Anorthosite formation and emplacement coupled with differential tectonic exhumation of ultrahigh-temperature rocks in a Sveconorwegian continental back-arc setting

• Published in: Precambrian research Vol. 376; p. 106695
• Main Authors: Slagstad, Trond, Henderson, Iain H.C., Roberts, Nick M.W., Kulakov, Evgeniy V., Ganerød, Morgan, Kirkland, Christopher L., Dalslåen, Bjørgunn, Creaser, Robert A., Coint, Nolwenn
• Format: Journal Article
• Language: English; Norwegian
• Published: Elsevier B.V 15.07.2022
• Subjects: Bjerkreim–Sokndal layered intrusion; Extensional detachment; Rogaland Anorthosite Province; Sveconorwegian Orogen; Thermo-rheological modeling; Extensional detachment; Sveconorwegian Orogen; Bjerkreim–Sokndal layered intrusion; Thermo-rheological modeling; Rogaland Anorthosite Province
• ISSN: 0301-9268; 1872-7433
• DOI: 10.1016/j.precamres.2022.106695

•The Rogaland Anorthosite complex took about 100 Myr to form.•Anorthosite emplacement involved different processes in an evolving stress regime.•The distribution of UHT rocks reflects differential tectonic exhumation.•At no point during orogeny did the crust in the study area thicken significantly.•Long-lived extension was interrupted by intermittent compression. The tectonic setting and mechanisms and duration of emplacement of Proterozoic massif-type anorthosites and the significance of typically associated ultrahigh-temperature (UHT) host rocks have been debated for decades. This is particularly true of the Rogaland Anorthosite Province (RAP) in the SW Sveconorwegian Orogen. Earlier studies suggest that the RAP was emplaced over 1–3 Myr around 930 Ma towards the end of orogenesis, resulting in an up to 15–20 km-wide contact metamorphic aureole. However, our structural observations show that the RAP is located in the footwall of a 15 km-wide extensional detachment (Rogaland Extensional Detachment, RED), separating the intrusions and their UHT host rocks from weakly metamorphosed rocks in the hanging wall. U–Pb zircon dating of leucosome in extensional pull-aparts associated with the RED yields ages of 950–935 Ma, consistent with Re–Os molybdenite ages from brittle extensional structures in the hanging-wall block that range between 980 and 930 Ma. A metapelite in the immediate vicinity of the RAP yields a 950 Ma U–Pb age of matrix-hosted monazite, and part of the RAP was intruded by the Storgangen norite dike at ca. 950 Ma, providing a minimum age of emplacement. These ages are consistent with Ar–Ar hornblende and biotite ages that show rapid cooling of the footwall before 930 Ma, but slow cooling of the hanging wall. Field and geochronologic data suggest that the RAP formed and was emplaced over a long period of time, up to 100 Myr, with different emplacement mechanisms reflecting an evolving regional stress regime. The distribution of UHT rocks around the RAP reflects differential extensional exhumation between 980 and 930 Ma, not contact metamorphism. The duration and style of orogenic activity and externally (as opposed to gravitationally) driven extension suggest that the RAP formed in a continental back-arc setting.