Geofluids

Papers
(The H4-Index of Geofluids is 14. The table below lists those papers that are above that threshold based on CrossRef citation counts [max. 250 papers]. The publications cover those that have been published in the past four years, i.e., from 2022-05-01 to 2026-05-01.)
ArticleCitations
Evaluation of the Oil-Bearing Properties of Shale and Shale Oil Mobility in the Fengcheng Formation in the Mahu Sag, Junggar Basin, Northwest China: A Case Study of Well Maye-156
Experimental Study on the Mechanical Mechanism of Arch-Chord-Coupled Antisliding Structure40
A Nonlinear Strength Criterion of Frozen Saline Sandy Soil at High Pressures31
Analytical Analysis of Infinite Heterogeneous Slope Stability considering Suction Influence27
Study of the Effect of Drying on the Pore Structure and Rate of Oxygen Consumption and Heat Release of Immersed Lignite26
Calculation of Cementing ECD for Well Annuli with Narrow or Varied Radial Sizes21
Experimental Study on Compaction Characteristics and Mechanical Behavior of Crushed Rock Masses19
Numerical Simulation of Gas-Solid Coupling in Pressure-Relief Gas Drainage of Short-Distance and Underprotective Steeply Inclined Coal Seam Mining17
Experimental Study for the Effects of Different Factors on the Sand-Carrying Capacity of Slickwater16
Saturation Height Modelling for Tight Sandstone Reservoirs with Gas Diffusion Dynamics Taken into Account16
Study on the Formation Mechanism of Seepage Network in Fractured Rock Mass Under the Coupling of Hydromechanical Process15
Influence of Drying–Wetting Cycles on the Water Retention and Microstructure of Residual Soil15
Experiment Analysis of Drilling Feedback Signal from Simulation of Roadway Roof15
Study of Impact Dynamic Characteristics and Damage Morphology of Layered Rock Mass15
Roof Water Damage Prediction and Evaluation of Sand-Mud Sedimentary Tectonic Strata14
Numerical Modeling of Shear Behavior in Rough Joints of Unsaturated Sandstone14
Thermal-Moisture Dynamics at Different Underlying Surfaces in Permafrost Regions of the Central Tibetan Plateau by considering the Effect of Rainfall14
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