The isotopic composition of carbonaceous matter in a metamorphic profile from the Swiss Alps

Details The isotopic composition of carbonaceous matter in a metamorphic profile from the Swiss Alps The isotopic composition of carbonaceous matter in a metamorphic profile from the Swiss Alps

Aug 1976

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1976gecoa..40..945h&link_type=abstract

Geochimica et Cosmochimica Acta, vol. 40, Issue 8, pp.945-951

Computer Science

22

Scientific paper

44 13 C -values for carbonaceous matter in a metamorphic profile from the Swiss Alps have been determined. The analyzed samples range from unmetamorphosed sediments to staurolite schists. The carbon isotopic composition is more-or-less constant with -values around -25%. in the unmetamorphosed sediments, but shifts towards higher 13 C-content with increasing grade of metamorphism. 13 C values of around -11%. were measured in the rocks of the highest metamorphic grade.

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