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The Emplacement of the Main Glencoe Fault-Intrusion at Stob Mhic Mhartuin

Published online by Cambridge University Press:  01 May 2009

John L. Roberts
John L. Roberts
Affiliation:
Department of Geology, The University, Newcastle-upon-Type, 2.
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Abstract

The contact relationships of the Fault-Intrusion are described, in detail, from the type locality. Textural and mineralogical evidence indicates that the fine-grained marginal facies of the Fault-Intrusion is not a priori evidence for magmatic emplacement. The production of “ flinty crush-rock ” from brecciated quartzites downfaulted within the Glencoe cauldron is described from the south-western inner contact, and is shown to be a result of gas attrition. “ Flinty crush-rock ” is recorded for the first time from the north-eastern contact with the country rocks outwith the cauldron, separated from the latter by a sheared microbreccia not found at the inner contact. The contact relations of the Fault-Intrusion with these “ flinty crush-rocks ”, more properly termed pseudotachylites, indicates that the Fault-Intrusion was emplaced as an entrained fluidized system of gas, solid phenocrysts and, probably, liquid droplets. The production of the sheared microbreccia at the outer contact is thought to be due to shearing stresses exerted by the entrained system on the heated wall-rocks.

Type
Articles
Information
Geological Magazine , Volume 103 , Issue 4 , August 1966 , pp. 299 - 316
Copyright
Copyright © Cambridge University Press 1966

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References

REFERENCES

Bailey, E. B., 1960. The geology of Ben Nevis and Glen Coe. (Sheet 53) 2nd ed. Mem. geol. Surv. U.K.Google Scholar
Bailey, E. B. and Maufe, H. B., 1916. The geology of Ben Nevis and Glen Coe. 1st ed. Mem. geol. Surv. U.K.Google Scholar
Bowen, N. L., 1928. The evolution of the igneous rocks. Princeton.Google Scholar
Cloos, H., 1941. Bau und tatigkeit von tuffschloten. Untersuchungen an dem Schwäbischenvulkan. Geol.Rdsch., 32, 709–800.CrossRefGoogle Scholar
Clough, C. T., Maufe, H. B., and Bailey, E. B., 1909. The cauldron-subsidence of Glen Coe, and the associated igneous phenomena. Q. Jl geol. Soc. Lond., 65, 611–674.CrossRefGoogle Scholar
Griggs, D. T., Turner, F. J., and Heard, H. C., 1960. Deformation of rocks at 500°C. to 800°C. Mem. geol. Soc. Am., 79, 76–102.Google Scholar
Reynolds, D. L., 1954. Fluidisation as a geological process, and its bearing on the problem of intrusive granites. Am. J. Sci., 252, 577–614.CrossRefGoogle Scholar
Reynolds, D. L., 1956. Calderas and ring-complexes. Nederl. Geol.-Mijnb. Gen. Verh. Geol. Ser., 16, 355–380.Google Scholar
Roberts, J. L., 1963. Source of the Glencoe ignimbrites. Nature, 199, 901.CrossRefGoogle Scholar
Roberts, J. L., 1966. Ignimbrite eruptions in the volcanic history of the Glencoe Cauldron Subsidence. Lpool. Manchr. geol. J, 5, 173–184.CrossRefGoogle Scholar
Shand, S. J., 1916. The pseudotachylite of Parijs (Orange Free State) and its relation to “trap-sholten gneiss” and “flinty crush-rock”. Q. Jl geol. Soc. Lond., 72, 198–221.CrossRefGoogle Scholar
Whitten, E. H. T., 1959. Tuffisites and magnetite tuffisites from Tory Island, Ireland, and related products of gas action. Am. J. Sci., 257, 113–137.CrossRefGoogle Scholar