Carbonatite Volcanism: Oldoinyo Lengai and the Petrogenesis of Natrocarbonatites: IAVCEI Proceedings in Volcanology, cartea 4
Editat de Keith Bell, Jörg Kelleren Limba Engleză Paperback – 22 noi 2011
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Specificații
ISBN-13: 9783642791840
ISBN-10: 3642791840
Pagini: 224
Ilustrații: XI, 210 p. 2 illus. in color.
Dimensiuni: 170 x 242 x 12 mm
Greutate: 0.36 kg
Ediția:Softcover reprint of the original 1st ed. 1995
Editura: Springer Berlin, Heidelberg
Colecția Springer
Seria IAVCEI Proceedings in Volcanology
Locul publicării:Berlin, Heidelberg, Germany
ISBN-10: 3642791840
Pagini: 224
Ilustrații: XI, 210 p. 2 illus. in color.
Dimensiuni: 170 x 242 x 12 mm
Greutate: 0.36 kg
Ediția:Softcover reprint of the original 1st ed. 1995
Editura: Springer Berlin, Heidelberg
Colecția Springer
Seria IAVCEI Proceedings in Volcanology
Locul publicării:Berlin, Heidelberg, Germany
Public țintă
ResearchCuprins
Historic and Recent Eruptive Activity of Oldoinyo Lengai.- Field Observations and Measurements of the Physical Properties of Oldoinyo Lengai Alkali Carbonatite Lavas, November 1988.- The Dynamics of Degassing at Oldoinyo Lengai.- Petrology and Geochemistry of Oldoinyo Lengai Lavas Extruded in November 1988: Magma Source, Ascent and Crystallization.- The Trace Element Composition and Petrogenesis of Natrocarbonatites.- Cathodoluminescence Observations of Natrocarbonatites and Related Peralkaline Nephelinites at Oldoinyo Lengai.- Nd and Sr Isotope Systematics of the Active Carbonatite Volcano, Oldoinyo Lengai.- Stable Isotope Characteristics of Recent Natrocarbonatites from Oldoinyo Lengai.- Decay Series Evidence for Transfer and Storage Times of Natrocarbonatite Magma.- An Assessment of the Alleged Role of Evaporites and Saline Brines in the Origin of Natrocarbonatite.- What are the Parental Magmas at Oldoinyo Lengai?.- Peralkaline Nephelinite/Carbonatite Liquid Immiscibility: Comparison of Phase Compositions in Experiments and Natural Lavas from Oldoinyo Lengai.- Experimental Constraints on the Possible Mantle Origin of Natrocarbonatite.