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Carbonatite Volcanism - Oldoinyo Lengai and the Petrogenesis of Natrocarbonatites (Paperback, Softcover reprint of the original 1st ed. 1995)
Loot Price: R1,584
Discovery Miles 15 840
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Carbonatite Volcanism - Oldoinyo Lengai and the Petrogenesis of Natrocarbonatites (Paperback, Softcover reprint of the original 1st ed. 1995)
Series: IAVCEI Proceedings in Volcanology, 4
Expected to ship within 10 - 15 working days
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During the last few years, carbonatites have received a
considerable amount of attention. Some of this interest was no
doubt kindled by the importance of volatiles in the Earth's mantle,
particularly CO , by the fact that carbonatites 2 can be used to
monitor the chemical evolution of the sub-continental upper mantle,
and by the fact that carbonatites may be effective metasomatizing
agents at both mantle and crustal levels. The interest in Oldoinyo
Lengai has extended over at least 100 years, but it was not until
the eruptions of 1960, when the unique carbonatitic nature of its
lavas was recognized, that the volcano took on special significance
in volcanology and igneous petrology. The recognition of
carbonatitic flows coin cided with the first successful laboratory
experiments carried out on carbonatitic melts. Since then, Oldoinyo
Lengai has formed a cornerstone in all carbonatite discussions. It
is probably true to say that the findings from Oldoinyo Lengai have
dominated our ideas about carbonatites, in spite of the fact that
the alkali rich, natrocarbonatitic lavas of Oldoinyo Lengai are
markedly different from other carbonatites.
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