Hostname: page-component-586b7cd67f-rcrh6 Total loading time: 0 Render date: 2024-11-26T19:12:04.305Z Has data issue: false hasContentIssue false

The occurrence of magnesian pyroxenes and magnetite in porphyritic acid glasses

Published online by Cambridge University Press:  14 March 2018

I. S. E. Carmichael*
Affiliation:
Department of Geology, Imperial College of Science and Technology, London S.W. 7

Summary

The problem of magnesian pyroxenes in acid liquids is considered in the light of new analyses of pyroxene and magnetite phenocrysts. It is suggested that the early precipitation of titaniferous magnetite, which will strongly deplete the liquid in iron, will decrease the iron:magnesium ratio of the pyroxene components in the liquid. Accordingly the iron:magnesium ratio of a pyroxene precipitating from an acid liquid may vary over a wide range depending upon the presence or amount of early magnetite.

Type
Research Article
Copyright
Copyright © 1963, The Mineralogical Society

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Basta, (E.Z.), 1957. Accurate determination of the cell dimensions of magnetite. Min. Mag,, vol. 31, p. 431.Google Scholar
Bowen, (N.L.) and Schairer, (J.F.), 1935. The system MgO-FeO-SiO2. Amer. Journ. Sei., ser. 5, vol. 29, p. 151.[M.A. 6-352].Google Scholar
Brown, (G.M.), 1957. Pyroxenes of the early and middle stages of fractionation of the Skaergaard intrusion, East Greenland. Min. Mag., vol. 31, p. 511.Google Scholar
Brown, (G.M.), 1960. The effects of ion substitution on the unit cell dimensions of the common clinopyroxenes. Amer. Min., vol. 45, p. 15.[M.A. 15-143].Google Scholar
Brown, (P.E.), 1961. Co-existing pyroxenes. Geol. Mag., vol. 98, p. 531.CrossRefGoogle Scholar
Carmichael, (I. S. E.), 1960. The pyroxenes and olivines from some Tertiary acid glasses. Journ. Petrology, vol. 1, p. 309.Google Scholar
Carmichael, (I. S. E.), 1962. Pantelleritic liquids and their phenocrysts. Min. Mag., vol. 33, p. 86.Google Scholar
Carmichael, (I. S. E.), and McDonald, (A.), 1961. The geochemistry of some natural acid glasses from the North Atlantic Tertiary volcanic province. Geochimica Acta, vol. 25, p. 189.Google Scholar
Hess, (H.H.), 1960. Stillwater igneous complex, Montana: a quantitative mineralogical study. Mem. Geol. Soc. Amer. no. 80.CrossRefGoogle Scholar
Muir, (I.D.), 1954. Crystallization of pyroxenes in an iron-rich diabase from Minnesota. Min. Mag., vol. 30, p. 376.Google Scholar
Phillips, (B.), and Muan, (A.), 1959. Phase equilibria in the system CaO-Iron oxide-SiO∼ in air. Journ. Amer. Ceramic Soc., vol. 42, p. 413.Google Scholar
Vincent, (E.A.) and Phillips, (R.), 1954. Iron-titanium oxide minerals in layered gabbros of the Skaergaard intrusion, East Greenland. Part I. Chemistry and ore-microscopy. Geochimica Acta, vol. 6, p. 1.Google Scholar
Vincent, (E.A.) Wright, (J.B.), Chevallier, (R.), and Mathieu, (S.), 1957. Heating experiments on some natural titaniferous magnetites. Min. Mag., vol. 31, p. 624.Google Scholar
Wager, (L.R.), 1956. A chemical definition of fractionation stages as a basis for comparison of Hawaiian, Hebridean and other basic lavas. Geochimica Acta, vol. 9, p. 217.Google Scholar
Wager, (L.R.), 1960. The major element variation of the layered series of the Skaergaard intrusion and a re-estimation of the average composition of the hidden layered series and of the successive residual magmas. Journ. Petrology, vol. 1, p. 364.Google Scholar