Inbunden, Engelska, 2018
323 kr
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Keith Bell – författare
Visar alla böcker från författaren Keith Bell. Handla med fri frakt och snabb leverans.
5 produkter
5 produkter
- Häftad, Engelska, 2018
245 kr
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- Inbunden, Engelska, 2018
387 kr
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Ready to find out what happened to Kilo and Kenya? Slim and Ivonne? Fresh and all his pieces? Cant forget about Quick. Ready to find out how they escaped the cartel? Or if they escaped? Get ready because its about to go down in the streets of Youngstown, Ohio, once again. - E-bokPDF, Engelska, 2012
718 kr
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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. - Del 4 - IAVCEI Proceedings in Volcanology
Carbonatite Volcanism
Oldoinyo Lengai and the Petrogenesis of Natrocarbonatites
Häftad, Engelska, 2011556 kr
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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.
