Petrogenesis of the Dunite Peak ophiolite, south-central Yukon, and the distinction between upper-plate and lower-plate settings: A new hypothesis for the late Paleozoic–early Mesozoic tectonic evolution of the Northern Cordillera-Reference-Cited by-同舟云学术

Petrogenesis of the Dunite Peak ophiolite, south-central Yukon, and the distinction between upper-plate and lower-plate settings: A new hypothesis for the late Paleozoic–early Mesozoic tectonic evolution of the Northern Cordillera

Published:2018-08-16 Issue:1-2 Volume:131 Page:274-298
ISSN:0016-7606
Container-title:GSA Bulletin
language:en
Short-container-title:

Author:

Parsons A.J.¹,Zagorevski A.²,Ryan J.J.¹,McClelland W.C.³,van Staal C.R.¹,Coleman M.J.⁴,Golding M.L.¹

Affiliation:

1. Geological Survey of Canada, 1500-605 Robson Street, Vancouver, British Columbia, V6B5J, Canada

2. Geological Survey of Canada, 601 Booth Street, Ottawa, Ontario, K1A 0E8, Canada

3. Department of Earth and Environmental Sciences, University of Iowa, 115 Trowbridge Hall, Iowa City, Iowa 52242, USA

4. Department of Earth and Environmental Sciences, University of Ottawa, 120 University, Ottawa, Ontario, K1N 6N5, Canada

Publisher

Geological Society of America

Subject

Geology

Link

https://pubs.geoscienceworld.org/gsa/gsabulletin/article-pdf/131/1-2/274/4604625/274.pdf

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