Low-sulfide PGE mineralization in layered intrusion ring,Vestfold Hills,Antarctica |
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Authors: | M S Egorov V S Semenov N L Alekseev |
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Institution: | 1. Polar Marine Geosurvey Expedition, ul. Pobedy 24, Lomonosov, Leningrad oblast, 198412, Russia 2. Institute of Precambrian Geology and Geochronology, Russian Academy of Sciences, nab. Makarova 2, St. Petersburg, 199034, Russia
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Abstract: | This paper presents results of the study of norite complex from the Vestfold Hills (East Antarctica) containing a low-sulfide type of mineralization. The ore mineralization occurs in specific rock types and along the contact of norites the host rocks. Three mineralization types: Fe–Ni–Cu sulfide, oxide, and PGE-bearing are known. PGE mineralization is represented by palladium–bismuth tellurides of the michenerite–merenskyite series. A model of ore-formation succession and a concept of the origin of low-sulfide PGE mineralization by means of crystallization and subsequent evolution of monosulfide and intermediate solid solutions have been developed. |
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