Results 191 to 200 of about 24,734 (270)

Research on Flow Patterns of Two-Phase Fracturing Fluid in Hydraulic Fracture Considering the Fluid Leak-off

open access: yesACS Omega
Yusong Chen   +7 more
doaj   +1 more source

Ice‐Rafted Detritus of the Southeast Grand Banks Slope, Newfoundland, Throughout Heinrich Layers 1 to 5a: 1. Petrology and Abundance

open access: yesGeochemistry, Geophysics, Geosystems, Volume 26, Issue 10, October 2025.
Abstract The Late Pleistocene stratigraphic sequence of Heinrich event layers 1 to 5a shows a high petrological diversity with systematically varying abundances of specific ice‐rafted detritus (IRD) species. Our study core GeoB18530‐1 from the southeastern Grand Banks Slope of Newfoundland resolves these in continuity and considerable detail.
S. Bukar   +7 more
wiley   +1 more source

A novel method for evaluating shale gas preservation conditions in an area on a regional scale. [PDF]

open access: yesSci Rep
Liu Y   +8 more
europepmc   +1 more source

Modeling Overpressure Development and the Mechanical Behavior of Sediments in a Complex, Tectonically Active Setting: East Coast Basin, New Zealand

open access: yesJournal of Geophysical Research: Solid Earth, Volume 130, Issue 10, October 2025.
Abstract The East Coast Basin (ECB) is a complex, active convergent margin located on the North Island of New Zealand, where variable but commonly very high overpressures occur in Cretaceous to Pleistocene stratigraphy. Using a consistent set of sediment physical properties and a single value for tectonic compression, a multi‐1D hydro‐mechanical ...
E. E. Calderon Medina   +5 more
wiley   +1 more source

Research and Evaluation of a Nanometer Plugging Agent for Shale Gas Horizontal Wells. [PDF]

open access: yesACS Omega
Tian Y   +10 more
europepmc   +1 more source

Growing Season Precipitation Percolates to Groundwater Past Older Water in Storage Across a Temperate Agricultural Catchment

open access: yesWater Resources Research, Volume 61, Issue 10, October 2025.
Abstract How water is stored within‐ and released from‐the vadose zone controls groundwater recharge, plant water uptake, and the movement of dissolved solutes (nutrients, carbon, pollutants). The goal of this study was to determine the age of water recharging groundwater during the growing season in a temperate agricultural catchment. We measured soil
Joshua W. Snarski   +3 more
wiley   +1 more source

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