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Pseudomorphs after olivine in Markle basalt

Published online by Cambridge University Press:  14 March 2018

W. W. Smith
W. W. Smith*
Affiliation:
The Macaulay Institute for Soil Research, Aberdeen, Scotland
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Summary

Pseudomorphs after olivine in Markle basalt from Holyrood Park, Edinburgh, consist of an intimate mixture of hematite and chlorite, along with a small percentage of quartz. A definite relationship exists between the orientations of the two main constituents and is dependent upon their structures.

Type
Research Article
Information
Mineralogical magazine and journal of the Mineralogical Society , Volume 32 , Issue 247 , December 1959 , pp. 324 - 331
Copyright
Copyright © 1959, The Mineralogical Society

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References

Hey, (M.H.), 1954. Min. Mag., vol. 30, p. 277.Google Scholar
Iddings, (J.P.), 1892. U.S. Geol. Survey, Monogr. 20, App. B, p. 388.Google Scholar
Lawson, (A.C.), 1893. Univ. Calif. Pub]. Geol. Sci., vol. 1, p. 1.Google Scholar
Mitchell, (B.D.) and Mackenzie, (R.C.), 1954. Soil Sci., vol. 77, p. 173.CrossRefGoogle Scholar
Ross, (C.S.) and S∼Annon, (E.V.), 1926. Proc. U.S. Nat. Mus., vol. 67, art. 7, p . 1.Google Scholar
Sun, (Ming-Shan), 1957. Amer. Min., vol. 42, p. 525.Google Scholar
Tomkeieff, (S.I.), 1934. Geol. Mag., vol. 71, p. 501.Google Scholar
Wilshire, (H.G.), 1958. Amer. Min. vol. 43, p. 120.Google Scholar