Experimental conditions and phase compositions of partial melting of nominally anhydrous model Martian mantle
We constrained the solidus of Lodders & Fegley (1997) model Martian composition with low bulk Mg# (molar MgO/(MgO+FeOT)×100 ~75) and high total alkali (Na2O+K2O=1.09 wt.%) concentration at 2 to 5 GPa by experiments. This dataset includes the experimental conditions and the composition of different phases present in each experiment.
How to cite this dataset:
Ding, S., Dasgupta, R., 2020. Experimental conditions and phase compositions of partial melting of nominally anhydrous model Martian mantle, Version 1.0. Interdisciplinary Earth Data Alliance (IEDA). https://doi.org/10.26022/IEDA/111511.
DOI Creation Date:
S. Ding, R. Dasgupta, K. Tsuno, The Solidus and Melt Productivity of Nominally Anhydrous Martian Mantle Constrained by New High Pressure-Temperature Experiments – Implications for Crustal Production and Mantle Source Evolution, JGR Planets (in review)
Creative Commons Attribution-NonCommercial-ShareAlike 4.0 International [CC-BY-NC-SA-4.0]
Packard Fellowship for Science and Engineering
National Aeronautics and Space Administration: 80NSSC18K0828
Coverage Scope: Space/Planetary
Geographic Location: Mars
User Contributed Keyword(s):
model Martian mantle, partial melting
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