Brittle-ductile Deformation Behaviour in the Middle Crust as Exemplified by Mullions (former "boudins") in the High-Ardenne Slate Belt, BelgiumLeuven University Press, 2004 - 127 pagina's |
Veelvoorkomende woorden en zinsdelen
analysis angle Appendix Ch3 Ardenne Ardenne culmination Ardenne-Eifel area aspect ratio Bastogne Collignon Bastogne Mardasson Bertrix Beugnies Boeur boudinage Bütgenbach chlorite cleavage-bedding competent layers corresponds cuspate-lobate geometry Dedenborn deformation Devonian differential stress Dinant Dinant synclinorium Eifel Emsian epizonal Fielitz and Mansy flow law fluid pressures folds foliation Fosset geographic coordinates High-Ardenne slate belt Houffalize hydraulic fracturing isolated fluid inclusions kinematic layer-parallel shortening located Lochkovian Lohest Longlier low-grade metamorphic Mabompré massif metamorphic zone middle crust minerals mixed aqueous/gaseous mudstones/pelites mullion formation multilayer structures observed Oignies Orientation data oriented oblique P-T conditions parameters pelite pelite-psammite interface Pragian primary fluid inclusions psammite layers quarry quartz veins quartzite quartzite layers recrystallized Remagne Rhenohercynian basin rheology Roches Rouette sandstones sedimentary Siegenian siltstones smaller veins Stainier Stereogram strain stress exponent synclinorium tectonic cleavage temperatures Th CO2 thickness Variscan Variscan orogeny vein quartz vein walls vein-bedding intersection veins occur Viséan width of picture