Detrital zircon U-Pb-Hf isotope signatures of Old Red Sandstone strata constrain the Silurian to Devonian paleogeography, tectonics, and crustal evolution of the Svalbard Caledonides

Luke P. Beranek, David G. Gee, Christopher M. Fisher

Research output: Contribution to journalArticlepeer-review

11 Citations (Scopus)

Abstract

Detrital zircon provenance studies of Mesoproterozoic basement and overlying Old Red Sandstone strata in northwestern Svalbard, Arctic Norway, were conducted to test competing models for Caledonian paleogeography and tectonics and constrain the magnitude of orogen-parallel, Silurian to Devonian strike-slip faulting following the Laurentia-Baltica collision. Mesoproterozoic basement strata, cut by earliest Tonian orthogneiss units, mostly yielded 1640-1050 Ma detrital zircon populations that are consistent with pre-Caledonian locations near northeast Greenland. Basal Old Red Sandstone deposits that filled pull-apart basins showed basement- derived signatures but also contained 530-450 Ma and 670-570 Ma populations with slightly subchondritic (εHf[t] = -4 to -2) Hf isotope compositions. These results are consistent with late Silurian-Early Devonian proximity to the northeast Greenland Caledonides and Pearya, which indicates limited (600 m.y. crustal residence times.
Original languageEnglish
Pages (from-to)1987-2003
Number of pages17
JournalBulletin of the Geological Society of America
Volume132
Issue number9-10
DOIs
Publication statusPublished - 1 Sep 2020
Externally publishedYes

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