The calcite-graphite isotope thermometer; data on graphite bearing marbles from Naxos, Greece

Details The calcite-graphite isotope thermometer; data on graphite bearing marbles from Naxos, Greece The calcite-graphite isotope thermometer; data on graphite bearing marbles from Naxos, Greece

Aug 1983

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1983gecoa..47.1527k&link_type=abstract

Geochimica et Cosmochimica Acta, vol. 47, Issue 8, pp.1527-1530

Computer Science

8

Scientific paper

Graphite bearing marbles occur in the regional metamorphic complex of Naxos over a continuous temperature range of 380 to 670°C. The graphite is of biogenic origin and changed its original isotopic composition towards values in equilibrium with the calcite. Partial isotope exchange took place at temperatures as low as 380°C, but near equilibrium values were generally not reached below 550°C. The data agree better with the theoretically derived fractionation curve of (1969) than with the empirical curve proposed by and (1981). We believe that the system will not provide a good thermometer.

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