Evaporitic sediments from the Max borehole (Mulhouse Potash Basin, southern Rhine Graben) were studied over an interval of about 40 m in the vicinity of sylvite beds. Total organic carbon (TOC) analyses of 450 samples showed that marly layers interbedded within the evaporites have TOC values that fl
β¦ LIBER β¦
Palaeoclimate controlled accumulation of organic matter in Oligocene evaporite sediments of the Mulhouse basin
β Scribed by P. Hofmann; D. Leythaeuser; B. Carpentier
- Book ID
- 116094446
- Publisher
- Elsevier Science
- Year
- 1993
- Tongue
- English
- Weight
- 966 KB
- Volume
- 20
- Category
- Article
- ISSN
- 0146-6380
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