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Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/1978
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dc.contributor.authorallRiaza, A.; Instituto Geológico y Minero de España (IGME), Madrid, Spainen
dc.contributor.authorallGarcia-Melendez, E.; Área de Geodinámica Externa, Facultad de Ciencias Ambientales, Universidad de León, Spainen
dc.contributor.authorallSuárez, M.; Departamento de Geología, Universidad de Salamanca, Spainen
dc.contributor.authorallHausold, A.; DLR_German Aerospace Research Establishment, Remote Sensing Data Centre, Oberpfaffenhofen, Wessling, Deutschlanden
dc.contributor.authorallBeisl, U.; DLR_German Aerospace Research Establishment, Remote Sensing Data Centre, Oberpfaffenhofen, Wessling, Deutschlanden
dc.contributor.authorallvan der Werff, H.; International Institute for Aerospace Survey and Earth Sciences (ITC), Enschede, The Netherlandsen
dc.date.accessioned2006-12-07T14:41:30Zen
dc.date.available2006-12-07T14:41:30Zen
dc.date.issued2006-02en
dc.identifier.urihttp://hdl.handle.net/2122/1978en
dc.description.abstractWetlands are particularly sensitive environments receiving attention from the natural sciences community due to their wealth of both flora and fauna, and often considered as natural parks. In the Tablas de Daimiel (La Mancha, Central Spain), Digital Airborne Imaging Spectrometer data (DAIS 7915) have been analyzed to map geological processes on areas around the receding wetland which have never been flooded by water in the past. Sediments permanently exposed to the atmosphere dehydrate and oxide, developing different mineralogical associations arranged on planation surfaces. Such planation surfaces are key in the geological knowledge of recent climate change and landscape evolution. Progressive iron oxide/hydroxide rate and decarbonation can be spectrally followed on the Holocene sands framing the current marshy area. Such mineralogical changes are geologically registered on flat surfaces at different heights over the receding shore of the paleolake. Interacting erosion and sedimentation processes are responsible for the development of the flat morphological surfaces with increasing dryness. Maps are built for four different morphological units consisting of planation surfaces following chronologically the receding marsh during the last 2000 years before the present. Interactive spectral responses of mineralogical associations are described on the imagery, field and laboratory spectra.en
dc.format.extent1315272 bytesen
dc.format.mimetypeapplication/pdfen
dc.language.isoEnglishen
dc.relation.ispartofseries1/49 (2006)en
dc.subjecthyperspectralen
dc.subjectiron bearing mineralsen
dc.subjectpaleoclimateen
dc.titleMapping of semi-arid iron bearing red sands on emerged areas around lake marshes (Tablas de Daimiel, Spain) using hyperspectral DAIS 7915 spectrometer dataen
dc.typearticleen
dc.type.QualityControlPeer-revieweden
dc.subject.INGV03. Hydrosphere::03.01. General::03.01.06. Paleoceanography and paleoclimatologyen
dc.subject.INGV04. Solid Earth::04.02. Exploration geophysics::04.02.05. Downhole, radioactivity, remote sensing, and other methodsen
dc.subject.INGV04. Solid Earth::04.04. Geology::04.04.03. Geomorphologyen
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Remote Sensing, 18 (16), 3361-3377.en
dc.description.journalTypeJCR Journalen
dc.description.fulltextopenen
dc.contributor.authorRiaza, A.en
dc.contributor.authorGarcia-Melendez, E.en
dc.contributor.authorSuárez, M.en
dc.contributor.authorHausold, A.en
dc.contributor.authorBeisl, U.en
dc.contributor.authorvan der Werff, H.en
dc.contributor.departmentInstituto Geológico y Minero de España (IGME), Madrid, Spainen
dc.contributor.departmentÁrea de Geodinámica Externa, Facultad de Ciencias Ambientales, Universidad de León, Spainen
dc.contributor.departmentDepartamento de Geología, Universidad de Salamanca, Spainen
dc.contributor.departmentDLR_German Aerospace Research Establishment, Remote Sensing Data Centre, Oberpfaffenhofen, Wessling, Deutschlanden
dc.contributor.departmentDLR_German Aerospace Research Establishment, Remote Sensing Data Centre, Oberpfaffenhofen, Wessling, Deutschlanden
dc.contributor.departmentInternational Institute for Aerospace Survey and Earth Sciences (ITC), Enschede, The Netherlandsen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextopen-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptInstituto Geológico y Minero de España (IGME), Madrid, Spain-
crisitem.author.deptÁrea de Geodinámica Externa, Facultad de Ciencias Ambientales, Universidad de León, Spain-
crisitem.author.deptDepartamento de Geología, Universidad de Salamanca, Spain-
crisitem.author.deptDLR_German Aerospace Research Establishment, Remote Sensing Data Centre, Oberpfaffenhofen, Wessling, Deutschland-
crisitem.author.deptDLR_German Aerospace Research Establishment, Remote Sensing Data Centre, Oberpfaffenhofen, Wessling, Deutschland-
crisitem.author.deptInternational Institute for Aerospace Survey and Earth Sciences (ITC), Enschede, The Netherlands-
crisitem.classification.parent03. Hydrosphere-
crisitem.classification.parent04. Solid Earth-
crisitem.classification.parent04. Solid Earth-
Appears in Collections:Annals of Geophysics
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