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POHOS'TY ,S PROOUCEO BY BECRYSTAU.IZATION OF UMESTONE TO DOLOMITE THE UMESTONE MAY BE LEACHEO WH1LE OOLOMITIZATION OCCURS
ARAGONITE OOLITE
INTERCRYSTALLINE POROSITY
*
OOLOMITIZATION OF GRAINS MAY BE SElECTlV£ OF MAGNESlAN CALCITE MICRITE ENVELOPES WHILE THE ARAGONITE IS C*SSOtV£D
DOLOMITE
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