Add to ORKGA Precambrian layered gabbroic intrusion about 560 km^2 in area, of the Skaergaard type, crops out on the middle north coast of Labrador. Border zones and a Layered series are recognized, and have the following characteristics and approximate mean thicknesses. The intrusion displays extreme fractionation resulting in larvikite consisting of mesoperthite, fayalite, ferroaugite, and ore as the uppermost differentiate. Mineral variation and differentiation are described by means of quantitative mineralogy
This report is based on the Field Work carried out by the writer during the summer of 1957, and on s...
Mafic layered intrusions in the Earth’s crust are natural laboratories for evaluating differentiatio...
Canada) is a large igneous body of c. 20 000 km3. From the base to the top, it consists of a Layered...
A Precambrian layered gabbroic intrusion about 560 km('2) in area, of the Skaergaard type, crops out...
Northern Labrador lies within the Canadian Shield, its bedrock being generally Precambrian in age or...
In the summer of 1949 a field party of the Geological Survey of Canada made a reconnaissance survey ...
A reconnaissance survey of the bedrock geology of a 30- to 60-km-wide by 120-km-long corridor betwee...
Labrador forms the eastern portion of the Precambrian Canadian Shield. It is divisible into four geo...
The Archaean Hopedale Block, in the southern Nain Province of Labrador, Canada, is host to three gen...
Includes bibliographical references.Includes illustrations.Mafic granulites surrounding the Kiglapai...
The central Labrador Trough is an Early Proterozoic volcano-sedimentary succession which preserves t...
grantor: University of TorontoThe South Voisey's Bay property held by Donner Minerals Limi...
The northeastern part of Kaipokok Bay is located in the Makkovik Province of Labrador, in the bounda...
The area lies along the "Grenville front" in a heavily glaciated area of southwestern Labrador. Abou...
For many years Labrador has been a land of mystery. The country is not well known, though today for ...
This report is based on the Field Work carried out by the writer during the summer of 1957, and on s...
Mafic layered intrusions in the Earth’s crust are natural laboratories for evaluating differentiatio...
Canada) is a large igneous body of c. 20 000 km3. From the base to the top, it consists of a Layered...
A Precambrian layered gabbroic intrusion about 560 km('2) in area, of the Skaergaard type, crops out...
Northern Labrador lies within the Canadian Shield, its bedrock being generally Precambrian in age or...
In the summer of 1949 a field party of the Geological Survey of Canada made a reconnaissance survey ...
A reconnaissance survey of the bedrock geology of a 30- to 60-km-wide by 120-km-long corridor betwee...
Labrador forms the eastern portion of the Precambrian Canadian Shield. It is divisible into four geo...
The Archaean Hopedale Block, in the southern Nain Province of Labrador, Canada, is host to three gen...
Includes bibliographical references.Includes illustrations.Mafic granulites surrounding the Kiglapai...
The central Labrador Trough is an Early Proterozoic volcano-sedimentary succession which preserves t...
grantor: University of TorontoThe South Voisey's Bay property held by Donner Minerals Limi...
The northeastern part of Kaipokok Bay is located in the Makkovik Province of Labrador, in the bounda...
The area lies along the "Grenville front" in a heavily glaciated area of southwestern Labrador. Abou...
For many years Labrador has been a land of mystery. The country is not well known, though today for ...
This report is based on the Field Work carried out by the writer during the summer of 1957, and on s...
Mafic layered intrusions in the Earth’s crust are natural laboratories for evaluating differentiatio...
Canada) is a large igneous body of c. 20 000 km3. From the base to the top, it consists of a Layered...