continental slope, South China Sea[J]. Journal of Jilin University （Earth Science Edition）, 2011, 41（4）： 992-998.
[3] Ashiru O R, Qin Y, Wu S. Structural controls on submarine channel morphology, evolution, and architecture, offshore western Niger Delta[J]. Marine and Petroleum Geology, 2020, 118： 104413.
[4] Posamentier H W. Depositional elements associated with a basin floor channel-levee system： Case study from the gulf of Mexico[J]. Marine and Petroleum Geology, 2003, 20（6/7/8）： 677-690.
[5] Dmitrieva E, Jackson C A L, Huuse M, et al. Paleocene deep-water depositional systems in the North Sea Basin： A 3D seismic and well data case study, offshore Norway[J]. Petroleum Geoscience, 2012, 18（1）： 97-114.
[6] 陈昱瑶,周江羽,钟佳,等. 南海西北缘深水水道体系的地震响应及其演化[J]. 海洋地质与第四纪地质,2014,34（2）：69-78.

Chen Yuyao, Zhou Jiangyu, Zhong Jia, et al. Seismic characteristics of deepwater channel system in northwestern margin of South China Sea and its evolution[J]. Marine Geology & Quaternary Geology, 2014, 34（2）： 69-78.
[7] 陈宇航,姚根顺,吕福亮,等. 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[J]. 石油学报,2017,38（9）：1047-1058.

Chen Yuhang, Yao Genshun, Fuliang Lü, et al. Sedimentary characteristics and controlling factors of Oligocene deep-water channel-lobe in Rovuma Basin of the East Africa[J]. Acta Petrolei Sinica, 2017, 38（8）： 1047-1058.
[8] 康洪全,孟金落,程涛,等. 巴西坎波斯盆地深水沉积体系特征[J]. 石油勘探与开发,2018,45（1）：93-104.

Kang Hongquan, Meng Jinluo, Cheng Tao, et al. Characteristics of deep water depositional system in Campos Basin, Brazil[J]. Petroleum Exploration and Development, 2018, 45（1）： 93-104.
[9] 姚悦,周江羽,雷振宇,等. 西沙海槽盆地强限制性中央峡谷水道地震相与内部结构的分段特征[J]. 沉积学报,2018,36（4）：787-795.

Yao Yue, Zhou Jiangyu, Lei Zhenyu, et al. High restriction seismic facies and inner structural segmentation features of the central canyon channel systems in Xisha trough basin[J]. Acta Sedimentologica Sinica, 2018, 36（4）： 787-795.
[10] Wu W, Li Q, Yu J, et al. The Central Canyon depositional patterns and filling process in east of Lingshui Depression, Qiongdongnan Basin, northern South China Sea[J]. Geological Journal, 2018, 53（6）： 3064-3081.
[11] 李全,吴伟,康洪全,等. 西非下刚果盆地深水水道沉积特征及控制因素[J]. 石油与天然气地质,2019,40（4）：917-929.

Li Quan, Wu Wei, Kang Hongquan, et al. Characteristics and controlling factors of deep-water channel sedimentation in Lower Congo Basin, West Africa[J]. Oil & Gas Geology, 2019, 40（4）： 917-929.
[12] 吴伟,刘俊成,刘琮滢,等. 珠江口盆地白云凹陷珠江组陆架边缘三角洲沉积与生物遗迹特征[J]. 中国石油大学学报（自然科学版）,2020,44（4）：152-162.

Wu Wei, Liu Juncheng, Liu Cong-ying, et al. Sedimentary and ichonology characteristics of continental shelf-edge delta of Zhujiang Formation in Baiyun Sag, Pearl River Mouth Basin[J]. Journal of China University of Petroleum （Edition of Natural Science）, 2020, 44（4）： 152-162.
[13] Deptuck M E, Steffens G S, Barton M, et al. Architecture and evolution of upper fan channel-belts on the Niger Delta slope and in the Arabian Sea[J]. Marine and Petroleum Geology, 2003, 20（6/7/8）： 649-676.
[14] Mayall M, Jones E, Casey M. Turbidite channel reservoirs—Key elements in facies prediction and effective development[J]. Marine and Petroleum Geology, 2006, 23（8）： 821-841.
[15] 张文彪,段太忠,刘志强,等. 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[J]. 地球科学,2017,42（2）：273-285.

Zhang Wenbiao, Duan Taizhong, Liu Zhiqiang, et al. Architecture model and sedimentary evolution of deepwater turbidity channel： A case study of M oilfield in West Africa[J]. Earth Science, 2017, 42（2）： 273-285.
[16] Wood L J, Mize-Spansky K L. Quantitative seismic geomorphology of a Quaternary leveed-channel system, offshore eastern Trinidad and Tobago, northeastern South America[J]. AAPG Bulletin, 2009, 93（1）： 101-125.
[17] 赵晓明,吴胜和,刘丽. 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[J]. 石油学报,2012,33（6）：1049-1058.

Zhao Xiaoming, Wu Shenghe, Liu Li. Characterization of reservoir architectures for Neogene deepwater turbidity channels of Akpo oilfield, Niger Delta Basin[J]. Acta Petrolei Sinica, 2012, 33（6）： 1049-1058.
[18] 赵晓明,刘丽,谭程鹏,等. 海底水道体系沉积构型样式及控制因素：以尼日尔三角洲盆地陆坡区为例[J]. 古地理学报,2018,20（5）：825-840.

Zhao Xiaoming, Liu Li, Tan Chengpeng, et al. Styles of submarine-channel architecture and its controlling factors： A case study from the Niger Delta Basin slope[J]. Journal of Palaeogeography, 2018, 20（5）： 825-840.
[19] Alpak F O, Barton M D, Naruk S J. The impact of fine-scale turbidite channel architecture on deep-water reservoir performance[J]. AAPG Bulletin, 2013, 97（2）： 251-284.
[20] Peakall J, McCaffrey B, Kneller B. A process model for the evolution, morphology, and architecture of sinuous submarine channels[J]. Journal of Sedimentary Research, 2000, 70（3）： 434-448.
[21] Gee M J R, Gawthorpe R L, Bakke K, et al. Seismic geomorphology and evolution of submarine channels from the Angolan continental margin[J]. Journal of Sedimentary Research, 2007, 77（5）： 433-446.
[22] Labourdette R. Integrated three-dimensional modeling approach of stacked turbidite channels[J]. AAPG Bulletin, 2007, 91（11）： 1603-1618.
[23] Harishidayat D, Omosanya K O, Johansen S E. 3D seismic interpretation of the depositional morphology of the Middle to Late Triassic fluvial system in eastern Hammerfest Basin, Barents Sea[J]. Marine and Petroleum Geology, 2015, 68： 470-479.
[24] Li Quan, Wu Wei, Liang Jianshe, et al. Deep-water channels in the Lower Congo Basin： Evolution of the geomorphology and depositional environment during the Miocene[J]. Marine and Petroleum Geology, 2020, 115： 104260.
[25] 袁圣强,曹锋,吴时国,等. 南海北部陆坡深水曲流水道的识别及成因[J]. 沉积学报,2010,28（1）：68-75.

Yuan Sheng- qiang, Cao Feng, Wu Shiguo, et al. Architecture and origin of deepwater sinuous channel on the slope of northern South China Sea[J]. Acta Sedimentologica Sinica, 2010, 28（1）： 68-75.
[26] Gong C L, Wang Y M, Zhu W L, et al. Upper Miocene to Quaternary unidirectionally migrating deep-water channels in the Pearl River Mouth Basin, northern South China Sea[J]. AAPG Bulletin, 2013, 97（2）： 285-308.
[27] Fonnesu M, Palermo D, Galbiati M, et al. A new world-class deep-water play-type, deposited by the syndepositional interaction of turbidity flows and bottom currents： The giant Eocene Coral Field in northern Mozambique[J]. Marine and Petroleum Geology, 2020, 111： 179-201.
[28] Bull S, Browne G H, Arnot M J, et al. Influence of mass transport deposit （MTD） surface topography on deep-water deposition： An example from a predominantly fine-grained continental margin, New Zealand[M]//Georgiopoulou A, Amy L A, Benetti S, et al. Subaqueous mass movements and their consequences： Advances in process understanding, monitoring and hazard assessments. London： Geological Society, 2020： SP 500-2019-192.
[29] King P R, Thrasher G P. Cretaceous-Cenozoic geology and petroleum systems of the Taranaki Basin, New Zealand[M]. Lower Hutt： Institute of Geological & Nuclear Sciences, 1996： X-191.
[30] Uruski C I. New Zealand’s deepwater frontier[J]. Marine and Petroleum Geology, 2010, 27（9）： 2005-2026.
[31] Rad F. PEP 38451 romney-1 well completion report[R]. PR4951, New Zealand： Company for NZP&M, 2015.
[32] Higgs K E, Arnot M J, Browne G H, et al. Reservoir potential of Late Cretaceous terrestrial to shallow marine sandstones, Taranaki Basin, New Zealand[J]. Marine and Petroleum Geology, 2010, 27（9）： 1849-1871.
[33] King P R, Scott G H, Robinson P H. Description, correlation and depositional history of Miocene sediments outcropping along north Taranaki coast[M]. Lower Hutt： Institute of Geological & Nuclear Sciences Limited, 1993： 199.
[34] Shell BP Todd Oil Services Ltd. Well resume Te ranga-1, Ppl 38107 Taranaki New Plymouth. Ministry of Economic Development unpublished petroleum report[R]. Wellington： Ministry of Economic Development, 1986 ： 809, 818.
[35] Wizevich M C, Thrasher G P, Bussell M R, et al. Evidence for marine deposition in the Late Cretaceous Pakawau group, northwest Nelson[J]. New Zealand Journal of Geology and Geophysics, 1992, 35（3）： 363-369.
[36] Sykes R, Zink K G, Funnell R H. Chemometric analysis of oil families and oil-source rock correlations in New Zealand Basins： Implications for source kitchens and migration pathways[C]//Proceedings of 2010 New Zealand petroleum conference： Conference proceedings： Transformation. Wellington： Crown Minerals, Ministry of Economic Development, 2010： 20.
[37] Hayward B W, Wood R A. Computer-generated geohistory plots for taranaki drillhole sequences[R]. New Zealand Geological Survey Report PAL 147, Lower Hutt： New Zealand Geological Survey, 1989： 73.
[38] King P R, Thrasher G P. Post-Eocene development of the Taranaki Basin, New Zealand： Convergent overprint of a passive margin[M]//Watkins J S, Feng Z Q, McMillen K J. Geology and geophysics of continental margins. Tulsa： American Association of Petroleum Geologists, 1992： 93-118.
[39] Nwoko J, Kane I, Huuse M. Mass transport deposit （MTD） relief as a control on post-MTD sedimentation： Insights from the Taranaki Basin, offshore New Zealand[J]. Marine and Petroleum Geology, 2020, 120： 104489.
[40] 谢清惠,邓宏文. 地层切片技术在中新统刚果扇中的应用[J]. 大庆石油地质与开发,2013,32（6）：135-140.

Xie Qinghui, Deng Hongwen. Application of strata slicing technique in Miocene Congo Fan[J]. Petroleum Geology & Oilfield Development in Daqing, 2013, 32（6）： 135-140.
[41] McHargue T, Pyrcz M J, Sullivan M D, et al. Architecture of turbidite channel systems on the continental slope： Patterns and predictions[J]. Marine and Petroleum Geology, 2011, 28（3）： 728-743.
[42] 李华,何幼斌,王振奇. 深水高弯度水道—堤岸沉积体系形态及特征[J]. 古地理学报,2011,13（2）：139-149.

Li Hua, He Youbin, Wang Zhenqi. Morphology and characteristics of deep water high sinuous channel-levee system[J]. Journal of Palaeogeography, 2011, 13（2）： 139-149.