Carbonate isotopes from high altitude Tso Moriri Lake (NW Himalayas) provide clues to late glacial and Holocene moisture source and atmospheric circulation changes
- Resource Type
- Article
- Source
- In
Palaeogeography, Palaeoclimatology, Palaeoecology 1 May 2015 425:76-83 - Subject
- Language
- ISSN
- 0031-0182