초록

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Abstract ▼ AI-Helper

Illite 'crystallinity' and chlorite chemistry are applied to the evaluation of the thermal grade of the Jigunsan Formation. Illite 'crystallinity' value of the formation has the range fom 4.48 to 32.5 in Weaver index (W.I.) and from $0.14{{\Delta}{\circ}}\;2{\Theta}$to $0.03{{\Delta}...

Illite 'crystallinity' and chlorite chemistry are applied to the evaluation of the thermal grade of the Jigunsan Formation. Illite 'crystallinity' value of the formation has the range fom 4.48 to 32.5 in Weaver index (W.I.) and from $0.14{{\Delta}{\circ}}\;2{\Theta}$to $0.03{{\Delta}{\circ}}\;2{\Theta}$in kubler index (K.I). Most of illite 'crystallinity' values in this formation belong to the epizone field (K.I.<$0.21{{\Delta}{\circ}}\;2{\Theta}$). The chemistry and calculated temperature of chlorites from this formation (Fe/(Fe+Mg)=0.45, Tet. Al/Octa. Al=0.84, the calculated temperature=250-270${\circ}C$) are similar to those of epizone chlorites in the literature. The results of this work show that the metamorphic grade of the Jigunsan Formation belongs to the epizone and the formation is believed to have been reached paleotemperatures of at least 300${\circ}C$.