Recognizable primary volcanic and sedimentary features in a low‐strain domain of the highly deformed, oldest known (≈ 3.7–3.8 Gyr) Greenstone Belt, Isua, West Greenland
- 1 March 1998
- journal article
- Published by Wiley in Terra Nova
- Vol. 10 (2) , 57-62
- https://doi.org/10.1046/j.1365-3121.1998.00162.x
Abstract
No abstract availableThis publication has 9 references indexed in Scilit:
- The Itsaq Gneiss Complex of southern West Greenland; the world's most extensive record of early crustal evolution (3900-3600 Ma)Published by Elsevier ,1999
- Extreme Nd-isotope heterogeneity in the early Archaean—fact or fiction? Case histories from northern Canada and West Greenland—ReplyChemical Geology, 1998
- ∼ 3710 and ⪖ 3790 Ma volcanic sequences in the Isua (Greenland) supracrustal belt; structural and Nd isotope implicationsChemical Geology, 1997
- Evidence for life on Earth before 3,800 million years agoNature, 1996
- The origin of metacarbonate rocks in the Archaean Isua supracrustal belt, West GreenlandAmerican Journal of Science, 1996
- Earliest part of Earth's stratigraphic record: A reappraisal of the >3.7 Ga Isua (Greenland) supracrustal sequenceGeology, 1996
- Sedimentology of archean greenstone belts: Signatures of tectonic evolutionEarth-Science Reviews, 1994
- Stratigraphic and geochemical evidence for the depositional environment of the early archaean isua supracrustal belt, southern west greenlandPrecambrian Research, 1984
- Continued mapping of the pre-3760 m.y. old supracrustal rocks of the Isua area, southern West GreenlandRapport Grønlands Geologiske Undersøgelse, 1976