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About this Earth and Planetary Sciences article

Reaction relationships of chrome-spinels in igneous rocks — further evidence from the layered intrusions of Rhum and Mull, Inner Hebrides, Scotland by Paul Henderson; Richard J. Wood is a Earth and Planetary Sciences article available to read on EtoBox.

Compositions of chrome-spinels in peridotites from the layered igneous rocks of Rhum and of the Ben Buie intrusion, Mull, show evidence of post-depositional reaction relationships with the cumulus olivine and/or the intercumulus liquid. Some seam-forming spinels in the Ben Buie intrusion are highly aluminous, more so than those in the Rhum intrusion. Occasional zoned spinels, in both intrusions, show enrichment in A1 towards their rims. The evidence suggests that the spinel reaction trend involving Cr-A1 exchange proceeds in the direction of Al-enrichmerit. Equilibrium between chrome-spinel and cumulus olivine appears to have been attained rarely, thus limiting the application of the olivine-spinel geothermometer.

It is typically read by researchers, students, and practitioners in Earth and Planetary Sciences.

Author
Paul Henderson; Richard J. Wood
Publisher
Springer; Springer-Verlag; Springer Verlag; Springer Science and Business Media LLC; Society for Mining, Metallurgy and Exploration Inc. (ISSN 0010-7999)
Published
1982
Language
EN
Field
Earth and Planetary Sciences (Physical Sciences)