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- Chapter contents
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Background and objectives
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Operations
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Lithostratigraphy
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Biostratigraphy
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Paleomagnetism
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Physical properties
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Geochemistry and microbiology
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Heat flow
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Downhole logging
- Stratigraphic correlation
- References
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Figures
- F1. Seismic dip profile.
- F2. Map of drilled and proposed sites.
- F3. Lithologic summary.
- F4. Core recovery and lithology, Hole U1354B.
- F5. Core recovery and lithology, Hole U1354C.
- F6. Lithostratigraphic correlation.
- F7. Homogeneous mud lithology, Unit I.
- F8. Additional Unit I lithologies.
- F9. Coarser Unit I lithologies.
- F10. Mineral and textural percentage estimations.
- F11. Correlation of Holocene–Pleistocene succession.
- F12. Sediment correlation based on lithostratigraphy and paleomagnetic ages.
- F13. Planktonic and benthic foraminifer correlation.
- F14. Planktonic foraminiferal abundance.
- F15. Paleodepth interpretation.
- F16. NRM paleomagnetic record, Hole U1354A.
- F17. NRM paleomagnetic record, Hole U1354B.
- F18. NRM paleomagnetic record, Hole U1354C.
- F19. Raw and filtered physical property data.
- F20. Bulk density comparison.
- F21. MS and NGR.
- F22. P-wave velocity.
- F23. L*a*b* color parameters.
- F24. Porosity comparison.
- F25. Bulk density, grain density, porosity, and void ratios.
- F26. Sediment shear strength.
- F27. CH4, C2H6, CO2, and C1/C2 in HS gas.
- F28. Carbonate carbon, TC, TN, TOCDIFF, and TOCDIFF/TN.
- F29. Salinity, chloride, Na, pH.
- F30. Ca, Mg, Mg/Ca, Sr, Sr/Ca, and alkalinity.
- F31. Sulfate and phosphate.
- F32. K, Ba, Li, Si.
- F33. B, Fe, Mn.
- F34. Alkalinity, SO4, Ca, Mg, CH4, Mg/Ca, Ba, PO4.
- F35. Stoichiometry of the sulfate-reduction zone.
- F36. Temperature data.
- F37. Thermal conductivity.
- F38. "Sonic combo" log data vs. physical properties.
- F39. Summary of "sonic combo" logs.
- F40. Spectral natural gamma ray.
- F41. Comparison of downhole and uphole logging passes.
- F42. Comparison of synthetic seismogram and EW00-01 Line 66.
- F43. Depth-adjusted MS and NGR records.
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Tables
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PDF file
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doi:10.2204/iodp.proc.317.106.2011
Site U13541
Expedition 317 Scientists2
Background and objectives
Hole U1354A
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Position: 44°50.8281′S, 171°47.2096′E
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Start hole: 0415 h, 29 December 2009
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End hole: 2300 h, 29 December 2009
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Time on hole (d): 0.78
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Seafloor (drill pipe measurement from rig floor, m DRF): 121.2 (APC mudline)
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Distance between rig floor and sea level (m): 11.4
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Water depth (drill pipe measurement from sea level, m): 109.8
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Total depth (drill pipe measurement from rig floor, m DRF): 206.6
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Total penetration (m DSF): 85.4
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Total length of cored section (m): 83.4
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Total core recovered (m): 84.43
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Core recovery (%): 101
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Total number of cores: 18
Hole U1354B
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Position: 44°50.8367′S, 171°47.2069′E
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Start hole: 2300 h, 29 December 2009
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End hole: 1245 h, 30 December 2009
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Time on hole (d): 0.57
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Seafloor (drill pipe measurement from rig floor, m DRF): 124.8 (APC mudline)
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Distance between rig floor and sea level (m): 11.4
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Water depth (drill pipe measurement from sea level, m): 113.4
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Total depth (drill pipe measurement from rig floor, m DRF): 202.0
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Total penetration (m DSF): 77.2
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Total length of cored section (m): 77.2
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Total core recovered (m): 77.52
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Core recovery (%): 100
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Total number of cores: 15
Hole U1354C
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Position: 44°50.8487′S, 171°47.2080′E
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Start hole: 0700 h, 31 December 2009
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End hole: 1200 h, 2 January 2010
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Time on hole (d): 2.21
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Seafloor (drill pipe measurement from rig floor, m DRF): 124.8 (by proxy, Hole U1354B)
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Distance between rig floor and sea level (m): 11.4
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Water depth (drill pipe measurement from sea level, m): 113.4
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Total depth (drill pipe measurement from rig floor, m DRF): 509.0
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Total penetration (m DSF): 384.2
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Total length of cored section (m): 319.2
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Total core recovered (m): 133.37
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Core recovery (%): 42
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Total number of cores: 35
Integrated Ocean Drilling Program (IODP) Site U1354 (proposed Site CB-02A) is located on the middle outer shelf (112 m water depth) within the Canterbury Bight between landward shelf Site U1353 (proposed Site CB-01A) and outer shelf Site U1351 (proposed Site CB-03B) within the Canterbury Basin drilling transect. Site U1354 is located on dip seismic Profile EW00-01-66 and crossing strike Profile EW00-01-07a (Figs. F1, F2).
The philosophy behind the transect approach is discussed in "Background and objectives" in the "Site U1351" chapter. Site U1354 occupies an intermediate position in the shelf portion of the transect. Lithologies and paleoenvironments were therefore expected to be intermediate between those found at Sites U1351 and U1353.
Site U1354 penetrates a middle Miocene to Holocene section containing seismic sequence boundaries U8–U19 (Lu and Fulthorpe, 2004). All sequence boundaries were penetrated landward of their rollovers or paleoshelf edges with the goal of recovering proximal facies, yielding evidence of shallow-water deposition, and providing optimal paleowater depths from benthic foraminiferal biofacies.
The principal objectives at Site U1354 were
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To sample facies landward of rollovers of progradational seismic sequence boundaries U8–U19 and in particular to use benthic foraminiferal biofacies to estimate paleowater depths both above and below sequence boundaries in order to calculate eustatic amplitudes using two-dimensional backstripping.
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To investigate the facies, paleoenvironments, and depositional processes associated with the sequence stratigraphic model in a proximal setting on a prograding continental margin where sequence architecture is well constrained by seismic imaging.
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