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 hangi...
A series of papers providing comments and description of itineraries in the Rogaland anorthosite pro...
Understanding mountain building processes requires a better integration of petrological and peochron...
AbstractMassif anorthosites form when basaltic magma differentiates in crustal magma chambers to for...
The Rogaland–Vest Agder Sector of southwestern Norway comprises high-grade metamorphic rocks intrude...
AbstractThe Rogaland–Vest Agder Sector of southwestern Norway comprises high-grade metamorphic rocks...
Recently it has been argued that the Sveconorwegian orogeny in southwest Fennoscandia comprised a se...
The Rogaland Anorthosite Province comprises three major massif-type anorthosites, two smaller-sized ...
The c. 930 Ma Åna-Sira anorthosite massif (ÅS) is a part of the Rogaland Anorthosite Province, situa...
This paper aims at testing the mechanical relevance of the petrological model of anorthosite massif ...
The Rogaland–Vest Agder Sector of southwestern Norway comprises high-grade metamorphic rocks intrude...
The norito-granitic zone is a thin septum of highly deformed banded rocks squeezed between two anort...
In the Rogaland-Vest Agder terrain of the Sveconorwegian Province of SW Norway, two main Sveconorweg...
The Sveconorwegian orogeny encompasses magmatic, metamorphic and deformational events between ca. 11...
Understanding mountain building processes requires a better integration of petrological and peochron...
peer reviewedSepta of banded gneisses crop out along the margin of the Proterozoic Sveconorwegian Eg...
A series of papers providing comments and description of itineraries in the Rogaland anorthosite pro...
Understanding mountain building processes requires a better integration of petrological and peochron...
AbstractMassif anorthosites form when basaltic magma differentiates in crustal magma chambers to for...
The Rogaland–Vest Agder Sector of southwestern Norway comprises high-grade metamorphic rocks intrude...
AbstractThe Rogaland–Vest Agder Sector of southwestern Norway comprises high-grade metamorphic rocks...
Recently it has been argued that the Sveconorwegian orogeny in southwest Fennoscandia comprised a se...
The Rogaland Anorthosite Province comprises three major massif-type anorthosites, two smaller-sized ...
The c. 930 Ma Åna-Sira anorthosite massif (ÅS) is a part of the Rogaland Anorthosite Province, situa...
This paper aims at testing the mechanical relevance of the petrological model of anorthosite massif ...
The Rogaland–Vest Agder Sector of southwestern Norway comprises high-grade metamorphic rocks intrude...
The norito-granitic zone is a thin septum of highly deformed banded rocks squeezed between two anort...
In the Rogaland-Vest Agder terrain of the Sveconorwegian Province of SW Norway, two main Sveconorweg...
The Sveconorwegian orogeny encompasses magmatic, metamorphic and deformational events between ca. 11...
Understanding mountain building processes requires a better integration of petrological and peochron...
peer reviewedSepta of banded gneisses crop out along the margin of the Proterozoic Sveconorwegian Eg...
A series of papers providing comments and description of itineraries in the Rogaland anorthosite pro...
Understanding mountain building processes requires a better integration of petrological and peochron...
AbstractMassif anorthosites form when basaltic magma differentiates in crustal magma chambers to for...