δ 13 C, δ 18 O and deposition rate of tufa in Xiangshui River, SW China: implications for land-cover change caused by climate and human impact during the late Holocene
Abstract
- Publication:
-
Geological Society of London Special Publications
- Pub Date:
- January 2011
- DOI:
- 10.1144/SP352.7
- Bibcode:
- 2011GSLSP.352...85L