Cement origin of supratidal dolomite, Andros Island, Bahamas

Z. Lasemi, M. R. Boardman, P. A. Sandberg

Research output: Contribution to journalArticlepeer-review

Abstract

These microcrystalline, calcian dolomite cements commonly occur in lithified lime mud crusts, but they also occur in unconsolidated sediments, mainly as intragranular precipitates. The voids in which the dolomite occurs vary in size from minute wall pores in rotaliid forams and endolithic borings to major intra- and interparticle pores. In the larger pores, dolomite commonly forms an isopachous fringe. -from Authors

Original languageEnglish (US)
Pages (from-to)249-257
Number of pages9
JournalJournal of Sedimentary Petrology
Volume59
Issue number2
StatePublished - Jan 1 1989
Externally publishedYes

ASJC Scopus subject areas

  • Environmental Science(all)
  • Earth and Planetary Sciences(all)

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