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Biscaye, P.E., 1965. Mineralogy and sedimentation of recent deep-sea clay in the Atlantic Ocean and adjacent seas and oceans. Geol. Soc. Am. Bull., 76(7):803–831. doi:10.1130/0016-7606(1965)76[803:MASORD]2.0.CO;2

Blaise, B., 1989. Clay-mineral assemblages from Late Quaternary deposits on Vancouver Island, southwestern British Columbia, Canada. Quat. Res., 31(1):41–56. doi:10.1016/0033-5894(89)90084-7

Brown, G., and Brindley, G.W., 1980. X-ray diffraction procedures for clay mineral identification. In Brindley, G.W., and Brown, G. (Eds.), Crystal Structures of Clay Minerals and Their X-ray Identification. Mineral. Soc. Monogr. London, 5:305–359.

Duncan, J.R., Kulm, L.D., and Griggs, G.B., 1970. Clay mineral composition of late Pleistocene and Holocene sediments of Cascadia Basin, northeastern Pacific Ocean. J. Geol., 78:213–221.

Gràcia, E., Martínez-Ruiz, F., Piñero, E., Larrasoaña, J.C., Vizcaino, A., and Ercilla, G., 2006. Data report: grain-size and bulk and clay mineralogy of sediments from the summit and flanks of southern Hydrate Ridge, Sites 1244–1250, ODP Leg 204. In Tréhu, A.M., Bohrmann, G., Torres, M.E., and Colwell, F.S. (Eds.), Proc. ODP, Sci. Results, 204: College Station, TX (Ocean Drilling Program), 1–19. doi:10.2973/

Holtzapffel, T., 1985. Les minéraux argileux: préparation, analyse diffractométrique et détermination. Publ. Soc. Geol. Nord., 12.

Karlin, R., 1980. Sediment sources and clay mineral distributions off the Oregon coast. J. Sediment. Petrol., 50:543–560.

Kulm, L.D., and Fowler, G.A., 1974. Oregon continental margin structure and stratigraphy: a test of the imbricate thrust model. In Burke, C.A., and Drake, C.L. (Eds.), The Geology of Continental Margins: New York (Springer), 261–284.

MacKay, M.E., Moore, G.F., Cochrane, G.R., Moore, J.C., and Kulm, L.D., 1992. Landward vergence and oblique structural trends in the Oregon margin accretionary prism: implications and effect on fluid flow. Earth Planet. Sci. Lett., 109(3–4):477–491. doi:10.1016/0012-821X(92)90108-8

Rettke, R.C., 1981. Probable burial diagenetic and provenance effects on Dakota Group clay mineralogy, Denver Basin. J. Sediment. Petrol., 51:541–551.

Underwood, M., and Torres, M., 2006. Data report: composition of clay minerals from hemipelagic sediments at Hydrate Ridge, Cascadia subduction zone. In Tréhu, A.M., Bohrmann, G., Torres, M.E., and Colwell, F.S. (Eds.), Proc. ODP, Sci. Results, 204: College Station TX (Ocean Drilling Program), 1–15. doi:10.2973/

Underwood, M.B., 2002. Strike-parallel variations in clay minerals and fault vergence in the Cascadia subduction zone. Geology, 30(2):155–158. doi:10.1130/0091-7613(2002)030<0155:SPVICM>2.0.CO;2

Vanderaveroet, P., Bout-Roumazeilles, V., Fagel, N., Chamley, H., and Deconinck, J.F., 2000. Significance of random illite-vermiculite mixed layers in Pleistocene sediments of the northwestern Altlantic Ocean. Clay Miner., 35(4):679–691. doi:10.1180/000985500547133