Add to ORKGA series of papers providing comments and description of itineraries in the Rogaland anorthosite province. A revised and amplified version is now available (published in 2003) under reference http://hdl.handle.net/2268/26
Monzonorites, members of the anorthositic suite of rocks, are usually considered as residual after t...
The Molde Peninsula lies at approximately 64oN, in the Basal Gneiss Complex of W Norway, which repre...
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 ...
peer reviewedThe Rogaland anorthosite province (RAP) – a typical Proterozoic Anorthosite-Mangerite-C...
AbstractThe Rogaland–Vest Agder Sector of southwestern Norway comprises high-grade metamorphic rocks...
The c. 930 Ma Åna-Sira anorthosite massif (ÅS) is a part of the Rogaland Anorthosite Province, situa...
The Rogaland–Vest Agder Sector of southwestern Norway comprises high-grade metamorphic rocks intrude...
The Rogaland–Vest Agder Sector of southwestern Norway comprises high-grade metamorphic rocks intrude...
peer reviewedSr and Nd isotopic data from the anorthosite-mangerite-charnockite (AMC) suite of the L...
The tectonic setting and mechanisms and duration of emplacement of Proterozoic massif-type anorthosi...
The geology of Southwest Norway is dominated by amphibolite-granulite facies gneisses along with gra...
peer reviewedThe massif-type anorthosites of the province were emplaced as crystal mushes of plagioc...
The norito-granitic zone is a thin septum of highly deformed banded rocks squeezed between two anort...
peer reviewedSepta of banded gneisses crop out along the margin of the Proterozoic Sveconorwegian Eg...
Monzonorites, members of the anorthositic suite of rocks, are usually considered as residual after t...
The Molde Peninsula lies at approximately 64oN, in the Basal Gneiss Complex of W Norway, which repre...
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 ...
peer reviewedThe Rogaland anorthosite province (RAP) – a typical Proterozoic Anorthosite-Mangerite-C...
AbstractThe Rogaland–Vest Agder Sector of southwestern Norway comprises high-grade metamorphic rocks...
The c. 930 Ma Åna-Sira anorthosite massif (ÅS) is a part of the Rogaland Anorthosite Province, situa...
The Rogaland–Vest Agder Sector of southwestern Norway comprises high-grade metamorphic rocks intrude...
The Rogaland–Vest Agder Sector of southwestern Norway comprises high-grade metamorphic rocks intrude...
peer reviewedSr and Nd isotopic data from the anorthosite-mangerite-charnockite (AMC) suite of the L...
The tectonic setting and mechanisms and duration of emplacement of Proterozoic massif-type anorthosi...
The geology of Southwest Norway is dominated by amphibolite-granulite facies gneisses along with gra...
peer reviewedThe massif-type anorthosites of the province were emplaced as crystal mushes of plagioc...
The norito-granitic zone is a thin septum of highly deformed banded rocks squeezed between two anort...
peer reviewedSepta of banded gneisses crop out along the margin of the Proterozoic Sveconorwegian Eg...
Monzonorites, members of the anorthositic suite of rocks, are usually considered as residual after t...
The Molde Peninsula lies at approximately 64oN, in the Basal Gneiss Complex of W Norway, which repre...
Recently it has been argued that the Sveconorwegian orogeny in southwest Fennoscandia comprised a se...