Browsing by Author "Boztug, D."
Now showing items 1-5 of 5
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Ar-40/Ar-39 geochronology and Sr-Pb isotopic evidence of post-collisional extensional volcanism of the eastern Pontide paleo-arc, NE Turkey
Arslan, M.; Boztug, D.; Temizel, I.; Kolayli, H.; Sen, C.; Abdioglu, E.; Ruffet, G.; Harlavan, Y. (PERGAMON-ELSEVIER SCIENCE LTD, 2007)… -
Geochemistry and K-Ar cooling ages of the Ilica, Cataldag (Balikesir) and Kozak (Izmir) granitoids, west Anatolia, Turkey
Boztug, D.; Harlavan, Y.; Jonckheere, R.; Can, I.; Sari, R. (JOHN WILEY & SONS LTD, 2009)The Ilica, Cataldag and Kozak granitoids, cropping out in the northern part ot the Izmir-Ankara (IA) suture zone in west Anatolia. Turkey, intrude metamorphic rocks of the Sakarya continent (SC) and Karakaya complex, and ... -
High-K, calc-alkaline I-type granitoids from the composite Yozgat batholith generated in a post-collisional setting following continent-oceanic island arc collision in central Anatolia, Turkey
Boztug, D.; Arehart, G. B.; Platevoet, B.; Harlavan, Y.; Bonin, B. (SPRINGER WIEN, 2007)The composite Yozgat batholith consists of a S-I-A-type granitoid association intruding the supra-subduction zone-type (SSZ-type) central Anatolian ophiolite and medium-to high-grade metasedimentary rocks of the central ... -
Timing of post-obduction granitoids from intrusion through cooling to exhumation in central Anatolia, Turkey
Boztug, D.; Jonckheere, R. C.; Heizler, M.; Ratschbacher, L.; Harlavan, Y.; Tichomirova, M. (ELSEVIER SCIENCE BV, 2009)The Middle to Late Cretaceous central Anatolian granitoids intrude the supra-subduction zone-type central Anatolian ophiolite and medium- to high-grade metasediments of central Anatolian crystalline complex and are overlain ... -
Titanite and zircon fission-track dating resolves successive igneous episodes in the formation of the composite Kackar batholith in the Turkish eastern Pontides
Boztug, D.; Jonckheere, R.; Wagner, G. A.; Ercin, A. I.; Yegingil, Z. (SPRINGER, 2007)The Kackar batholith in the Turkish eastern Pontides comprises several intrusive units with distinctive textural, mineralogical and geochemical characteristics. Their titanite and zircon fission-track ages confirm that the ...