The Precambrian of Finnish Lapland: Evolution and regime of metamorphism
- 1 February 1982
- journal article
- research article
- Published by Springer Nature in International Journal of Earth Sciences
- Vol. 71 (1) , 230-244
- https://doi.org/10.1007/bf01825039
Abstract
No abstract availableKeywords
This publication has 14 references indexed in Scilit:
- Significance of Fe-Mg Cordierite Stability Relations on Temperature, Pressure, and Water Pressure in Cordierite GranulitesPublished by Wiley ,2013
- Relationships between granite-gneiss terrains, greenstone belts and granulite belts in the archean crust of Lapland (Fennoscandia)International Journal of Earth Sciences, 1980
- Trace Element Geochemistry and Petrogenesis of Finnish Greenstone BeltsJournal of Petrology, 1980
- Osumilite-sapphirine-quartz granulites from Enderby Land, Antarctica: P-T conditions of metamorphism, implications for garnet-cordierite equilibria and the evolution of the deep crustContributions to Mineralogy and Petrology, 1980
- An experimental study of the effect of Ca upon garnet-clinopyroxene Fe-Mg exchange equilibriaContributions to Mineralogy and Petrology, 1979
- Chemical and Thermal Evolution of Archaean Sialic Crust, Southern West GreenlandJournal of Petrology, 1979
- Evolution of the Archean crust in FinlandPrecambrian Research, 1978
- Experimental calibration of the partitioning of Fe and Mg between biotite and garnetContributions to Mineralogy and Petrology, 1978
- The Origin of the Apsley Gneiss, OntarioCanadian Journal of Earth Sciences, 1972
- Red corundum, sapphirine and kornerupine from Kittilä, Finnish LaplandBulletin of the Geological Society of Finland, 1971