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Co-existing Pyroxenes in Igneous Assemblages: a Re-evaluation of the Existing Data on Tie-line Orientations

Published online by Cambridge University Press:  01 May 2009

G. M. Brown
Affiliation:
Department of Geology and Mineralogy, University Museum, Oxford.

Abstract

Tie-line data are presented for twelve analysed igneous pyroxene pairs, from which it is demonstrated that a precise point of intersection, at or close to Wo75 En25 in the ternary diagram, does not exist. Eight tie-lines for pyroxene pairs from ultrabasic nodules in basalts are also considered. The tie-lines for metamorphic pyroxenes are compared with the igneous, and are shown to intersect over a similarly wide range, the average (Ca82 Mg18) being the same for both assemblages. It is shown that no conclusions can be drawn as to the genesis of the pyroxene assemblage, from the assumption of a characteristic tie-line intersection point. Optical determinations are considered, and shown to be of little practical value in this particular problem.

Type
Articles
Copyright
Copyright © Cambridge University Press 1961

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References

REFERENCES

Brown, G. M., 1957. Pyroxenes from the early and middle stages of fractionation of the Skaergaard intrusion, East Greenland. Miner. Mag., 31, 511543.Google Scholar
Carmichael, I. S. E., 1960. Pyroxenes and olivines from Tertiary acid glasses. J. Petrol., 1, 309336.Google Scholar
Hess, H. H., 1941. Pyroxenes of common mafic magmas, part 2. Amer. Min., 26, 573594.Google Scholar
Hess, H. H., 1949. Chemical composition and optical properties of common clinopyroxenes, part 1. Amer. Min., 34, 621666.Google Scholar
Hess, H. H., 1952. Orthopyroxenes of the Bushveld type, ion substitutions and changes in unit cell dimensions. Amer. J. Sci., Bowen Volume, 173187.Google Scholar
Hess, H. H., 1960. Stillwater igneous complex, Montana: a quantitative mineralogical study. Geol. Soc. Amer. Mem. 80, 1230.Google Scholar
Howie, R. A., 1955. The geochemistry of the charnockite series of Madras, India. Trans, roy. Soc. Edinb., 62, 725768.CrossRefGoogle Scholar
Howie, R. A., 1958. African charnockites and related rocks. Bull. Serv. géol. Congo Belge, 8, fasc. 2, 16 pp.Google Scholar
Muir, I. D., 1951. The clinopyroxenes of the Skaergaard intrusion, Eastern Greenland. Miner. Mag., 29, 690714.Google Scholar
Muir, I. D., and Tilley, C. E., 1957. Contributions to the petrology of Hawaiian basalts, I. The picrite basalts of Kilauea. Amer. J. Sci., 255, 244253.CrossRefGoogle Scholar
Muir, I. D., and Tilley, C. E., 1958. The compositions of co-existing pyroxenes in metamorphic assemblages. Geol Mag., 95, 403408.CrossRefGoogle Scholar
Ross, C. S., Foster, M. D., and Myers, A. T., 1954. Origin of dunites and of olivine-rich inclusions in basaltic rocks. Amer. Min., 39, 693737.Google Scholar
Wager, L. R., 1958. Beneath the Earth's crust. Pres. Add. Brit. Assocn., Adv. Sci. No. 58, 15 pp.Google Scholar
Wager, L. R., Brown, G. M., and Wadsworth, W. J., 1960. Types of igneous cumulates. J. Petrol., 1, 7385.CrossRefGoogle Scholar
Wilson, A. F., 1960. Co-existing pyroxenes: some causes of variation and anomalies in the optically derived compositional tie-lines, with particular reference to charnockitic rocks. Geol. Mag., 97, 117.CrossRefGoogle Scholar