Hostname: page-component-cd9895bd7-7cvxr Total loading time: 0 Render date: 2024-12-24T02:13:00.377Z Has data issue: false hasContentIssue false

The Ordovician Rocks of New Zealand

Published online by Cambridge University Press:  01 May 2009

Extract

Throughout the western portion of the South Island of New Zealand there extends a series of high ranges made up very largely of unfossiliferous greywacke and argillite, with rarely limestone. Parts of these formations have been variously grouped as the Aorere and Mount Arthur series and considered to be of Ordovician age.

Type
Original Articles
Copyright
Copyright © Cambridge University Press 1936

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

Literature Cited

Benson, W. N., and Bartrum, J. A., 1935. “The Geology of the Region about Preservation and Chalky Inlets, Southern Fiordland, N.Z. Part 3: Petrology”, Trans. Roy. Soc. N.Z., 65, 108152.Google Scholar
Trans. Roy. Soc. N.Z. Benson, W. N., and Keble, R. A., 1935., Part 4: “Stratigraphy and Palaeontology of the Fossiliferous Ordovician Rocks” 244294.Google Scholar
Trans. Roy. Soc. N.Z. Benson, W. N., and Keble, R. A., 1936. (With King, L. C., and Mckee, J. T.) “The Ordovician Graptolites of North-west Nelson, N.Z.” 357382.Google Scholar
Trans. Roy. Soc. N.Z. Chapman, F., 1934. “On some Brachiopods from the Ordovician of Preservation Inlet, New Zealand” Trans. Roy. Soc. N.Z., 64, 115–16.Google Scholar
Trans. Roy. Soc. N.Z. Chapman, F., 1934 a. “On some Phyllocarids from the Ordovician of Preservation Inlet, New Zealand,” Trans. Roy. Soc. N.Z., 105114.Google Scholar
Clarke, E. de c., 1907. (In Bell, J. M., and others.) “The Geology of the Parapara Subdivision,” Bull. Geol. Surv. N.Z., No. 3, 3537.Google Scholar
Elles, G. L., 1925. “The Characteristic Assemblages of the Graptolite Zones of the British Isles,” Geol. Mag., 62, 337347.CrossRefGoogle Scholar
Elles, G. L., 1932. (In David, Sir T. W. E.) Explanatory notes to accompany a new Geological Map of the Commonwealth of Australia, Sydney, p. 40.Google Scholar
Elles, G.L., 1933. “Lower Ordovician Graptolite Faunas with special reference to the Skiddaw Slate,” Geol. Surv. Gt. Brit., Summary of Progress, 1932, pt. 2, 94198.Google Scholar
Hall, T. S., 1894. “Notes on the Distribution of Graptolites in the Rocks of Castlemaine,” Aust. Assoc. Adv. Science, 4, 374–6.Google Scholar
Hall, T. S., 1915. “On the Occurrence of Lower Ordovician Graptolites in Western Otago,” Trans. N.Z. Inst., 47, 410–11.Google Scholar
Trans. N.Z. Inst. Hall, T. S., 1915 a. “The Golden Ridge Graptolites,” Trans. N.Z. Inst., 411–12.Google Scholar
Harris, W. J., 1935. “The Graptolite Succession of Bendigo East with suggested Zoning,” Proc. Roy. Soc. Vict., 47, 314337.Google Scholar
Harris, W. J., and Keble, R. A., 1932. “Victorian Graptolite Zones with Correlations and Descriptions of New Species,” Proc. Roy. Soc. Vict., 44, 2548.Google Scholar
Keble, R. A., 1927. “Graptolites from Cape Providence, Chalky Inlet, Southland,” Trans. N.Z. Inst., 58, 157–9.Google Scholar
Trans. N.Z. Inst. Keble, R. A., and Benson, W. N., 1929. “Ordovician Graptolites of North-West Nelson, N.Z.,” Trans. N.Z. Inst., 59, 840863.Google Scholar
Kobayashi, T., 1934. “The Cambro-Ordovician Formations and Faunas of Southern Chosen: Part I,” Journ. Fac. Sci. Imp. Univ. Tokyo, 3, pt. 8, 470, 486.Google Scholar
Reed, F. R. C., 1927. “New Trilobites from the Ordovician Beds of New Zealand,” Trans. N.Z. Inst., 57, 310–14.Google Scholar
Shakespear, E. M. R., 1908. “On Some New Zealand Graptolites,” Geol. Mag., 145–8.CrossRefGoogle Scholar
Thomas, D. E., 1935. “Cambrian and Ordovician” (in Outline of the Physiography and Geology of Victoria). Handbook for Victoria, Melbourne meeting, Aust. and N.Z. Assoc. Adv. Science, pp. 96105.Google Scholar
Thomas, D. E., and Keble, R. A., 1933. “The Ordovician and Silurian of the Bulla-Sunbury Area, and discussion of the Sequence of the Melbourne Area,” Proc. Roy. Soc. Vict., 45, 4956.Google Scholar