Titlebook: Water-Rock Interaction; Ingrid Stober,Kurt Bucher Book 2002 Springer Science+Business Media Dordrecht 2002 environment.formation.mineral.m

Communal

惡名聲

A combined isotopic tool box for the investigation of water-rock interaction: An overview of Sr, B, er low temperature-low porosity conditions has modified the .O and/or .H compositions of the liquid phase. Example where .U has been preferentially mobilised relative to .U is presented and discussed in relation to two main processes of U mobility: preferential solution related to oxidative paleo-ev

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中和

Water-rock reaction experiments with Black Forest gneiss and granitely crushed gneiss and granite (grain size > 1 mm) 5 and 8 mg Cl was extractable per kg rock, respectively. Average measured Cl/Br ratio was about 100 (on a ppm basis), a value typical of primary high-T fluids trapped in fluid inclusions. The Cl/Br-ratios of leachates from granite and gneiss were ver

fatty-acids

Water-rock reaction experiments with Black Forest gneiss and granitely crushed gneiss and granite (grain size > 1 mm) 5 and 8 mg Cl was extractable per kg rock, respectively. Average measured Cl/Br ratio was about 100 (on a ppm basis), a value typical of primary high-T fluids trapped in fluid inclusions. The Cl/Br-ratios of leachates from granite and gneiss were ver

甜得發(fā)膩

The distribution of rare earth elements and yttrium in water-rock interactions: field observations a of the anomalous behaviour of Eu, Ce, and Y. Anomalies inherited from the source rock can be distinguished from those acquired during fluid migration. Leachates only show inherited ones, whereas both types of anomalies occur in the natural waters. By comparing REY/Ca ratios of leachates and waters

助記

The distribution of rare earth elements and yttrium in water-rock interactions: field observations a of the anomalous behaviour of Eu, Ce, and Y. Anomalies inherited from the source rock can be distinguished from those acquired during fluid migration. Leachates only show inherited ones, whereas both types of anomalies occur in the natural waters. By comparing REY/Ca ratios of leachates and waters

DOSE

Friction

GREG

Water-Rock Reactions in a Barite-Fluorite Underground Mine, Black Forest (Germany)e are very close to quartz saturation. They are saturated or slightly undersaturated with respect to calcite after relatively short flow distances through the fracture pore space. All waters are undersaturated regarding dolomite or gypsum. On pertinent activity diagrams, all waters fall into the sta