The Pelican Thrust Zone: basal detachment between the Archean Sask Craton and Paleoproterozoic Flin Flon – Glennie Complex, western Trans-Hudson Orogen.

Autor: Ashton, K. E.1 kashton@ir.gov.sk.ca, Lewry, J. F.2, Heaman, L. M.3, Hartlaub, R. P.3, Stauffer, M. R.4, Tran, H. T.5
Zdroj: Canadian Journal of Earth Sciences. Apr2005, Vol. 42 Issue 4, p685-706. 22p.
Databáze: Academic Search Ultimate