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Derivation of intermediate to silicic magma from the basalt analyzed at the Vega 2 landing site, Venus
Geochemical modeling using the basalt composition analyzed at the Vega 2 landing site indicates that intermediate to silicic liquids can be generated by fractional crystallization and equilibrium partial melting. Fractional crystallization modeling using variable pressures (0.01 GPa to 0.5 GPa) and...
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
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Public Library of Science
2018
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| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5870967/ https://www.ncbi.nlm.nih.gov/pubmed/29584745 http://dx.doi.org/10.1371/journal.pone.0194155 |