Textural and geochemical alternations in Late Cenozoic Bahamian dolomites

J. M. Dawans, Peter K Swart

Research output: Contribution to journalArticle

67 Citations (Scopus)

Abstract

Describes variations of two texturally and geochemical distinct end-members. Differences in texture and geochemistry are suggested as arising through differential rates of crystallization produced as a result of variations in permeability and reactivity of the precursor sediments and rocks. -from Authors

Original languageEnglish (US)
Pages (from-to)385-403
Number of pages19
JournalSedimentology
Volume35
Issue number3
StatePublished - 1988

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dolomite
crystallization
texture
geochemistry
permeability
rock
sediment
rate

ASJC Scopus subject areas

  • Geology
  • Stratigraphy

Cite this

Textural and geochemical alternations in Late Cenozoic Bahamian dolomites. / Dawans, J. M.; Swart, Peter K.

In: Sedimentology, Vol. 35, No. 3, 1988, p. 385-403.

Research output: Contribution to journalArticle

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