|Name||Condrey Mountain Schist|
|Geologic age||Paleozoic(?) to Jurassic|
Metamorphic > Schist (Greenschist)Includes metasedimentary rocks (graphitic quartz-albite-muscovite schist) and metavolcanic greenschist.
Sedimentary > Chemical > Chert (Bed)
Metamorphic > Metaigneous > Serpentinite
Metamorphic > Metaigneous > Metaintrusive > Metagabbro
Walker, G.W. and MacLeod, N.S., 1991, Geologic map of Oregon: U.S. Geological Survey, scale 1:500,000.
Irwin, W.P., 1994, Geologic map of the Klamath Mountains, California and Oregon: U.S. Geological Survey Miscellaneous Investigations Series Map I-2148, scale 1:500,000.
Helper, M.A., 1986, Deformation and high P/T metamorphism in the central part of the Condrey Mountain window, north-central Klamath Mountains, California and Oregon, in Evans, B.W., and Brown, E.H., eds., Blueschists and eclogites: Geological Society of America Memoir 164, p. 125-141.
Coleman, R.G., Manning, C.E., Mortimer, N., Donato, M.M., and Hill, L.B., 1988, Tectonic and regional metamorphic framework of the Klamath Mountains and adjacent Coast Ranges, California and Oregon, in Ernst, W.G., ed., Metamorphism and crustal evolution of the western United States: Englewood Cliffs, N.J., Prentice-Hall, p. 1061-1097.
Saleeby, J..B., and Harper, G.D., 1993, Tectonic relations between the Galice Formation and the Condrey Mountain Schist, Klamath Mountains, Northern California, in Dunne, G.C., and McDougall, K.A., eds., Mesozoic paleogeography of the western United States - II: Pacific Section Society of Economic Paleontologists and Mineralogists, Book 71, p. 61-80.
Lanphere, M.A., Irwin, W.P., and Hotz, P.E., 1968, Isotopic age of the Nevadan orogeny and older plutonic and metamorphic events in the Klamath Mountains, California: Geological Society of America Bulletin, v. 79, p. 1027-1052.
Suppe, John, and Armstrong, R.L., 1972, Potassium-argon dating of Fransican metamorphic rocks: American Journal of Science, v. 272, p. 217-233.