Metamorphism of the ca. 3800 Ma supracrustal rocks at Isua, West Greenland: implications for early Archaean crustal evolution
- 1 June 1982
- journal article
- Published by Elsevier in Earth and Planetary Science Letters
- Vol. 59 (1), 155-176
- https://doi.org/10.1016/0012-821x(82)90123-6
Abstract
No abstract availableKeywords
This publication has 38 references indexed in Scilit:
- Eastern Indian 3800-Million-Year-Old Crust and Early Mantle DifferentiationScience, 1981
- Continental geotherms during the ArchaeanNature, 1979
- Heat loss from the earth: A constraint on Archaean tectonics from the relation between geothermal gradients and the rate of plate productionEarth and Planetary Science Letters, 1978
- The role of fluids in the formation and subsequent development of early continental crustContributions to Mineralogy and Petrology, 1978
- Archean basin–craton complexes and the growth of Precambrian shieldsCanadian Journal of Earth Sciences, 1977
- Deformation of the Isua block, West Greenland: a remnant of the earliest stable continental crustCanadian Journal of Earth Sciences, 1976
- The Ameralik dykes of West Greenland, the earliest known basaltic rocks intruding stable continental crustEarth and Planetary Science Letters, 1976
- The evolution of early precambrian crustal rocks at Isua, West Greenland — Geochemical and isotopic evidenceEarth and Planetary Science Letters, 1975
- A Discussion on the evolution of the Precambrian crust - The early Precambrian gneisses of the Godthåb district, West GreenlandPhilosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences, 1973
- Speculations on the Earth's Thermal HistoryGSA Bulletin, 1965