Szczegóły publikacji
Opis bibliograficzny
Two garnet growth events in polymetamorphic rocks in southwest Spitsbergen, Norway: insight in the history of Neoproterozoic and early Paleozoic metamorphism in the High Arctic / Jarosław MAJKA, Karolina KOŚMIŃSKA, Stanisław Mazur, Jerzy CZERNY, Karsten Piepjohn, Maciej DWORNIK, Maciej MANECKI // Canadian Journal of Earth Sciences ; ISSN 0008-4077. — 2015 — vol. 52 iss. 12, s. 1045–1061. — Bibliogr. s. 1060–1061, Abstr., Rés. — Publikacja dostępna online od: 2015-12-23. — Jarosław Majka – dod. afiliacja: Uppsala University
Autorzy (7)
- AGHMajka Jarosław
- AGHKośmińska Karolina
- Mazur Stanisław
- AGHCzerny Jerzy
- Piepjohn Karsten
- AGHDwornik Maciej
- AGHManecki Maciej
Dane bibliometryczne
| ID BaDAP | 94787 |
|---|---|
| Data dodania do BaDAP | 2016-01-13 |
| DOI | 10.1139/cjes-2015-0142 |
| Rok publikacji | 2015 |
| Typ publikacji | artykuł w czasopiśmie |
| Otwarty dostęp |  |
| Czasopismo/seria | Canadian Journal of Earth Sciences = Revue Canadienne des Sciences de la Terre |
Abstract
Geochronological studies in northern Wedel Jarlsberg Land, southwestern Svalbard (Norway), showed that the Tonian (c. 950 Ma) igneous rocks were subjected to metamorphism during the Torellian (c. 640 Ma) and early Caledonian (470-460 Ma) events. Predominant augen gneisses, derived from a Tonian protolith, are intercalated in that area, with schists comprising two distinct metamorphic mineral assemblages. The M1 (Torellian) assemblage containing garnet-I + quartz + plagioclase-I + biotite-I + muscovite-I was formed under amphibolite-facies conditions at c. 550-600 degrees C and 5-8 kbar (1 kbar = 100 MPa). The M2 (Caledonian) assemblage comprising garnet-II + quartz + plagioclase-II + biotite-II + muscovite-II + zoisite + chlorite crystallized at c. 500-550 degrees C and 9-12 kbar, corresponding to epidote-amphibolite facies conditions. The M2 mineral assemblage constitutes the pervasive Caledonian fabric of the schists that was subsequently reactivated in a left-lateral strike-slip shear regime. The subsequent c. 70 degrees clockwise rotation of the original structure to its present position was caused by a large-scale passive rotation during the Paleogene Eurekan orogeny. The new pressure-temperature estimates suggest that metamorphic basement in the study area was consolidated during the Torellian middle-grade event and then overprinted by Caledonian moderate-to high-pressure subduction-related metamorphism. A following sinistral shear zone assembled the present structure of basement units. Our results pose a question about the possible extent of Torellian precursor to the Caledonian basement across the High Arctic and the scale of its subsequent involvement in early Caledonian subduction. In conjunction with previous studies, the results suggest a possible correlation between southwestern Spitsbergen and the Pearya Terrane in Ellesmere Island.
