Wang, Zhengrong and Eiler, John and Kitchen, Nami (2003) New insight into the origin of the low δ^(18)O magmas in Iceland. Geochimica et Cosmochimica Acta, 67 (18). A524-A524. ISSN 0016-7037. doi:10.1016/S0016-7037(03)00515-5. https://resolver.caltech.edu/CaltechAUTHORS:20130711-150844018
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Abstract
Iceland contains abundant low δ^(18)O volcanic rocks, reflecting ^(18)O-depleted sources and/or crustal contamination by assimilation and/or mixing with crustal melts. Previous attempts to distinguish among these mechanisms have been based principally on oxygen isotope measurements of whole-rocks, glasses, or mixed populations of phenocrysts. Here we add further constraints from micro-analyses of individual phenocrysts and xenocrysts.
| Item Type: | Article | |||||||||
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| Additional Information: | © 2003 Published by Elsevier Ltd. | |||||||||
| Issue or Number: | 18 | |||||||||
| DOI: | 10.1016/S0016-7037(03)00515-5 | |||||||||
| Record Number: | CaltechAUTHORS:20130711-150844018 | |||||||||
| Persistent URL: | https://resolver.caltech.edu/CaltechAUTHORS:20130711-150844018 | |||||||||
| Official Citation: | Abstracts, Geochimica et Cosmochimica Acta, Volume 67, Issue 18, Supplement, September 2003, Pages 501-550, ISSN 0016-7037, http://dx.doi.org/10.1016/S0016-7037(03)00515-5. | |||||||||
| Usage Policy: | No commercial reproduction, distribution, display or performance rights in this work are provided. | |||||||||
| ID Code: | 39325 | |||||||||
| Collection: | CaltechAUTHORS | |||||||||
| Deposited By: | Tony Diaz | |||||||||
| Deposited On: | 17 Jul 2013 22:19 | |||||||||
| Last Modified: | 09 Nov 2021 23:44 |
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