Carbonatite Volcanism: Oldoinyo Lengai and the Petrogenesis of Natrocarbonatites
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-c...
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| Format: | Elektronisch E-Book |
| Sprache: | English |
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Berlin, Heidelberg
Springer Berlin Heidelberg
1995
|
| Schriftenreihe: | IAVCEI Proceedings in Volcanology
4 |
| Schlagworte: | |
| Online-Zugang: | BTU01 URL des Erstveröffentlichers |
| Zusammenfassung: | 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 |
| Beschreibung: | 1 Online-Ressource (XI, 210 p. 2 illus. in color) |
| ISBN: | 9783642791826 |
| DOI: | 10.1007/978-3-642-79182-6 |
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| 520 | |a 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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Datensatz im Suchindex
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| dewey-ones | 551 - Geology, hydrology, meteorology |
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| discipline | Geologie / Paläontologie |
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| indexdate | 2024-07-10T08:10:46Z |
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| isbn | 9783642791826 |
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| spelling | Carbonatite Volcanism Oldoinyo Lengai and the Petrogenesis of Natrocarbonatites edited by Keith Bell, Jrg Keller Berlin, Heidelberg Springer Berlin Heidelberg 1995 1 Online-Ressource (XI, 210 p. 2 illus. in color) txt rdacontent c rdamedia cr rdacarrier IAVCEI Proceedings in Volcanology 4 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 Earth Sciences Geology Geochemistry Mineralogy Earth sciences Karbonatit (DE-588)4205492-8 gnd rswk-swf Gesteinsbildung (DE-588)4157153-8 gnd rswk-swf Natrokarbonatit (DE-588)4382536-9 gnd rswk-swf Ol Doinyo Lengai (DE-588)4371949-1 gnd rswk-swf 1\p (DE-588)1071861417 Konferenzschrift 1990 Mainz gnd-content Ol Doinyo Lengai (DE-588)4371949-1 g Karbonatit (DE-588)4205492-8 s Gesteinsbildung (DE-588)4157153-8 s 2\p DE-604 Natrokarbonatit (DE-588)4382536-9 s 3\p DE-604 Bell, Keith edt Keller, Jrg edt Erscheint auch als Druck-Ausgabe 9783642791840 https://doi.org/10.1007/978-3-642-79182-6 Verlag URL des Erstveröffentlichers Volltext 1\p cgwrk 20201028 DE-101 https://d-nb.info/provenance/plan#cgwrk 2\p cgwrk 20201028 DE-101 https://d-nb.info/provenance/plan#cgwrk 3\p cgwrk 20201028 DE-101 https://d-nb.info/provenance/plan#cgwrk |
| spellingShingle | Carbonatite Volcanism Oldoinyo Lengai and the Petrogenesis of Natrocarbonatites Earth Sciences Geology Geochemistry Mineralogy Earth sciences Karbonatit (DE-588)4205492-8 gnd Gesteinsbildung (DE-588)4157153-8 gnd Natrokarbonatit (DE-588)4382536-9 gnd |
| subject_GND | (DE-588)4205492-8 (DE-588)4157153-8 (DE-588)4382536-9 (DE-588)4371949-1 (DE-588)1071861417 |
| title | Carbonatite Volcanism Oldoinyo Lengai and the Petrogenesis of Natrocarbonatites |
| title_auth | Carbonatite Volcanism Oldoinyo Lengai and the Petrogenesis of Natrocarbonatites |
| title_exact_search | Carbonatite Volcanism Oldoinyo Lengai and the Petrogenesis of Natrocarbonatites |
| title_full | Carbonatite Volcanism Oldoinyo Lengai and the Petrogenesis of Natrocarbonatites edited by Keith Bell, Jrg Keller |
| title_fullStr | Carbonatite Volcanism Oldoinyo Lengai and the Petrogenesis of Natrocarbonatites edited by Keith Bell, Jrg Keller |
| title_full_unstemmed | Carbonatite Volcanism Oldoinyo Lengai and the Petrogenesis of Natrocarbonatites edited by Keith Bell, Jrg Keller |
| title_short | Carbonatite Volcanism |
| title_sort | carbonatite volcanism oldoinyo lengai and the petrogenesis of natrocarbonatites |
| title_sub | Oldoinyo Lengai and the Petrogenesis of Natrocarbonatites |
| topic | Earth Sciences Geology Geochemistry Mineralogy Earth sciences Karbonatit (DE-588)4205492-8 gnd Gesteinsbildung (DE-588)4157153-8 gnd Natrokarbonatit (DE-588)4382536-9 gnd |
| topic_facet | Earth Sciences Geology Geochemistry Mineralogy Earth sciences Karbonatit Gesteinsbildung Natrokarbonatit Ol Doinyo Lengai Konferenzschrift 1990 Mainz |
| url | https://doi.org/10.1007/978-3-642-79182-6 |
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