Evidence for extreme fractionation of peralkaline silicic magmas, the Boseti volcanic complex, Main...
Evidence for extreme fractionation of peralkaline silicic magmas, the Boseti volcanic complex, Main Ethiopian Rift
About this item
Full title
Author / Creator
Publisher
Vienna: Springer Vienna
Journal title
Language
English
Formats
Publication information
Publisher
Vienna: Springer Vienna
Subjects
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Scope and Contents
Contents
Matrix glass and melt inclusions in phenocrysts from pantellerite lavas of the Boseti volcanic complex, Ethiopia, record extreme fractionation of peralkaline silicic magma, with Al
2
O
3
contents as low as 2.3 wt.%, FeO* contents up to 17 wt.% and SiO
2
contents ~65 wt.%. The new data, and published data for natural and experiment...
Alternative Titles
Full title
Evidence for extreme fractionation of peralkaline silicic magmas, the Boseti volcanic complex, Main Ethiopian Rift
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Primary Identifiers
Record Identifier
TN_cdi_proquest_miscellaneous_1805503832
Permalink
https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_proquest_miscellaneous_1805503832
Other Identifiers
ISSN
0930-0708
E-ISSN
1438-1168
DOI
10.1007/s00710-011-0184-4
