The Italian Solfatara as an analog for Mars fumarolic alteration
Autor: | Janice L. Bishop, Simone Silvestro, Isabelle Daniel, Damien Loizeau, Jessica Flahaut, Dario Tedesco |
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Přispěvatelé: | Flahaut, J., Bishop, J. L., Silvestro, S., Tedesco, D., Daniel, I., Loizeau, D., Centre de Recherches Pétrographiques et Géochimiques (CRPG), Institut national des sciences de l'Univers (INSU - CNRS)-Université de Lorraine (UL)-Centre National de la Recherche Scientifique (CNRS), Search for Extraterrestrial Intelligence Institute (SETI), INAF - Osservatorio Astronomico di Capodimonte (OAC), Istituto Nazionale di Astrofisica (INAF), University of the Study of Campania Luigi Vanvitelli, Osservatorio Vesuviano, Istituto Nazionale di Geofisica e Vulcanologia - Sezione di Napoli (INGV), Istituto Nazionale di Geofisica e Vulcanologia-Istituto Nazionale di Geofisica e Vulcanologia, Laboratoire de Géologie de Lyon - Terre, Planètes, Environnement [Lyon] (LGL-TPE), Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Claude Bernard Lyon 1 (UCBL), Université de Lyon-Université de Lyon-École normale supérieure - Lyon (ENS Lyon), Institut d'astrophysique spatiale (IAS), Université Paris-Sud - Paris 11 (UP11)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS), Laboratoire de Géologie de Lyon - Terre, Planètes, Environnement (LGL-TPE), École normale supérieure de Lyon (ENS de Lyon)-Université Claude Bernard Lyon 1 (UCBL), Université de Lyon-Université de Lyon-Institut national des sciences de l'Univers (INSU - CNRS)-Université Jean Monnet - Saint-Étienne (UJM)-Centre National de la Recherche Scientifique (CNRS), Université Paris-Sud - Paris 11 (UP11)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Centre National d’Études Spatiales [Paris] (CNES) |
Rok vydání: | 2019 |
Předmět: |
010504 meteorology & atmospheric sciences
XRD hydrothermalism Special Collection [SDU.STU]Sciences of the Universe [physics]/Earth Sciences fumarole 010502 geochemistry & geophysics 01 natural sciences Astrobiology alteration pattern symbols.namesake Geochemistry and Petrology Solfatara ComputingMilieux_MISCELLANEOUS alteration patterns 0105 earth and related environmental sciences vents Mars Exploration Program Earth Analogs for Martian geological materials and processe Fumarole Mars analog Geophysics [SDU]Sciences of the Universe [physics] 13. Climate action Raman spectroscopy vent symbols fumaroles VNIR spectroscopy Geology |
Zdroj: | American Mineralogist American Mineralogist, Mineralogical Society of America, 2019, 104 (11), pp.1565-1577. ⟨10.2138/am-2019-6899⟩ The American Mineralogist The American Mineralogist, 2019, 104 (11), pp.1565-1577. ⟨10.2138/am-2019-6899⟩ |
ISSN: | 1945-3027 0003-004X |
DOI: | 10.2138/am-2019-6899 |
Popis: | The first definitive evidence for continental vents on Mars is the in situ detection of amorphous silica-rich outcrops by the Mars Exploration Rover Spirit. These outcrops have been tentatively interpreted as the result of either acid sulfate leaching in fumarolic environments or direct precipitation from hot springs. Such environments represent prime targets for upcoming astrobiology missions but remain difficult to identify with certainty, especially from orbit. To contribute to the identification of fumaroles and hot spring deposits on Mars, we surveyed their characteristics at the analog site of the Solfatara volcanic crater in central Italy. Several techniques of mineral identification (VNIR spectroscopy, Raman spectroscopy, XRD) were used both in the field and in the laboratory on selected samples. The faulted crater walls showed evidence of acid leaching and alteration into the advanced argillic-alunitic facies, with colorful deposits containing alunite, jarosite, and/or hematite. Sublimates containing various Al and Fe hydroxyl-sulfates were observed around the active fumarole vents at 90 °C. One vent at 160 °C was characterized by different sublimates enriched in As and Hb sulfide species. Amorphous silica and alunite assemblages that are diagnostic of silicic alteration were also observed at the Fangaia mud pots inside the crater. A wide range of minerals was identified at the 665 m diameter Solfatara crater that is diagnostic of acid-steam heated alteration of a trachytic, porous bedrock. Importantly, this mineral diversity was captured at each site investigated with at least one of the techniques used, which lends confidence for the recognition of similar environments with the next-generation Mars rovers. |
Databáze: | OpenAIRE |
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