Low-Mg calcite marine cement in Cretaceous turbidites: origin, spatial distribution and relationship to seawater chemistry

ABSTRACT Lower Cretaceous (Hauterivian) bioclastic sandstone turbidites in the Scapa Member (North Sea Basin) were extensively cemented by low‐Mg calcite spars, initially as rim cements and subsequently as concretions. Five petrographically distinct cement stages form a consistent paragenetic sequen...

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Veröffentlicht in:Sedimentology 1996-10, Vol.43 (5), p.877-900
Hauptverfasser: HENDRY, JAMES P., TREWIN, NIGEL H., FALLICK, ANTHONY E.
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Sprache:eng
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