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aflejringsmateriale, hvor mindst 50 % af de primære og/eller rekrystalliserede bestanddele består af en (eller flere) af karbonatmineralerne calcit, aragonit og dolomit i partikler af intrabassinal oprindelse.
sedimentary material in which at least 50 percent of the primary and/or recrystallized constituents are composed of one (or more) of the carbonate minerals calcite, aragonite and dolomite, in particles of intrabasinal origin.
