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The (?) mid Triassic volcanic rocks of Lakonia, Greece

Published online by Cambridge University Press:  01 May 2009

G. Pe-Piper ,
A. G. Panagos ,
D. J. W. Piper  and
C. N. Kotopouli
G. Pe-Piper
Affiliation:
Geological Laboratory, University of Patras, Patras, Greece
A. G. Panagos
Affiliation:
Geological Laboratory, University of Patras, Patras, Greece
D. J. W. Piper
Affiliation:
Geological Laboratory, University of Patras, Patras, Greece
C. N. Kotopouli
Affiliation:
Geological Laboratory, University of Patras, Patras, Greece
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Summary

Thick subaerial volcanic sequences of probable mid Triassic age rest unconformably on Permo-Carboniferous limestones in the ‘Phyllite Series’ within the Gavrovo-Tripolitsa zone of the external Hellenide nappes. The volcanic rocks are varied in character. Pyroclastic rocks (often reddened) predominate, but minor basalt or andesite and rhyolitic hypabyssal intrusions and flows are also found. The rocks have experienced low-grade metamorphism and the only relict primary minerals are pyroxene and rare plagioclase in basic rocks and potash feldspar in acid rocks. The most important metamorphic phases are albite, chlorite, potassium mica, epidote, hematite, quartz and pumpellyite. Twenty-seven whole-rock major-element analyses suggest that there has been some exchange of Na2O and K2O for CaO during metamorphism, but that other elements have been relatively stable. A genetic interpretation of the rocks is attempted using published geochemical discriminator diagrams. The basic rocks are tholeiitic in major element chemistry and pyroxene composition. Trace element (Hf, Ta, Th, Ce, Yb) distribution suggests magma generation at a destructive plate margin.

Type
Articles
Information
Geological Magazine , Volume 119 , Issue 1 , January 1982 , pp. 77 - 85
Copyright
Copyright © Cambridge University Press 1982

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