Comment on: 'A late Pleistocene clockwise rotation phase of Zakynthos (Greece) and implications for the evolution of the western Aegean Arc'
Publication date
2001-01-17
Authors
Duermeijer, C.E.
Krijgsman, W.
Langereis, C.G.
Meulenkamp, J.E.
Triantaphyllou, M.V.
Zachariasse, W.J.
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Abstract
In a recent paper, Duermeijer et al. [1] report
new palaeomagnetic results from the island of Zakynthos
(Greece). In many cases, these authors
have re-sampled the original sites of Laj et al.
[2] and the results are virtually identical to those
of the earlier study except for much more precise
biostratigraphic age control. Three middle Pleistocene
sites (Bochali, Zakynthos town and Porto
Roma) which were not sampled by Laj et al.
document signi¢cant clockwise rotations. From
the results obtained from these three new sites,
the authors conclude that the 25° clockwise rotation
of Zakynthos described by Laj et al. as affecting
the entire western Hellenic margin more or
less progressively over the last 5 Myr is much
more recent (early Pleistocene).