The varied sources of faculae-forming brines in Ceres’ Occator crater emplaced via hydrothermal brine effusion
The second extended phase of the Dawn mission provided high resolution observations of Occator crater of the dwarf planet Ceres. Here, the authors show that the central faculae were sourced in an impact-induced melt chamber, with a contribution from the deep brine reservoir, while the Vinalia Facula...
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Nature Portfolio
2020
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oai:doaj.org-article:99a65a34c2af4a3fa0b1553e10bc31e52021-12-02T16:27:51ZThe varied sources of faculae-forming brines in Ceres’ Occator crater emplaced via hydrothermal brine effusion10.1038/s41467-020-15973-82041-1723https://doaj.org/article/99a65a34c2af4a3fa0b1553e10bc31e52020-08-01T00:00:00Zhttps://doi.org/10.1038/s41467-020-15973-8https://doaj.org/toc/2041-1723The second extended phase of the Dawn mission provided high resolution observations of Occator crater of the dwarf planet Ceres. Here, the authors show that the central faculae were sourced in an impact-induced melt chamber, with a contribution from the deep brine reservoir, while the Vinalia Faculae were sourced by the deep brine reservoir alone.J. E. C. ScullyP. M. SchenkJ. C. Castillo-RogezD. L. BuczkowskiD. A. WilliamsJ. H. PasckertK. D. DuarteV. N. RomeroL. C. QuickM. M. SoriM. E. LandisC. A. RaymondA. NeesemannB. E. SchmidtH. G. SizemoreC. T. RussellNature PortfolioarticleScienceQENNature Communications, Vol 11, Iss 1, Pp 1-11 (2020) |
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EN |
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Science Q |
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Science Q J. E. C. Scully P. M. Schenk J. C. Castillo-Rogez D. L. Buczkowski D. A. Williams J. H. Pasckert K. D. Duarte V. N. Romero L. C. Quick M. M. Sori M. E. Landis C. A. Raymond A. Neesemann B. E. Schmidt H. G. Sizemore C. T. Russell The varied sources of faculae-forming brines in Ceres’ Occator crater emplaced via hydrothermal brine effusion |
| description |
The second extended phase of the Dawn mission provided high resolution observations of Occator crater of the dwarf planet Ceres. Here, the authors show that the central faculae were sourced in an impact-induced melt chamber, with a contribution from the deep brine reservoir, while the Vinalia Faculae were sourced by the deep brine reservoir alone. |
| format |
article |
| author |
J. E. C. Scully P. M. Schenk J. C. Castillo-Rogez D. L. Buczkowski D. A. Williams J. H. Pasckert K. D. Duarte V. N. Romero L. C. Quick M. M. Sori M. E. Landis C. A. Raymond A. Neesemann B. E. Schmidt H. G. Sizemore C. T. Russell |
| author_facet |
J. E. C. Scully P. M. Schenk J. C. Castillo-Rogez D. L. Buczkowski D. A. Williams J. H. Pasckert K. D. Duarte V. N. Romero L. C. Quick M. M. Sori M. E. Landis C. A. Raymond A. Neesemann B. E. Schmidt H. G. Sizemore C. T. Russell |
| author_sort |
J. E. C. Scully |
| title |
The varied sources of faculae-forming brines in Ceres’ Occator crater emplaced via hydrothermal brine effusion |
| title_short |
The varied sources of faculae-forming brines in Ceres’ Occator crater emplaced via hydrothermal brine effusion |
| title_full |
The varied sources of faculae-forming brines in Ceres’ Occator crater emplaced via hydrothermal brine effusion |
| title_fullStr |
The varied sources of faculae-forming brines in Ceres’ Occator crater emplaced via hydrothermal brine effusion |
| title_full_unstemmed |
The varied sources of faculae-forming brines in Ceres’ Occator crater emplaced via hydrothermal brine effusion |
| title_sort |
varied sources of faculae-forming brines in ceres’ occator crater emplaced via hydrothermal brine effusion |
| publisher |
Nature Portfolio |
| publishDate |
2020 |
| url |
https://doaj.org/article/99a65a34c2af4a3fa0b1553e10bc31e5 |
| work_keys_str_mv |
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