Zdjęcie176

Zdjęcie176



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


POROSITY


Mg CALCITE ARAGONITE


DOLOMITE


Zrodło hltp//$trat


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