Geochemistry of phonolites and trachytes from the summit region of Mt. Kenya |
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Authors: | R C Price R W Johnson C M Gray F A Frey |
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Institution: | (1) Geology Department, La Trobe University, 3083 Bundoora, Vic., Australia;(2) Bureau of Mineral Resources, GPO Box 378, 2601 Canberra;(3) Department of Earth and Planetary Sciences, M.I.T., 02139 Cambridge, Massachusetts, USA |
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Abstract: | Two suites of felsic eruptives and intrusives are represented in a set of samples from the summit region of the Plio-Pleistocene
volcano, Mt. Kenya. Most of the samples are moderately or strongly undersaturated and have 87Sr/86Sr initial ratios in the range 0.70360–0.70368 (mean=0.70362). Members of this phonolitic suite are phonolites, nepheline
syenites or kenytes and as a group they show a wide variation in TiO2, FeO, P2O5, Sr, Ba, Zr and Nb. The minor and trace element geochemistry reflect variation in the nature of the parental basaltic magmas
from which the phonolitic rocks evolved and variation in the crystal fractionation process in individual cases. Crystal fractionation
involving plagioclase, alkali feldspar, clinopyroxene, olivine and magnetite is the process by which most of the phonolitic
rocks evolved and variation in the relative proportions of these phases in individual cases has led to a broad spectrum of
trace and minor element behaviour.
The second suite of felsic samples is critically saturated and consists of trachytes showing either slight oversaturation
or slight undersaturation with respect to SiO2. This trachyte suite has lower initial 87Sr/86Sr ratios (mean=0.70355) and is derived from transitional alkalic basalts by low pressure (crustal) crystal fractionation
involving feldspar, clinopyroxene, magnetite and olivine.
The range in minor and trace element chemistry observed among the felsic rocks is a consequence of variation in the parental
basalts which is related to mantle source variation and to the specific nature of the crystal fractionation process. |
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