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Fracture As a Mechanism of Flow in Naturally Deformed Layered Rocks
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Quantitative characterization of fracture network in large sheath-fold: field and UAV-based digital outcrop model analysis (Ligurian Alps, Italy)
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inferred← citeshttps://doi.org/10.1029/2002jb002289openalex-snapshot
The formation of conjugate normal fault systems in folded sandstone by sequential jointing and shearing, Waterpocket monocline, Utah
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The effects of pressure and porosity on the micromechanics of the brittle‐ductile transition in quartzite
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Syntectonic infiltration by meteoric waters along the Sevier thrust front, southwest Montana
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