Hostname: page-component-cd9895bd7-q99xh Total loading time: 0 Render date: 2024-12-27T07:46:20.906Z Has data issue: false hasContentIssue false

The Lower Hecla Hoek Rocks of Ny Friesland, Spitsbergen

Published online by Cambridge University Press:  01 May 2009

M. B. Bayly
Affiliation:
Sedgwick Museum, Cambridge.

Abstract

The Lower Hecla Hpek rocks of Ny Friesland are described petrographically, and evidence is presented relating to some granitic rocks in this group whose mode of origin is uncertain.

Type
Articles
Copyright
Copyright © Cambridge University Press 1957

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

REFERENCES

Blömstrand, C. A., 1864. Geognostika iakttagelser under en resa till Spetsbergen år 1861. Konglia Svenska Vet. Akad. Handl., iv, No. 6, 146.Google Scholar
Chayes, F., 1949. A simple point counter for thin section analysis. Amer. Min., xxxiv, 111.Google Scholar
Chayes, F., 1950 a. Composition of the granites of Westerly and Bradford, Rhode Island. Amer. Journ. Sci., ccxlviii, 378407.CrossRefGoogle Scholar
Chayes, F., 1950 b. Composition of some New England granites. Trans. N.Y. Acad. Sci., ser. 2, xii, 144151.CrossRefGoogle Scholar
Chayes, F., 1951. In Fairbairn, H. W. et al. : A co-operative investigation of precision and accuracy in chemical, spectro-chemical and modal analyses of silicate rocks. Bull. U.S. Geol. Surv., 980, 5968.Google Scholar
Chayes, F., 1952 a. The finer-grained calcalkaline granites of New England. Journ. Geol., ix, 207254.CrossRefGoogle Scholar
Chayes, F., 1952 b. Notes on the staining of potash feldspar with sodium cobaltinitrite in thin section. Amer. Min., xxxvii, 337340.Google Scholar
Chayes, F., and Fairbairn, H. W., 1951. A test of the precision of thin section analysis by point counter. Amer. Min., xxxvi, 704712.Google Scholar
Fairbairn, P. E., 1933. The petrology of the Hecla Hook formation in central Spitsbergen. Geol. Mag., lxx, 437454.CrossRefGoogle Scholar
Francis, G. H., 1956. Facies boundaries in pelites at the middle grades of regional metamorphism. Geol. Mag., xciii, 353368.CrossRefGoogle Scholar
Hall, A. J., 1941. The relation between colour and chemical composition in the biotites. Amer. Min., xxvi, 2933.Google Scholar
Harland, W. B., 1941. Geological notes on the Stubendorff Mountains, West Spitsbergen. Proc. Roy. Soc. Edinb., B, lxi, pt. 2, No. 10, 119129.Google Scholar
Harland, W. B., (MS.). The Caledonian sequence in Ny Friesland, Spitsbergen. (To be published in the Quart. Journ. Geol. Soc.)Google Scholar
Harland, W. B., and Wilson, C. B., 1956. The Hecla Hoek succession in Ny Friesland, Spitsbergen. Geol. Mag., xciii, 265286.CrossRefGoogle Scholar
Ramberg, H., 1952. The origin of metamorphic and metasomatic rocks. Univ. of Chicago Press, Chicago.Google Scholar
Turner, F. J., and Verhoogen, J., 1951. Igneous and Metamorphic Petrology. McGraw-Hill Book Co.Google Scholar