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Origin of low delta O-18, pre-compactional ferroan carbonates in the marine Sto formation (Middle Jurassic), offshore NW Norway
Uppsala University, Teknisk-naturvetenskapliga vetenskapsområdet, Earth Sciences, Department of Earth Sciences.
1996 (English)In: MARINE AND PETROLEUM GEOLOGY, ISSN 0264-8172, Vol. 13, no 2, 263-276 p.Article in journal (Refereed) Published
Abstract [en]

Siderite (delta(18)O(PDB) = -9.3 to - 5.7 parts per thousand) and Fe-dolomite/ankerite (delta(18)O(PDB) = -13.7 to -7.7 parts per thousand) occur as texturally early diagenetic, pre-compactional cements in sandstones and mudstones of the nearshore to inne

Place, publisher, year, edition, pages
BUTTERWORTH-HEINEMANN LTD , 1996. Vol. 13, no 2, 263-276 p.
Keyword [en]
sandstone diagenesis; siderite; ankerite; ISOTOPIC COMPOSITION; DIAGENETIC HISTORY; PORE-WATER; GEOTHERMAL BRINE; CENTRAL ENGLAND; SIDERITE; CONCRETIONS; SEDIMENTS; CALCITE; CEMENTS
Identifiers
URN: urn:nbn:se:uu:diva-27946OAI: oai:DiVA.org:uu-27946DiVA: diva2:55842
Note
Addresses: Morad S, UPPSALA UNIV, INST EARTH SCI, SEDIMENTARY GEOL RES GRP, NORBYVAGEN 18B, S-75236 UPPSALA, SWEDEN. UNIV WINDSOR, DEPT EARTH SCI, WINDSOR, ON N9B 3P4, CANADA. UNIV FED RIO GRANDE SUL, INST GEOCIENCIAS, BR-91501970 PORTO ALEGRE, RS, BRAZILAvailable from: 2008-10-17 Created: 2008-10-17 Last updated: 2011-01-15

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