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Diagenesis of siliciclastic and volcaniclastic sediments in the Cretaceous and Miocene sequences of the NW African margin (DSDP Leg 47A, Site 397)
Uppsala University, Teknisk-naturvetenskapliga vetenskapsområdet, Earth Sciences, Department of Earth Sciences.
1997 (English)In: SEDIMENTARY GEOLOGY, ISSN 0037-0738, Vol. 112, no 1-2, 137-156 p.Article in journal (Refereed) Published
Abstract [en]

The Lower Cretaceous and Miocene sequences of the NW African passive continental margin consist of siliciclastic, volcaniclastic and hybrid sediments, These sediments contain a variety of diagenetic carbonates associated with zeolites, smectite clays and

Place, publisher, year, edition, pages
ELSEVIER SCIENCE BV , 1997. Vol. 112, no 1-2, 137-156 p.
Keyword [en]
sediment diagenesis; sandstone; deep-sea; carbonates; zeolites; smectite; passive margin; ISOTOPIC COMPOSITION; STABLE ISOTOPE; NORTH-SEA; ORIGIN; CARBONATES; CLASSIFICATION; PRECIPITATION; REDUCTION; EVOLUTION; SIDERITE
Identifiers
URN: urn:nbn:se:uu:diva-27861OAI: oai:DiVA.org:uu-27861DiVA: diva2:55757
Note
Addresses: DeRos LF, UNIV FED RIO GRANDE SUL, INST GEOCIENCIAS, DEPT MINERAL & PETROL, AV BENTO GONCALVES 9500, BR-91501970 PORTO ALEGRE, RS, BRAZIL. UPPSALA UNIV, INST EARTH SCI, SEDIMENTARY GEOL RES GRP, S-75236 UPPSALA, SWEDEN. UNIV WINDSOR, DEPT EARTHAvailable from: 2008-10-17 Created: 2008-10-17 Last updated: 2011-01-15

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