Hostname: page-component-5c6d5d7d68-wbk2r Total loading time: 0 Render date: 2024-08-23T05:27:24.496Z Has data issue: false hasContentIssue false

Evidence of co-genesis of the Troodos Lavas, Cyprus

Published online by Cambridge University Press:  01 May 2009

A. P. Desmet
Affiliation:
Laboratoire de Pétrologie, Université de Nancy, France

Summary

Petrological and geochemical features of recently discovered basalts of the Troodos Massif, Cyprus — a dyke in the Basal Group and altered pillow lavas in the Lower Pillow Lavas — suggest that all the lavas are part of a single volcanic suite.

Type
Articles
Copyright
Copyright © Cambridge University Press 1976

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

Bear, L. M. 1959. Useful criteria for distinguishing between the Upper and Lower Pillow Lavas and the Pillow Lavas of the Basal Group. In Ingham, F. T.: Cyprus Annual Report for the Year 1958, pp. 1214. Geological Survey Department, Nicosia.Google Scholar
Bishopp, D. W. 1958. Ultrabasic pillow lavas from Cyprus. Geol. Mag. 95, 436–8.CrossRefGoogle Scholar
Desmet, A. P. 1973. Aperçu sur l'évolution générale des Pillow lavas du Troodos (Chypre). Réunion annuelle des Sciences de la Terre. Résumé Soc. Geol. France, Paris, p. 165.Google Scholar
Gass, I. G. 1958. Ultrabasic pillow lavas from Cyprus. Geol. Mag. 95, 241–51.CrossRefGoogle Scholar
Gass, I. G. 1960. The geology and mineral resources of the Dhali area, Cyprus. Mem. geol. Surv. Cyprus 4, 116 pp.Google Scholar
Gass, I. G. & Smewing, J. D. 1973. Intrusion, Extrusion and Metamorphism at constructive margins: Evidence from the Troodos Massif, Cyprus. Nature, Lond. 242, 26–9.CrossRefGoogle Scholar
MacDonald, G. A. & Katsura, T. 1964. Chemical composition of Hawaiian lavas. J. Petrology 5, 82133.CrossRefGoogle Scholar
Mantis, M. 1971. Paleontological evidence defining the age of the Troodos Pillow Lavas Series in Cyprus. Kypriakos Logos, Nicosia.Google Scholar
Miyashiro, A. 1973. The Troodos ophiolitic complex was probably formed in an island arc. Earth Planet. Sci. Letts, 19, 218–24.CrossRefGoogle Scholar
Parrot, J. F. 1974. Les différentes manifestations effusives de la région ophiolitique du Baër Bassit (N-O de la Syrie). Comparaison pétrographique et geochimique. C. R. Acad. Sci. Paris D 279, 627–30.Google Scholar
Pearce, J. A. 1975. Basalt geochemistry used to investigate past tectonic environments on Cyprus. Tectonophysics 25, 4167.CrossRefGoogle Scholar
Searle, D. I. & Vokes, P. M. 1969. Layered ultrabasic lavas from Cyprus. Geol. Mag. 106, 515–30.CrossRefGoogle Scholar