Glossary: Geochemistry and diagenesis
See also the companion Glossary of Petrography and Petrology 1:1 clay layers: All crystalline clay minerals are formed by bonding […]
See also the companion Glossary of Petrography and Petrology 1:1 clay layers: All crystalline clay minerals are formed by bonding […]
See companion glossaries: Geochemistry and diagenesis Paleontology Sedimentary facies and processes Actinolite: see Tremolite Aegirine – aegirine augite: NaFe3+(SiO3)2 Clinopyroxenes
Companion glossaries Abyssal plain: The deepest parts of the oceans at 4000-8000 m, covering 83% of Earth’s total ocean area.
Companion glossaries Angle of repose: The natural slope of loose, cohesionless sedimentary particles (sand, gravel) under static conditions, as a
Companion glossaries Ablation: The removal of ice and snow by melting, evaporation, wind erosion, sublimation (solid to vapour phase without
Henry Darcy’s pivotal experiments with sand-filled tubes (in 1856) established an empirical relationship between hydraulic gradient (that is basically an
Forearc basins are kinematically linked to accretionary prisms. Forearc basins and accretionary prisms are located in the arc-trench gap
Some terminology for Thrust faults, duplexes, imbricate fans, and fold-thrust belts. Thrusts are reverse faults having fault plane dips <45o,
Basins formed by flexure of oceanic and continental lithosphere; foreland basin exemplars. What is flexure? The way we define the
A fault is a plane or linear zone of displacement, where rocks on one side of the plane slip past