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Maliva, R. G., Dickson, J. A. D., Råheim, A. (1991) Modelling of chalk diagenesis (Eldfisk Field, Norwegian North Sea) using whole rock and laser ablation stable isotopic data. Geological Magazine, 128 (1) 43-49 doi:10.1017/s0016756800018033

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Reference TypeJournal (article/letter/editorial)
TitleModelling of chalk diagenesis (Eldfisk Field, Norwegian North Sea) using whole rock and laser ablation stable isotopic data
JournalGeological Magazine
AuthorsMaliva, R. G.Author
Dickson, J. A. D.Author
Råheim, A.Author
Year1991 (January)Volume128
Issue1
PublisherCambridge University Press (CUP)
DOIdoi:10.1017/s0016756800018033Search in ResearchGate
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Mindat Ref. ID254910Long-form Identifiermindat:1:5:254910:5
GUID0
Full ReferenceMaliva, R. G., Dickson, J. A. D., Råheim, A. (1991) Modelling of chalk diagenesis (Eldfisk Field, Norwegian North Sea) using whole rock and laser ablation stable isotopic data. Geological Magazine, 128 (1) 43-49 doi:10.1017/s0016756800018033
Plain TextMaliva, R. G., Dickson, J. A. D., Råheim, A. (1991) Modelling of chalk diagenesis (Eldfisk Field, Norwegian North Sea) using whole rock and laser ablation stable isotopic data. Geological Magazine, 128 (1) 43-49 doi:10.1017/s0016756800018033
In(1991, January) Geological Magazine Vol. 128 (1) Cambridge University Press (CUP)
Abstract/NotesAbstractLaser ablation techniques permit the determination of the stable isotopic ratios of finely crystalline calcite cements in chalks for the first time. Modelling of fluid–rock interaction using whole rock and laser ablation stable isotopic data indicates that carbonate mineral diagenesis in the Eldfisk Field consisted largely of the dissolution and reprecipitation of calcite with little associated loss of porosity. Cementation by calcite derived from stylolites apparently occurred throughout the Eldfisk Field chalk, but had only a subsidiary effect on whole rock isotopic ratios. Oxygen isotopic data indicates a pore water temperature of 50–80 °C during the bulk of chalk recrystallization. Increases in whole rock δ13C values with depth are likely the result of bacterial methanogenesis during chalk recrystallization.


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