| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 5783036 | Chemical Geology | 2017 | 8 Pages |
Abstract
A set of quantitative models are used to evaluate the role and rate of the different processes and suggest that because of the independent evolution of U(IV) and U(VI) over time, their relative fraction and isotopic compositions can be used to evaluate the formation ages of seafloor phosphorites, which has so far not been possible using U-decay series.
Keywords
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geochemistry and Petrology
Authors
Yehoshua Kolodny, Adi Torfstein, Keren Weiss-Sarusi, Yevgeni Zakon, Ludwik Halicz,