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- En_echelon_veins abstract "In structural geology, en échelon veins or "en échelon gash fractures" are structures within rock caused by noncoaxial shear. They appear as sets of short, parallel, lenses on the surface of a rock. They are planar structures within the rock. They originate as tension fractures and are subsequently filled by precipitation of a mineral, typically quartz or calcite.".
- En_echelon_veins thumbnail En_echelon1.jpg?width=300.
- En_echelon_veins wikiPageID "19750198".
- En_echelon_veins wikiPageRevisionID "602287295".
- En_echelon_veins hasPhotoCollection En_echelon_veins.
- En_echelon_veins subject Category:Structural_geology.
- En_echelon_veins comment "In structural geology, en échelon veins or "en échelon gash fractures" are structures within rock caused by noncoaxial shear. They appear as sets of short, parallel, lenses on the surface of a rock. They are planar structures within the rock. They originate as tension fractures and are subsequently filled by precipitation of a mineral, typically quartz or calcite.".
- En_echelon_veins label "En echelon veins".
- En_echelon_veins sameAs m.04n0qp4.
- En_echelon_veins sameAs Q5375052.
- En_echelon_veins sameAs Q5375052.
- En_echelon_veins wasDerivedFrom En_echelon_veins?oldid=602287295.
- En_echelon_veins depiction En_echelon1.jpg.
- En_echelon_veins isPrimaryTopicOf En_echelon_veins.