First recorded eruption of Nabro volcano,Eritrea, 2011     

Berhe Goitom  Clive Oppenheimer  James O. S. Hammond  Raphaël Grandin  Talfan Barnie  Amy Donovan  Ghebrebrhan Ogubazghi  Ermias Yohannes  Goitom Kibrom  J- Michael Kendall  Simon A. Carn  David Fee  Christine Sealing  Derek Keir  Atalay Ayele  Jon Blundy  Joanna Hamlyn  Tim Wright  Seife Berhe 《Bulletin of Volcanology》2015,77(10):1-21

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Integrated field, satellite and petrological observations of the November 2010 eruption of Erta Ale   总被引：2，自引：1，他引：1  

Lorraine Field  Talfan Barnie  Jon Blundy  Richard A. Brooker  Derek Keir  Elias Lewi  Kate Saunders 《Bulletin of Volcanology》2012,74(10):2251-2271

Erta Ale volcano, Ethiopia, erupted in November 2010, emplacing new lava flows on the main crater floor, the first such eruption from the southern pit into the main crater since 1973, and the first eruption at this remote volcano in the modern satellite age. For many decades, Erta Ale has contained a persistently active lava lake which is ordinarily confined, several tens of metres below the level of the main crater, within the southern pit. We combine on-the-ground field observations with multispectral imaging from the SEVIRI satellite to reconstruct the entire eruptive episode beginning on 11 November and ending prior to 14 December 2010. A period of quiescence occurred between 14 and 19 November. The main eruptive activity developed between 19 and 22 November, finally subsiding to pre-eruptive levels between 8 and 15 December. The estimated total volume of lava erupted is ??0.006?km³. The mineralogy of the 2010 lava is plagioclase?+?clinopyroxene?+?olivine. Geochemically, the lava is slightly more mafic than previously erupted lava lining the caldera floor, but lies within the range of historical lavas from Erta Ale. SIMS analysis of olivine-hosted melt inclusions shows the Erta Ale lavas to be relatively volatile-poor, with H₂O contents ??1,300?ppm and CO₂ contents of ??200?ppm. Incompatible trace and volatile element systematics of melt inclusions show, however, that the November 2010 lavas were volatile-saturated, and that degassing and crystallisation occurred concomitantly. Volatile saturation pressures are in the range 7?C42?MPa, indicating shallow crystallisation. Calculated pre-eruption and melt inclusion entrapment temperatures from mineral/liquid thermometers are ??1,150?°C, consistent with previously published field measurements.  相似文献