δ13C–δ18C covariance as a paleohydrological indicator for closed-basin lakes
- 1 September 1997
- journal article
- Published by Elsevier in Palaeogeography, Palaeoclimatology, Palaeoecology
- Vol. 133 (1-2) , 69-80
- https://doi.org/10.1016/s0031-0182(96)00153-8
Abstract
No abstract availableKeywords
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