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Filiberto, Justin; Baratoux, David; Beaty, David; Breuer, Doris; Farcy, Benjamin J.; Grott, Matthias; Jones, John H.; Kiefer, Walter S.; Mane, Prajkta; McCubbin, Francis M. and Schwenzer, Susanne P.
(2016).
DOI: https://doi.org/10.1111/maps.12680
Abstract
Multiple observations from missions to Mars have revealed compelling evidence for a volatile-rich Martian crust. A leading theory contends that eruption of basaltic magmas was the ultimate mechanism of transfer of volatiles from the mantle toward the surface after an initial outgassing related to the crystallization of a magma ocean. However, the concentrations of volatile species in ascending magmas and in their mantle source regions are highly uncertain. This work and this special issue of Meteoritics & Planetary Science summarize the key findings of the workshop on Volatiles in the Martian Interior (Nov. 3–4, 2014), the primary open questions related to volatiles in Martian magmas and their source regions, and the suggestions of the community at the workshop to address these open questions.
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About
- Item ORO ID
- 47799
- Item Type
- Journal Item
- ISSN
- 1086-9379
- Project Funding Details
-
Funded Project Name Project ID Funding Body Mars Fundamental Research Program NNX13AG35G NASA Mars Fundamental Research Program NNX13AG44G NASA Mars Fundamental Research Program NNX14AJ94G NASA Mars Fundamental Research Program NNX14AG41G NASA Cosmochemistry Program NNX11AK75G NASA - Keywords
- Mars; planetary crust; volatiles; halogens; noble gases
- Academic Unit or School
-
Faculty of Science, Technology, Engineering and Mathematics (STEM) > Environment, Earth and Ecosystem Sciences
Faculty of Science, Technology, Engineering and Mathematics (STEM) - Research Group
- ?? space ??
- Copyright Holders
- © 2016 The Meteoritical Society
- Depositing User
- Susanne Schwenzer