Sediment-sea-water interaction at 200 and 300^oC, 500 bars pressure: the role of sediment composition in diagenesis and low- grade metamorphism of marine clay.

Keyphrases

• Diagenesis 100%
• Seawater 100%
• Amorphous Silica 100%
• Water Interaction 100%
• Sediment Composition 100%
• Marine Clay 100%
• Low-grade Metamorphism 100%
• Salton Sea 50%
• Water-rock Interaction 50%
• Organic Carbon 50%
• Gulf Coast 50%
• Acidity 50%
• Oxidation State 50%
• Sedimentary Basin 50%
• Relative Proportion 50%
• Silicate Phases 50%
• Data Assemblage 50%
• Alteration Processes 50%
• Smectite 50%
• Silica Concentration 50%
• Cristobalite 50%
• Saturation Level 50%
• Experimental Fluids 50%
• Oxide Phase 50%
• Fluid Data 50%
• Silica Saturation 50%
• Mineralogical Assemblage 50%
• Ferromanganese Oxides 50%

Earth and Planetary Sciences

• Water-Rock Interaction 100%
• Diagenesis 100%
• Sedimentary Basin 100%
• Montmorillonite 100%
• Water Interaction 100%
• Low Grade Metamorphism 100%
• Cristobalite 100%
• Silicate 100%
• Organic Carbon 100%