Macdonald, R.; Rogers, N. W and Tindle, A. G.
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|DOI (Digital Object Identifier) Link:||http://doi.org/10.1180/minmag.2007.071.6.703|
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Germanium abundances, determined by laser ablation-inductively coupled plasma-mass spectrometry, are presented for phenocrysts and glass matrices from a metaluminous trachyte and four peralkaline rhyolites from the Greater Olkaria Volcanic Complex, Kenya Rift Valley, Africa. Abundances (in ppm) are: sanidine 0.45-0.61; fayalite 4.8-11.7; hedenbergite 5.1-9.0; titanomagnetite 2.7; ilmenite 0.48; amphibole 8.3-8.9; biotite 7.0; chevkinite-(Ce) 309; trachyte glass 3.0; rhyolitic glasses 2.3-3.9. These values are generally greater than those recorded for silicic rocks in the literature, whilst the chevkinite-(Ce) value is the largest yet found in a magmatic mineral. Apparent partition coefficients range from 0.15-0.26 in sanidine to 124 in chevkinite-(Ce). Those for fayalite and hedenbergite increase with whole-rock peralkalinity and Fe content. The possibility of a role for accessory phases in influencing Ge distribution in rock-forming minerals is also raised.
|Item Type:||Journal Article|
|Copyright Holders:||2007 The Mineralogical Society|
|Academic Unit/Department:||Science > Environment, Earth and Ecosystems
|Interdisciplinary Research Centre:||Centre for Earth, Planetary, Space and Astronomical Research (CEPSAR)|
|Depositing User:||Nick Rogers|
|Date Deposited:||01 Sep 2008 08:03|
|Last Modified:||23 Feb 2016 21:37|
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