Hostname: page-component-cd9895bd7-jkksz Total loading time: 0 Render date: 2024-12-28T03:34:20.469Z Has data issue: false hasContentIssue false
  • English
  • Français

Lower Tertiary Tholeiitic Basalts from Southern New Caledonia

Published online by Cambridge University Press:  05 July 2018

K. A. Rodgers
K. A. Rodgers*
Affiliation:
Department of Geology, University of Auckland, Auckland I, New Zealand
Get access Rights & Permissions [Opens in a new window]

Summary

Eocene tholeiitic basalts occur throughout the length of New Caledonia where their emplacement preceded that of the peridotite massifs. In the south, two areas of basaltic rocks are intimately associated with Eocene sediments, which have been overridden by the peridotites. The aphyric, holocrystalline basalts consist of plagioclase, clinopyroxene, titanomagnetite, and minor quartz together with their abundant alteration products, which include epidote and uralite. The chemical compositions of these rocks fail to show agreement with oceanic tholeiitites, as suggested by earlier writers, although strong similarities exist with the basalts of the Papuan Ultramafic Belt.

Type
Research Article
Information
Mineralogical Magazine , Volume 40 , Issue 309 , March 1975 , pp. 25 - 32
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1975

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

Avias, (J.), 1955. Sciences Terre, No. hors serie, 213-34.Google Scholar
Avias, (J.), 1956a. Compt. Rend. Séanc. Soc. géol. Fr. 16, 307.Google Scholar
Avias, (J.), 1956b. Rep. 2oth Internat. Geol. Congr., part 8.Google Scholar
Brothers, (R. N.) and Blake, (M. C.), 1973. Tectonophysics, 17, 337-58.CrossRefGoogle Scholar
Burns, (R. E.) and Andrews, (J. E.), 1973. Initial reports of the Deep Sea Drilling projects, Leg 21, Washington, U.S. Government Printing Office.CrossRefGoogle Scholar
Cann, (J. R.), 1971. Phil. Trans. Roy. Soc. 268A, 495-505.CrossRefGoogle Scholar
Challis, (G. A.) and Guillon, (J. H.), 1971. Bull. Bur. Réch. min (Deuxieme Serie), Section IV, No. 2, (1971), 39-46.Google Scholar
Crenn, (Y.), 1953. Annls. Gdophys. 9, 291-9.Google Scholar
Davies, (H. L.), 1968. Rep. 23rd Internat. Geol. Congr. part 1, 209-20.Google Scholar
Davies, (H. L.), 1971. Bull. Bur. Miner. Resour. Geol. Geophys. Aust. 128, 48 p.Google Scholar
Engel, (A. E. J.), Engel ((2. G.), and Havens, (R. G.), 1965. Bull. GeoL Soc. Amer. 76, 719-34.CrossRefGoogle Scholar
Espirat, (J. J.), 1963. Etude géologique de regions de la Nouvelle Calédonie septentrionale. Clermont thesis (unpublished).Google Scholar
Fromager, (D.), Gonord, (H.), and Guillon, (J. H.), 1967. Compt. Rend. Sdanc. Soc. géol Fr. 6, 242.Google Scholar
Guillon, (J. H.), 1969. Cahiers O.R.S.T.O.M., serie Géol. 1, 7–26.Google Scholar
Guillon, (J. H.), and Gonord, (H.), 1972. Compt. Rend. Séanc. Acad. Sci. Paris, 275D, 309-12.Google Scholar
Guillon, (J. H.), and Routnier, (P.), 1971. Bull. Bur. Réch. min. (Deuxieme Serie), Section IV, No. 2 (1971), 5-38.Google Scholar
Harpum, (J. R.), 1954. Bull. Geol. Soc. Amer. 65, 1075-92.CrossRefGoogle Scholar
Hayatsu, (A.) and Carmicrtael, (C. M.), 1970. Earth Planetary Sci. Letts, 8, 71-6.CrossRefGoogle Scholar
Oliver, (T. A.), 1951. Amer. Min. 36, 421-9.Google Scholar
Rodgers, (K. A.), 1973. Geol. Mag. 110, 125-31.CrossRefGoogle Scholar
Rodgers, (K. A.), 1974. A comparison of the ultramafic belts of Papua and New Caledonia. (In press, Journ. Geol.). Google Scholar
Routitier, (P.), 1953. Mem. Soc. géol. Fr. 67, 271 p.Google Scholar
Thayer, (T. P.), 1967. In Wyllie, P. J. (ed.), Ultramafic and Related Rocks. New York (Wiley).Google Scholar
Tissot, (B.) and Noesman, (A.), 1958. Inst. Ft. Pdtrole Rev. 13, 739-59.Google Scholar