Author:
DANELIAN TANIEL,ROBERTSON ALASTAIR H. F.
Abstract
This paper presents new radiolarian biostratigraphic and igneous/metamorphic geochemical
data for a Mesozoic volcanic–sedimentary mélange on the island of Evia (Euboea or Evvoia), eastern
Greece. This mélange includes dismembered thrust sheets and blocks of radiolarian chert and basalt.
Biostratigraphic age data show that radiolarites interbedded with basalt-derived, coarse clastic sediments
near the base of a coherent succession were deposited in Middle and Late Triassic time (Late
Ladinian–Carnian, Norian?). Geochemical evidence shows that associated extrusive rocks, of inferred
Triassic age, range from ‘enriched’ alkaline basalts, to ‘transitional’ basalts, and more ‘depleted’ mid-ocean
ridge-type basalts. Amphibolite facies meta-basalts from the metamorphic sole of the over-riding
Evia ophiolite exhibit similar chemical compositions. Both the basalts and the meta-basalts commonly
show an apparent subduction-related influence (e.g. relative Nb depletion) that may have been inherited
from a previous subduction event in the region. The basalts are interpreted to have erupted during
Middle–Late Triassic time (Late Ladinian–Carnian), related to initial opening of a Neotethyan ocean
basin adjacent to a rifted continental margin. Radiolarites located stratigraphically higher in the coherent
succession studied are dated as Middle Jurassic (Late Bathonian–Early Callovian). Similar-aged
radiolarites are depositionally associated with ophiolitic rocks (including boninites), in some other areas
of Greece and Albania. During initial ocean basin closure (Bajocian–Bathonian) the adjacent shallow-water
carbonate platform (Pelagonian zone) disintegrated to form basins in which siliceous sediments
were deposited and highs on which shallow-water carbonates continued to accumulate. This facies differentiation
is seen as a response to crustal flexure as the Neotethyan ocean began to close. The over-riding
Pagondas Mélange and other similar units in the region are interpreted as accretionary prisms related to
subduction of Neotethyan oceanic crust in Middle–Late Jurassic time. These mélanges were emplaced,
probably diachronously during Oxfordian–Kimmeridgian time, when the passive margin collapsed,
creating a foredeep ahead of advancing thrust sheets of mélange and ophiolites.
Publisher
Cambridge University Press (CUP)
Cited by
48 articles.
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