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Diagenesis and reservoir-quality evolution of fluvial sandstones during progressive burial and uplift: Evidence from the Upper Jurassic Boipeba Member, Reconcavo basin, northeastern Brazil
Uppsala University, Teknisk-naturvetenskapliga vetenskapsområdet, Earth Sciences, Department of Earth Sciences.
Uppsala University, Teknisk-naturvetenskapliga vetenskapsområdet, Earth Sciences, Department of Earth Sciences. Solid Earth Geology. (Sedimentary Petrology)
2000 (English)In: AAPG BULLETIN-AMERICAN ASSOCIATION OF PETROLEUM GEOLOGISTS, ISSN 0149-1423, Vol. 84, no 7, p. 1015-1040Article in journal (Refereed) Published
Abstract [en]

The reservoir quality of fluvial sandstones of the Upper Jurassic Boipeba Member, Reconcavo basin, northeastern Brazil, is highly heterogeneous and controlled by eodiagenesis under semiarid climate, mesodiagenesis during burial to a depth of 3500 m, and t

Place, publisher, year, edition, pages
2000. Vol. 84, no 7, p. 1015-1040
Keywords [en]
NORWEGIAN CONTINENTAL-SHELF; NORTH-SEA; QUARTZ CEMENTATION; PHANEROZOIC TIME; POROSITY; COMPACTION; HALTENBANKEN; CARBONATE; SEDIMENTS; REDUCTION
Identifiers
URN: urn:nbn:se:uu:diva-37746OAI: oai:DiVA.org:uu-37746DiVA, id: diva2:65645
Note
Addresses: Salem AM, Tanta Univ, Fac Educ, Kafr El Sheikh, Egypt. Uppsala Univ, Inst Earth Sci, SE-75236 Uppsala, Sweden. Petrobras SA, E&P BA, BR-41856900 Salvador, BA, Brazil. Univ Windsor, Dept Earth Sci, Windsor, ON N9B 3P4, Canada.Available from: 2006-12-02 Created: 2006-12-02 Last updated: 2011-01-14

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