Article Geochemistry 3 Volume 4, Number 11 Geophysics 15 November 2003 8624, doi:10.1029/2003GC000558 GeosystemsG G ISSN: 1525-2027 AN ELECTRONIC JOURNAL OF THE EARTH SCIENCES Published by AGU and the Geochemical Society Melt mixing and crystallization under Theistareykir, northeast Iceland J. Maclennan Bullard Laboratories, Department of Earth Sciences, Madingley Road, Cambridge, CB3 0EZ, UK Now at Laboratoire de Ge´osciences Marines, Institut de Physique du Globe de Paris, France (
[email protected]) D. McKenzie Bullard Laboratories, Department of Earth Sciences, Madingley Road, Cambridge, CB3 0EZ, UK (
[email protected]) K. Gro¨nvold Nordic Volcanological Institute, Reykjavik, Iceland (
[email protected]) N. Shimizu Department of Geology and Geophysics, Woods Hole Oceanographic Institution, Woods Hole, Massachusetts 02543, USA (
[email protected]) J. M. Eiler and N. Kitchen Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, California 91125, USA (
[email protected]) [1] Analysis of the compositions of crystals and melt inclusions from a suite of 40 gabbroic and wehrlitic nodules in a single eruptive body provides a record of concurrent mixing and crystallization of melts under NE Iceland. The crystals in the nodules have a similar range of compositions to those found as phenocrysts in the flow, and many of the nodules may have been generated by crystallization of a magma with a similar composition to that of the host flow. While plagioclase is only present in nodules where the average forsterite content of olivines is <Fo88.5, clinopyroxene is found in nodules with average olivine forsterite contents of up to Fo91.6.