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Quantitative morphometric analysis of a deep-water channel in the Taranaki Basin, New Zealand

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  • Marine Geology
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Abstract

The morphological changes of deep-water channels have an important influence on the distributions of channel sand reservoirs, so it is important to explore the morphological change process of deep-water channel for the exploration and development of deep-water oil and gas. Based on a typical sinuous Quaternary channel (Channel I) in the Taranaki Basin, New Zealand, a variety of seismic interpretation techniques were applied to quantitatively characterize the morphological characteristics of the Channel I, and the relationships between the quantitative parameters and the morphological changes of the Channel I, as well as the controlling factors affecting those morphological changes, were discussed. The results are as follows: (1) in the quantitative analysis, six parameters were selected: the channel depth, width, sinuosity, and aspect ratio (width/depth), the channel swing amplitude (λ) and the channel bend frequency (ω); (2) according to the quantitative morphological parameters of the channel (mainly including three parameters such as channel sinuosity, ω and λ), the Channel I was divided into three types: the low-sinuous channel (LSC), the high-sinuous channel (HSC), the moderate-sinuous channel (MSC). U-shaped channel cross-sections developed in the LSC, V-shaped channel cross-sections developed in the HSC, including inclined-V and symmetric-V cross-sections, and dish-shaped channel cross-sections developed in the MSC; (3) the morphological characteristics of the LSC and MSC were related to their widths and depths, while the morphology of the HSC was greatly affected by the channel width, a change in depth did not affect the HSC morphology; (4) the morphological changes of the Channel I were controlled mainly by the slope gradient, the restricted capacity of the channel and the differential in fluid properties.

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References

  • 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

    Article  Google Scholar 

  • 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: https://doi.org/10.1306/04021211067

    Article  Google Scholar 

  • 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: https://doi.org/10.1016/S0264-8172(02)00009-0

    Article  Google Scholar 

  • 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: https://doi.org/10.2110/jsr.2010.078

    Article  Google Scholar 

  • Biscara L, Mulder T, Martinez P, et al. 2011. Transport of terrestrial organic matter in the Ogooué deep sea turbidite system (Gabon). Marine and Petroleum Geology, 28(5): 1061–1072, doi: https://doi.org/10.1016/j.marpetgeo.2010.12.002

    Article  Google Scholar 

  • Carter R M, Norris R J. 1976. Cainozoic history of southern New Zealand: an accord between geological observations and plate-tectonic predictions. Earth and Planetary Science Letters, 31(1): 85–94, doi: https://doi.org/10.1016/0012-821X(76)90099-6

    Article  Google Scholar 

  • Clark J D, Kenyon N H, Pickering K T. 1992. Quantitative analysis of the geometry of submarine channels: implications for the classification of submarine fans. Geology, 20(7): 633–636, doi: https://doi.org/10.1130/0091-7613(1992)020<0633:QAOTGO>2.3.CO;2

    Article  Google Scholar 

  • 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

    Google Scholar 

  • Dai Zhijun, Liu James T, Fu Gui, et al. 2013. A thirteen-year record of bathymetric changes in the North Passage, Changjiang (Yangtze) estuary. Geomorphology, 187: 101–107, doi: https://doi.org/10.1016/j.geomorph.2013.01.004

    Article  Google Scholar 

  • Dai Zhijun, Mei Xuefei, Darby S E, et al. 2018. Fluvial sediment transfer in the Changjiang (Yangtze) river-estuary depositional system. Journal of Hydrology, 566: 719–734, doi: https://doi.org/10.1016/j.jhydrol.2018.09.019

    Article  Google Scholar 

  • 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: https://doi.org/10.1016/j.marpetgeo.2017.04.012

    Article  Google Scholar 

  • Deptuck M E, Steffens G S, Barton M, et al. 2003. Architecture and evolution of upper fan channel-belts on the Niger Delta slope and in the Arabian Sea. Marine and Petroleum Geology, 20(6–8): 649–676

    Article  Google Scholar 

  • 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

    Article  Google Scholar 

  • Dott R H. 1963. Dynamics of subaqueous gravity depositional processes. AAPG Bulletin, 47(1): 104–128

    Google Scholar 

  • Gabet E J. 1998. Lateral migration and bank erosion in a saltmarsh tidal channel in San Francisco Bay, California. Estuaries, 21(4): 745–753, doi: https://doi.org/10.2307/1353278

    Article  Google Scholar 

  • 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: https://doi.org/10.1016/j.marpetgeo.2015.02.035

    Article  Google Scholar 

  • 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: https://doi.org/10.1016/j.marpetgeo.2006.01.002

    Article  Google Scholar 

  • Gee M J R, Gawthorpe R L, Bakke K, et al. 2007. Seismic geomorphology and evolution of submarine channels from the Angolan continental margin. Journal of Sedimentary Research, 77(5): 433–446, doi: https://doi.org/10.2110/jsr.2007.042

    Article  Google Scholar 

  • Giba M, Walsh J J, Nicol A, et al. 2013. Investigation of the spatio-temporal relationship between normal faulting and arc volcanism on million-year time scales. Journal of the Geological Society, 170(6): 951–962, doi: https://doi.org/10.1144/jgs2012-121

    Article  Google Scholar 

  • Harishidayat D, Omosanya K O, Johansen S E. 2015. 3D seismic interpretation of the depositional morphology of the middle to late Triassic fluvial system in eastern Hammerfest Basin, Barents Sea. Marine and Petroleum Geology, 68: 470–479, doi: https://doi.org/10.1016/j.marpetgeo.2015.09.007

    Article  Google Scholar 

  • 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: https://doi.org/10.1016/j.marpetgeo.2010.08.002

    Article  Google Scholar 

  • Hudson P F, Kesel R H. 2000. Channel migration and meander-bend curvature in the lower Mississippi River prior to major human modification. Geology, 28(6): 531–534, doi: https://doi.org/10.1130/0091-7613(2000)28<531:CMAMCI>2.0.CO;2

    Article  Google Scholar 

  • Janocko M, Nemec W, Henriksen S, et al. 2013. The diversity of deep-water sinuous channel belts and slope valley-fill complexes. Marine and Petroleum Geology, 41: 7–34, doi: https://doi.org/10.1016/j.marpetgeo.2012.06.012

    Article  Google Scholar 

  • Khripounoff A, Vangriesheim A, Babonneau N, et al. 2003. Direct observation of intense turbidity current activity in the Zaire submarine valley at 4000 m water depth. Marine Geology, 194(3–4): 151–158

    Article  Google Scholar 

  • King P R. 2000. New Zealand’s changing configuration in the last 100 million years: plate tectonics, basin development, and depositional setting. In: 2000 New Zealand Petroleum Conference Proceedings. Wellington: Crown Minerals, Ministry of Commerce Wellington, New Zealand

    Google Scholar 

  • King P R, Thrasher G P. 1996. Cretaceous-Cenozoic geology and petroleum systems of the Taranaki Basin, New Zealand [dissertation]. Lower Hutt: Institute of Geological & Nuclear Sciences

    Google Scholar 

  • Kolla V. 2007. A review of sinuous channel avulsion patterns in some major deep-sea fans and factors controlling them. Marine and Petroleum Geology, 24(6–9): 450–469

    Article  Google Scholar 

  • Labourdette R. 2007. Integrated three-dimensional modeling approach of stacked turbidite channels. AAPG Bulletin, 91(11): 1603–1618, doi: https://doi.org/10.1306/06210706143

    Article  Google Scholar 

  • Li Quan, Wu Wei, Yu Shui, et al. 2017a. The application of three-dimensional seismic spectral decomposition and semblance attribute to characterizing the Deepwater channel depositional elements in the Taranaki Basin of New Zealand. Acta Oceanologica Sinica, 36(9): 79–86, doi: https://doi.org/10.1007/s13131-017-1113-0

    Article  Google Scholar 

  • Li Lei, Yan Rui, Li Ningtao, et al. 2015. Characteristics and origin of deep-water channels in Rio Muni Basin, West Africa. Geoscience (in Chinese), 29(1): 80–88

    Google Scholar 

  • Li Quan, Yu Shui, Wu Wei, et al. 2017b. 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: https://doi.org/10.1080/00288306.2017.1307230

    Article  Google Scholar 

  • Li Lei, Zou Yun, Zhang Peng, et al. 2019. Quantitative analysis of the geometry of sinuous submarine channels: a case from the Rio Muni Basin of Equatorial Guinea. Marine Geology Frontiers (in Chinese), 35(10): 23–35

    Google Scholar 

  • Liu Xinying, Yu Shui, Hu Xiaolin, et al. 2012. Quantitative relation between the gradient and sinuosity of Deepwater channel and its control: a case study in the Rio Muni Basin, West Africa. Journal of Jilin University (Earth Science Edition) (in Chinese), 42(S1): 127–134

    Google Scholar 

  • Lowe D R, Graham S A, Malkowski M A, et al. 2019. The role of avulsion and splay development in deep-water channel systems: sedimentology, architecture, and evolution of the deep-water Pliocene Godavari “A” channel complex, India. Marine and Petroleum Geology, 105: 81–99, doi: https://doi.org/10.1016/j.marpetgeo.2019.04.010

    Article  Google Scholar 

  • Malkowski M A, Jobe Z R, Sharman G R, et al. 2018. Down-slope facies variability within deep-water channel systems: insights from the Upper Cretaceous Cerro Toro Formation, southern Patagonia. Sedimentology, 65(6): 1918–1946, doi: https://doi.org/10.1111/sed.12452

    Article  Google Scholar 

  • Masalimova L U, Lowe D R, Sharman G R, et al. 2016. Outcrop characterization of a submarine channel-lobe complex: the lower mount messenger formation, Taranaki Basin, New Zealand. Marine and Petroleum Geology, 71: 360–390, doi: https://doi.org/10.1016/j.marpetgeo.2016.01.004

    Article  Google Scholar 

  • 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: https://doi.org/10.1016/j.marpetgeo.2006.08.001

    Article  Google Scholar 

  • McHargue T, Pyrcz M J, Sullivan M D, et al. 2011. Architecture of turbidite channel systems on the continental slope: patterns and predictions. Marine and Petroleum Geology, 28(3): 728–743, doi: https://doi.org/10.1016/j.marpetgeo.2010.07.008

    Article  Google Scholar 

  • Mei Xuefei, Dai Zhijun, Wei Wen, et al. 2018. Secular bathymetric variations of the North Channel in the Changjiang (Yangtze) Estuary, China, 1880–2013: causes and effects. Geomorphology, 303: 30–40, doi: https://doi.org/10.1016/j.geomorph.2017.11.014

    Article  Google Scholar 

  • 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. Dordrecht: Springer, 1–38

    Google Scholar 

  • Niyazi Y, Eruteya O E, Omosanya K O, et al. 2018. Seismic geomorphology of submarine channel-belt complexes in the Pliocene of the Levant Basin, offshore central Israel. Marine Geology, 403: 123–138, doi: https://doi.org/10.1016/j.margeo.2018.05.007

    Article  Google Scholar 

  • 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: https://doi.org/10.1306/2DC4091C-0E47-11D7-8643000102C1865D

    Article  Google Scholar 

  • Pichevin L, Bertrand P, Boussafir M, et al. 2004. Organic matter accumulation and preservation controls in a deep sea modern environment: an example from Namibian slope sediments. Organic Geochemistry, 35(5): 543–559, doi: https://doi.org/10.1016/j.orggeochem.2004.01.018

    Article  Google Scholar 

  • Pirmez C, Imran J. 2003. Reconstruction of turbidity currents in Amazon channel. Marine and Petroleum Geology, 20(6–8): 823–849

    Article  Google Scholar 

  • 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

    Article  Google Scholar 

  • 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: https://doi.org/10.1016/j.marpetgeo.2016.09.024

    Article  Google Scholar 

  • 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: https://doi.org/10.1016/j.marpetgeo.2016.06.003

    Article  Google Scholar 

  • Rotzien J R. 2013. Processes of sedimentation, stratigraphic architecture, and provenance of deep-water depositional systems: the upper Miocene Upper Mount messenger formation, Taranaki Basin, New Zealand and Pliocene Repetto and Pico formations, Ventura Basin, California [dissertation]. Stanford: Stanford University, 218

    Google Scholar 

  • Rotzien J R, Lowe D R, King P R, et al. 2014. Stratigraphic architecture and evolution of a deep-water slope channel-levee and overbank apron: the Upper Miocene Upper Mount Messenger Formation, Taranaki Basin. Marine and Petroleum Geology, 52: 22–41, doi: https://doi.org/10.1016/j.marpetgeo.2014.01.006

    Article  Google Scholar 

  • Stagpoole V M, Hill M, Thornton S, et al. 2002. New Zealand Basin development and depositional systems evolution: quantification and Visualisation. In: 2002 New Zealand Petroleum Conference Proceedings. Auckland: GNS Science, 351–362

    Google Scholar 

  • Straub K M, Mohrig D, Buttles J, et al. 2011. Quantifying the influence of channel sinuosity on the depositional mechanics of channelized turbidity currents: a laboratory study. Marine and Petroleum Geology, 28(3): 744–760, doi: https://doi.org/10.1016/j.marpetgeo.2010.05.014

    Article  Google Scholar 

  • Sutherland R. 1999. Basement geology and tectonic development of the greater New Zealand region: an interpretation from regional magnetic data. Tectonophysics, 308(3): 341–362, doi: https://doi.org/10.1016/S0040-1951(99)00108-0

    Article  Google Scholar 

  • Tek D E, McArthur A D, Poyatos-Moré M, et al. 2022. Controls on the architectural evolution of deep-water channel overbank sediment wave fields: insights from the Hikurangi Channel, offshore New Zealand. New Zealand Journal of Geology and Geophysics, 65(1): 141–178, doi: https://doi.org/10.1080/00288306.2021.1978509

    Article  Google Scholar 

  • Uruski C I. 2008. Deepwater Taranaki, New Zealand: structural development and petroleum potential. Exploration Geophysics, 39(2): 94–107, doi: https://doi.org/10.1071/EG08013

    Article  Google Scholar 

  • Uruski C I. 2010. New Zealand’s Deepwater frontier. Marine and Petroleum Geology, 27(9): 2005–2026, doi: https://doi.org/10.1016/j.marpetgeo.2010.05.010

    Article  Google Scholar 

  • 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

    Article  Google Scholar 

  • Xu Jie, Snedden J W, Galloway W E, et al. 2017. Channel-belt scaling relationship and application to early Miocene source-to-sink systems in the Gulf of Mexico Basin. Geosphere, 13(1): 179–200, doi: https://doi.org/10.1130/GES01376.1

    Article  Google Scholar 

  • Yao Yue, Zhou Jiangyu, Lei Zhenyu, et al. 2018. High restriction seismic facies and inner structural segmentation features of the central canyon channel systems in Xisha trough basin. Acta Sedimentologica Sinica (in Chinese), 36(4): 787–795

    Google Scholar 

  • 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

    Google Scholar 

  • 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: https://doi.org/10.1016/j.marpetgeo.2018.04.015

    Article  Google Scholar 

  • Zhou Xiaoyan, Dai Zhijun, Mei Xuefei. 2020. The multi-decadal morphodynamic changes of the mouth bar in a mixed fluvialtidal estuarine channel. Marine Geology, 429: 106311, doi: https://doi.org/10.1016/j.margeo.2020.106311

    Article  Google Scholar 

  • 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: https://doi.org/10.1016/j.marpetgeo.2017.01.002

    Article  Google Scholar 

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Authors and Affiliations

  1. Institute of Resources and Environment, Henan Polytechnic University, Jiaozuo, 454003, China

    Wei Wu, Guangxu Wang, Weiqing Liu, Quan Li & Shuyuan Ning

  2. School of Ocean Science, China University of Geosciences, Beijing, 100083, China

    Changsong Lin

  3. Institute of Exploration Technology, CNOOC International Ltd., Beijing, 100028, China

    Quan Li

  4. College of Safety Science and Engineering, Henan Polytechnic University, Jiaozuo, 454003, China

    Zhendong Feng

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  1. Wei Wu
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  2. Guangxu Wang
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Correspondence to Weiqing Liu.

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Foundation item: The National Natural Science Foundation of China under contract Nos 42077410, 41872112 and 42002031; the Key Scientific Research Projects in University of Henan Province under contract No. 18A170007.

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Wu, W., Wang, G., Lin, C. et al. Quantitative morphometric analysis of a deep-water channel in the Taranaki Basin, New Zealand. Acta Oceanol. Sin. 42, 42–56 (2023). https://doi.org/10.1007/s13131-022-2024-2

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