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Landsat 8 and Alos DEm geological mapping reveals the architecture of the giant mesoproterozoic Kunene Complex anorthosite suite(Angola/Namibia)

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Geoscience Frontiers 2023年第5期14卷 308-328页

作者： Jeremie Lehmann Alan m.Brower trishya m.owen-smith Grant m.Bybee Ben Hayes Department of Geology University of JohannesburgSouth Africa Jurumani Solutions Midrand 1685South Africa School of Geosciences University of the Witwatersrand2050 JohannesburgSouth Africa

The quasi-monomineralic composition and huge spatial extent of massif-type anorthosites make detecting lithological regions and boundaries *** use processed Landsat 8 OLI multispectral images and ALOS digital elevation models integrated with field and petrographic observations to characterize the architecture of the≥17,000 km2 mesoproterozoic Kunene Complex(KC)anorthosite suite in Angola and *** of false colour composite bands 6,4 and 1 and band ratios 4/2(ferric minerals),6/5(ferrous minerals)and 6/7(OH-bearing minerals),as well as assessment of the PCA and mNF matrices of eigenvectors and eigenvalues from Landsat 8 data using available spectral libraries,have substantially improved the interpretation of the Kunene Complex rock types and *** dataset shows that the reflectance signature of KC anorthositic rocks is primarily a function of the degree of metasomatism,which is most significant in olivine-poor rock *** weathering intensity of the olivine-bearing anorthosite substrate is another control on the remote sensing *** remote sensing and field-based approach has enabled us to divide the KC anorthosite suite into six distinct spectral and architecture domains and at least four distinct magmatic plutons when considering available high-precision geochronological *** northernmost pluton(ca.1380 ma)of massive,olivine-bearing anorthosite shows distinct remote sensing signatures in the band ratio and mNF images marked by the dominance of OH-bearing and subordinate ferric *** central pluton(1412–1400 ma)is composed of NNE-to N-striking steeply dipping interlayered olivine-bearing and olivinepoor anorthosite,which correspond to ridges of dark-coloured,low albedo rocks with subordinate slightly oxidised ferrous mineral spectral signatures,and valleys of low albedo and OH-bearing mineral spectral signatures.A NNE-striking tectonic zone along a linear belt of KC granite gneiss separates the northern and central plu

关键词： Remote sensing Structural geology LANDSAT 8 Alos DEm Lineaments Proterozoic massif-type anorthosite

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