Material flux and porosity changes during sediment diagenesis
- 1 March 1992
- journal article
- Published by Springer Nature in Nature
- Vol. 356 (6364) , 52-54
- https://doi.org/10.1038/356052a0
Abstract
No abstract availableKeywords
This publication has 11 references indexed in Scilit:
- Carbon, oxygen and sulphur isotope variations in concretions from the Upper Lias of N.E. EnglandPublished by Elsevier ,2003
- Supercomputer Analysis of Sedimentary BasinsScience, 1988
- The application of fluid inclusions to migration of oil and diagenesis in petroleum reservoirsApplied Geochemistry, 1987
- Pore water evolution during sediment burial from isotopic and mineral chemistry of calcite, dolomite and siderite concretionsGeochimica et Cosmochimica Acta, 1986
- Diagenetic Reactions in SandstonesPublished by Springer Nature ,1983
- Mechanism of burial metamorphism of argillaceous sediment: 1. Mineralogical and chemical evidenceGSA Bulletin, 1976
- Stable Carbon Isotope Ratios within Carbonate Concretions: a Clue to Place and Time of FormationNature, 1972
- Clay-Ironstone Concretion Preserving Fabrics Due to Progressive CompactionGSA Bulletin, 1972
- THE GROWTH OF CAMBRIAN AND LIASSIC CONCRETIONSSedimentology, 1971
- Ton, Geoden und Minerale des Barrême von HoheneggelsenInternational Journal of Earth Sciences, 1955