Volume 42 Issue 11
Nov.  2023
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Guangxu Wang, Wei Wu, Changsong Lin, Quan Li, Xiaoming Zhao, Yongsheng Zhou, Weiqing Liu, Shiqin Liang. Sedimentary elements, evolutions and controlling factors of the Miocene channel system: a case study of the deep-water Taranaki Basin in New Zealand[J]. Acta Oceanologica Sinica, 2023, 42(11): 44-58. doi: 10.1007/s13131-023-2191-9
Citation: Guangxu Wang, Wei Wu, Changsong Lin, Quan Li, Xiaoming Zhao, Yongsheng Zhou, Weiqing Liu, Shiqin Liang. Sedimentary elements, evolutions and controlling factors of the Miocene channel system: a case study of the deep-water Taranaki Basin in New Zealand[J]. Acta Oceanologica Sinica, 2023, 42(11): 44-58. doi: 10.1007/s13131-023-2191-9

Sedimentary elements, evolutions and controlling factors of the Miocene channel system: a case study of the deep-water Taranaki Basin in New Zealand

doi: 10.1007/s13131-023-2191-9
Funds:  The National Natural Science Foundation of China under contract Nos 42077410 and 41872112.
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  • Corresponding author: E-mail: wei@hpu.edu.cn
  • Received Date: 2022-12-10
  • Accepted Date: 2023-02-22
  • Available Online: 2023-12-25
  • Publish Date: 2023-11-01
  • Deep-water channel systems are important petroleum reservoirs, and many have been discovered worldwide. Understanding deep-water channel sedimentary elements and evolution is helpful for deep-sea petroleum exploration and development. Based on high-resolution 3D seismic data, the Miocene channel system in the deep-water Taranaki Basin, New Zealand, was analyzed by using seismic interpretation techniques such as interlayer attribute extraction and strata slicing. The channel system was divided into five composite channels (CC-I to CC-V) according to four secondary level channel boundaries, and sedimentary elements such as channels, slump deposits, inner levees, mass transport deposits, and hemipelagic drape deposits were identified in the channel system. The morphological characteristics of several composite channels exhibited stark variances, and the overall morphology of the composite channels changed from relatively straight to highly sinuous to relatively straight. The evolution of the composite channels involved a gradual and repeated process of erosion and filling, and the composite channels could be divided into three evolutionary stages: initial erosion-filling, later erosion-filling (multistage), and channel abandonment. The middle Miocene channel system may have formed as a consequence of combined regional tectonic activity and global climatic change, and its intricate morphological alterations may have been influenced by the channel’s ability to self-regulate and gravity flow properties. When studying the sedimentary evolution of a large-scale deep-water channel system in the Taranaki Basin during the Oligocene−Miocene, which transitioned from a passive margin to plate convergence, it can be understood how tectonic activity affected the channel and can also provide a theoretical reference for the evolution of the deep-water channels in areas with similar tectonic conversion environments around the world.
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  • Abreu V, Sullivan M, Pirmez C, et al. 2003. Lateral accretion packages (LAPS): an important reservoir element in deep water sinuous channels. Marine and Petroleum Geology, 20(6–8): 631–648. doi: 10.1016/j.marpetgeo.2003.08.003
    Alpak F O, Barton M D, Naruk S J. 2013. The impact of fine-scale turbidite channel architecture on deep-water reservoir performance. AAPG Bulletin, 97(2): 251–284. doi: 10.1306/04021211067
    Babonneau N, Savoye B, Cremer M, et al. 2002. Morphology and architecture of the present canyon and channel system of the Zaire deep-sea fan. Marine and Petroleum Geology, 19(4): 445–467. doi: 10.1016/S0264-8172(02)00009-0
    Babonneau N, Savoye B, Cremer M, et al. 2004. Multiple terraces within the deep incised Zaire Valley (ZaiAngo Project): are they confined levees?. In: Lomas S A, Joseph P, eds. Confined Turbidite Systems. Geological Society Special Publications, 91-114
    Babonneau N, Savoye B, Cremer M, et al. 2010. Sedimentary architecture in meanders of a submarine channel: detailed study of the present Congo turbidite channel (Zaiango Project). Journal of Sedimentary Research, 80(10): 852–866. doi: 10.2110/jsr.2010.078
    Baur J R. 2012. Regional seismic attribute analysis and Tectono-stratigraphy of offshore south-western Taranaki Basin, New Zealand [dissertation]. Wellington: Victoria University of Wellington, 373
    Bull S, Nicol A, Strogen D, et al. 2019. Tectonic controls on Miocene sedimentation in the Southern Taranaki Basin and implications for New Zealand plate boundary deformation. Basin Research, 31(2): 253–273. doi: 10.1111/bre.12319
    Chima K I, Do Couto D, Leroux E, et al. 2019. Seismic stratigraphy and depositional architecture of Neogene intraslope basins, offshore western Niger Delta. Marine and Petroleum Geology, 109: 449–468. doi: 10.1016/j.marpetgeo.2019.06.030
    Clark J D, Pickering K T. 1996. Architectural elements and growth patterns of submarine channels: application to hydrocarbon exploration. AAPG Bulletin, 80(2): 194–220
    Collot J, Herzer R, Lafoy Y, et al. 2009. Mesozoic history of the Fairway-Aotea basin: implications for the early stages of Gondwana fragmentation. Geochemistry, Geophysics, Geosystems, 10(12): Q12019
    D’Alpaos A, Ghinassi M, Finotello A, et al. 2017. Tidal meander migration and dynamics: a case study from the Venice Lagoon. Marine and Petroleum Geology, 87: 80–90. doi: 10.1016/j.marpetgeo.2017.04.012
    Deptuck M E, Sylvester Z, Pirmez C, et al. 2007. Migration-aggradation history and 3-D seismic geomorphology of submarine channels in the pleistocene benin-major canyon, western Niger delta slope. Marine and Petroleum Geology, 24(6–9): 406–433. doi: 10.1016/j.marpetgeo.2007.01.005
    Eschard R, Albouy E, Deschamps R, et al. 2003. Downstream evolution of turbiditic channel complexes in the Pab Range outcrops (Maastrichtian, Pakistan). Marine and Petroleum Geology, 20(6–8): 691–710. doi: 10.1016/j.marpetgeo.2003.02.004
    Fonnesu M, Palermo D, Galbiati M, et al. 2020. 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. Marine and Petroleum Geology, 111: 179–201. doi: 10.1016/j.marpetgeo.2019.07.047
    Gamboa D, Alves T M. 2015. Spatial and dimensional relationships of submarine slope architectural elements: a seismic-scale analysis from the Espírito Santo Basin (SE Brazil). Marine and Petroleum Geology, 64: 43–57. doi: 10.1016/j.marpetgeo.2015.02.035
    Gee M J R, Gawthorpe R L. 2006. Submarine channels controlled by salt tectonics: examples from 3D seismic data offshore Angola. Marine and Petroleum Geology, 23(4): 443–458. doi: 10.1016/j.marpetgeo.2006.01.002
    Gong Chenglin, Wang Yingmin, Zhu Weilin, et al. 2013. Upper Miocene to Quaternary unidirectionally migrating deep-water channels in the Pearl River Mouth Basin, northern South China Sea. AAPG Bulletin, 97(2): 285–308. doi: 10.1306/07121211159
    Haq B U, Hardenbol J, Vail P R. 1987. Chronology of fluctuating sea levels since the Triassic. Science, 235(4793): 1156–1167. doi: 10.1126/science.235.4793.1156
    Higgs K E, Arnot M J, Browne G H, et al. 2010. Reservoir potential of Late Cretaceous terrestrial to shallow marine sandstones, Taranaki Basin, New Zealand. Marine and Petroleum Geology, 27(9): 1849–1871. doi: 10.1016/j.marpetgeo.2010.08.002
    Higgs K E, King P R. 2018. Sandstone provenance and sediment dispersal in a complex tectonic setting: Taranaki Basin, New Zealand. Sedimentary Geology, 372: 112–139. doi: 10.1016/j.sedgeo.2018.05.004
    Jia Jianzhong, Kang Hongquan, Liu Xiaolong, et al. 2019. Climate events and their bearing on turbidite channels of the Congo Fan. Marine Geology Frontiers (in Chinese), 35(5): 2–10
    King P R. 2000. Tectonic reconstructions of New Zealand: 40 Ma to the Present. New Zealand Journal of Geology and Geophysics, 43(4): 611–638. doi: 10.1080/00288306.2000.9514913
    King P R, Thrasher G P. 1992. Post-Eocene development of the Taranaki Basin, New Zealand: Convergent overprint of a passive margin. In: Watkins J S, Feng Zhiqiang, McMillen K J, eds. Geology and Geophysics of Continental Margins. Tulsa: American Association of Petroleum Geologists, 93–118
    King P R, Thrasher G P. 1996. Cretaceous-cenozoic Geology and Petroleum Systems of the Taranaki Basin, New Zealand. Lower Hutt: Institute of Geological & Nuclear Sciences Monograph, 243
    Kolla V, Posamentier H W, Wood L J. 2007. Deep-water and fluvial sinuous channels—Characteristics, similarities and dissimilarities, and modes of formation. Marine and Petroleum Geology, 24(6–9): 388–405. doi: 10.1016/j.marpetgeo.2007.01.007
    La Marca K, Bedle H. 2022. Deepwater seismic facies and architectural element interpretation aided with unsupervised machine learning techniques: Taranaki Basin, New Zealand. Marine and Petroleum Geology, 136: 105427. doi: 10.1016/j.marpetgeo.2021.105427
    La Marca Molina K, Bedle H, Tellez J. 2020. Seismic attributes and analogs to characterize a large fold in the Taranaki Basin. Interpretation, 8(4): SR27–SR31. doi: 10.1190/INT-2020-0018.1
    Li Chao, Chen Guojun, Shen Huailei, et al. 2013. Depositional filling and reservoir distribution patterns of the central canyon in Qiongdongnan Basin. Acta Petrolei Sinica (in Chinese), 34(S2): 74–82
    Li Pan, Kneller B, Hansen L. 2021. Anatomy of a gas-bearing submarine channel-lobe system on a topographically complex slope (offshore Nile Delta, Egypt). Marine Geology, 437: 106496. doi: 10.1016/j.margeo.2021.106496
    Li Quan, Wu Wei, Kang Hongquan, et al. 2019. Characteristics and controlling factors of deep-water channel sedimentation in Lower Congo Basin, West Africa. Oil & Gas Geology (in Chinese), 40(4): 917–929
    Li Quan, Wu Wei, Liang Jianshe, et al. 2020. Deep-water channels in the Lower Congo Basin: Evolution of the geomorphology and depositional environment during the Miocene. Marine and Petroleum Geology, 115: 104260. doi: 10.1016/j.marpetgeo.2020.104260
    Li Quan, Yu Shui, Wu Wei, et al. 2017. Detection of a deep-water channel in 3D seismic data using the sweetness attribute and seismic geomorphology: a case study from the Taranaki Basin, New Zealand. New Zealand Journal of Geology and Geophysics, 60(3): 199–208. doi: 10.1080/00288306.2017.1307230
    Livermore R, Nankivell A, Eagles G, et al. 2005. Paleogene opening of Drake Passage. Earth and Planetary Science Letters, 236(1–2): 459–470. doi: 10.1016/j.jpgl.2005.03.027
    Mayall M, Jones E, Casey M. 2006. Turbidite channel reservoirs—Key elements in facies prediction and effective development. Marine and Petroleum Geology, 23(8): 821–841. doi: 10.1016/j.marpetgeo.2006.08.001
    Mayall M, Lonergan L, Bowman A, et al. 2010. The response of turbidite slope channels to growth-induced seabed topography. AAPG Bulletin, 94(7): 1011–1030. doi: 10.1306/01051009117
    Moscardelli L, Wood L. 2008. New classification system for mass transport complexes in offshore Trinidad. Basin Research, 20(1): 73–98. doi: 10.1111/j.1365-2117.2007.00340.x
    Muir R J, Bradshaw J D, Weaver S D, et al. 2000. The influence of basement structure on the evolution of the Taranaki Basin, New Zealand. Journal of the Geological Society, 157(6): 1179–1185. doi: 10.1144/jgs.157.6.1179
    Nwoko J, Kane I, Huuse M. 2020. Mass transport deposit (MTD) relief as a control on post-MTD sedimentation: Insights from the Taranaki Basin, offshore New Zealand. Marine and Petroleum Geology, 120: 104489. doi: 10.1016/j.marpetgeo.2020.104489
    Panpichityota N, Morley C K, Ghosh J. 2018. Link between growth faulting and initiation of a mass transport deposit in the northern Taranaki Basin, New Zealand. Basin Research, 30(2): 237–248. doi: 10.1111/bre.12251
    Peakall J, McCaffrey B, Kneller B. 2000. A process model for the evolution, morphology, and architecture of sinuous submarine channels. Journal of Sedimentary Research, 70(3): 434–448. doi: 10.1306/2DC4091C-0E47-11D7-8643000102C1865D
    Pirmez C, Imran J. 2003. Reconstruction of turbidity currents in Amazon Channel. Marine and Petroleum Geology, 20(6–8): 823–849. doi: 10.1016/j.marpetgeo.2003.03.005
    Posamentier H W. 2003. Depositional elements associated with a basin floor channel-levee system: case study from the Gulf of Mexico. Marine and Petroleum Geology, 20(6–8): 677–690. doi: 10.1016/j.marpetgeo.2003.01.002
    Prather B E. 2003. Controls on reservoir distribution, architecture and stratigraphic trapping in slope settings. Marine and Petroleum Geology, 20(6–8): 529–545. doi: 10.1016/j.marpetgeo.2003.03.009
    Qi Kun, Gong Chenglin, Fauquembergue K, et al. 2022. Did eustatic sea-level control deep-water systems at Milankovitch and timescales? An answer from Quaternary Pearl River margin. Sedimentary Geology, 439: 106217. doi: 10.1016/j.sedgeo.2022.106217
    Qin Yongpeng, Alves T M, Constantine J, et al. 2016. Quantitative seismic geomorphology of a submarine channel system in SE Brazil (Espírito Santo Basin): scale comparison with other submarine channel systems. Marine and Petroleum Geology, 78: 455–473. doi: 10.1016/j.marpetgeo.2016.09.024
    Rebesco M, Camerlenghi A, Munari V, et al. 2021. Bottom current-controlled Quaternary sedimentation at the foot of the Malta Escarpment (Ionian Basin, Mediterranean). Marine Geology, 441: 106596. doi: 10.1016/j.margeo.2021.106596
    Reimchen A P, Hubbard S M, Stright L, et al. 2016. Using sea-floor morphometrics to constrain stratigraphic models of sinuous submarine channel systems. Marine and Petroleum Geology, 77: 92–115. doi: 10.1016/j.marpetgeo.2016.06.003
    Shanmugam G. 2000. 50 years of the turbidite paradigm (1950s–1990s): deep-water processes and facies models—a critical perspective. Marine and Petroleum Geology, 17(2): 285–342. doi: 10.1016/S0264-8172(99)00011-2
    Steel R J, Olariu C, Zhang Jinyu, et al. 2020. What is the topset of a shelf-margin prism?. Basin Research, 32(2): 263–278. doi: 10.1111/bre.12394
    Strogen D P, Bland K J, Nicol A, et al. 2014. Paleogeography of the Taranaki Basin region during the latest Eocene–Early Miocene and implications for the ‘total drowning’ of Zealandia. New Zealand Journal of Geology and Geophysics, 57(2): 110–127. doi: 10.1080/00288306.2014.901231
    Uruski C I. 2008. Deepwater Taranaki, New Zealand: structural development and petroleum potential. Exploration Geophysics, 39(2): 94–107. doi: 10.1071/EG08013
    Uruski C I. 2010. New Zealand’s deepwater frontier. Marine and Petroleum Geology, 27(9): 2005–2026. doi: 10.1016/j.marpetgeo.2010.05.010
    Uruski C I, Stagpoole V, Isaac M J, et al. 2002. Seismic Interpretation Report—Astrolabe Survey, Taranaki Basin, New Zealand. Institute of Geological & Nuclear Sciences confidential client report 2002/70 Open-file Petroleum Report 3072. Ministry of Commerce
    Uruski C I., Warburton J. 2015. Sequence stratigraphy and facies prediction: PEP 38451, Deepwater Taranaki Basin. https://www.researchgate.net/publication/265980985
    Wang Guangxu, Wu Wei, Lin Changsong, et al. 2022. Migration rules and depositional model of Quaternary deep-water channel in Taranaki Basin, New Zealand. Journal of China University of Petroleum: Edition of Natural Science (in Chinese), 46(3): 13–24
    Wu Wei, Li Quan, Yu Jing, et al. 2018. The central canyon depositional patterns and filling process in east of Lingshui depression, Qiongdongnan basin, northern South China Sea. Geological Journal, 53(6): 3064–3081. doi: 10.1002/gj.3143
    Wu Wei, Liu Weiqing, Lin Changsong, et al. 2014. Sedimentary evolution of the lower Zhujiang group continental shelf edge in the north slope of Baiyun Sag, Pearl River mouth basin. Acta Geologica Sinica (in Chinese), 88(9): 1719–1727
    Wynn R B, Cronin B T, Peakall J. 2007. Sinuous deep-water channels: genesis, geometry and architecture. Marine and Petroleum Geology, 24(6–9): 341–387. doi: 10.1016/j.marpetgeo.2007.06.001
    Xie Qinghui, Deng Hongwen. 2013. Application of strata slicing technique in Miocene Congo Fan. Petroleum Geology and Oilfield Development in Daqing (in Chinese), 32(6): 135–140
    Xie Yuhong, Fan Caiwei, Zhou Jiaxiong, et al. 2016. Sedimentary features and controlling factors of the gravity flows in submarine fan of Middle Miocene in the Qiongdongnan Basin. Natural Gas Geoscience (in Chinese), 27(2): 220–228
    Yu Shui. 2018. Depositional characteristics and pattern of Miocene deep water gravity flow deposits in Lower Cango Basin, West Africa. China Offshore Oil and Gas (in Chinese), 30(4): 13–19
    Zachos J, Pagani M, Sloan L, et al. 2001. Trends, rhythms, and aberrations in global climate 65 Ma to present. Science, 292(5517): 686–693. doi: 10.1126/science.1059412
    Zhao Xiaoming, Liu Li, Tan Chengpeng, et al. 2018a. Styles of submarine-channel architecture and its controlling factors: a case study from the Niger Delta Basin slope. Journal of Palaeogeography (in Chinese), 20(5): 825–840
    Zhao Xiaoming, Qi Kun, Liu Li, et al. 2018b. Development of a partially-avulsed submarine channel on the Niger Delta continental slope: architecture and controlling factors. Marine and Petroleum Geology, 95: 30–49. doi: 10.1016/j.marpetgeo.2018.04.015
    Zucker E, Gvirtzman Z, Steinberg J, et al. 2017. Diversion and morphology of submarine channels in response to regional slopes and localized salt tectonics, Levant Basin. Marine and Petroleum Geology, 81: 98–111. doi: 10.1016/j.marpetgeo.2017.01.002
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