Marine diagenesis of feldspathic sand: A flow-through experimental study at 200°C, 1 kbar
- 1 January 1991
- journal article
- Published by Elsevier in Chemical Geology
- Vol. 89 (3-4) , 359-377
- https://doi.org/10.1016/0009-2541(91)90025-m
Abstract
No abstract availableKeywords
This publication has 34 references indexed in Scilit:
- Seawater-basalt interaction at 200°C and 500 bars: Implications for origin of sea-floor heavy-metal deposits and regulation of seawater chemistryPublished by Elsevier ,2002
- Integrated Diagenetic Modeling: A Process-Oriented Approach for Clastic SystemsAnnual Review of Earth and Planetary Sciences, 1987
- The effect of fluid/rock ratio on feldspar dissolution and illite formation under reservoir conditionsClay Minerals, 1986
- Organic-inorganic reactions during progressive burial: key to porosity and permeability enhancement and preservationPhilosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences, 1985
- Sediment–sea-water interaction at 200 and 300 °C, 500 bars pressure: The role of sediment composition in diagenesis and low-grade metamorphism of marine clayGSA Bulletin, 1985
- Experimental authigenesis of phyllosilicates from feldspathic sandsSedimentology, 1975
- DIAGENETIC ORIGIN OF GRAYWACKE MATRIX MINERALSSedimentology, 1970
- Use of hydrothermal solution equipment to determine the solubility of anhydrite in water from 100 degrees C to 275 degrees C and from 1 bar to 1000 bars pressureAmerican Journal of Science, 1963
- The Surface Chemistry of Feldspars as an Influence on Their Decomposition ProductsClays and clay minerals (National Conference on Clays and Clay Minerals), 1957
- Evolution of the Central Texas GranitesThe Journal of Geology, 1941