In a gravity core from the eastern Mediterranean Sea, a chemically and mineralogically distinct, 5.5-cm-thick layer is present above sapropel S-1 and overlain by hemipelagic marls. Calcite is completely absent in this exotic layer, dolomite is present only in small amounts, and the Cr concentrations
β¦ LIBER β¦
Humic substances in an Arabian shelf sediment and the S1 sapropel from the Eastern Mediterranean
β Scribed by E.-L. Poutanen; R.J. Morris
- Book ID
- 115813945
- Publisher
- Elsevier Science
- Year
- 1985
- Tongue
- English
- Weight
- 815 KB
- Volume
- 51
- Category
- Article
- ISSN
- 0009-2541
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