Facies-dependent δ13C variation and diagenetic overprinting at the onset of the Sturtian glaciation in North-East Greenland
Time-significant surfaces are used to construct a stratigraphic test of the intrabasinal reproducibility of a 16‰ Neoproterozoic carbon-isotope (δ 13 C) anomaly in the NE Greenland Caledonides. The δ 13 C excursion from +6‰ to -10‰ occurs in the carbonate-dominated Andrée Land Group and lies below g...
| Main Authors: | , , , , |
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| Format: | Journal article |
| Published: |
Elsevier
2017
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