Origin of continental crust of 1.9-1.7 ga age: nd isotopes in the svecofennian orogenic terrains of sweden
Authors:
- P.Jonathan PatchettPPP.Jonathan Patchett
- Wolfgang TodtWTWolfgang Todt
- Roland GorbatschevRGRoland Gorbatschev
- 1 April 1987
- journal article
- Published by Elsevier in Precambrian Research
- Vol. 35, 145-160
Abstract
No abstract availableKeywords
This publication has 15 references indexed in Scilit:
- Formation of Canadian 1.9 Ga old continental crust. I: Nd isotopic dataCanadian Journal of Earth Sciences, 1987
- 1,700-Myr greenstone volcanic successions in southwestern North America and isotopic evolution of Proterozoic mantleNature, 1984
- Origin of continental crust of 1.9-1.7 Ga age defined by Nd isotopes in the Ketilidian terrain of South GreenlandContributions to Mineralogy and Petrology, 1984
- Zircon ages of metavolcanic and synorogenic granitic rocks from the Svärdsjö and Yxsjöberg areas, south central SwedenGeologiska Föreningen i Stockholm Förhandlingar, 1983
- Improved accuracy of U-Pb zircon ages by the creation of more concordant systems using an air abrasion techniqueGeochimica et Cosmochimica Acta, 1982
- Post-Svecokarelian andinotype evolution in central SwedenInternational Journal of Earth Sciences, 1982
- The Precambrian development of southern SwedenGeologiska Föreningen i Stockholm Förhandlingar, 1980
- Precambrian geochronology of south-eastern SwedenGeologiska Föreningen i Stockholm Förhandlingar, 1978
- Rare earth element patterns and crustal evolution—I. Australian post-Archean sedimentary rocksGeochimica et Cosmochimica Acta, 1976
- A low-contamination method for hydrothermal decomposition of zircon and extraction of U and Pb for isotopic age determinationsGeochimica et Cosmochimica Acta, 1973