Structures in the Canyon Mountain Ophiolite indicate an island-arc intrusion
- 10 December 1985
- journal article
- Published by Elsevier in Tectonophysics
- Vol. 120 (3-4) , 191-209
- https://doi.org/10.1016/0040-1951(85)90051-4
Abstract
No abstract availableKeywords
This publication has 20 references indexed in Scilit:
- Paleomagnetism and Mesozoic tectonics of the Seven Devils Volcanic Arc in northeastern OregonJournal of Geophysical Research, 1982
- An island arc origin for the Canyon Mountain ophiolite complex, eastern Oregon, U.S.A.Earth and Planetary Science Letters, 1981
- Petrology and geochemistry of plagiogranite in the Canyon Mountain ophiolite, OregonContributions to Mineralogy and Petrology, 1981
- 40Ar-39Ar ages of some pre-Tertiary plutonic and metamorphic rocks of eastern Oregon and their geologic relationshipsGeology, 1980
- Geochemical discrimination between ocean-floor and island-arc tholeiites—application to some ophiolitesCanadian Journal of Earth Sciences, 1979
- Mesozoic forearc basin in central OregonGeology, 1979
- Characteristics of back arc spreading in the Mariana TroughJournal of Geophysical Research, 1978
- Structure and petrology of the Lanzo peridotite massif (Piedmont Alps)GSA Bulletin, 1978
- Rifting of a tethyan continent — Rare earth evidence of an accreting plate marginEarth and Planetary Science Letters, 1976
- Origin and development of marginal basins in the western PacificJournal of Geophysical Research, 1971