U/Pb and Pb/Pb zircon ages for arc‐related intrusions of the Bolu Massif (W Pontides, NW Turkey): evidence for Late Precambrian (Cadomian) age

Abstract We present new U/Pb and Pb/Pb radiometric age data from two tectono‐stratigraphic units of the regionally extensive Bolu Massif, in the W Pontides (İstanbul Fragment), N Turkey. A structurally lower unit (Sünnice Group) is cut by small meta‐granitic intrusions, whereas the structurally higher unit comprises meta‐volcanic rocks (Çaşurtepe Fm) cut by meta‐granitic plutons (Tüllükiriş and Kapıkaya plutons). U/Pb single‐crystal dating of zircons from the Kapıkaya Pluton yielded a concordant cluster, with a mean 238 U/ 206 Pb age of 565.3 ± 1.9 Ma. Zircons from the Tüllükiriş Pluton (affected by Pb loss) gave a 207 Pb/ 206 Pb age of 576 ± 6 Ma age (Late Precambrian). Small meta‐granitic intrusions cutting the Sünnice Group yielded a less precise 207 Pb/ 206 Pb age of 262 ± 19 Ma (Early Permian). The older ages from the Bolu Massif confirm the existence of latest Precambrian arc magmatism related to subduction of a Cadomian ocean. We infer that the Bolu Massif represents a fragment of a Cadomian active margin. Cadomian orogenic units were dispersed as exotic terranes throughout the Variscan and Tethyan orogens, and the Bolu Massif probably reached its present position prior to latest Palaeozoic time. Our dating results also confirm that NW Turkey was affected by Hercynian magmatism related to subduction of Palaeotethys, as inferred for other areas of the Pontides.