Geochemistry of the Hepworth Carboniferous sediment sequence and origin of the diagenetic iron minerals and concretions
- 2 June 1979
- journal article
- research article
- Published by Elsevier in Geochimica et Cosmochimica Acta
- Vol. 43 (6) , 927-941
- https://doi.org/10.1016/0016-7037(79)90230-8
Abstract
No abstract availableThis publication has 22 references indexed in Scilit:
- Isotopic evidence for source of diagenetic carbonates formed during burial of organic-rich sedimentsNature, 1977
- Early diagenesis in anaerobic lake sediments: chemical equilibria in interstitial watersGeochimica et Cosmochimica Acta, 1976
- Mineralogy, chemistry, and origin of a concretionary siderite sheet (clay-ironstone band) in the Westphalian of YorkshireMineralogical Magazine, 1975
- Stable Carbon Isotope Ratios within Carbonate Concretions: a Clue to Place and Time of FormationNature, 1972
- Magnesium-Iron Replacement in Clay Minerals in Anoxic Marine SedimentsScience, 1971
- Consolidation and Cementation of Recent Sediments in the Atchafalaya BasinGSA Bulletin, 1969
- Gibt es rezente rot-sedimente in der Adria?Marine Geology, 1968
- Diagenetic iron minerals in some British Carboniferous sedimentsGeochimica et Cosmochimica Acta, 1967
- Iron Sulfides Formed from Aqueous Solution at Low Temperatures and Atmospheric PressureThe Journal of Geology, 1964
- A combined gravimetric and photometric procedure for determining silica in silicate rocks and mineralsThe Analyst, 1960