Proc. IODP, 314/315/316, Data report: clay mineral assemblages from the Nankai Trough accretionary prism and the Kumano Basin, IODP Expeditions 315 and 316, NanTroSEIZE Stage 1

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Chapter contents Abstract Introduction Methods Calculations of mineral abundance Sample preparation X-ray diffraction parameters Results Kumano Basin, Site C0002 Shallow megasplay fault, Sites C0001, C0004, and C0008 Frontal thrust, Sites C0006 and C0007 Acknowledgments References Figures F1. Kumano transect region. F2. 3-D seismic in-line section. F3. X-ray diffractograms. F4. Lithostratigraphy, Site C0002. F5. Lithologic units, Site C0002. F6. Lithostratigraphy, Site C0001. F7. Lithologic units, Sites C0001, C0004, and C0008. F8. Lithostratigraphy, Site C0004. F9. Lithostratigraphy, Site C0008. F10. Lithostratigraphy, Site C0006. F11. Lithologic units, Sites C0006 and C0007. F12. Lithostratigraphy, Site C0007. Tables T1. SVD normalization factors. T2. X-ray diffraction for clay-size fraction. T3. Calculated mineral abundances. T4. Maximum, minimum, average, and standard deviation. PDF file			Previous \| Next doi:10.2204/iodp.proc.314315316.202.2012 Acknowledgments This research used samples provided by the Integrated Ocean Drilling Program (IODP). We thank Captains Ichiyama and Onda, as well as the drilling crew, laboratory technicians, and fellow scientists aboard D/V Chikyu for their dedicated assistance during IODP Expeditions 315 and 316. M. Strasser provided the samples of mudstone clasts and matrix from Site C0008. Funding was granted by the Consortium for Ocean Leadership, U.S. Science Support Program (grant T315B58 to Underwood and grant T315C58 to Guo) and the National Science Foundation (grant OCE-07518190). U. Shriniwar, H. Banno, D.M. Hillix, M. Rader, and H. Wu assisted with sample preparation and data reduction. We thank Cedric John for his review of the manuscript. Top of page \| Previous \| Next

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