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The AAPG/Datapages Combined Publications Database
GCAGS Transactions
Abstract
Abstract: Carbonate Dolomitization in Geochemistry
Saleh M. Billo
ABSTRACT
Although many researchers believe that most, if not all, dolomites are mainly formed by secondary replacement of limestones anywhere from soon after deposition, diagenesis, to now, a controversy over dolomite origin still remains. This is fueled by the fact that (a) thinly laminated wholly unfossiliferous dolomites closely associated with bedded anhydrite recur frequently in the stratigraphic record and (b) the discovery of Recent primary or evaporitic penecontemporanceous dolomites in the intertidal and supratidal regions of the Arabian Gulf, Florida, and the Bahamas, and other areas. Yet, no one has been able to synthesize dolomite in a laboratory simulating normal marine conditions; albeit experimental work at low temperatures has recently produced dolomite from solutions at pH's greater than 9.5 while maintaining high concentrations of SO4 and NO3. Now there is new evidence from carbonate geochemistry showing the precipitation of primary dolomites is related to kinetics or reaction rates.
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ACKNOWLEDGMENTS AND ASSOCIATED FOOTNOTES
King Saud University, Riyadh, Saudi Arabia
Copyright © 1999 by The Gulf Coast Association of Geological Societies