Results 101 to 110 of about 663 (130)
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Outcrop 13. Tres Pasos Formation Slope Minibasin Fill, El Chingue Bluff

2009
Abstract Outcrop accessibility: moderate Outcrop Coordinates: 51.1537°S, 72.4725°W Refer to outcrop 13 on location map Limited exposures of sandstone are present in the Tres Pasos Formation between Sierra Contreras and Laguna Figueroa; an important exception is a 60 m thick succession dominated by coarse-grained turbiditic
M.R. Shultz, S.M. Hubbard
openaire   +1 more source

Experiment on Turbidity Currents and Their Deposits in a Model 3D Subsiding Minibasin

Journal of Sedimentary Research, 2005
Abstract Minibasins on the continental slope are formed by the movement of salt or mud layers in the subsurface. The north slope of the Gulf of Mexico (GOM), for example, is riddled with salt-withdrawal minibasins ranging in scale from a few kilometers to tens of kilometers.
J. Violet   +5 more
openaire   +1 more source

Structure and Stratigraphy of the Calcasieu Lake Salt-Withdrawal Minibasin, Onshore Louisiana

AAPG Bulletin, 2001
ABSTRACT The Calcasieu Lake salt-withdrawal minibasin, central Cameron Parish, Louisiana, forms an E-W elliptical shape of ~15 mi by 10 mi. Complex normal-fault systems occur along the basin's periphery, commonly down-to-the-basin and flanking adjacent salt-cored uplifts, including Hackberry, Big Lake, Sweet Lake and Creole. Calcasieu Lake salt dome, a
openaire   +1 more source

Shortening of Diapir Provinces: Translation, Tilting and Rotation of Minibasins in Isolated Minibasin Systems

2019 AAPG Annual Convention and Exhibition, 2019
Tim Dooley   +3 more
openaire   +1 more source

Origin and evolution of salt minibasins on the Algerian margin

2023
Travan, Gaia   +3 more
openaire   +1 more source

The role of post-salt carbonates on salt tectonic minibasin formation

Salt tectonics on passive margins is driven by sediment loading and gliding with minimal influence from basement-involved tectonics and is associated with variable and complex salt structures such as minibasins and diapirs. A major enigma in salt tectonics is the origin of load-driven diapir-flanked minibasins, synclinal depocenters formed by localized
Leonardo Muniz Pichel   +3 more
openaire   +1 more source

Influence of minibasin obstruction on canopy dynamics in the northern Gulf of Mexico

Basin Research, 2021
Naiara Fernandez   +2 more
exaly  

Minibasin depocentre migration during diachronous salt welding, offshore Angola

Basin Research, 2020
Zhiyuan Ge, Rob Gawthorpe, Atle Rotevatn
exaly  

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