Thanks, are given to Schlumberger for the donation of the Petrel E&P licenses, to the Virtual Outcrop Geology Group for the donation of LIME licenses, to Petroleum Experts for the donation of MOVE licenses, to Innovmetric for the donation of the Polyworks license and to Agisoft for the donation of the Agisoft Photoscan license. Magda Chmielewska is acknowledged for the technical support during the virtual outcrop processing. Support from the Ministerio de Economía y Competitividad (Project SEROS CGL2014-55900-P) and from the Generalitat de Catalunya (2017SGR596) is gratefully acknowledged. Thanks to reviewers Brian Willis and César Viseras and also to the Associate Editor Luca Colombera for their constructive comments, which have improved t...
The present study examined two sandstone deposits in the Aliaga outcrop as a reservoir analogue over...
The reconstruction of meander belts was approached by detailed geological mapping, the interpretatio...
The sedimentary facies of fluvial systems reflect their original depositional environment. The facie...
Abstract: Three heterogeneous models of a channel sandbody of braided stream origin were constructed...
Geological heterogeneity includes variations in porosity, lithology, mechanical properties, structur...
The variety of controls on the deposition of fluvial systems, whether autocyclic or allocyclic inclu...
Fluvial and aeolian sedimentary successions represent porous media that can host both groundwater an...
textThe Esdolomada Sandstone member 2 crops out in the Tremp-Graus Basin of north-central Spain and ...
Exploration and production from formations deposited in low-gradient fluvial systems is typically as...
The upper reservoir intervals of the Lower Jurassic Åre Formation in the Heidrun Field (Offshore mid...
Improved prediction of the recovery of oil-in-place in basin-floor fan reservoirs requires accurate ...
Improved prediction of the recovery of oil-in-place in basin-floor fan reservoirs requires accurate ...
The spatial organisation of meandering‐river deposits varies greatly within the sedimentary fills of...
An integrated stratigraphic, sedimentological and petrophysical analysis is presented to document th...
Sandstone reservoirs deposited in wave-dominated, shallow-marine environments are inherently heterog...
The present study examined two sandstone deposits in the Aliaga outcrop as a reservoir analogue over...
The reconstruction of meander belts was approached by detailed geological mapping, the interpretatio...
The sedimentary facies of fluvial systems reflect their original depositional environment. The facie...
Abstract: Three heterogeneous models of a channel sandbody of braided stream origin were constructed...
Geological heterogeneity includes variations in porosity, lithology, mechanical properties, structur...
The variety of controls on the deposition of fluvial systems, whether autocyclic or allocyclic inclu...
Fluvial and aeolian sedimentary successions represent porous media that can host both groundwater an...
textThe Esdolomada Sandstone member 2 crops out in the Tremp-Graus Basin of north-central Spain and ...
Exploration and production from formations deposited in low-gradient fluvial systems is typically as...
The upper reservoir intervals of the Lower Jurassic Åre Formation in the Heidrun Field (Offshore mid...
Improved prediction of the recovery of oil-in-place in basin-floor fan reservoirs requires accurate ...
Improved prediction of the recovery of oil-in-place in basin-floor fan reservoirs requires accurate ...
The spatial organisation of meandering‐river deposits varies greatly within the sedimentary fills of...
An integrated stratigraphic, sedimentological and petrophysical analysis is presented to document th...
Sandstone reservoirs deposited in wave-dominated, shallow-marine environments are inherently heterog...
The present study examined two sandstone deposits in the Aliaga outcrop as a reservoir analogue over...
The reconstruction of meander belts was approached by detailed geological mapping, the interpretatio...
The sedimentary facies of fluvial systems reflect their original depositional environment. The facie...