Marine molluscs have long been recognised as potential records of palaeoclimate change using the patterns and differences in the stable isotopic composition of the carbonate shells. The aim of this study is to improve the robustness of this approach for aragonitic molluscs by completing the first ex
โฆ LIBER โฆ
Oxygen isotope fractionation between calcite and tremolite: an experimental study
โ Scribed by Y. -F. Zheng; P. Metz; M. Satir
- Publisher
- Springer
- Year
- 1994
- Tongue
- English
- Weight
- 751 KB
- Volume
- 118
- Category
- Article
- ISSN
- 0010-7999
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