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Identification of Phyllosilicates in the Antarctic Environment Using ASTER Satellite Data: Case Study from the Mesa Range, Campbell and Priestley Glaciers, Northern Victoria Land

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dc.contributor.authorPour, Amin Beiranvand-
dc.contributor.authorSekandari, Milad-
dc.contributor.authorRahmani, Omeid-
dc.contributor.authorCrispini, Laura-
dc.contributor.authorLaeufer, Andreas-
dc.contributor.authorPark, Yongcheol-
dc.contributor.authorHong, Jong Kuk-
dc.contributor.authorPradhan, Biswajeet-
dc.contributor.authorHashim, Mazlan-
dc.contributor.authorHossain, Mohammad Shawkat-
dc.contributor.authorMuslim, Aidy M.-
dc.contributor.authorMehranzamir, Kamyar-
dc.date.accessioned2021-04-30T04:45:57Z-
dc.date.available2021-04-30T04:45:57Z-
dc.date.issued2020-01-
dc.identifier.urihttps://repository.kopri.re.kr/handle/201206/11789-
dc.description.abstractIn Antarctica, spectral mapping of altered minerals is very challenging due to the remoteness and inaccessibility of poorly exposed outcrops. This investigation evaluates the capability of Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) satellite remote sensing imagery for mapping and discrimination of phyllosilicate mineral groups in the Antarctic environment of northern Victoria Land. The Mixture-Tuned Matched-Filtering (MTMF) and Constrained Energy Minimization (CEM) algorithms were used to detect the sub-pixel abundance of Al-rich, Fe3+-rich, Fe2+-rich and Mg-rich phyllosilicates using the visible and near-infrared (VNIR), short-wave infrared (SWIR) and thermal-infrared (TIR) bands of ASTER. Results indicate that Al-rich phyllosilicates are strongly detected in the exposed outcrops of the Granite Harbour granitoids, Wilson Metamorphic Complex and the Beacon Supergroup. The presence of the smectite mineral group derived from the Jurassic basaltic rocks (Ferrar Dolerite and Kirkpatrick Basalts) by weathering and decomposition processes implicates Fe3+-rich and Fe2+-rich phyllosilicates. Biotite (Fe2+-rich phyllosilicate) is detected associated with the Granite Harbour granitoids,Wilson Metamorphic Complex and Melbourne Volcanics. Mg-rich phyllosilicates are mostly mapped in the scree, glacial drift, moraine and crevasse fields derived from weathering and decomposition of the Kirkpatrick Basalt and Ferrar Dolerite. Chlorite (Mg-rich phyllosilicate) was generally mapped in the exposures of Granite Harbour granodiorite and granite and partially identified in the Ferrar Dolerite, the Kirkpatrick Basalt, the Priestley Formation and Priestley Schist and the scree, glacial drift and moraine. Statistical results indicate that Al-rich phyllosilicates class pixels are strongly discriminated, while the pixels attributed to Fe3+-rich class, Fe2+-rich and Mg-rich phyllosilicates classes contain some spectral mixing due to their subtle spectral differences in the VNIR+SWIR bands of ASTER. Results derived from TIR bands of ASTER show that a high level of confusion is associated with mafic phyllosilicates pixels (Fe3+-rich, Fe2+-rich and Mg-rich classes), whereas felsic phyllosilicates (Al-rich class) pixels are well mapped. Ground truth with detailed geological data, petrographic study and X-ray diffraction (XRD) analysis verified the remote sensing results. Consequently, ASTER image-map of phyllosilicate minerals is generated for the Mesa Range, Campbell and Priestley Glaciers, northern Victoria Land of Antarctica.en_US
dc.languageEnglishen_US
dc.language.isoen_USen_US
dc.subjectEnvironmental Sciences & Ecologyen_US
dc.subjectGeologyen_US
dc.subjectRemote Sensingen_US
dc.subjectImaging Science & Photographic Technologyen_US
dc.subject.classificationJang Bogo Stationen_US
dc.titleIdentification of Phyllosilicates in the Antarctic Environment Using ASTER Satellite Data: Case Study from the Mesa Range, Campbell and Priestley Glaciers, Northern Victoria Landen_US
dc.title.alternative위성 자료를 이용한 남극 빅토리아 지역 Phyllosilicates 확인en_US
dc.typeArticleen_US
dc.identifier.bibliographicCitationAmin Beiranvand Pour, et al. 2020. "Identification of Phyllosilicates in the Antarctic Environment Using ASTER Satellite Data: Case Study from the Mesa Range, Campbell and Priestley Glaciers, Northern Victoria Land". <em>REMOTE SENSING</em>, 13(1): 38-74.en_US
dc.citation.titleREMOTE SENSINGen_US
dc.citation.volume13en_US
dc.citation.number1en_US
dc.identifier.doi10.3390/rs13010038-
dc.citation.startPage38en_US
dc.citation.endPage74en_US
dc.description.articleClassificationSCIE-
dc.description.jcrRateJCR 2018:23.333en_US
dc.subject.keywordphyllosilicatesen_US
dc.subject.keywordalterationen_US
dc.subject.keywordASTERen_US
dc.subject.keywordAntarctic environmentsen_US
dc.subject.keywordmesa rangeen_US
dc.subject.keywordPriestley Glacieren_US
dc.subject.keywordnorthern Victoria Landen_US
dc.subject.keywordAntarcticaen_US
dc.identifier.localId2020-0297-
dc.identifier.scopusid2-s2.0-85098761835-
dc.identifier.wosid000606307100001-
Appears in Collections  
2020-2020, The Study on the cause of Polar 3 geomagnetic anomaly and its effect on the West Antarctic Rift System (20-20) / Park, Yongcheol (PE20230)
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