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A model for allochthonous salt sheet emplacement is preserved to explain overthrusting of thick sediment columns above these sheets. This model proposes that initial emplacement, either as extrusive sheets or horizontal intrusions near the sea floor, sometimes yields to shearing along thrust fault ...
Get Priceallochthonous salt sheets, which was emplaced during the Early Cretaceous. The geologic framework, during this period, produces conditions for a predominantly gravity-driven deformation: extension has produced space for the salt to rise; vigorous differential sedimentation created differential loading that resulted in the emplacement and extrusion of a large volume of Triassic salt and ...
Get PriceAllochthonous salt sheets advance in four ways: (1) extrusive advance, (2) open-toed advance, (3) thrust advance, and (4) salt-wing intrusion. These mechanisms are determined primarily by the geometry and thickness of the roof that overlies the advancing sheet. An extrusive sheet spreads without a roof or with a roof of negligible mechanical strength. An open-toed sheet is partially covered by ...
Get PriceAnimation of allochthonous salt sheets. Get Price; EMARC University of Colorado Boulder... and the various timing of emplacement of salt sheets. ... The Effect of Allochthonous Salt on Petroleum Systems of Northern Green Canyon and Ewing Bank Areas, ... Get Price; Hindered Settling... and salt sheets. ... Animation showing how downbuilding works. Blue represents salt, ... check out this recent ...
Get PriceThe Bled Dogra salt structure is one of these submarine allochthonous salt sheets, which was emplaced during the Early Cretaceous. The geologic framework, during this period, produces conditions for a predominantly gravity-driven deformation: extension has produced space for the salt to rise; vigorous differential sedimentation created differential loading that resulted in the emplacement and ...
Get Pricepresent 40-km-long Lansarine–Baouala salt structure with its unique mass of allochthonous Triassic salt at surface was fed from at least four stems. The salt structure is recognized as one of the few examples worldwide of a subaerial salt canopy due to the coalescence of submarine sheets of Triassic salt extruded in Cretaceous times.
Get PriceA model for allochthonous salt sheet emplacement is preserved to explain overthrusting of thick sediment columns above these sheets. This model proposes that initial emplacement, either as extrusive sheets or horizontal intrusions near the sea floor, sometimes yields to shearing along thrust fault ...
Get PriceHudec, M.R. and Jackson, M.P.A. (2006) Advance of Allochthonous Salt Sheets in Passive Margins and Orogens. American Association of Petroleum Geologist Bulletin, 90, 1535-1564. has been cited by the following article: TITLE: Tectonic Geomorphology of Iran's Salt Structures. AUTHORS: Mehran Arian, Hamideh Noroozpour
Get PriceDepositional and halokinetic-sequence stratigraphy of the Neoproterozoic Wonoka Formation adjacent to Patawarta allochthonous salt sheet, Central Flinders Ranges, South Australia Author(s) Rachelle A. Kernen Rachelle A. Kernen 1. Department of Geological Sciences, New Mexico State University, P.O. Box 30001, Las Cruces, NM 88003, USA . Search for other works by this author on: GSW. Google ...
Get PriceThese salt sheets are the result of Cretaceous thick and/or thin-skinned extension along the south Tethyan margin. The Bled Dogra salt structure is one of these submarine allochthonous salt sheets, which was emplaced during the Early Cretaceous. The geologic framework, during this period, produces conditions for a predominantly gravity-driven deformation: extension has produced space for the ...
Get PriceFrom these calculations and by geologically realistic numerical simulations it can be shown that free convection beneath allochthonous salt sheets has the potential for being a significant mechanism for both salt dissolution and mass transport, even if the underlying sediments have permeabilities as low as 10 -17 m 2 (0.01 mD). The calculated maximum Darcy fluxes and rates of salt dissolution ...
Get PriceAllochthonous salt sheets advance in four ways: (1) extrusive advance, (2) open-toed advance, (3) thrust advance, and (4) salt-wing intrusion. These mechanisms are determined primarily by the geometry and thickness of the roof that overlies the advancing sheet. An extrusive sheet spreads without a roof or with a roof of negligible mechanical strength. An open-toed sheet is partially covered by ...
Get PriceSubmarine allochthonous salt sheets: Gravity-driven deformation of North African Cretaceous passive margin in Tunisia – Bled Dogra case study and nearby salt structures
Get PriceAllochthonous salt sheets advance in four ways: (1) extrusive advance, (2) open-toed advance, (3) thrust advance, and (4) salt-wing intrusion. These mechanisms are determined primarily by the geometry and thickness of the roof that overlies the advancing sheet. An extrusive sheet spreads without a roof or with a roof of negligible mechanical strength. An open-toed sheet is partially covered by ...
Get PriceAllochthonous Salt Sheets Associated with Cretaceous Rifting in the North African Margin, Examples from North Tunisia and Petroleum Implication* Amara Masrouhi1 and Olivier Bellier2 Search and Discovery Article #30270 (2013)** Posted June 17, 2013 *Adapted from oral presentation given at AAPG European Regional Conference & Exhibition, Barcelona, Spain, April 8-10, 2013 **AAPG©2013 Serial ...
Get PriceAnimation of allochthonous salt sheets. Get Price; EMARC University of Colorado Boulder... and the various timing of emplacement of salt sheets. ... The Effect of Allochthonous Salt on Petroleum Systems of Northern Green Canyon and Ewing Bank Areas, ... Get Price; Hindered Settling... and salt sheets. ... Animation showing how downbuilding works. Blue represents salt, ... check out this recent ...
Get PriceA salt canopy is an allochthonous salt layer formed from salt that migrated up the stratigraphic section. Salt is fed into the canopy by multiple feeder stocks which reach the canopy level as diapiric structures. In the Sigsbee canopy, salt sheets sourced from more than 100 feeders have coalesced in this way to form a canopy covering more than 137 000 km 2, an area roughly the size of England ...
Get PriceFrom these calculations and by geologically realistic numerical simulations it can be shown that free convection beneath allochthonous salt sheets has the potential for being a significant mechanism for both salt dissolution and mass transport, even if the underlying sediments have permeabilities as low as 10 -17 m 2 (0.01 mD). The calculated maximum Darcy fluxes and rates of salt dissolution ...
Get PriceHouse WM, Pritchett JA (1995) Fluid migration and formation pressures associated with allochthonous salt sheets in the northern Gulf of Mexico. In: Salt, sediment and hydrocarbons; Gulf Coast Section SEPM Foundation Sixteenth Annual Research Conference, 1995. pp 121–124 Google Scholar. Huber WF (1989) Ewing Bank thrust fault zone Gulf of Mexico and its relationship to salt sill emplacement ...
Get Price"A New Mechanism for Advance of Allochthonous Salt Sheets" (PDF). Salt-Sediment Interactions and Hydrocarbon Prospectivity: Concepts, Applications, and Case Studies for the 21st Century. p. 11. Retrieved 16 November 2014.
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