Add to ORKGThe 1.0–0.9 Ga plutons of the HBG suite (Hornblende-Biotite Granitoids) associated with the Rogaland anorthosites belong to the Sveconorwegian post-collisional magmatism in southwestern Norway. The comparison between experimental and natural phase equilibria indicates that the Lyngdal granodiorite (HBG suite) crystallized between 4 and 2 kbar, the magma having 6 wt% H2O in melt at early stages and an fO2 in the range NNO/NNO+1 (Bogaerts et al., 2002)
The tectonic evolution of the Late Mesoproterozoic Sveconorwegian Province has traditionally been co...
AbstractThe Rogaland–Vest Agder Sector of southwestern Norway comprises high-grade metamorphic rocks...
The Rogaland–Vest Agder Sector of southwestern Norway comprises high-grade metamorphic rocks intrude...
The Proterozoic (950 Ma) Lyngdal granodiorite of southern Norway belongs to a series of hornblende–b...
Norway belongs to a series of hornblende–biotite metaluminous ferroan granitoids (HBG suite) coeval ...
In south-western Norway, the Sveconorwegian orogenic thickening (1024–970 Ma) is followed by an impo...
Major and trace elements, Sr and Nd isotopic data as well as mineral compositions are presented for ...
Major and trace elements, Sr and Nd isotopic data as well as mineral compositions are presented for ...
peer reviewedSepta of banded gneisses crop out along the margin of the Proterozoic Sveconorwegian Eg...
Recently it has been argued that the Sveconorwegian orogeny in southwest Fennoscandia comprised a se...
International audienceThe Lyngen Magmatic Complex (LMC) is the lowest unit of the Lyngsfjellet Nappe...
The Western Gneiss Region (WGR) of the Scandinavian Caledonides is an archetypal terrain for high-pr...
The geology of the Suldal Sector, southwest Norway, comprises exposures from three orogenic periods;...
Laser ablation ICPMS U–Pb and Lu–Hf isotope data on granitic-granodioritic gneisses of the Precambri...
The geology of SW Norway is dominated by high-grade amphibolite to granulite facies gneisses with a...
The tectonic evolution of the Late Mesoproterozoic Sveconorwegian Province has traditionally been co...
AbstractThe Rogaland–Vest Agder Sector of southwestern Norway comprises high-grade metamorphic rocks...
The Rogaland–Vest Agder Sector of southwestern Norway comprises high-grade metamorphic rocks intrude...
The Proterozoic (950 Ma) Lyngdal granodiorite of southern Norway belongs to a series of hornblende–b...
Norway belongs to a series of hornblende–biotite metaluminous ferroan granitoids (HBG suite) coeval ...
In south-western Norway, the Sveconorwegian orogenic thickening (1024–970 Ma) is followed by an impo...
Major and trace elements, Sr and Nd isotopic data as well as mineral compositions are presented for ...
Major and trace elements, Sr and Nd isotopic data as well as mineral compositions are presented for ...
peer reviewedSepta of banded gneisses crop out along the margin of the Proterozoic Sveconorwegian Eg...
Recently it has been argued that the Sveconorwegian orogeny in southwest Fennoscandia comprised a se...
International audienceThe Lyngen Magmatic Complex (LMC) is the lowest unit of the Lyngsfjellet Nappe...
The Western Gneiss Region (WGR) of the Scandinavian Caledonides is an archetypal terrain for high-pr...
The geology of the Suldal Sector, southwest Norway, comprises exposures from three orogenic periods;...
Laser ablation ICPMS U–Pb and Lu–Hf isotope data on granitic-granodioritic gneisses of the Precambri...
The geology of SW Norway is dominated by high-grade amphibolite to granulite facies gneisses with a...
The tectonic evolution of the Late Mesoproterozoic Sveconorwegian Province has traditionally been co...
AbstractThe Rogaland–Vest Agder Sector of southwestern Norway comprises high-grade metamorphic rocks...
The Rogaland–Vest Agder Sector of southwestern Norway comprises high-grade metamorphic rocks intrude...