Results 181 to 190 of about 6,606 (218)
Logging-data-driven lithology identification of conglomerate reservoir by the assistance of integrated machine learning methods. [PDF]
Liu J, Xu D.
europepmc +1 more source
ABSTRACT This study investigated the formation mechanism responsible for anomalously high permeability (AHP) observed in the Eocene sandstones at depths from 3824 to 3832 m in the Huizhou Sag, Pearl River Mouth Basin, China, using helium porosity and permeability measurements, thin section, scanning electron microscopy, electron probe X‐ray ...
Changgui Xu +12 more
wiley +1 more source
Evaluating the impact of CO<sub>2</sub> on the geomechanical and geochemical properties of different rock types. [PDF]
Dontoh WH +5 more
europepmc +1 more source
ABSTRACT Shelf‐edge deltas are commonly interpreted to record basinward facies migration across uninterrupted, gently dipping shelf margins; however, examples from mixed siliciclastic‐carbonate margins reveal more complex depositional dynamics. Periods and areas of carbonate sedimentation within mixed siliciclastic‐carbonate margins can modify shelf ...
Abdulkarim Al‐Hussaini +3 more
wiley +1 more source
Quantitative reconstruction and sedimentary response of a Jurassic paleodrainage system. [PDF]
Li N +7 more
europepmc +1 more source
Downcurrent variation in submarine channel‐fill architecture from the shelf to upper slope
ABSTRACT The transition between the shelf and the upper slope is often considered an area of sediment bypass, where steeper gradients increase flow velocities and maintain particles in suspension. In addition to transferring sediments into deeper basins, upper‐slope areas can also host channelised submarine deposits.
Moreno Pizzutto +6 more
wiley +1 more source
A stress-controlled reservoir formation model for ultra-deep sandstones in foreland thrust belts: case study of the cretaceous bashijiqike formation, bozi-dabei area, kuqa depression, tarim basin. [PDF]
Wang C, Zhong D, Mo T, Sun H.
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ABSTRACT Thin, discontinuous, organic‐rich oil shale beds in the siliciclastic‐evaporitic Salt Range Formation (SRF) of Pakistan are of approximate Neoproterozoic to Cambrian age based on stratigraphic constraints. The beds are enriched (26–43 wt.% total organic carbon, TOC) in aliphatic organic matter (OM) of low thermal maturity despite their ...
Paul C. Hackley +4 more
wiley +1 more source
Influence of microcrack types on macroscopic cracking of sandstone under freeze-thaw erosion. [PDF]
Sun Y, Liang B, Ma J, Jin J, Liu D.
europepmc +1 more source

