TY - JOUR AU - Karipi, S. AU - Tsikouras, B. AU - Hatzipanagiotou, K. PY - 2007/01/01 Y2 - 2024/03/28 TI - PETROLOGY AND GEOCHEMISTRY OF GRANITIC PEBBLES IN THE PARNASSOS FLYSCH AT ITI MOUNTAIN, CONTINENTAL CENTRAL GREECE JF - Bulletin of the Geological Society of Greece JA - geosociety VL - 40 IS - 2 SE - Mineralogy-Petrology-Geochemistry-Economic Geology DO - 10.12681/bgsg.16724 UR - https://ejournals.epublishing.ekt.gr/index.php/geosociety/article/view/16724 SP - 816-828 AB - <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> ER -