TY - DATA T1 - Late Cambrian–Ordovician northeastern Gondwanan terranes in the basement of the Apuseni Mountains, Romania PY - 2016/06/21 AU - I. Balintoni AU - C. Balica AU - M.N. Ducea AU - L. Zaharia AU - Fukun Chen AU - M. Cliveţi AU - H.P. Hann AU - Li-Qiu Li AU - L. Ghergari UR - https://geolsoc.figshare.com/articles/dataset/Late_Cambrian_Ordovician_northeastern_Gondwanan_terranes_in_the_basement_of_the_Apuseni_Mountains_Romania/3454886 DO - 10.6084/m9.figshare.3454886.v1 L4 - https://ndownloader.figshare.com/files/5427212 L4 - https://ndownloader.figshare.com/files/5427215 L4 - https://ndownloader.figshare.com/files/5427218 L4 - https://ndownloader.figshare.com/files/5427221 L4 - https://ndownloader.figshare.com/files/5427224 L4 - https://ndownloader.figshare.com/files/5427227 KW - Apuseni Mountains KW - magmatic zircon populations KW - Baia KW - Detrital zircon ages KW - Ma KW - terrane KW - Arie KW - Geology N2 - The pre-Alpine basement of the Apuseni Mountains (Romanian Carpathians) comprises three terranes: Someş, Baia de Arieş and Biharia. Metaigneous rocks within these terranes record Late Cambrian–Ordovician U–Pb zircon crystallization ages. Two samples from an orthogneiss layer in the Someş terrane yielded an age of 459.8 ± 2.7 Ma. In the Baia de Arieş terrane, an augen gneiss yielded an age of 470.8 ± 3.8 Ma, a porphyroid yielded an age of 467.8 ± 3.8 Ma and two metagranites yielded ages of 467.8 ± 4.7 Ma and 467.1 ± 3.9 Ma, respectively. Three samples from a metagranitoid outcrop located in the lower part of the Biharia terrane yielded an age of 495.0 ± 2.1 Ma. Three other samples from a metabasite layer situated lithostratigraphically several hundred metres above the metagranitoid yielded an age of 477.8 ± 3.2 Ma. Detrital U/Pb zircon ages from a paragneiss interlayered within the Baia de Arieş terrane scatter between 548 and 3518 Ma. Detrital zircon ages together with the inherited ages recorded by magmatic zircon populations suggest a northeastern Gondwanan provenance for the Someş, Baia de Arieş and Biharia terranes, adjacent to the Arabian–Nubian Shield. Lead loss in some zircons is interpreted to have taken place during the Variscan orogeny. ER -