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doi:10.2204/iodp.proc.317.205.2014 ReferencesAdams, C.J., and Kelley, S., 1998. Provenance of Permian-Triassic and Ordovician metagreywacke terranes in New Zealand: evidence from 40Ar/39Ar dating of detrital micas. Geol. Soc. Am. Bull., 110(4):422–432. doi:10.1130/0016-7606(1998)110<0422:POPTAO>2.3.CO;2 Andrews, J.T., and Eberl, D.D., 2007. Quantitative mineralogy of surface sediments on the Iceland shelf, and application to down-core studies of Holocene ice-rafted sediments. J. Sediment. Res., 77(6):469–479. doi:10.2110/jsr.2007.045 Andrews, J.T., and Eberl, D.D., 2011. Surface (sea floor) and near-surface (box cores) sediment mineralogy in Baffin Bay as a key to sediment provenance and ice sheet variations. Can. J. Earth Sci., 48(9):1307–1328. doi:10.1139/e11-021 Andrews, J.T., and Eberl, D.D., 2012. Determination of sediment provenance by unmixing the mineralogy of source-area sediments: the “SedUnMix” program. Mar. Geol., 291–294:24–33. doi:10.1016/j.margeo.2011.10.007 Andrews, J.T., Jennings, A.E., Coleman, G.C., and Eberl, D.D., 2010. Holocene variations in mineral and grain-size composition along the East Greenland glaciated margin (ca 67°–70°N): local versus long-distance sediment transport. Quat. Sci. Rev., 29(19–20):2619–2632. doi:10.1016/j.quascirev.2010.06.001 Catuneanu, O., 2006. Principles of Sequence Stratigraphy (1st Ed.): Amsterdam (Elsevier). Davis, J.C., 2002. Statistics and Data Analysis in Geology (3rd Ed.): New York (John Wiley & Sons). Eberl, D.D., 2003. User’s guide to RockJock: a program for determining quantitative mineralogy from powder X-ray diffraction data. Open-File Rep.–U.S. Geol. Surv., 2003-78. http://pubs.usgs.gov/of/2003/of03-078/ Eberl, D.D., 2004. Quantitative mineralogy of the Yukon River system: changes with reach and season, and determining sediment provenance. Am. Mineral., 89:1784–1794. http://pubs.er.usgs.gov/publication/70026557 Expedition 317 Scientists, 2011a. Expedition 317 summary. In Fulthorpe, C.S., Hoyanagi, K., Blum, P., and the Expedition 317 Scientists, Proc. IODP, 317: Tokyo (Integrated Ocean Drilling Program Management International, Inc.). doi:10.2204/iodp.proc.317.101.2011 Expedition 317 Scientists, 2011b. Site U1351. In Fulthorpe, C.S., Hoyanagi, K., Blum, P., and the Expedition 317 Scientists, Proc. IODP, 317: Tokyo (Integrated Ocean Drilling Program Management International, Inc.). doi:10.2204/iodp.proc.317.103.2011 Expedition 317 Scientists, 2011c. Site U1352. In Fulthorpe, C.S., Hoyanagi, K., Blum, P., and the Expedition 317 Scientists, Proc. IODP, 317: Tokyo (Integrated Ocean Drilling Program Management International, Inc.). doi:10.2204/iodp.proc.317.104.2011 Expedition 317 Scientists, 2011d. Site U1353. In Fulthorpe, C.S., Hoyanagi, K., Blum, P., and the Expedition 317 Scientists, Proc. IODP, 317: Tokyo (Integrated Ocean Drilling Program Management International, Inc.). doi:10.2204/iodp.proc.317.105.2011 Expedition 317 Scientists, 2011e. Site U1354. In Fulthorpe, C.S., Hoyanagi, K., Blum, P., and the Expedition 317 Scientists, Proc. IODP, 317: Tokyo (Integrated Ocean Drilling Program Management International, Inc.). doi:10.2204/iodp.proc.317.106.2011 Fulthorpe, C.S., and Carter, R.M., 1991. Continental-shelf progradation by sediment-drift accretion. Geol. Soc. Am. Bull., 103(2):300–309. doi:10.1130/0016-7606(1991)103<0300:CSPBSD>2.3.CO;2 Kleeberg, R., Monecke, T., and Hillier, S., 2008. Preferred orientation of mineral grains in sample mounts for quantitative XRD measurements: how random are powder samples? Clays Clay Miner., 56(4):404–415. doi:10.1346/CCMN.2008.0560402 Lu, H., and Fulthorpe, C.S., 2004. Controls on sequence stratigraphy of a middle Miocene–Holocene, current-swept, passive margin: offshore Canterbury Basin, New Zealand. Geol. Soc. Am. Bull., 116(11–12):1345–1366. doi:10.1130/B2525401.1 Lu, H., Fulthorpe, C.S., and Mann, P., 2003. Three-dimensional architecture of shelf-building sediment drifts in the offshore Canterbury Basin, New Zealand. Mar. Geol., 193(1–2):19–47. doi:10.1016/S0025-3227(02)00612-6 Mackinnon, T.C., 1983. Origin of the Torlesse terrane and coeval rocks, South Island, New Zealand. Geol. Soc. Am. Bull., 94(8):967–985. doi:10.1130/0016-7606(1983)94<967:OOTTTA>2.0.CO;2 Moore, D.M., and Reynolds, R.C., Jr., 1997. X-ray Diffraction and the Identification and Analysis of Clay Minerals (2nd ed.): Oxford (Oxford Univ. Press). Mortimer, N., 1993. Geology of the Otago schist and adjacent rocks. Map.—Inst. Geol. Nucl. Sci., 7. http://trove.nla.gov.au/work/30107893 Mortimer, N., and Roser, B.P., 1992. Geochemical evidence for the position of the Caples–Torlesse boundary in the Otago schist, New Zealand. J. Geol. Soc. (London, U. K.), 149(6):967–977. doi:10.1144/gsjgs.149.6.0967 Omotoso, O., McCarty, D.K., Hillier, S., and Kleeberg, R., 2006. Some successful approaches to quantitative mineral analysis as revealed by the 3rd Reynolds Cup contest. Clays Clay Miner., 54(6):748–760. doi:10.1346/CCMN.2006.0540609 Ortiz, J.D., Polyak, L., Grebmeier, J.M., Darby, D., Eberl, D.D., Naidu, S., and Nof, D., 2009. Provenance of Holocene sediment on the Chukchi-Alaskan margin based on combined diffuse spectral reflectance and quantitative X-ray diffraction analysis. Global Planet. Change, 68(1–2):73–84. doi:10.1016/j.gloplacha.2009.03.020 Shapiro, S.A., Marsaglia, K.M., and Carter, L., 2007. The petrology and provenance of sand in the Bounty submarine fan, New Zealand. In Arribas, J., Johnsson, M.J., and Critelli, S. (Eds.), Sedimentary Provenance and Petrogenesis: Perspectives from Petrography and Geochemistry. Spec. Pap.—Geol. Soc. Am., 420:277–296. doi:10.1130/2006.2420(17) Środoń, J., Drits, V.A., McCarty, D.K., Hsieh, J.C.C., and Eberl, D.D., 2001. Quantitative X-ray diffraction analysis of clay-bearing rocks from random preparations. Clays Clay Miner., 49(6):514–528. http://ccm.geoscienceworld.org/cgi/content/abstract/49/6/514 Tucker, M.E., 1988. Techniques in Sedimentology: Boston (Blackwell Scientific). |