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Geochemistry of amphibolitized eclogites and cross-cutting tonalitic–trondhjemitic dykes in the Metamorphic Kimi Complex in East Rhodope (N.E. Greece): implications for partial melting at the base of a thickened crust

Perdikatsis Vasilis, E. Mposkos, I. Baziotis

Απλή Εγγραφή


URIhttp://purl.tuc.gr/dl/dias/C136B696-AA65-4E8A-A4C1-AC017A811AE8-
Αναγνωριστικόhttp://link.springer.com/article/10.1007/s00531-007-0175-1-
Αναγνωριστικόhttps://doi.org/10.1007/s00531-007-0175-1-
Γλώσσαen-
Μέγεθος19 pagesen
ΤίτλοςGeochemistry of amphibolitized eclogites and cross-cutting tonalitic–trondhjemitic dykes in the Metamorphic Kimi Complex in East Rhodope (N.E. Greece): implications for partial melting at the base of a thickened crusten
ΔημιουργόςPerdikatsis Vasilisen
ΔημιουργόςΠερδικατσης Βασιληςel
ΔημιουργόςE. Mposkosen
ΔημιουργόςI. Baziotis en
ΕκδότηςSpringer Verlagen
ΠερίληψηIn the ultra-high pressure Metamorphic Kimi Complex widespread tonalitic–trondhjemitic dykes, with an intrusion age ca. 65–63 Ma, cross-cut boudins and layers of amphibolitized eclogites. Geochemical investigation proclaims the tied genetic relationship of the amphibolitized eclogites and the associated tonalitic–trondhjemitic dykes. The major and trace element contents and rare earth element patterns of the amphibolitized eclogites indicate formation of their protoliths by fractional crystallization of tholeiitic magmas in a back-arc environment. The tonalites and trondhjemites are characterized by moderate to high Sr contents (>130 ppm), and low Y (<8.2 ppm) and heavy rare earth element contents (Yb content of 0.19–0.88 ppm). The chemical composition of the tonalitic and trondhjemitic dykes are best explained by partial melting of a tholeiitic source like the amphibolitized eclogites with residual garnet and amphibole, at the base of a thickened crust during Early Tertiary subduction/accretion at the southern margins of the European continent.en
ΤύποςPeer-Reviewed Journal Publicationen
ΤύποςΔημοσίευση σε Περιοδικό με Κριτέςel
Άδεια Χρήσηςhttp://creativecommons.org/licenses/by/4.0/en
Ημερομηνία2015-12-02-
Ημερομηνία Δημοσίευσης2008-
Θεματική ΚατηγορίαRhodopeen
Θεματική Κατηγορία Kimi Complex en
Θεματική ΚατηγορίαUHPen
Θεματική ΚατηγορίαPartial melting en
Θεματική ΚατηγορίαTonalites–trondhjemites en
Θεματική ΚατηγορίαAmphibolitized eclogites en
Βιβλιογραφική ΑναφοράI. Baziotis, E. Mposkos, and V. Perdikatsis, "Geochemistry of amphibolitized eclogites and cross-cutting tonalitic–trondhjemitic dykes in the Metamorphic Kimi Complex in East Rhodope (N.E. Greece): implications for partial melting at the base of a thickened crust", Int. J. Earth Sci., vol. 97, no. 3, pp. 459-477, May 2008. doi:10.1007/s00531-007-0175-1en

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