Zobrazeno 1 - 5
of 5
pro vyhledávání: '"Tor E. Aas"'
Autor:
Rob L. Gawthorpe, Tor E. Aas, Gavin M. Elliott, Christopher A.-L. Jackson, Elisabeth Royce‐Rogers
Publikováno v:
Basin Research. 31:514-538
“Salt” giants are typically halite‐dominated, although they invariably contain other evaporite (e.g. anhydrite, bittern salts) and non‐evaporite (e.g. carbonate, clastic) rocks. Rheological differences between these rocks mean they impact or
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::26ecdedf457131db7a4908beea4ef631
https://doi.org/10.1111/bre.12332
https://doi.org/10.1111/bre.12332
Publikováno v:
Geological Society, London, Special Publications. 387:247-269
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3e107a65e69218bf0ab0bf5eff6aa74a
https://doi.org/10.1144/sp387.9
https://doi.org/10.1144/sp387.9
Publikováno v:
Second Conference on Forward Modelling of Sedimentary Systems.
The deterministic software MassFLOW-3D™ has been successfully used to construct a 3D model for the simulation of turbidity currents and predict bed geometry and grain size distribution in a single bed (Marker Unit 5) from the deep-marine Peira Cava
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a3debb7c456a0403894d695f47529267
https://doi.org/10.3997/2214-4609.201600376
https://doi.org/10.3997/2214-4609.201600376
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
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::700ee6394908503bd93c543aab039cc8
https://doi.org/10.1144/0016-76492009-005
https://doi.org/10.1144/0016-76492009-005
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
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f2efbfa6e8ad256be79133664419e2eb
https://doi.org/10.1016/j.marpetgeo.2009.10.014
https://doi.org/10.1016/j.marpetgeo.2009.10.014