Results 101 to 110 of about 416 (127)

Preliminary results of structural analyses of core samples recovered from NanTroSEIZE Stage 1A

Annual Meeting of the Geological Society of Japan, 2008
Yamaguchi, Asuka, Kanagawa, Kyuichi, Ujiie, Kohtaro, IODP Exp. 314 & 315 & 316, Shipboard Scientist   +3 more
openaire   +1 more source

Evolution of the accretionary prism and the forearc basin of the Nankai Trough off Kumano? Shipboard results of stratigraphy and age from NanTroSEIZE Stage 1A Expeditions [PDF]

, 2008
NanTroSEIZE Stage 1A Shipboard Scientists, Kimura, G., Kanamatsu, T., Ashi, J., Kinoshita, M., Masago, H., Kitamura, Yujin, Curewitz, D., Lallemant, S., Screaton, E., Moe, K. T., Tobin, H.   +11 more
core  

Preliminary report of physical properties measurements from IODP NanTroSEIZE Stage 1A, Expedition 316

Annual Meeting of the Geological Society of Japan, 2008
Tsutsumi, Akito, Goldsby, David, Harris, Robert, Jiang, Tao, Knuth, Matt, Louis, Laurent, Expedition 314-316, Scientist   +6 more
openaire   +3 more sources

Paleo-thermal environment of fault zone in IODP NanTroSEIZE Exp316, and new vitrinite reflectance analysis

Annual Meeting of the Geological Society of Japan, 2008
Sakaguchi, Arito, IODP Exp.316 Shipboard Scientists, IODP Exp.316 Shipboard Scientists   +1 more
openaire   +1 more source

Paleo-temperature of fault zone in IODP NanTroSEIZE Exp316 based on vitrinite reflectance analysis

Annual Meeting of the Geological Society of Japan, 2009
openaire   +1 more source

Engineering Specifications on LTBMS Telemetry System for NanTroSEIZE 3.5 km Riser Hole

Engineering Specifications on LTBMS Telemetry System for NanTroSEIZE 3.5 km Riser Hole
openaire  

Present‐day principal horizontal stress orientations in the Kumano forearc basin of the southwest Japan subduction zone determined from IODP NanTroSEIZE drilling Site C0009 [PDF]

Geophysical Research Letters, 2010
A 1.6 km riser borehole was drilled at site C0009 of the NanTroSEIZE, in the center of the Kumano forearc basin, as a landward extension of previous drilling in the southwest Japan Nankai subduction zone.
Weiren Lin, J Casey Moore, Lisa C Mcneill   +2 more
exaly   +3 more sources

Quantification of free gas in the Kumano fore-arc basin detected from borehole physical properties: IODP NanTroSEIZE drilling Site C0009 [PDF]

Geochemistry, Geophysics, Geosystems, 2011
The Kumano fore-arc basin overlies the Nankai accretionary prism, formed by the subduction of the Philippine Sea Plate beneath the Eurasian plate offshore the Kii Peninsula, SW Honshu, Japan.
Mai-Linh Doan, Marianne Conin, Pierre Henry   +2 more
exaly   +3 more sources

Structural styles across the Nankai accretionary prism revealed from LWD borehole images and their correlation with seismic profile and core data: Results from NanTroSEIZE Stage 1 expeditions [PDF]

Geochemistry, Geophysics, Geosystems, 2011
Four drill sites of IODP NanTroSEIZE Stage 1 Expedition transected the Nankai Trough, offshore SW Japan, from the deformation front to the Kumano fore-arc basin.
Yasuhiro Yamada, Lisa C Mcneill, J Casey Moore   +2 more
exaly   +3 more sources

Growth of borehole breakouts with time after drilling: Implications for state of stress, NanTroSEIZE transect, SW Japan [PDF]

Geochemistry, Geophysics, Geosystems, 2011
Resistivity at the bit tools typically provide images of wellbore breakouts only a few minutes after the hole is drilled. In certain cases images are taken tens of minutes to days after drilling of the borehole.
J Casey Moore, Chandong Chang, Lisa C Mcneill   +2 more
exaly   +3 more sources