Rb-Sr whole-rock isochron ages were determined on the Lutzow-Holm and Yamato-Belgica Complexes from eastern Queen Maud Land. Metamorphic rocks from East Ongul Island, Nesoya, Sinnan Rocks and the Yamato Mountains gave ages ranging between 683.0 and 722.1Ma. Rocks from Skarvsnes gave older ages of 1131 and 1033Ma. All these ages are interpreted to represent the times of high-grade metamorphism. The Skarvsnes area was apparently not affected by the 700Ma metamorphism. The initial ^Sr/^Sr ratios of metamorphic rocks show a considerable variation on local as well as regional scale. The higher initial ratios of the Yamato Mountains suggest that the protolith of the Yamato-Belgica Complex is older than that of the Lutzow-Holm Complex
Kasumi Rock is situated in the amphibolite-facies metamorphic zone in the Lutzow-Holm Complex, East ...
In the sector of 30-45°E in East Antarctica, two high-grade metamorphic complexes, the Lutzow-Holm C...
Oku-iwa Rock in the Liitzow-Holm Complex East Antaictica is situated in a transitional between granu...
Rb-Sr mineral isochron ages were determined for three metamorphic rocks around Syowa Station and fro...
Geochronological study using the Rb-Sr whole-rock isochron method was carried out on the metamorphic...
Rb-Sr age determinations have been carried out on rock samples collected in the area along the east ...
The K-Ar age determination on micas from the metamorphic rocks and granites in the Ongul Islands and...
A Rb-Sr and Sm-Nd isotope study of meta-trondhjemites and a pelitic gneiss from Cape Hinode, Lutzow-...
We report the preliminary results of whole-rock Rb-Sr and Sm-Nd isochrons dating on granulite-facies...
The Sm-Nd whole rock isochron age was determined for metamorphic rocks from Mount Pardoe, Napier Com...
In eastern Dronning Maud Land (DML), East Antarctica, there are several discrete, isolated magmatic ...
Rb-Sr whole rock isochron ages were determined on the two plutonic bodies from the Sør Rondane Mount...
In eastern Dronning Maud Land (DML), East Antarctica, there are several discrete, isolated magmatic ...
The bedrock of Mühlig-Hofmannfjella, central Dronning Maud Land in eastern Antarctica, is part of th...
The bedrock of Mühlig-Hofmannfjella, central Dronning Maud Land in eastern Antarctica, is part of th...
Kasumi Rock is situated in the amphibolite-facies metamorphic zone in the Lutzow-Holm Complex, East ...
In the sector of 30-45°E in East Antarctica, two high-grade metamorphic complexes, the Lutzow-Holm C...
Oku-iwa Rock in the Liitzow-Holm Complex East Antaictica is situated in a transitional between granu...
Rb-Sr mineral isochron ages were determined for three metamorphic rocks around Syowa Station and fro...
Geochronological study using the Rb-Sr whole-rock isochron method was carried out on the metamorphic...
Rb-Sr age determinations have been carried out on rock samples collected in the area along the east ...
The K-Ar age determination on micas from the metamorphic rocks and granites in the Ongul Islands and...
A Rb-Sr and Sm-Nd isotope study of meta-trondhjemites and a pelitic gneiss from Cape Hinode, Lutzow-...
We report the preliminary results of whole-rock Rb-Sr and Sm-Nd isochrons dating on granulite-facies...
The Sm-Nd whole rock isochron age was determined for metamorphic rocks from Mount Pardoe, Napier Com...
In eastern Dronning Maud Land (DML), East Antarctica, there are several discrete, isolated magmatic ...
Rb-Sr whole rock isochron ages were determined on the two plutonic bodies from the Sør Rondane Mount...
In eastern Dronning Maud Land (DML), East Antarctica, there are several discrete, isolated magmatic ...
The bedrock of Mühlig-Hofmannfjella, central Dronning Maud Land in eastern Antarctica, is part of th...
The bedrock of Mühlig-Hofmannfjella, central Dronning Maud Land in eastern Antarctica, is part of th...
Kasumi Rock is situated in the amphibolite-facies metamorphic zone in the Lutzow-Holm Complex, East ...
In the sector of 30-45°E in East Antarctica, two high-grade metamorphic complexes, the Lutzow-Holm C...
Oku-iwa Rock in the Liitzow-Holm Complex East Antaictica is situated in a transitional between granu...