Bulletin of the Geological Society of Greece Vol. 40, 2007 PETROLOGY AND GEOCHEMISTRY OF GRANITIC PEBBLES IN THE PARNASSOS FLYSCH AT ITI MOUNTAIN, CONTINENTAL CENTRAL GREECE Karipi S. University ofPatras, Department of Geology, Section of Earth Materials Tsikouras B. University ofPatras, Department of Geology, Section of Earth Materials Hatzipanagiotou K. University ofPatras, Department of Geology, Section of Earth Materials https://doi.org/10.12681/bgsg.16724 Copyright © 2018 S. Karipi, B. Tsikouras, K. Hatzipanagiotou To cite this article: Karipi, S., Tsikouras, B., & Hatzipanagiotou, K. (2007). PETROLOGY AND GEOCHEMISTRY OF GRANITIC PEBBLES IN THE PARNASSOS FLYSCH AT ITI MOUNTAIN, CONTINENTAL CENTRAL GREECE. Bulletin of the Geological Society of Greece, 40(2), 816-828. doi:https://doi.org/10.12681/bgsg.16724 http://epublishing.ekt.gr | e-Publisher: EKT | Downloaded at 21/02/2020 05:34:34 | Δελτίο της Ελληνικής Γεωλογικής Εταιρίας τομ. ΧΧΧΧ, Bulletin of the Geological Society of Greece vol. XXXX, 2007 2007 Proceedings of the 11th International Congress, Athens, May, Πρακτικά 11ου Διεθνούς Συνεδρίου, Αθήνα, Μάιος 2007 2007 PETROLOGY AND GEOCHEMISTRY OF GRANITIC PEBBLES IN THE PARNASSOS FLYSCH AT ITI MOUNTAIN, CONTINENTAL CENTRAL GREECE Karipi S.1, Tsikouras B.1, and Hatzipanagiotou K.1 / University ofPatras, Department of Geology, Section of Earth Materials, GR-26 500 Patras, Greece,
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[email protected] Abstract 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 char acteristics. 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 compo nent.