Deep-water sedimentation controlled by interaction between bottom current and gravity flow: A case study of Rovuma Basin, East Africa

[1]  I. Davison,et al.  Geology and hydrocarbon potential of the East African continental margin: a review , 2017, Petroleum Geoscience.

[2]  S. Darby,et al.  Flow dynamics and mixing processes in hydraulic jump arrays: Implications for channel-lobe transition zones , 2016 .

[3]  Yingmin Wang,et al.  Middle Miocene reworked turbidites in the Baiyun Sag of the Pearl River Mouth Basin, northern South China Sea margin: Processes, genesis, and implications , 2016 .

[4]  Shenghe Wu,et al.  Research on the architecture of submarine-fan lobes in the Niger Delta Basin, offshore West Africa , 2016 .

[5]  G. Shanmugam.  Submarine fans: A critical retrospective (1950-2015) , 2016 .

[6]  A. M. Hoguane,et al.  Observations of strong ocean current events offshore Pemba, Northern Mozambique , 2016 .

[7]  J. Peakall,et al.  Giant scour-fills in ancient channel-lobe transition zones: formative processes and depositional architecture , 2015 .

[8]  S. Clark,et al.  Cretaceous–Cenozoic sedimentary budgets of the Southern Mozambique Basin: Implications for uplift history of the South African Plateau , 2015 .

[9]  J. Peakall,et al.  Submarine channel flow processes and deposits: A process-product perspective , 2015 .

[10]  S. Ayers,et al.  Areas 2 and 5 offshore Mozambique: Mass-movements on a deep-water margin with scant adjacent shelf , 2015 .

[11]  Yu Lin,et al.  Reservoir quality variations within a sinuous deep water channel system in the Niger Delta Basin, offshore West Africa , 2015 .

[12]  D. Franke,et al.  The Rovuma Delta deep-water fold-and-thrust belt, offshore Mozambique , 2014 .

[13]  W. Jokat,et al.  Seafloor morphology in the Mozambique Channel: evidence for long-term persistent bottom-current flow and deep-reaching eddy activity , 2013, Marine Geophysical Research.

[14]  M. Francis,et al.  Frontier exploration offshore the Zambezi Delta, Mozambique , 2013 .

[15]  J. Shaw,et al.  Megaflutes in a continental shelf setting, Placentia Bay, Newfoundland , 2013 .

[16]  D. H. Sapri,et al.  Sequence Stratigraphic Study of Areas 3 & 6, Rovuma Basin, Mozambique , 2013 .

[17]  Yingmin Wang,et al.  Upper Miocene to Quaternary unidirectionally migrating deep-water channels in the Pearl River Mouth Basin, northern South China Sea , 2013 .

[18]  S. McPhail,et al.  New insights into the morphology, fill, and remarkable longevity (>0.2 m.y.) of modern deep-water erosional scours along the northeast Atlantic margin , 2011 .

[19]  Mathijs W. Schouten,et al.  Long-term observations of transport, eddies, and Rossby waves in the Mozambique Channel , 2009 .

[20]  R. May,et al.  Characteristics of Pleistocene deep-water fan lobes and their application to an upper Miocene reservoir model, offshore East Kalimantan, Indonesia , 2008 .

[21]  J. Powell,et al.  Revised lithostratigraphy of the Mesozoic-Cenozoic succession of the onshore Rovuma Basin, northern coastal Mozambique , 2008 .

[22]  R. Wynn,et al.  Sinuous deep-water channels: Genesis, geometry and architecture , 2007 .

[23]  G. Parker,et al.  The response of turbidity currents to a canyon–fan transition: internal hydraulic jumps and depositional signatures , 2006 .

[24]  E. Jones,et al.  Turbidite channel reservoirs—Key elements in facies prediction and effective development , 2006 .

[25]  R. Thomas,et al.  Himalayan-type indenter-escape tectonics model for the southern part of the late Neoproterozoic–early Paleozoic East African– Antarctic orogen , 2004 .

[26]  R. Wynn,et al.  Characterization and recognition of deep-water channel-lobe transition zones , 2002 .

[27]  Johann R. E. Lutjeharms,et al.  Observations of the flow in the Mozambique Channel , 2002 .

[28]  Warren T. Wood,et al.  Methane Hydrate and Free Gas on the Blake Ridge from Vertical Seismic Profiling , 1996, Science.

[29]  I. Abdula,et al.  Development of the Mozambique and Ruvuma sedimentary basins, offshore Mozambique , 1995 .

[30]  I. Lerche,et al.  Geology, basin analysis, and hydrocarbon potential of Mozambique and the Mozambique Channel , 1991 .

[31]  S. Lawrence,et al.  MOZAMBIQUE: A NEW GEOLOGICAL FRAMEWORK FOR HYDROCARBONS EXPLORATION , 1989 .

[32]  R. Sætre,et al.  The circulation of the Mozambique channel , 1984 .

[33]  R. Walker.  Deep-Water Sandstone Facies and Ancient Submarine Fans: Models for Exploration for Stratigraphic Traps , 1979 .

[34]  M. Langseth,et al.  Spreading of Antarctic Bottom Water and its effects on the floor of the Indian Ocean inferred from bottom-water potential temperature, turbidity, and sea-floor photography , 1976 .

[35]  W. Normark.  Growth Patterns of Deep-Sea Fans , 1970 .

[36]  D. Palermo,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 , 2020 .

[37]  M. Wit,et al.  Tight Reassembly of Gondwana Exposes Phanerozoic Shears in Africa as Global Tectonic Players , 2004 .

[38]  A. Saller,et al.  Linked lowstand delta to basin-floor fan deposition, offshore Indonesia: An analog for deep-water reservoir systems , 2004 .

[39]  M. Link,et al.  Seismic facies and sedimentary processes of submarine fans and turbidite systems , 1991 .