Hostname: page-component-cd9895bd7-q99xh Total loading time: 0 Render date: 2024-12-24T16:47:45.837Z Has data issue: false hasContentIssue false
  • English
  • Français

The Provenance and Emplacement of Upper Arenigian Turbidites in Co. Mayo, Eire.

Published online by Cambridge University Press:  01 May 2009

John Frederick Dewey
John Frederick Dewey
Affiliation:
Geology Department, The University, Manchester, 13.
Get access Rights & Permissions [Opens in a new window]

Abstract

Five thousand feet of Upper Arenig turbidites are described with reference to their provenance and mechanism of emplacement. The turbidites were emplaced in a gently curving E.–W. trough whose width was approximately 20 miles and minimum length 50 miles. Axial and lateral derivation are recognized and it is suggested that entirely different mechanisms were responsible for the emplacement of each type.

Type
Articles
Information
Geological Magazine , Volume 99 , Issue 3 , June 1962 , pp. 238 - 252
Copyright
Copyright © Cambridge University Press 1962

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

Alper, A. M., and Poldervaart, A., 1957. Zircons from the Animas stock and associated rocks, New Mexico. Econ. Geol., 52, 952.CrossRefGoogle Scholar
Kingma, J. T., 1960. The tectonic significance of graded bedding in geosynclinal sedimentary systems. Int. Geol. Cong. Report of twentyfirst session, Norden. Part XXI, 305.Google Scholar
Knill, J. L., 1960. Axial and marginal sedimentation in geosynclinal basins. J. sediment. Petrol., 29, 317.Google Scholar
Kuenen, Ph. H., 1956. The difference between sliding and turbidity flow. Deep-Sea Research, 3, 134.Google Scholar
Kuenen, Ph. H., 1958. Problems concerning the source and transportation of Flysch sediments. Geol. en Minjb. (N.S.), 20 e, 329–339.Google Scholar
McKie, D., and Burke, K. C., 1955. The geology of the Islands of South Connemara. Geol. Mag., 92, 487.CrossRefGoogle Scholar
Sanders, J. E., 1960. Origin of convoluted laminae. Geol. Mag., 97, 409.CrossRefGoogle Scholar
Wood, A., and Smith, A. J., 1959. Sedimentation and sedimentary history of the Aberystwyth Grits. Quart. J. geol. Soc. Lond., 114, 163.CrossRefGoogle Scholar