Evolution of natrocarbonatite from a wollastonite nephelinite parent: Evidence from the June, 1993 eruption of Oldoinyo Lengai, Tanzania
Lapilli and unusually thick, high viscosity lavas extruded from Oldoinyo Lengai in June, 1993 are composed of crystal-rich natrocarbonatite containing a small proportion of porphyritic silicate spheroids. The silicate spheroids are of wollastonite nephelinite mineralogy, but they also contain natroc...
Prif Awduron: | Dawson, J, Pyle, D, Pinkerton, H |
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Fformat: | Journal article |
Cyhoeddwyd: |
1996
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Eitemau Tebyg
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SHORT-LIVED DECAY SERIES DISEQUILIBRIA IN THE NATROCARBONATITE LAVAS OF OLDOINYO LENGAI, TANZANIA - CONSTRAINTS ON THE TIMING OF MAGMA GENESIS
gan: Pyle, D, et al.
Cyhoeddwyd: (1991) -
JUNE 1993 ERUPTION OF OLDOINYO-LENGAI, TANZANIA - EXCEPTIONALLY VISCOUS AND LARGE CARBONATITE LAVA FLOWS AND EVIDENCE FOR COEXISTING SILICATE AND CARBONATE MAGMAS
gan: Dawson, J, et al.
Cyhoeddwyd: (1994) -
PHYSICOCHEMICAL PROPERTIES OF ALKALI CARBONATITE LAVAS - DATA FROM THE 1988 ERUPTION OF OLDOINYO LENGAI, TANZANIA
gan: Dawson, J, et al.
Cyhoeddwyd: (1990) -
Open-path Fourier transform spectroscopy of gas emissions from Oldoinyo Lengai volcano, Tanzania
gan: Oppenheimer, C, et al.
Cyhoeddwyd: (2002) -
Early carbonatite magmatism at Oldoinyo Lengai volcano (Tanzania): carbonatite–silicate melt immiscibility in Lengai I melt inclusions
gan: France, Lydéric, et al.
Cyhoeddwyd: (2021-12-01)