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Intrusive Phenomena of the Whin Sill, East of the R. North Tyne

Published online by Cambridge University Press:  01 May 2009

B. A. O. Randall
B. A. O. Randall
Affiliation:
Dept. of Geology, King's College, Newcastle upon Tyne.
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Abstract

The Whin Sill of this district has the form of a series of sills at different stratigraphical levels. Minor scarps at right angles to the main trend of the sill are explained by intrusion of offshoots, from its upper surface, along low angled fractures in the superincumbent strata. An intrusion mechanism is suggested to account for the presence of the Oxford Limestone both above and below the Whin Sill.

Type
Articles
Information
Geological Magazine , Volume 96 , Issue 5 , October 1959 , pp. 385 - 392
Copyright
Copyright © Cambridge University Press 1959

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References

Holmes, A and Harwood, H. F., 1928. The age and composition of the Whin Sill and related dikes of the north of England. Miner. Mag., xxi, 493.Google Scholar
Johnson, G. A. L., 1953. The Biostratigraphy of the Carboniferous Middle Limestone Group succession between Tipalt Burn and the River North Tyne in S.W. Northumberland. Unpublished Ph.D. Thesis.Google Scholar
Smythe, J. A., 1930. A Chemical Study of the Whin Sill. Trans. Nat. Hist. Soc. Northumberland, Durham and Newcastle upon Tyne, vii, 16.Google Scholar
Smythe, J. A., 1931. Intrusion phenomena of the Whin Sill. Proc. Geol. Assoc., xlii, 272.Google Scholar
Smythe, J. A., 1950. Metamorphism of Sedimentary Rocks by the Whin Sill. Proc. Univ. Durham Phil. Soc., x, 541.Google Scholar
Topley, W and Lebour, G. A., 1877. On the intrusive character of the Whin Sill of Northumberland. Quart. Journ. Geol. Soc., xxxiii, 406.CrossRefGoogle Scholar
Weyman, G., 1910. On the section of the Great Whin Sill near Gunnerton. Proc. Univ. Durham Phil. Soc., iii, 201.Google Scholar