Results 1 to 10 of about 663 (130)
Seafloor topography can affect turbidity current dynamics on deep‐water slopes, significantly influencing the dispersal of sediment. Despite the common occurrence of topographic complexity, there are few detailed investigations of topographic ...
Rebecca G Englert +2 more
exaly +5 more sources
Circulation of hydraulically ponded turbidity currents and the filling of continental slope minibasins [PDF]
Natural depressions on continental margins termed minibasins trap turbidity currents, a class of sediment-laden seafloor density driven flow. These currents are the primary downslope vectors for clastic sediment, particulate organic carbon, and ...
J. Kevin Reece +2 more
doaj +6 more sources
The Bolon Secondary Minibasin (BSM) evolved on the now eroded Elda Salt Sheet, which contains fragments of the diapiric roof and syn-contractional sediments.
Eduard Roca +2 more
exaly +4 more sources
How Fast Can Minibasins Translate Down a Slope? Observations from 2D Numerical Models
Minibasins are important features in salt-bearing basins and are abundant in salt-detached continental slopes where the salt and the overlying sedimentary cover (including minibasins) undergo seaward translation due to gravity.
Naiara Fernandez +5 more
doaj +5 more sources
Spatial and temporal variations in minibasin geometry and evolution in salt tectonic provinces: Lower Congo Basin, offshore Angola [PDF]
In passive margin salt basins, the distinct kinematic domains of thin‐skinned extension, translation and contraction exert important controls on minibasin evolution. However, the relationship between various salt minibasin geometries and kinematic domain
Zhiyuan Ge, Leo Zijerveld, Rob Gawthorpe
exaly +3 more sources
Extension and inversion of salt-bearing rift systems [PDF]
We used physical models to investigate the structural evolution of segmented extensional rifts containing syn-rift evaporites and their subsequent inversion. An early stage of extension generated structural topography consisting of a series of en-échelon
T. P. Dooley, M. R. Hudec
doaj +1 more source
Stretching and Contraction of Extensional Basins With Pre-Rift Salt: A Numerical Modeling Approach
We present a series of 2D thermo-mechanical numerical experiments of thick-skinned crustal extension including a pre-rift salt horizon and subsequent thin-, thick-skinned, or mixed styles of convergence accompanied by surface processes.
Pablo Granado +4 more
doaj +1 more source
The Mirim and Patos Lagoons form the largest lagoon complex in South America. Wind is one of the dominant climatic elements of circulation and water levels in the basin.
Thais Magalhães Possa +5 more
doaj +1 more source
Forward Modelling for Structural Stratigraphic Analysis, Offshore Sureste Basin, Mexico
The stratal architecture of deep-water minibasins is dominantly controlled by the interplay of two factors, structure growth and sediment supply. In this paper we explore the utility of a reduced-complexity, fast computational method (Onlapse-2D) to ...
Donald N. Christie +3 more
doaj +1 more source
Rising and falling diapirs, shifting depocenters, and flap overturning in the Cretaceous Sopeira and Sant Gervàs subbasins (Ribagorça Basin, southern Pyrenees) [PDF]
The halokinetic structure of inverted salt-related continental margins is frequently obliterated by compressional overprinting. The Cretaceous Sopeira and Sant Gervàs subbasins of the Ribagorça Basin (south central Pyrenees) show evidence of salt-related
Ardèvol I Oró, Lluís +3 more
core +5 more sources

