High-temperature arc-parallel normal faulting and transtension at the roots of an obliquely convergent orogen, Klepeis, K. A., and Crawford, M. L.
Geology, v. 27, p. 7–10 (January 1999)
References to work on dextral transpression and extension in the Coast Mountains developed independently by colleagues at Princeton University as part of the ACCRETE project were omitted from this University as part of the ACCRETE project were omitted from this that the observations published in these references appear completely compatible with their model of sinistral transtension. They also acknowledge the Princeton group for collaboration during the course of these studies.
Andronicos C. L., Hollister, L. S., and Davidson, C., 1997, Dextral transpressive shearing at the eastern margin of the Quottoon pluton: Implications for the evolution of the Coast shear zone: Geological Society of America Abstracts with Programs, v. 29, no. 6, p. 83.
Chardon, D., and Andronicos, C. L., 1997, The Central Gneiss Complex: An asymmetrical extensional gneiss dome bounded by the Coast shear zone: Geological Society of America Abstracts with Programs, v. 29, no. 6, p. 84.
Hollister, L. S., and Andronicos, C. L., 1997, A candidate for the Baja British Columbia fault system in the Coast Plutonic Complex: GSA Today, no. 11, p. 1–7.