Stabilization of garnet in metamorphosed altered turbidites near the St. Eugene lead–zinc deposit, southeastern British Columbia: Equilibrium and kinetic controls-Reference-Cited by-同舟云学术

Stabilization of garnet in metamorphosed altered turbidites near the St. Eugene lead–zinc deposit, southeastern British Columbia: Equilibrium and kinetic controls

Published:2012-03 Issue: Volume:134-135 Page:221-235
ISSN:0024-4937
Container-title:Lithos
language:en
Short-container-title:Lithos

Author:

Pattison David R.M.,Seitz JennaLee D.

Funder

NSERC

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference64 articles.

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2. Geochemistry and isotope chemistry of the Moyie Sills: implications for the early tectonic setting of the Mesoproterozoic Purcell basin;Anderson,2000

3. U–Pb geochronological evidence for the geological history of the Belt–Purcell Supergroup, southeastern British Columbia;Anderson,2000

4. The metamorphism of the Dalradian rocks of Scotland;Atherton;Scottish Journal of Geology,1977

5. Berry, A.D., 1951. A study of the Aldridge Formation, St. Mary Lake area, British Columbia. Unpublished MSc thesis, University of Alberta.

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