Oxygen isotope heterogeneity and disequilibria of olivine crystals in large volume Holocene basalts from Iceland: Evidence for magmatic digestion and erosion of Pleistocene hyaloclastites

Author:

Bindeman Ilya,Gurenko Andrey,Sigmarsson Olgeir,Chaussidon Marc

Publisher

Elsevier BV

Subject

Geochemistry and Petrology

Reference67 articles.

1. Reactive bulk assimilation: a model for crust-mantle mixing in silicic magmas;Beard;Geology,2005

2. Bell J. D. and Humphries D. J. (1972) Lakagigar fissure eruption. In Progress in Experimental Petrology. National Environmental Rec Council, UK Publ. Series, D2, pp. 110–112.

3. A practical petrological method for determination of volume proportions of magma chamber refilling;Bindeman;J. Volcanol. Geotherm. Res.,1993

4. Kamchatka Peninsula: a province with high-δ18O magma sources and large scale 18O/16O depletion of the upper crust;Bindeman;Geochim. Cosmochim. Acta,2004

5. Time constraints on the origin of large volume basalts derived from O-isotope and trace element mineral zoning and U-series disequilibria in the Laki and Grı´msvötn volcanic system;Bindeman;Earth Planet Sci. Lett.,2006

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