First age dating of the Lydian stones in the Inner Hellenides (Mount Parnis, Greece); geological significances.

Citation
M. Caridroit et al., First age dating of the Lydian stones in the Inner Hellenides (Mount Parnis, Greece); geological significances., CR AC S IIA, 331(6), 2000, pp. 413-418
Citations number
13
Categorie Soggetti
Earth Sciences
Journal title
COMPTES RENDUS DE L ACADEMIE DES SCIENCES SERIE II FASCICULE A-SCIENCES DELA TERRE ET DES PLANETES
ISSN journal
12518050 → ACNP
Volume
331
Issue
6
Year of publication
2000
Pages
413 - 418
Database
ISI
SICI code
1251-8050(20000930)331:6<413:FADOTL>2.0.ZU;2-H
Abstract
Using radiolarian and conodont remains, a Tournaisian age has been obtained from the Lydian rocks (or lydites) of the Parnis Mount (Greece); this resu lt is the first direct age dating of the Lydian rocks of continental Greece . In the same area, some limestone strata, interbedded in sandstones, yield Carboniferous and Permian foraminifers; the established stratigraphy is no t consistent and so, the Lydian rocks have to be considered as blocks in an olistostrome unconformably overlain or thrusted by Triassic limestones. Ot herwise, the Lydian rocks are interpreted as biogenic siliceous deposits du e to the absence of carbonate sedimentation (not as a high siliceous produc tion). (C) 2000 Academie des sciences / Editions scientifiques et medicales Elsevier SAS.