Abstract
Carbonate speleothems that contain ppb-ppm levels of uranium can be dated by the 238U-234U-230Th and 235U- 231Pa disequilibrium techiques. Accurate ages are possible if the initial concentrations of 230Th and 231Pa are well constrained and if the system has remained closed to post-depositional exchange of uranium, thorium, and protactinium.
| Original language | English |
|---|---|
| Title of host publication | Studies of Cave Sediments |
| Subtitle of host publication | Physical and Chemical Records of Paleoclimate |
| Publisher | Springer Netherlands |
| Pages | 177-197 |
| Number of pages | 21 |
| ISBN (Print) | 9781402053269 |
| DOIs | |
| State | Published - 2007 |
| Externally published | Yes |