Carbon isotope ratios of graphites in the Bundnerschiefer series of the Tauern Window and the Koszeg-Rechnitz Windows (Austria and western Hungary): origin of organic matter and sedimentary facies correlation

A. Demény, R. Kreulen

Research output: Contribution to journalArticle

4 Citations (Scopus)

Abstract

Based on the δ13C values, a distinction can be made between sediments deposited in the southernmost part of the Penninic ocean basin and sediments deposited more to the north. The results are used for possible sedimentary facies correations between rocks in the Alpine Penninic windows. -from Authors

Original languageEnglish
Pages (from-to)3-9
Number of pages7
JournalGeologica Carpathica
Volume44
Issue number1
Publication statusPublished - 1993

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carbon isotope ratio
organic matter
ocean basin
sediment
rock

ASJC Scopus subject areas

  • Earth and Planetary Sciences (miscellaneous)

Cite this

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abstract = "Based on the δ13C values, a distinction can be made between sediments deposited in the southernmost part of the Penninic ocean basin and sediments deposited more to the north. The results are used for possible sedimentary facies correations between rocks in the Alpine Penninic windows. -from Authors",
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AU - Kreulen, R.

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