Martian magmas contained abundant chlorine, but little water
By J. Filiberto, A. Treiman. 2009
148 citations recorded by the source corpus.
Subfields: Astronomy and Astrophysics, Atmospheric Science
View Paper: https://www.semanticscholar.org/paper/8c03cf80b7deddc2ad1fe1879ab902394d0a8158
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In Astronomy and Astrophysics
- F. Gaillard
- Bruno Scaillet
- F. McCubbin
- T. O. S. University
- Research School of Earth Sciences
- D. Geology
- T. Yoshizaki
- William F. McDonough Department of Earth Science
In Atmospheric Science
Citations in the corpus
- The composition of Mars (2019, background): “Many have attempted to filter Martian meteorite data affected by such secondary processes (Dreibus and Wanke, 1985; Dreibus and Wänke, 1987; Treiman, 2003; Filiberto and Treiman, 2009; Filiberto et al., 2016, 2019).”
- Hydrous melting of the martian mantle produced both depleted and enriched shergottites (2012, background): “References: [1] Filiberto and Treiman (2009) Geology 37.”
- A theoretical framework for volcanic degassing chemistry in a comparative planetology perspective and implications for planetary atmospheres (2014, background): “…relationships) in basalts remains unknown _but we recognize their likely high importance in the magmatic degassing of Martian volcanoes (Filiberto and Treiman, 2009),_ (2) noble gases, since both their abundances in the Earth mantle (Marty, 2012) and their solubilities in basalts…”