Textures in Partially Solidified Crystalline Nodules: a Window into the Pore Structure of Slowly Cooled Mafic Intrusions (2007)
Attributed to:
Oxygen isotope variation in Icelandic gabbros: Deep hydrothermal flow or mantle heterogeneity?
funded by
NERC
Abstract
No abstract provided
Bibliographic Information
Digital Object Identifier: http://dx.doi.org/10.1093/petrology/egm016
Publication URI: http://dx.doi.org/10.1093/petrology/egm016
Type: Journal Article/Review
Parent Publication: Journal of Petrology
Issue: 7