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Par Collection Par Auteur- EREZ, J. (1)
- 1979 (1)
- Modification of the oxygen-isotope record in deep-sea cores by Pleistocene dissolution cycles
- The glacial-interglacial amplitude (GIA) of oxygen-isotope curves in sediment cores from the Atlantic Ocean is much higher than the amplitude in the Pacific. This difference is explained by nonsynchronous CaCO dissolution cycles during the Upper
- 1979