Zobrazeno 1 - 7
of 7
pro vyhledávání: '"Michal Janocko"'
Publikováno v:
Hansen, L, Janocko, M, Kane, I & Kneller, B C 2017, ' Submarine channel evolution, terrace development, and preservation of intra-channel thin-bedded turbidites : Mahin and Avon channels, offshore Nigeria ', Marine Geology . https://doi.org/10.1016/j.margeo.2016.11.011
Terraces on the modern seafloor are defined as topographically flat areas above the active submarine channel thalweg but within the confines of the channel-belt. They have been described from many modern submarine channels, but the controls on terrac
Autor:
Michal Janocko, M. Warchol, C. Siversen, E. R. Schomacker, A. Fuhrmann, Ian A. Kane, Ross A. Ferguson, Rufus L. Brunt
Publikováno v:
Scopus-Elsevier
This contribution presents an integrated case study of Well X, which targeted a drift-influenced slope channel complex in Cretaceous and Neogene stratigraphy of Block 2, offshore Tanzania. The large-scale architecture of several channel complexes rev
Publikováno v:
Marine and Petroleum Geology. 41:7-34
The study combines interpretation of 3D seismic imagery of submarine sinuous channel belts in offshore West Africa with observations from a range of outcrop analogues. Five main architectural elements of slope channel belts are recognized: lateral-ac
Publikováno v:
Journal of the Geological Society. 167:857-875
Sea-floor bathymetry is one of the principal controls on the routing of turbidity currents and the subsequent distribution of deposited sediments. Re-created sea-floor bathymetry is thus one of the main inputs for process-based numerical simulation o
Publikováno v:
Marine and Petroleum Geology. 27:412-434
It is widely recognised that palaeobathymetry is a key control on the distribution of turbidite deposits. Thus, the utilisation of palaeobathymetric surfaces as an input for numerical turbidity current modelling offers a potentially powerful method t
Autor:
Riccardo Basani, Ernst W. M. Hansen, Joris T. Eggenhuisen, Matthieu J.B. Cartigny, Michal Janocko
Publikováno v:
From Depositional Systems to Sedimentary Successions on the Norwegian Continental Margin
Turbidity currents are the most important mechanism for the dispersal and deposition of sand in the deep-sea setting and thus the main phenomenon leading to the formation of oil and gas reservoirs in deep water deposits. The flow characteristics of t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4b5bad166d7fd566de7e0262d56a886d
https://doi.org/10.1002/9781118920435.ch20
https://doi.org/10.1002/9781118920435.ch20
Publikováno v:
Marine and Petroleum Geology, 41, 222. Elsevier
This study explores the relationship between the hydraulics of turbidity currents in erodible sinuous channels and the resulting intra-channel sediment depocentres (channel bars). Four factors are considered to exert critical control on sedimentation
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::e6ca9ef1117301dda53383cda3f6eee2
https://dspace.library.uu.nl/handle/1874/282637
https://dspace.library.uu.nl/handle/1874/282637