Nd isotopic evidence from Wopmay Orogen for 2.0–2.4 Ga crust in western North America
- 1 September 1989
- journal article
- Published by Elsevier in Earth and Planetary Science Letters
- Vol. 94 (3-4) , 217-230
- https://doi.org/10.1016/0012-821x(89)90141-6
Abstract
No abstract availableKeywords
This publication has 42 references indexed in Scilit:
- Tectono-magmatic evolution of the 1.9-Ga great bear magmatic zone, Wopmay orogen, northwestern CanadaPublished by Elsevier ,2003
- Lead Isotopic Study of Early Proterozoic Wopmay Orogen, Nw Canada: Role of Continental Crust in Arc MagmatismThe Journal of Geology, 1989
- Nd Isotope Systematics of Coarse- and Fine-Grained Sediments: Examples from the Middle Proterozoic Belt-Purcell SupergroupThe Journal of Geology, 1987
- The metamorphic internal zone of Wopmay Orogen (Early Proterozoic), Canada: 30 km of structural relief in a composite section based on plunge projectionTectonics, 1986
- Geochronology of the Big Spruce Lake alkaline intrusionCanadian Journal of Earth Sciences, 1986
- Rapid production of continental crust 1.7 to 1.9 b.y. ago: Nd isotopic evidence from the basement of the North American mid-continentGSA Bulletin, 1985
- Petrology and provenance of pre–Late Devonian sandstones, Shoo Fly Complex, northern Sierra Nevada, CaliforniaGSA Bulletin, 1985
- Continental intra-arc depressions: A nonextensional model for their origin, with a Proterozoic example from Wopmay orogenGeology, 1984
- Age and isotope evidence for the evolution of continental crustPhilosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences, 1978
- The Siberian Connection: A case for Precambrian separation of the North American and Siberian cratonsGeology, 1978