作者: Paul Bilong , Paul-Désiré Ndjigui , Robert Temdjim , Elisé Sababa
DOI: 10.1016/J.CHEMER.2010.07.001
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摘要: Abstract Peridotite and granite xenoliths, in the early stage of weathering, occur Nyos volcanic region (NW Cameroon). Geochemical data shows that peridotites are marked by high concentrations MgO (42.30 wt.%, with SiO 2 /MgO ∼ 1), chromium (2100 ppm), nickel (2100 ppm) cobalt (104 ppm), as well low lanthanide contents (ΣREE: 7.41 ppm). Granites display (70–73 wt.%), mostly peraluminous (1.40 > A/CNK The geochemical survey Platinum-Group Elements (PGE) done these rocks weathering PGE less than 7 ppb peridotites. highly concentrated elements ruthenium (6.26 ppb) platinum (5.53 ppb). total content is 14.57 ppb. These normalized respect to chondrites a flat spectrum from iridium platinum. granites below detection limit except for two samples (LNY01 LNY02) whose close 0.23 ppb.