title: Dolomitization: Observations on the Island of Bonaire, Netherlands Antittes.
abstract: Evaporation of sea water and gypsum precipitation on south Bonaire produce dense brines having a high ratio of magnesium to calcium. Recent dolomite is a common replacement product in the associated carbonate sediments. A mass balance indicates that brine is being refluxed downward today, and the Pleistocene dolomite on north Bonaire could have been produced by similar reflux of brine.
authors.forename: K S
authors.initials: KS
authors.lastname: Deffeyes
authors.forename: F J
authors.initials: FJ
authors.lastname: Lucia
authors.forename: P K
authors.initials: PK
authors.lastname: Weylt