@article{Karipi_Tsikouras_Hatzipanagiotou_2007, title={PETROLOGY AND GEOCHEMISTRY OF GRANITIC PEBBLES IN THE PARNASSOS FLYSCH AT ITI MOUNTAIN, CONTINENTAL CENTRAL GREECE}, volume={40}, url={https://ejournals.epublishing.ekt.gr/index.php/geosociety/article/view/16724}, DOI={10.12681/bgsg.16724}, abstractNote={<p><em>Granite rocks occur as pebbles within the Parnassos flysch deposits, in the area of Iti (Central Greece). The granites are per aluminous, calcic rocL· with S-type characteristics. Geochemical features reveal that these rocL· are not co-genetic to the Iti ophiolite but they have been derived from magmas affected by a subduction component. They display common characteristics with VAG-type lithologies. Geochemically, they mostly resemble nearby granite clastsfrom a Triassic flyschoid from Evia (Liri Unit), and lesser those within the Parnassos flysch at Amfissa and Pliocene fluvial deposits at Patras</em></p>}, number={2}, journal={Bulletin of the Geological Society of Greece}, author={Karipi, S. and Tsikouras, B. and Hatzipanagiotou, K.}, year={2007}, month={Jan.}, pages={816–828} }