scholarly journals A new perspective of the subduction zone derived from the Ocean Drilling Program for the Nankai Trough Seismogenic Zone Experiment (NanTroSEIZE)

2018 ◽  
Vol 124 (1) ◽  
pp. 47-65
Author(s):  
Gaku Kimura ◽  
Masataka Kinoshita ◽  
Kyuichi Kanagawa ◽  
Toshiya Kanamatsu ◽  
Jyuichiro Ashi ◽  
...  
Keyword(s):  
Subduction Zone ◽  
Nankai Trough ◽  
Seismogenic Zone ◽  
Ocean Drilling Program ◽  
Ocean Drilling ◽  
New Perspective

scholarly journals The IODP Expedition 332 : Eyes on the Prism, The NanTroSEIZE Observatories

2012 ◽  
Vol 14 ◽  
pp. 34-38 ◽  
Author(s):  
S. T. Toczko ◽  
A. J. Kopf ◽  
E. Araki ◽  
Keyword(s):  
Nankai Trough ◽  
Temperature Data ◽  
Seismogenic Zone ◽  
Plate Boundaries ◽  
Transient Pressure ◽  
Ocean Drilling Program ◽  
Ocean Drilling ◽  
Integrated Ocean Drilling Program ◽  
Drilling Project

The Nankai Trough Seismogenic Zone Experiment (NanTroSEIZE) is a major long-term drilling project designed to investigate the seismogenic behavior of subduction zone plate boundaries. Integrated Ocean Drilling Program (IODP) Expedition 332 deployed a long-term borehole monitoring system (LTBMS), an advanced Circulation Obviation Retrofit Kit (CORK)-type observatory. The recovery of pressure and temperature data from a temporary observatory (SmartPlug) deployed during IODP Expedition 319 helped prove the SmartPlug concept. The permanent LTBMS was deployed n the upper 1000 m of Site C0002, while the SmartPlug was recovered from Site C0010 and replaced with a more capable "GeniusPlug", incorporating an extension with a geochem-ical sampler and biological experiment to the original SmartPlug design. SmartPlug pressure and temperature data showed signs of transient pressure events. <br><br> doi:<a href="http://dx.doi.org/10.2204/iodp.sd.14.04.2012" target="_blank">10.2204/iodp.sd.14.04.2012</a>

scholarly journals Diversity of prokaryotes and methanogenesis in deep subsurface sediments from the Nankai Trough, Ocean Drilling Program Leg 190

2004 ◽  
Vol 6 (3) ◽  
pp. 274-287 ◽  
Author(s):  
Carole J. Newberry ◽  
Gordon Webster ◽  
Barry A. Cragg ◽  
R. John Parkes ◽  
Andrew J. Weightman ◽  
...  
Keyword(s):  
Nankai Trough ◽  
Ocean Drilling Program ◽  
Deep Subsurface ◽  
Ocean Drilling ◽  
Subsurface Sediments

scholarly journals IODP Expedition 333: Return to Nankai Trough Subduction Inputs Sites and Coring of Mass Transport Deposits

2012 ◽  
Vol 14 ◽  
pp. 4-17 ◽  
Author(s):  
P. Henry ◽  
T. Kanamatsu ◽  
K. T. Moe ◽  
M. Strasser ◽  
Keyword(s):  
Heat Flow ◽  
Mass Transport ◽  
Nankai Trough ◽  
Seismogenic Zone ◽  
Ocean Drilling Program ◽  
Flow Measurements ◽  
Integrated Ocean Drilling Program ◽  
Shikoku Basin ◽  
Lower Temperature ◽  
Mass Transport Deposits

Integrated Ocean Drilling Program (IODP) Expedition 333 returned to two sites drilled during IODP Expedition 322 on the ocean side of the Nankai Trough to pursue the characterization of the inputs to the Nankai subduction and seismogenic zone, as part of the Nankai Trough Seismogenic Experiment (NanTroSEIZE) multi-expedition project. Site C0011 is located at the seaward edge of the trench and Site C0012 on a basement high, Kashinozaki Knoll (Fig. 1). The main objectives of drilling again at these sites were to fill coring gaps in the upper part (<350 m) of the sedimentary sequence, to measure heat flow, and to core the oceanic basement to a greater depth on the Knoll. New results include the observation of a diagenetic boundary within the Shikoku Basin sediments that may be compared to one documented further west by ODP Legs 131, 190 and 196 but occurs here at a lower temperature. Borehole heat flow measurements confirm spatial variations in the Shikoku Basin that were indicated by short probe surveys. Heat flow variations between topographic highs and lows may be related to fluid convection within the basement. This expedition also included the objectives of the Nankai Trough Submarine LandSLIDE history (NanTroSLIDE) Ancillary Project Letter (APL) and cored at Site C0018 a pile of mass transport deposits on the footwall of the megasplay fault, a major out of sequence thrust that presumably slips coseismically during large subduction earthquakes. This brought new insight on the timing of these mass wasting events and on the deformation within the sliding slope sediments. <br><br> doi:<a href="http://dx.doi.org/10.2204/iodp.sd.14.01.2012" target="_blank">10.2204/iodp.sd.14.01.2012</a>

scholarly journals IODP Expedition 322 Drills Two Sites to Document Inputs to The Nankai Trough Subduction Zone

2010 ◽  
Vol 10 ◽  
pp. 14-25 ◽  
Author(s):  
M. B. Underwood ◽  
S. Saito ◽  
Y. Kubo ◽  
Keyword(s):  
Nankai Trough ◽  
Seismogenic Zone ◽  
Sedimentation Rates ◽  
Ocean Drilling Program ◽  
Plate Interface ◽  
Integrated Ocean Drilling Program ◽  
Shikoku Basin ◽  
Dehydration Reactions ◽  
Basement High ◽  
Geochemical Profiles

The primary goals during Expedition 322 of the Integrated Ocean Drilling Program were to sample and log the incoming sedimentary strata and uppermost igneous basement of the Shikoku Basin, seaward of the Nankai Trough (southwestern Japan). Characterization of these subduction inputs is one piece of the overall science plan for the Nankai Trough Seismogenic Zone Experiment. Before we can assess how various material properties evolve down the dip of the plate interface, and potentially change the fault’s behavior from stable sliding to seismogenic slip, we must determine the initial pre-subduction conditions. Two sites were drilled seaward of the trench to demonstrate how facies character and sedimentation rates responded to bathymetric architecture. Site C0011 is located on the northwest flank of a prominent basement high (Kashinosaki Knoll), and Site C0012 is located near the crest of the seamount. Even though significant gaps remain in the coring record, and attempts to recover wireline logs at Site C0012 failed, correlations can be made between stratigraphic units at the two sites. Sedimentation rates slowed down throughout the condensed section above the basement high, but the seafloor relief was never high enough during the basin’s evolution to prevent the accumulation of sandy turbidites near the crest of the seamount. We discovered a new stratigraphic unit, the middle Shikoku Basin facies, which is typified by late Miocene volcaniclastic turbidites. The sediment-basalt contact was recovered intact at Site C0012, giving a minimum basement age of 18.9 Ma. Samples of interstitial water show a familiar freshening trend with depth at Site C0011, but chlorinity values at Site C0012 increase above the values for seawater toward the basement contact. The geochemical trends at Site C0012 are probably a response to hydration reactions in the volcaniclastic sediment and diffusional exchange with seawater-like fluid in the upper igneous basement. These data are important because they finally establish an authentic geochemical reference site for Nankai Trough, unaffected by dehydration reactions, and they provide evidence for active fluid flow within the upper igneous crust. Having two sets of geochemical profiles also shows a lack of hydrogeological connectivity between the flank and the crest of the Kashinosaki Knoll. <br><br> doi:<a href="http://dx.doi.org/10.2204/iodp.sd.10.02.2010" target="_blank">10.2204/iodp.sd.10.02.2010</a>

scholarly journals New insights into deformation and fluid flow processes in the Nankai Trough accretionary prism: Results of Ocean Drilling Program Leg 190

2001 ◽  
Vol 2 (10) ◽  
pp. n/a-n/a ◽  
Author(s):  
Gregory F. Moore ◽  
Asahiko Taira ◽  
Adam Klaus ◽  
Luann Becker ◽  
Babette Boeckel ◽  
...  
Keyword(s):  
Fluid Flow ◽  
Nankai Trough ◽  
Accretionary Prism ◽  
Ocean Drilling Program ◽  
Ocean Drilling ◽  
Flow Processes
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