Results 71 to 80 of about 2,166 (183)

Characteristics of Lacustrine Diamictite and Analysis of Diagenetic Reservoir Facies in the Neogene Lower Youshashan Formation in the Dafengshan Tectonic Belt in the Qaidam Basin

open access: yesEnergy Science & Engineering
To address persistent challenges in lithological classification and diagenetic characterization of mixed sedimentary rocks in the Lower Youshashan Formation (Neogene) of the Fengxi area, Dafengshan structural belt, northwestern Qaidam Basin, an ...
Lin Xie   +7 more
doaj   +1 more source

Two Distinct Growth Styles of Riedel Shear Zones in Cratonic Strike‐Slip Fault System, Tarim Basin, NW China

open access: yesJournal of Geophysical Research: Solid Earth, Volume 131, Issue 8, August 2026.
Abstract The kinematics and progressive evolution of Riedel shear zones have been extensively studied, yet the factors controlling their distinct evolutionary styles in natural settings remain debated. Understanding such fracture network architecture has great implications, such as predicting subsurface fluid flow and assessing seismic hazards.
Jiajun Chen   +7 more
wiley   +1 more source

Source‐to‐sink sediment transport reversals during glacial sea‐level lowstands sustain soil formation on pericoastal carbonate terrains

open access: yesSedimentology, Volume 73, Issue 5, Page 1892-1910, August 2026.
ABSTRACT Understanding the processes that drive soil formation is crucial for developing sustainable land‐use strategies, as changing land‐use practices and climate change exacerbate soil erosion. The formation of substantial arable soils on carbonate bedrock requires substantial dust accretion as the underlying bedrock lacks siliciclastic material. In
Daniel Palchan   +3 more
wiley   +1 more source

A reservoir rock wettability modifier for ultra-high temperature and high salinity environment

open access: yesEnergy Geoscience
During drilling process, the water phase in drilling fluids infiltrates rock fractures through capillary action. The surface wettability of dolomite is governed by multiple factors, resulting in an unstable wetting state. Studies have shown that altering
Ling Lin   +4 more
doaj   +1 more source

Exsolution, Evolution, and Hysteresis of CO2 Nanobubbles in Water‐Saturated Sandstone

open access: yesGeophysical Research Letters, Volume 53, Issue 13, 16 July 2026.
Abstract Understanding CO2 nanobubble formation in water‐saturated sandstone is critical for understanding fluid behavior in CO2 storage systems. Here, CO2 exsolution from an aqueous phase in a sandstone was investigated using small‐angle neutron scattering at 50°C during cyclic depressurization from 12 to 0.7 MPa.
Amirsaman Rezaeyan   +6 more
wiley   +1 more source

Sedimentary facies and reservoir characteristics of fourth Member of Dengying Formation in Well DB1 area, north-central Sichuan Basin

open access: yesYouqi dizhi yu caishoulu
The reservoir lithology of the fourth Member of Dengying Formation in the north-central Sichuan Basin is complex with strong heterogeneity, which limits the gas reservoir exploration in the fourth Member of Dengying Formation.
CHEN Hongwei   +5 more
doaj   +1 more source

Are Time and Temperature the Simple Answer to the Dolomite Problem?

open access: yesGeophysical Research Letters, Volume 53, Issue 13, 16 July 2026.
Abstract Dolomite is among the most common carbonate minerals in ancient rocks but its formation is rarely observed today, a longstanding puzzle known as the “Dolomite Problem.” Recent advances in experimental mineralogy, geochemistry, and global abundance reconstructions have begun to resolve this problem.
Ian Winkelstern
wiley   +1 more source

Modeling of a carbonate reservoir of ultraviscous oil of the Kazanian Stage to determine priority areas for development

open access: yesGeoresursy
The presented analysis of the three-dimensional geological model of the Gorsky ultraviscous oil reservoir, located on the eastern side of the Melekess Depression (the border of the Republic of Tatarstan and the Samara region).
R. A. Mudarisova   +5 more
doaj   +1 more source

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