Proc. IODP, 340, Site U1395

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Chapter contents Background and objectives Operations Transit to Site U1395 Site U1395 Lithostratigraphy Unit A Unit B Unit C Unit D Unit E Unit F Unit G Unit H Unit I Paleontology and biostratigraphy Calcareous nannofossils Planktonic foraminifers Benthic foraminifers Geochemistry Physical properties Stratigraphic correlation between Holes U1395A and U1395B Gamma ray attenuation density, magnetic susceptibility, and P-wave velocity Thermal conductivity Shear strength P-wave velocity Moisture and density Downhole temperature Paleomagnetism Results Downhole logging Operations Data processing and quality assessment Logging stratigraphy Formation MicroScanner images References Figures F1. Site U1395 maps. F2. Pumice-rich bed. F3. Biozonation. F4. XRD patterns. F5. Solid-phase geochemical depth profiles. F6. Pore water geochemical depth profiles. F7. Magnetic susceptibility correlation. F8. Physical properties measurements. F9. Temperature as a function of depth. F10. Intensity, inclination, and declination, Hole U1395A. F11. Intensity, inclination, and declination, Hole U1395B. F12. Magnetic susceptibility correlations. F13. Biostratigraphy. F14. Tool string deployments. F15. Triple combo logs. F16. FMS-sonic logs. F17. Log comparison. F18. Spectral NGR measurements. F19. FMS images. Tables T1. Coring summary. T2. Solid-phase geochemistry. T3. Interstitial pore water. T4. Correlation point picks and depth shifts. T5. Paleomagnetism samples. PDF file			Previous \| Next doi:10.2204/iodp.proc.340.105.2013 References Cande, S.C., and Kent, D.V., 1995. Revised calibration of the geomagnetic polarity timescale for the Late Cretaceous and Cenozoic. J. Geophys. Res., [Solid Earth], 100(B4):6093–6095. doi:10.1029/94JB03098 Expedition 340 Scientists, 2013a. Methods. In Le Friant, A., Ishizuka, O., Stroncik, N.A., and the Expedition 340 Scientists, Proc. IODP, 340: Tokyo (Integrated Ocean Drilling Program Management International, Inc.). doi:10.2204/iodp.proc.340.102.2013 Expedition 340 Scientists, 2013b. Site U1394. In Le Friant, A., Ishizuka, O., Stroncik, N.A., and the Expedition 340 Scientists, Proc. IODP, 340: Tokyo (Integrated Ocean Drilling Program Management International, Inc.). doi:10.2204/iodp.proc.340.104.2013 Fuller, M., Molina-Garza, R., Touchard, Y., and Kidane, T., 2006. Paleomagnetic records from carbonate legs in the Southern Oceans and attendant drilling and coring related effects. In Sager, W.W., Acton, G.D., Clement, B.M., and Fuller, M. (Eds.), ODP Contributions to Paleomagnetism. Phys. Earth Planet. Int., 156(3–4):242–260. doi:10.1016/j.pepi.2005.08.007 Garcia, M.O., Sherman, S.B., Moore, G.F., Goll, R., Popova-Goll, I., Natland, J.H., and Acton, G., 2006. Frequent landslides from Koolau volcano: results from ODP Hole 1223A. J. Volcanol. Geotherm. Res., 151(1–3):251–268. doi:10.1016/j.jvolgeores.2005.07.035 Gartner, S., 1977. Calcareous nannofossil biostratigraphy and revised zonation of the Pleistocene. Mar. Micropaleontol., 2:1–25. doi:10.1016/0377-8398(77)90002-0 Hayward, B.W., Kawagata, S., Grenfell, H.R., Droxler, A.W., and Shearer, M., 2006. Mid-Pleistocene extinction of bathyal benthic foraminifera in the Caribbean Sea. Micropaleontology, 52(3):245–265. doi:10.2113/gsmicropal.52.3.245 Heesemann, M., Villinger, H., Fisher, A.T., Tréhu, A.M., and White, S., 2006. Data report: testing and deployment of the new APCT-3 tool to determine in situ temperatures while piston coring. In Riedel, M., Collett, T.S., Malone, M.J., and the Expedition 311 Scientists. Proc. IODP, 311: Washington, DC (Integrated Ocean Drilling Program Management International, Inc.). doi:10.2204/iodp.proc.311.108.2006 Hunt, J.E., Wynn, R.B., Masson, D.G., Talling, P.J., and Teagle., D.A.H., 2011. Sedimentological and geochemical evidence for multistage failure of volcanic island landslides: a case study from Icod landslide on north Tenerife, Canary Islands. Geochem., Geophys., Geosyst., 12:Q12007. doi:10.1029/2011GC003740 Manga, M., Hornbach, M.J., Le Friant, A., Ishizuka, O., Stroncik, N., Adachi, T., Aljahdali, M., Boudon, G., Breitkreuz, C., Fraass, A., Fujinawa, A., Hatfield, R., Jutzeler, M., Kataoka, K., Lafuerza, S., Maeno, F., Martinez-Colon, M., McCanta, M., Morgan, S., Palmer, M.R., Saito, T., Slagle, A., Stinton, A.J., Subramanyam, K.S.V., Tamura, Y., Talling, P.J., Villemant, B., Wall-Palmer, D., and Wang, F., 2012. Heat flow in the Lesser Antilles island arc and adjacent backarc Grenada basin. Geochem., Geophys., Geosyst., 13:Q08007. doi:10.1029/2012GC004260 Okada, H., and Bukry, D., 1980. Supplementary modification and introduction of code numbers to the low-latitude coccolith biostratigraphic zonation (Bukry, 1973; 1975). Mar. Micropaleontol., 5:321–325. doi:10.1016/0377-8398(80)90016-X Trofimovs, J., Amy, L., Boudon, G., Deplus, C., Doyle, E., Fournier, N., Hart, M.B., Komorowski, J.C., Le Friant, A., Lock, E.J., Pudsey, C., Ryan, G., Sparks, R.S.J., and Talling, P.J., 2006. Submarine pyroclastic deposits formed at the Soufrière Hills Volcano, Montserrat (1995–2003): what happens when pyroclastic flows enter the ocean? Geology, 34(7):549–552. doi:10.1130/G22424.1 Wynn, R.B., and Masson, D.G., 2003. Canary Islands landslides and tsunami generation: can we use turbidite deposits to interpret landslide processes? In Locat, J., and Mienert, J. (Eds.), Submarine Mass Movements and Their Consequences. Adv. Nat. Technol. Hazards Res., 19(2):325–332. doi:10.1007/978-94-010-0093-2_36 Top of page \| Previous \| Next

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