Autor: |
A.E. Schoch, C.A. Myburgh, W.A. van der Westhuizen, H. de Bruiyn |
Rok vydání: |
2000 |
Předmět: |
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Zdroj: |
Journal of African Earth Sciences. 31:657-668 |
ISSN: |
1464-343X |
DOI: |
10.1016/s0899-5362(00)80013-5 |
Popis: |
A basalt flow in the Katse area of Lesotho displays composite features with tholeiitic characteristics along its margins and a picritic composition in the centre. Geochemical modelling of the magma and the composition of microscopic melt inclusions indicate that the primary magma was olivine-rich. The chemical variation of the flow is evidence for fractionation of olivine from the magma, causing a trend towards tholeiitic compositions. The derived lava flow was modified by flow differentiation so that olivine concentrated progressively towards the centre, owing to differential flow velocity. Evidence from geochemical modelling corroborates these conclusions. |
Databáze: |
OpenAIRE |
Externí odkaz: |
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