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Discovery of a significant cave entrance in stripe karst, Horsethief Creek Group, Wells Gray Provincial Park, British Columbia, Canada
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Notre histoire - Français
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Etude par analogie de l'influence d'une crue sur l'evolution d'une nappe phréatique placée à proximité d'une rivière
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Mid Century Modern Cushion Coverabstract Pillow Casebohemian - Etsy Israel
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The role of gravitational body forces in the development of metamorphic core complexes | Nature Communications
SE - Relations - Regional-scale paleofluid system across the Tuscan Nappe–Umbria–Marche Apennine Ridge (northern Apennines) as revealed by mesostructural and isotopic analyses of stylolite–vein networks
Deep subduction, melting, and fast cooling of metapelites from the Cima Lunga Unit, Central Alps - Piccoli - 2022 - Journal of Metamorphic Geology - Wiley Online Library
Hydrology | Free Full-Text | Surface and Groundwater Interactions: A Review of Coupling Strategies in Detailed Domain Models
LARGE WOODY DEBRIS ACCUMULATIONS IN THE LATE PENNSYLVANIAN TROPICS—EVOLUTIONARY SIGNAL OR TECTONO-CLIMATIC ARCHIVE?
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Land-surface subsidence in the Houston-Galveston region, Texas
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SE - Relations - Regional-scale paleofluid system across the Tuscan Nappe–Umbria–Marche Apennine Ridge (northern Apennines) as revealed by mesostructural and isotopic analyses of stylolite–vein networks
How post‐salt sediment flux and progradation rate influence salt tectonics on rifted margins: Insights from geodynamic modelling - Pichel - Basin Research - Wiley Online Library
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Water | Free Full-Text | Do the Volume-of-Fluid and the Two-Phase Euler Compete for Modeling a Spillway Aerator?
Nanopore Evolution of the Upper Permian Organic-Rich Shales from Dalong Formation, Sichuan Basin, during Artificial Hydrous Pyrolysis | Energy & Fuels
Fiber Optic Technology for Environmental Monitoring: State of the Art and Application in the Observatory of Transfers in the Vadose Zone-(O-ZNS) | SpringerLink
SE - Regional-scale paleofluid system across the Tuscan Nappe–Umbria–Marche Apennine Ridge (northern Apennines) as revealed by mesostructural and isotopic analyses of stylolite–vein networks
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