The Mesoproterozoic Sveconorwegian orogeny: orogen scale interpretation of metamorphic and magmatic patterns supports an ultra-hot collision model

• Main Authors: Bernard Bingen, Giulio Viola, Charlotte Möller, Jacqueline Vander Auwera, Antonin Laurent, Jenny Andersson
• Format: Conference Object
• Language: English
• Published: 2018
• Subjects: Mesoproterozoic orogen; Sveconorwegian belt; Geochronology; Kongsberg; Fennoscandia
• Online Access: http://hdl.handle.net/11585/628700

The Sveconorwegian orogeny is a representative Grenvillian orogeny, involving multiphase reworking of the margin of Fennoscandia at the end of the Mesoproterozoic, between 1150 and 900 Ma. The asthenosphere was possibly c. 100C hotter than today, having a major impact on tectonic style in the lithosphere. Two geodynamic models compete: a collision between Fennoscandia and another continent to contribute to Rodinia assembly, versus an accretionary (tectonic switch) model at the margin of Fennoscandia. Here we provide an analysis of the structural, metamorphic and magmatic record across the entire Sveconorwegian orogenic belt, through time, supporting the collision model. Convergence-related metamorphism is observed in narrow belts, with increasingly high pressure signature eastwards, towards the (cratonic) Fennoscandia foreland, with time. Peak P-T-t conditions of 1.15 GPa - 850 C - 1145 Ma are recorded in the Bamble-Kongsberg Lithotectonic Units, 1.5 GPa - 740 C - 1046 Ma in the Idefjorden Unit, and 1.8 GPa - 870 C - 990 Ma in the Eastern Segment. Peak metamorphism is followed by isothermal decompression and partial melting. These events are attributed to the pull effect of delamination and foundering of the heavy continental lithospheric mantle in three steps towards the east. This delamination is paired with the formation of an orogenic plateau, growing with time from the centre of the orogen towards the east and west, and associated with protracted mantle upwelling, magmatism, crustal melting, low-pressure metamorphism and upper crustal extension. Orogenic plateau construction started with bimodal magmatism between 1280 and 1145 Ma, overlapping with demonstrably extensional intramontane basin sedimentation between c. 1210 and 1050 Ma, in the Telemarkia Lithotectonic Unit. In the east of the orogen, it was eventually limited by the mid crustal ramp (Mylonite Zone) overlying the Eastern Segment. In the westernmost exposed part of the orogen, the 1066–1020 Ma Sirdal-Feda high-K calc-alkaline magmatic suite is ...