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- Contents
- Title page
- Publisher′s notes
- Abstract
- Schedule for Expedition 356
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Introduction
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Background
- Scientific objectives
- Drilling and coring strategy
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Downhole measurements strategy
- Risks and contingency
- Sampling and data sharing strategy
- References
- Tables
- Figures
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Site summaries
- Appendix figures
- AF1. Bathymetric map, Sites NWS-6A, NWS-5A, NWS-13A, and NWS-12A.
- AF2. Multichannel seismic profile, Site NWS-6A.
- AF3. Multichannel seismic profile, Sites NWS-6A and NWS-13A.
- AF4. Multichannel seismic profile, Site NWS-5A.
- AF5. Multichannel seismic profile, Sites NWS-5A and NWS-12A.
- AF6. Bathymetric map, Sites NWS-3A, NWS-4A, NWS-9A, NWS-10A and NWS-11A.
- AF7. Multichannel seismic profile, Sites NWS-10A and NWS-11A.
- AF8. Multichannel seismic profile, Site NWS-4A.
- AF9. Multichannel seismic profile, Sites NWS-3A and NWS-9A.
- AF10. Multichannel seismic profile, Site NWS-9A.
- AF11. Bathymetric map, Sites NWS-1A, NWS-2A, NWS-7A, and NWS-8A.
- AF12. Multichannel seismic profile, Sites NWS-2A and NWS-8A.
- AF13. Multichannel seismic profile, Site NWS-8A.
- AF14. Multichannel seismic profile, Site NWS-1A.
- AF15. Multichannel seismic profile, Sites NWS-1A and NWS-7A.
- Expedition scientists and scientific participants
- PDF file
- Errata
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doi:10.14379/iodp.sp.356.2014
Site summaries (continued)
Site NWS-12A
Priority:
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Alternate
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Position:
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27.2802°S, 112.8881°E
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Water depth (m):
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200
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Target drilling depth (mbsf):
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366
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Approved maximum penetration (mbsf):
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366
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Survey coverage (track map; seismic profile):
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Track map (Fig. AF1)
Seismic profile (Fig. AF5)
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Objective(s):
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An alternate to Site NWS-5A, this site is located at the northern edge of the modern winter-dominated rainfall zone of southwestern Australia. It is south of a climatic divide between the Australian monsoon–dominated north and the westerly wind-driven, winter rainfall–dominated south. This site is near the southern end of the north-south latitudinal transect and may provide a shelf to shelf-edge record of the tropical–subtropical transition related to Leeuwin Current activity. It is also influenced by the anticlockwise, colder West Australian Current gyre and the relative influence of this gyre versus the Leeuwin Current produces variations in paleoproductivity that may be documented over millions of years. Subsidence rates in this region are estimated to be significantly less than in the Carnarvon Basin further north because of variations in mantle dynamic subsidence between the Perth and Carnarvon Basins. Paleobathymetric analyses may produce the first detailed greater than million year subsidence record for this part of the West Australian margin, where previous subsidence estimates only extend to 125 ka.
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Drilling program:
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Triple APC, double XCB
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Logging program or downhole measurements program:
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Triple combo, FMS, VSP
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Nature of rock anticipated:
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Calcarenites, calcilutites
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