EVOLUTION OF THE RUSSELL LAKE ALLOCHTHON AND THE SOAPSTONE RIDGE COMPLEX IN GEORGIA, SOUTHERN APPALACHIANS: INFERENCES FROM CHLORITE GEOTHERMOMETRY
Chlorite occurs together with zoned amphiboles, and chlorite crystals in the RLA have rather low total iron atoms per formula unit and they dominantly plots in the ripidolite field whereas SSR chlorites are even poorer in total iron and almost all are clinochores. Application of chlorite thermometry to rocks of the RLA yields temperatures which range from ~280oC to ~320oC, whereas chlorites from the SSR yield temperatures which range from ~200oC to ~250oC. These calculated temperatures indicate that chlorites in the RLA were formed at higher temperatures in comparison to those from the SSR, which may suggest that these bodies underwent different metamorphic conditions and may also have originated under different tectonic settings. Since these two geographically distinct locations where metamorphosed mafic/ultramafic bodies crop out are at least 100km apart, and a terrane boundary occurs between them, it is interpreted here that they were each metamorphosed, and perhaps formed, in different regions and each was later thrusted onto its country rocks during the final stages of the assembly of Pangea.