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- Chapter contents
- Background and objectives
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Operations
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Lithology
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Structural geology
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Biostratigraphy
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Paleomagnetism
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Inorganic geochemistry
- Salinity, chloride, and sodium
- Pore fluid constituents controlled by microbially mediated reactions
- Major cations (Ca, Mg, and K)
- Minor elements (B, Li, H4SiO4, Sr, Ba, Mn, and Fe)
- Trace elements (Rb, Cs, V, Cu, Zn, Mo, Pb, U, and Y)
- δ18O
- Summary
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Organic geochemistry
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Microbiology and biogeochemistry
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Physical properties
- References
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Figures
- F1. Hole locations.
- F2. 3-D seismic profiles.
- F3. Core recovery and sand and silt distribution.
- F4. XRD data.
- F5. Core examples.
- F6. Pyrite in sand.
- F7. Ash layers and volcanic clasts.
- F8. Gravel and sand.
- F9. CT number.
- F10. Distribution of planar structures.
- F11. Projections of poles to bedding surfaces.
- F12. Normal faults.
- F13. Healed faults.
- F14. Projections of poles to faults.
- F15. Age and depth, Hole C0008A.
- F16. Age and depth, Hole C0008C.
- F17. Radiolarian and nannofossil zones and events.
- F18. Magnetic susceptibility and NRM, Hole C0008A.
- F19. Magnetic susceptibility and NRM, Hole C0008C.
- F20. AF demagnetization.
- F21. Thermal demagnetization.
- F22. Magnetic inclination, polarity, biostratigraphy, and lithology, Hole C0008A.
- F23. Magnetic inclination, polarity, biostratigraphy, and lithology, Hole C0008C.
- F24. Salinity, Cl, Na, and Na/Cl.
- F25. pH, SO4, alkalinity, and Ba.
- F26. NH4, PO4, and Br.
- F27. Ca, Mg, K, and H4SO4, Rb, and Cs.
- F28. Li, B, and Br.
- F29. Mg, Fe, Mo, Pb, Mn, U, and Y.
- F30. δ18O profile.
- F31. Methane, ethane, and C1/C2.
- F32. CaCO3, TOC, TN, C/N ratio, TS.
- F33. Microbial cell abundance.
- F34. Density and porosity.
- F35. Discrete sample measurements.
- F36. Thermal data, Hole C0008A.
- F37. Thermal data, Hole C0008C.
- F38. Temperature time series, Hole C0008A.
- F39. Temperature time series, Hole C0008C.
- F40. Shear strength.
- F41. L*, a*, and b*, Hole C0008A.
- F42. L*, a*, and b*, Hole C0008C.
- F43. Magnetic susceptibility.
- F44. NGR values with depth.
- F45. NGR counts from cores.
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Tables
- T1. Coring summary, Hole C0008A.
- T2. Coring summary, Holes C0008B and C0008C.
- T3. Lithologic summary, Hole C0008A.
- T4. Lithologic summary, Hole C0008C.
- T5. XRD data, Holes C0008A and C0008C.
- T6. XRD mineralogy.
- T7. Calcareous nannofossil range chart, Hole C0008A.
- T8. Calcareous nannofossil range chart, Hole C0008C.
- T9. Nannofossil events, Hole C0008A.
- T10. Nannofossil events, Hole C0008C.
- T11. Uncorrected geochemistry.
- T12. Uncorrected minor elements.
- T13. Uncorrected trace elements and δ18O.
- T14. Headspace hydrocarbon gases.
- T15. Hydrocarbon gas analysis.
- T16. CaCO3, TOC, TN, C/N ratio, TS.
- T17. Sample depth and processing, Hole C0008A.
- T18. Sample depth and processing, Holes C0008B and C0008C.
- T19. Thermal conductivity, Hole C0008A.
- T20. Thermal conductivity, Hole C0008C.
- T21. Temperature measurements, Hole C0008A.
- T22. Temperature measurements, Hole C0008C.
- PDF file
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doi:10.2204/iodp.proc.314315316.136.2009
Expedition 316 Site C00081
Expedition 316 Scientists2
Background and objectives
Integrated Ocean Drilling Program (IODP) Site C0008 was proposed as contingency Site NT2-10 in an addendum to the IODP Expedition 316 Scientific Prospectus (Kimura et al., 2007). This site examined the slope basin seaward of the splay fault penetrated at IODP Site C0004. Site C0008 is ~1 km seaward of Site C0004 (Figs. F1, F2). This contingency site was selected during Expedition 316 because of its good fit with the available time window and the scientific objectives of Expedition 316. Recovered material from this basin will help assess the timing and relative age of past fault motions via identification of provenance and age of basin material. The age difference between newly deposited basin sediments and older uplifted fault blocks will constrain the deformation history. The permeability and geotechnical properties of the basin material will provide reference properties for the section overrun by the splay fault. Shipboard and shore-based study of these properties will constrain the fluid flow and consolidation response of the footwall to splay fault movement. In situ temperature data were also collected to assess the thermal gradient and heat flow in this area for comparison with the temperatures recorded at Site C0004.
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