Evolution of water reservoirs in the early solar system through their oxygen isotopic composition
A new technique has been developed to enable analyses of δ<sup>17</sup>0 and δ<sup>18</sup>0 from small water samples extracted from meteorites. Isotopic measurements are made using a continuous-flow, isotope ratio mass spectrometer (Delta C, Finnigan Mat) utilising a helium...
| Main Author: | |
|---|---|
| Published: |
Open University
2001
|
| Subjects: | |
| Online Access: | http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.523916 |