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Magmas and volatile components

Wyllie, Peter J. (1979) Magmas and volatile components. American Mineralogist, 64 (5-6). pp. 469-500. ISSN 0003-004X. http://resolver.caltech.edu/CaltechAUTHORS:20160210-102641552

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Abstract

The trivial quantities of CO_2 and H_2O (or reduced combination of C-H-O-S) in the upper mantle have little effect on the abundant basalts, but H_2O influences magmas generated in peridotite overlying subducted, hydrated oceanic crust, and CO_2 causes the generation of alkalic subsilicic magmas from peridotite beneath continental shields. PT sections through the (partly schematic) phase diagram for peridotite-CO_2-H_2O with low (CO_2 + H_2O) and selected CO_2/H_2O, compared with isotherms, illustrate the petrological structure of the upper mantle for different tectonic environments. If vapor is present, the cooler the geotherm, the higher is H_2O/CO_2: only in regions of upwelling can CO_2-rich vapor exist. The solidus surface for peridotite-CO_2-H_2O (P, T, X^V) has been mapped with tentative boundaries marking changes in normative compositions of near-solidus magmas. The restricted area for quartz-normative magmas suggests that if these are to be generated from mantle in subduction zones, there must be active asthenospheric convection carrying hot mantle to shallow levels above dehydration fronts in subducted oceanic crust. Changes in the relative positions of dehydration fronts and solidus boundaries for warm and cool subduction models are illustrated in new diagrams, unencumbered by the need for precise temperatures and depths. Tests for processes require knowledge of the phase relationships in the system basalt-andesite-dacite-rhyolite-H_2O from magma sources at depth to the surface. Data from scattered sources have been synthesized in a PTX(SiO_2)X(H_2O) framework to 35 kbar, and illustrated in sections and projections, including liquidus surfaces for the rock series to 35 kbar, dry, with 5 percent H_2O, and with excess H_2O (saturated). The volatile components become prominent in residual magmas: pegmatites from granitic magmas are enriched in H_2O, and carbonatites from alkalic magmas are extraordinarily enriched in CO_2. The behavior of another volatile component is illustrated by experimental data in NaAlSi_3O_8-H_2O-HF at 2.75 kbar. The vapor-saturated liquidus field boundary extends from 808°C-8.5 percent H_2O to 777°C-(9.2 percent H_2O + 1.0 percent HF), and three-phase boundaries demonstrat1i strong partition of HF into liquid compared with vapor. Details remain uncertain for the sources of volatile components, in mantle reservoirs or recycled through subduction, and of oxygen fugacity and temperature variation with depth in different tectonic environments.


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http://www.minsocam.org/msa/collectors_corner/amtoc/toc1979.htmPublisherIssue Table of Contents
Additional Information:© 1979 Mineralogical Society of America. Manuscript received, January 22. 1979, accepted for publication, January 22, 1979. This research was supported by NSF grants EAR 76-20410 and EAR 76-20413 (Earth Sciences Section). I thank also the many graduate students and research associates who have helped gather the data that guided my pencil in the construction of the phase diagrams, and A. L. Boettcher for review of some of the figures.
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Funding AgencyGrant Number
NSFEAR 76-20410
NSFEAR 76-20413
Record Number:CaltechAUTHORS:20160210-102641552
Persistent URL:http://resolver.caltech.edu/CaltechAUTHORS:20160210-102641552
Usage Policy:No commercial reproduction, distribution, display or performance rights in this work are provided.
ID Code:64374
Collection:CaltechAUTHORS
Deposited By: Tony Diaz
Deposited On:10 Feb 2016 19:30
Last Modified:10 Feb 2016 19:30

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