Published September 2014
| Published
Journal Article
Open
Characterizing Early Solar System Fluids on the Allende (CV3) Parent Body: Nanosims Study of Phosphate Volatile Contents
Chicago
Abstract
Much of our knowledge about the early Solar System comes from the study of CV3 meteorites, in particular Allende. Hydrothermal alteration is recognized as an important, ubiquitous process within these rocks (e.g. [1]). Nevertheless, we know little regarding the nature of these fluids. Volatile element abundances in phosphates from carbonaceous chondrites could constrain relative fugacities of H_2O, HF and HCl in the fluid present during metasomatism in primitive planetesimals.
Additional Information
© 2014 The Meteoritical Society. Article first published online: 8 Sep. 2014.Attached Files
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Additional details
- Eprint ID
- 50733
- DOI
- 10.1111/maps.12359
- Resolver ID
- CaltechAUTHORS:20141023-105133561
- Created
-
2014-10-23Created from EPrint's datestamp field
- Updated
-
2021-11-10Created from EPrint's last_modified field
- Caltech groups
- Division of Geological and Planetary Sciences (GPS)