Skip to main content
Log in

The geochemistry of the Dunedin Volcano, East Otago, New Zealand: Rare earth elements

  • Published:
Contributions to Mineralogy and Petrology Aims and scope Submit manuscript

Abstract

A variety of alkaline lavas from the Dunedin Volcano have been analyzed for the rare earth elements (REE) La-Yb. The compositions analyzed were: basalt-hawaiite-mugearite-benmoreite; basanite, nepheline hawaiite, nepheline trachyandesite and nepheline benmoreite; trachyte; phonolite. The series from basalt to mugearite shows continuous enrichment in the REE, consistent with a crystal fractionation model involving removal of olivine and clinopyroxene. From mugearite to benmoreite there is a depletion in the REE which is explained by the appearance of apatite as a liquidus phase. The chondrite normalized REE patterns for the phonolites are characterized by strong enrichment and fractionation coupled with a sharp depletion in Eu. Removal of plagioclase from benmoreite magma is suggested for the derivation of the phonolites. The series basanite-nepheline hawaiite, and basanite-nepheline hawaiite-nepheline benmoreite appear to be high pH2O analogues of the series basalt-ben-moreite, with enrichment of the REE being achieved by removal of clinopyroxene, kaersutite and olivine. Compared with other lavas the trachyte has low REE abundances and is characterized by a striking positive Eu anomaly.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Institutional subscriptions

Similar content being viewed by others

References

  • Benson, W. N.: Mineralogical notes from the University of Otago, N. Z. No. 3. Trans. Roy. Soc. New Zealand 69, 283–308 (1939).

    Google Scholar 

  • Benson, W. N.: Cainozoic petrographic provinces in New Zealand and their residual magmas. Am. J. Sci. 239, 537–552 (1941 a).

    Google Scholar 

  • Benson, W. N.: The basic igneous rocks of Eastern Otago and their tectonic environment. Part I. Trans. Roy. Soc. New Zealand 71, 208–222 (1941 b).

    Google Scholar 

  • Benson, W. N.: The basic igneous rocks of Eastern Otago and their tectonic environment. Part II. Trans. Roy. Soc. New Zealand 72, 85–118 (1942a).

    Google Scholar 

  • Benson, W. N.: The basic igneous rocks of Eastern Otago and their tectonic environment. Part III. Trans. Roy. Soc. New Zealand 72, 160–185 (1942b).

    Google Scholar 

  • Benson, W. N., Turner, F. J.: Mineralogical notes from the University of Otago, N.Z. No. 2. Trans. Roy. Soc. New Zealand 69, 56–72 (1939).

    Google Scholar 

  • Coombs, D. S.: Dunedin Volcanic Complex and Waipiata Volcanic Formation. N.Z. Dept. Sci. Indus. Res. Information Series No. 51, 54–67 (1965).

    Google Scholar 

  • Coombs, D. S., White, A. J. R., Hamilton, D.: Age relations of the Dunedin Volcanic Complex and some palaeogeographic implications. New Zealand J. Geol. Geophys. 3, 325–336, 572–579 (1960).

    Google Scholar 

  • Coombs, D. S., Wilkinson, J. F. G.: Lineages and fractionation trends in unsaturated volcanic rocks from the East Otago Volcanic Province (New Zealand) and related rocks. J. Petrol. 3, 440–501 (1969).

    Google Scholar 

  • Flower, M. F. J.: Rare earth element distribution in lavas and ultramafic xenoliths from the Comores Archipelago, Western Indian Ocean. Contr. Mineral. and Petrol. 31, 335–346 (1971).

    Google Scholar 

  • Gill, R. C. O.: Chemistry of peralkaline dykes from the Grønnedal-Ika area, South Greenland. Contr. Mineral. and Petrol. 34, 87–100 (1972).

    Google Scholar 

  • Green, D. H.: Composition of basaltic magmas as indicators of conditions of origin: application to oceanic volcanism. Phil. Trans. Roy. Soc. London, Ser. A 268, 707–725 (1971).

    Google Scholar 

  • Gunn, B. M.: The fractionation effect of kaersutite in basaltic magmas. Can. Mineralogist 11, 840–850 (1972).

    Google Scholar 

  • Haskin, L. A., Frey, F. A., Schmidt, R. A., Smith, R. H.: Meteoritic, solar and terrestrial rare earth distributions. Phys. Chem. Earth 7, 167–321 (1966).

    Google Scholar 

  • Kesson, S., Price, R. C.: The major and trace element chemistry of kaersutite and its bearing on the petrogenesis of alkaline rocks. Contr. Mineral. and Petrol. 35, 119–124 (1972).

    Google Scholar 

  • Marshall, P.: The geology of Dunedin (New Zealand). Quart. J. Geol. Soc. Lond. 62, 381–422 (1906).

    Google Scholar 

  • Marshall, P.: The sequence of lavas at the North Head, Otago Harbour, Quart. J. Geol. Soc. Lond. 70, 382–408 (1914).

    Google Scholar 

  • Philpotts, J. A., Schnetzler, C. C.: Europium anomalies and the genesis of basalt. Chem. Geol. 3, 5–13 (1968).

    Google Scholar 

  • Reilly, W. I.: Gravitational expression of the Dunedin Volcano. New Zealand J. Geol. Geophys. 15, 16–21 (1971).

    Google Scholar 

  • Taylor, S. R.: Geochemical analysis by spark source mass spectrography. Geochim. Cosmochim. Acta 29, 1243–1261 (1965).

    Google Scholar 

  • Taylor, S. R.: Geochemical application of spark source mass spectrography—II. Photoplate data processing. Geochim. Cosmochim. Acta 35, 1187–1196 (1971).

    Google Scholar 

  • Ulrich, G. H. F.: On the occurrence of nepheline-bearing rocks in New Zealand. Rep. Australas. Ass. Advmt. Sci. 3, 127–150 (1891).

    Google Scholar 

Download references

Author information

Authors and Affiliations

Authors

Rights and permissions

Reprints and permissions

About this article

Cite this article

Price, R.C., Taylor, S.R. The geochemistry of the Dunedin Volcano, East Otago, New Zealand: Rare earth elements. Contr. Mineral. and Petrol. 40, 195–205 (1973). https://doi.org/10.1007/BF00373784

Download citation

  • Received:

  • Issue Date:

  • DOI: https://doi.org/10.1007/BF00373784

Keywords

Navigation