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Carbonatite Volcanism

Name: Carbonatite Volcanism
Brand: Springer-Verlag Berlin and Heidelberg GmbH & Co. KG
SKU: 9783642791840
Price: 52.77 EUR
Availability: InStock

Oldoinyo Lengai and the Petrogenesis of Natrocarbonatites

Автор: Keith Bell, Jörg Keller

Език:

Корици: С меки корици

Издател: Springer-Verlag Berlin and Heidelberg GmbH & Co. KG

Наличност: Външен склад

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52.77 € 103.22 лв

During the last few years, carbonatites have received a considerable amount of attention. Some of th...

Информация за книгата

Автор

Keith Bell, Jörg Keller

Език

Английски език

Корици

Книга - С меки корици

Издадена

2011

страници

210

EAN

9783642791840

ISBN

9783642791840

Enbook ID

06620555

Издател

Springer-Verlag Berlin and Heidelberg GmbH & Co. KG

Теглоt

392

Размери

170 x 242 x 13

Пълно описание

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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Carbonatite Volcanism

Oldoinyo Lengai and the Petrogenesis of Natrocarbonatites

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