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• W2949528887 abstract "Listvenites normally form during hydrothermal/metasomatic alteration of mafic and ultramafic rocks and represent a key indicator for the occurrence of ore mineralizations in orogenic systems. Hydrothermal/metasomatic alteration mineral assemblages are one of the significant indicators for ore mineralizations in the damage zones of major tectonic boundaries, which can be detected using multispectral satellite remote sensing data. In this research, Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) multispectral remote sensing data were used to detect listvenite occurrences and alteration mineral assemblages in the poorly exposed damage zones of the boundaries between the Wilson, Bowers and Robertson Bay terranes in Northern Victoria Land (NVL), Antarctica. Spectral information for detecting alteration mineral assemblages and listvenites were extracted at pixel and sub-pixel levels using the Principal Component Analysis (PCA)/Independent Component Analysis (ICA) fusion technique, Linear Spectral Unmixing (LSU) and Constrained Energy Minimization (CEM) algorithms. Mineralogical assemblages containing Fe2+, Fe3+, Fe-OH, Al-OH, Mg-OH and CO3 spectral absorption features were detected in the damage zones of the study area by implementing PCA/ICA fusion to visible and near infrared (VNIR) and shortwave infrared (SWIR) bands of ASTER. Silicate lithological groups were mapped and discriminated using PCA/ICA fusion to thermal infrared (TIR) bands of ASTER. Fraction images of prospective alteration minerals, including goethite, hematite, jarosite, biotite, kaolinite, muscovite, antigorite, serpentine, talc, actinolite, chlorite, epidote, calcite, dolomite and siderite and possible zones encompassing listvenite occurrences were produced using LSU and CEM algorithms to ASTER VNIR+SWIR spectral bands. Several potential zones for listvenite occurrences were identified, typically in association with mafic metavolcanic rocks (Glasgow Volcanics) in the Bowers Mountains. Comparison of the remote sensing results with geological investigations in the study area demonstrate invaluable implications of the remote sensing approach for mapping poorly exposed lithological units, detecting possible zones of listvenite occurrences and discriminating subpixel abundance of alteration mineral assemblages in the damage zones of the Wilson-Bowers and Bowers-Robertson Bay terrane boundaries and in intra-Bowers and Wilson terranes fault zones with high fluid flow. The satellite remote sensing approach developed in this research is explicitly pertinent to detecting key alteration mineral indicators for prospecting hydrothermal/metasomatic ore minerals in remote and inaccessible zones situated in other orogenic systems around the world." @default.
• W2949528887 created "2019-06-27" @default.
• W2949528887 creator A5030671146 @default.
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• W2949528887 date "2019-06-13" @default.
• W2949528887 modified "2023-10-10" @default.
• W2949528887 title "Mapping Listvenite Occurrences in the Damage Zones of Northern Victoria Land, Antarctica Using ASTER Satellite Remote Sensing Data" @default.
• W2949528887 cites W1124698651 @default.
• W2949528887 cites W1650360804 @default.
• W2949528887 cites W1778870018 @default.
• W2949528887 cites W1856071063 @default.
• W2949528887 cites W1969100778 @default.
• W2949528887 cites W1969494932 @default.
• W2949528887 cites W1971488501 @default.
• W2949528887 cites W1972349245 @default.
• W2949528887 cites W1976137296 @default.
• W2949528887 cites W1988588474 @default.
• W2949528887 cites W1991036305 @default.
• W2949528887 cites W1998626624 @default.
• W2949528887 cites W2006219621 @default.
• W2949528887 cites W2008193189 @default.
• W2949528887 cites W2010522912 @default.
• W2949528887 cites W2012263328 @default.
• W2949528887 cites W2017988770 @default.
• W2949528887 cites W2018065282 @default.
• W2949528887 cites W2018194343 @default.
• W2949528887 cites W2019985866 @default.
• W2949528887 cites W2024484366 @default.
• W2949528887 cites W2029422460 @default.
• W2949528887 cites W2032051771 @default.
• W2949528887 cites W2033457942 @default.
• W2949528887 cites W2034135043 @default.
• W2949528887 cites W2041067110 @default.
• W2949528887 cites W2043847362 @default.
• W2949528887 cites W2044025263 @default.
• W2949528887 cites W2047888525 @default.
• W2949528887 cites W2057774402 @default.
• W2949528887 cites W2066696084 @default.
• W2949528887 cites W2069188138 @default.
• W2949528887 cites W2074405817 @default.
• W2949528887 cites W2079646219 @default.
• W2949528887 cites W2082787951 @default.
• W2949528887 cites W2086141541 @default.
• W2949528887 cites W2087181663 @default.
• W2949528887 cites W2089752283 @default.
• W2949528887 cites W2093671576 @default.
• W2949528887 cites W2096357585 @default.
• W2949528887 cites W2096842752 @default.
• W2949528887 cites W2099007620 @default.
• W2949528887 cites W2099581743 @default.
• W2949528887 cites W2104032373 @default.
• W2949528887 cites W2109205984 @default.
• W2949528887 cites W2118424996 @default.
• W2949528887 cites W2122452972 @default.
• W2949528887 cites W2123649031 @default.
• W2949528887 cites W2123966256 @default.
• W2949528887 cites W2126275569 @default.
• W2949528887 cites W2127495569 @default.
• W2949528887 cites W2129659014 @default.
• W2949528887 cites W2130674132 @default.
• W2949528887 cites W2134893701 @default.
• W2949528887 cites W2136296807 @default.
• W2949528887 cites W2136625467 @default.
• W2949528887 cites W2136954203 @default.
• W2949528887 cites W2138167459 @default.
• W2949528887 cites W2140103896 @default.
• W2949528887 cites W2140219630 @default.
• W2949528887 cites W2142645945 @default.
• W2949528887 cites W2144700058 @default.
• W2949528887 cites W2146956557 @default.
• W2949528887 cites W2149921367 @default.
• W2949528887 cites W2150780458 @default.
• W2949528887 cites W2152753533 @default.
• W2949528887 cites W2153245148 @default.
• W2949528887 cites W2154236340 @default.
• W2949528887 cites W2156746831 @default.
• W2949528887 cites W2158148944 @default.
• W2949528887 cites W2159694534 @default.
• W2949528887 cites W2161125505 @default.
• W2949528887 cites W2166917517 @default.
• W2949528887 cites W2191083387 @default.
• W2949528887 cites W2509347419 @default.
• W2949528887 cites W2522678430 @default.
• W2949528887 cites W2532514397 @default.
• W2949528887 cites W2551031612 @default.
• W2949528887 cites W2563061818 @default.
• W2949528887 cites W2606412288 @default.
• W2949528887 cites W2607211607 @default.
• W2949528887 cites W2728096264 @default.

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