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Deriving iron contents from past and future Venus surface spectra with new high-temperature laboratory emissivity data

In situ information on the surface composition of Venus is based on measurements of a small number of landing sites. In the laboratory, we measured the emissivity of a range of igneous rocks at temperatures up to 480°C. We show that high-temperature laboratory spectra of basalts are consistent with...

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Detalles Bibliográficos
Autores principales: Helbert, J., Maturilli, A., Dyar, M. D., Alemanno, G.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: American Association for the Advancement of Science 2021
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7810366/
https://www.ncbi.nlm.nih.gov/pubmed/33523894
http://dx.doi.org/10.1126/sciadv.aba9428