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Amphibole-bearing Cumulate Inclusions, Grand Canyon, Arizona and their bearing on Silica-Undersaturated Hydrous Magmas in the Upper Mantle

M. G. Best
- 01 Jan 1975 - 
- Vol. 16, Iss: 1, pp 212-236
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This article is published in Journal of Petrology.The article was published on 1975-01-01. It has received 70 citations till now. The article focuses on the topics: Amphibole & Canyon.

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Petrogenetic implications of Ti, Zr, Y, and Nb variations in volcanic rocks

TL;DR: In this paper, a table of mineral-liquid distribution coefficients for Ti, Zr, Y, and Nb for basic, intermediate and acid melt compositions were used to interpret variations of these elements, first in basalts and second during fractional crystallization from basic to acid magmas.
Journal ArticleDOI

Characteristics and tectonic significance of supra subduction zone ophiolites

TL;DR: Supra-subduction zone ophiolites have the geochemical characteristics of island arcs but the structure of oceanic crust and are thought to have formed by sea-floor spreading directly above subducted oceanic lithosphere.
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Ultramafic inclusions from San Carlos, Arizona: Petrologic and geochemical data bearing on their petrogenesis

TL;DR: In this article, the authors classified ultramafic inclusions from San Carlos, Arizona into two groups: Group I inclusions are dominated by magnesian (Mg/Mg + ΣFe= 0.86-0.91), olivine-rich peridotites containing Cr-rich clinopyroxene and spinel.
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Lateral variation in upper mantle viscosity: role of water

TL;DR: In this paper, geochemical data on the water contents of western US lavas and mantle xenoliths, compared these data to water solubility in olivine, and calculate the corresponding effective viscosity of olivines, the major constituent of the upper mantle, using a power law creep rheological model.
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