Evidence for transition from a continental forearc to a collisional pro-foreland basin in the eastern Trans-Hudson Orogen: Detrital zircon provenance analysis in the Labrador Trough, Canada

Author:

Henrique-Pinto R.,Guilmette C.,Bilodeau C.,McNicoll V.

Funder

MERN

Geological Survey of Canada

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference76 articles.

1. Baragar, W.R.A., 1967. Wakuach Lake map-area, Quebec-Labrador (23 O). Geological Survey of Canada, Memoir, 344, p. 174.

2. The circum-superior belt: a proterozoic plate margin?;Baragar;Develop. Precambr. Geol.,1981

3. Numerical tabulation of the distribution of Kolmogorov's statistic for finite sample size;Birnbaum;J. Am. Stat. Assoc.,1952

4. A structural cross-section of the northern Labrador Trough, New Quebec. The Early Proterozoic Trans-Hudson Orogen. Edited by JF Lewry and MR Stauffer;Boon;Geol. Assoc. Can. Spec. Pap.,1990

5. Cabri, L.J., Rudashevsky, N.S., Rudashevsky, V.N., Oberthür, T. 2008. Electric-pulse disaggregation (Epd), hydroseparation (Hs) and their use in combination for mineral processing and advanced characterization of ores. In: Proceedings of the 40th Annual Canadian Mineral Processors Conference Paper, 14, 211–235.

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