Maier Wolfgang D., Rasmussen Birger, Fletcher Ian Robert, Li Chusi, Barnes Sarah-Jane et Huhma Hannu. (2013). The Kunene anorthosite complex, Namibia, and its satellite intrusions : geochemistry, geochronology, and economic potential. Economic Geology and the Bulletin of the Society of Economic Geologists, 108, (5), p. 953-986.
URL officielle: http://geoscienceworld.org/georef/2013-059100
The Kunene Complex of Namibia-Angola is one of the largest anorthosite massifs on Earth (up to 18,000 km (super 2) ), consisting of several distinct anorthosite and leucotroctolite intrusions. The Namibian portion of the Kunene Complex measures approximately 80 x 50 km, approximately 4,000 km (super 2) , and is dominated by the Zebra Mountain lobe, a approximately 16-km-thick dome-like mass of interlayered, relatively unaltered dark leucotroctolite with relatively altered, "white," anorthosite. Past studies and the present work have found evidence for intrusion of two distinct phases of dark leucotroctolite into the white anorthosite, namely a relatively early, deformed, phase dated at 1363 + or - 17 Ma (U-Pb in baddelyite), and a relatively later and undeformed phase whose absolute age remains unknown. The Kunene leucotroctolites are among the least evolved troctolites known from anorthosite complexes, with olivine containing 59 to 77 mol % forsterite and up to 1,700 ppm Ni, and plagioclase containing 56 to 69 mol % anorthosite. Our isotope data from the troctolites indicate a relatively small crustal component (delta (super 18) O, approximately 5.3-7.3; delta (super 34) S, 0.5-1; and epsilon Nd (sub T) , 0.9-1.8), whereas Nd and oxygen isotope data from the white anorthosites, published by other workers, showed a slightly larger crustal component (e.g., epsilon Nd (sub T) as low as -3; delta (super 18) O up to 7.5 per mil). In the periphery of the Kunene Complex are several, relatively small (<10 km (super 2) ), mafic-ultramafic intrusions comprising peridotite, pyroxenite, gabbro, troctolite, and anorthosite. Some of these bodies are Ni-Cu-PGE mineralized, including the Ohamaremba troctolite, the Oncocua pyroxenite, and the Ombuku peridotite-gabbronorite. The latter additionally contains a massive chromitite layer. A new U-Pb baddelyite age of 1220 + or - 15 Ma for Ohamaremba indicates that the latter postdates the main Kunene Complex by approximately 140 Ma. The relative enrichment in MgO, Cr, and Ni, and the O, Nd, and S isotope characteristics of Kunene magmatism suggest that the primary magmas were predominantly mantle-derived picrites or basalts. The massif-type anorthosites formed through ascent of feldspathic slurries followed by downward draining of residual liquid. Subsequent magma pulses formed troctolitic sills within the anorthosite plutons and mafic-ultramafic satellite intrusions in the periphery of the anorthosites. The recurring nature of Kunene mafic-ultramafic magmatism results from several successive mantle upwellings. Partial mantle melts ascended through reactivated translithospheric lineaments along the southern margin of the Congo craton.
|Type de document:||Article publié dans une revue avec comité d'évaluation|
|Version évaluée par les pairs:||Oui|
|Sujets:||Sciences naturelles et génie > Sciences naturelles > Sciences de la terre (géologie, géographie)|
|Département, module, service et unité de recherche:||Départements et modules > Département des sciences appliquées > Unité d'enseignement en sciences de la Terre|
|Mots-clés:||absolute age, Africa, anorthosite, baddeleyite,chemical composition, Congo Craton, copper ores, cores, dates, gabbros, geochemistry, igneous rocks, intrusions, ion probe data, isotope ratios, isotopes, Kunene Complex, leucotroctolite, linéaments, lithogeochemistry, magmas, magmatism, mass spectra, metal ores, metals, mineral composition, Namibia, Nd-144/Nd-143, neodymium, nickel ores, O-18/O-16, Ohamaremba Troctolite, Ombuku Peridotite-Gabbronorite, Oncocua Pyroxenite, oxides, oxygen, partial melting, platinum group, platinum ores, plutonic rocks, plutons, Precambrian, Proterozoic, rare earths, reactivation, S-34/S-32, SHRIMP data, sills, Southern Africa, spectra, stable isotopes, sulfur, tectonics, troctolite, U/Pb, upper Precambrian, whole rock, Zebra Mountain|
|Déposé le:||14 juin 2016 13:35|
|Dernière modification:||09 déc. 2016 14:56|
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