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Authordc.contributor.authorIto, Gen
Authordc.contributor.authorFlahaut, Jessica
Authordc.contributor.authorGonzález Maurel, Osvaldo
Authordc.contributor.authorGodoy Neira, Benigno Emilio
Authordc.contributor.authorPayet, Vincet
Authordc.contributor.authorBarthez, Marie
Cita de ítemdc.identifier.citationRemote Sens. 2022, 14, 2081es_ES
Abstractdc.description.abstractThe Altiplano-Puna Volcanic Complex (APVC) of the Central Andes is an arid region with extensive volcanism, possessing various geological features comparable to those of other solar system objects. The unique features of the APVC, e.g., hydrothermal fields and evaporite salars, have been used as planetary analogs before, but the complexity of the APVC presents a wealth of opportunities for more analog studies that have not been exploited previously. Motivated by the potential of using the APVC as an analog of the volcanic terrains of solar system objects, we mapped the mineralogy and silica content of the APVC up to similar to 100,000 km(2) in northern Chile based on a combination of remote sensing data resembling those of the Moon and Mars. The band ratio indices of Landsat 8 Operational Land Imager multispectral images and mineral classifications based on spectral hourglass approach using Earth Observing-1 Hyperion hyperspectral images (both in the visible to shortwave infrared wavelengths) were used to map iron-bearing and alteration minerals. We also used Hyperion imagery to detect feldspar spectral signatures and demonstrated that feldspar minerals can be detected on non-anorthosites, which may influence interpretations of feldspar spectral signatures on Mars. From the Terra Advanced Spaceborne Thermal Emission and Reflection Radiometer Global Emissivity Dataset, we derived the silica percentage of non-evaporite rocks within errors of approximately 2-3 wt.% SiO2 for those in the 60-70 wt.% range (about 8 wt.% errors for the 50-60 wt.% range). Based on an integrated assessment of the three datasets, we highlighted three regions of particular interest worthy of further field investigation. We also evaluated the benefits and limitations of all three remote sensing methods for mapping key minerals and capturing rock diversity, based on available samples and existing geological maps.es_ES
Patrocinadordc.description.sponsorshipCNRS Momentum grant LUE future leader 'Viscous' project Agence Nationale de la Recherche (ANR) FONDAP 15090013 15200001es_ES
Type of licensedc.rightsAttribution-NonCommercial-NoDerivs 3.0 United States*
Link to Licensedc.rights.uri*
Sourcedc.sourceRemote Sensinges_ES
Keywordsdc.subjectMineral mappinges_ES
Keywordsdc.subjectPlanetary analoges_ES
Títulodc.titleRemote sensing survey of altiplano-puna volcanic complex rocks and minerals for planetary analog usees_ES
Document typedc.typeArtículo de revistaes_ES
dc.description.versiondc.description.versionVersión publicada - versión final del editores_ES
dcterms.accessRightsdcterms.accessRightsAcceso abiertoes_ES
Indexationuchile.indexArtículo de publícación WoSes_ES

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Attribution-NonCommercial-NoDerivs 3.0 United States
Except where otherwise noted, this item's license is described as Attribution-NonCommercial-NoDerivs 3.0 United States