SEDIS - Publications
SEDIS Home
Home
Login
Ikari, Matt J. et al. (2012): Frictional healing and compressibility of sheared sediment from fault zones, sites C0004 and C0007
Leg/Site/Hole:
Related Expeditions:
IODP 316
IODP 314 C0004
IODP 316 C0004
IODP 316 C0007
Identifier:
ID:
2012-071774
Type:
georefid
ID:
10.2204/iodp.proc.314315316.219.2012
Type:
doi
Creator:
Name:
Ikari, Matt J.
Affiliation:
Pennsylvania State University, Department of Geosciences, University Park, PA, United States
Role:
author
Name:
Knuth, Matthew W.
Affiliation:
University of Wisconsin at Madison, United States
Role:
author
Name:
Marone, Chris
Affiliation:
Ecole Nationale Supeieure de Geologie, France
Role:
author
Name:
Saffer, Demian M.
Affiliation:
Chungnam National University, South Korea
Role:
author
Identification:
Title:
Frictional healing and compressibility of sheared sediment from fault zones, sites C0004 and C0007
Year:
2012
Source:
In: Kinoshita, Masataka, Tobin, Harold, Thu, Moe Kyaw, Gaillot, Philippe, Bourlange, Sylvain, Chang, Chandong, Conin, Marianne, Gulick, Sean, Rodriguez, Maria Jose Jurado, Martin, Kylara M., McNeill, Lisa, Miyakawa, Ayumu, Moore, J. Casey, Nakamura, Yasuyuki, Saito, Saneatsu, Sawyer, Dale S., Tudge, Joanne, Yamada, Yasuhiro, Ashi, Juichiro, Lallemant, Siegfried, Masago, Hideki, Behrmann, Jan H., Boeckel, Babette, Byrne, Timothy, Calves, Gerome, Famin, Vincent, Guo, Junhua, Hashimoto, Yoshitaka, Hayashi, Hiroki, Henry, Pierre, Hirono, Tetsuro, Hulme, Samuel M., Kaksonen, Anna Henriikka, Kanagawa, Kyuichi, Kanamatsu, Toshiya, Kopf, Achim, Lewis, Jonathan C., Likos, William John, Pares, Josep Maria, Saito, Hiroyuki, Schmidt-Schierhorn, Friederike, Tomaru, Hitoshi, Underwood, Michael, Zhu, Wen-Lu, Kimura, Gaku, Screaton, Elizabeth J., Curewitz, Daniel, Chester, Frederick, Fabbri, Olivier, Fergusson, Chris, Girault, France E., Goldsby, David, Harris, Robert, Inagaki, Fumio, Jiang, Tao, Kitamura, Yujin, Knuth, Matthew W., Li Chun-Feng, Liljedahl, Lillemor Claesson, Louis, Laurent, Milliken, Kitty, Nicholson, Uisdean, Riedinger, Natascha, Sakaguchi, Arito, Solomon, Evan, Strasser, Michael, Su Xin, Tsutsumi, Akito, Ujiie, Kohtaro, Yamaguchi, Asuka, Zhao, Xixi, Proceedings of the Integrated Ocean Drilling Program; NanTroSEIZE Stage 1; investigations of seismogenesis, Nankai Trough, Japan; Expeditions 314, 315, and 316 of the riser drilling platform from and to Shingu, Japan; Sites C0001-C0006, 21 September-15 November 2007; and Sites C0001 and C0002, 16 November-18 December 2007; and Sites C0004 and C0006-C0008, 19 December 2007-5 February 2008
Publisher:
IODP Management International, Washington, DC, United States
Volume:
314/315/316
Issue:
Pages:
1-19
Abstract:
We conducted shearing tests on samples spanning key fault zones recovered from Integrated Ocean Drilling Program (IODP) Sites C0004 and C0007 from Expedition 316 to the Nankai Trough offshore Japan. Results of slide-hold-slide and normal stress stepping procedures allow quantification of frictional healing, time-dependent compaction, and compressibility of sheared gouge layers. Samples were sheared as thin layers in the double-direct shear configuration at 25 degrees C in a true-triaxial pressure vessel at constant effective normal stress of 25 MPa and pore pressure of 5 MPa using a water-based brine saturated with 3.5 wt% NaCl. We monitored the poromechanical drainage state during shear by holding the pore pressure at the upstream end of the sample at 5 MPa while monitoring the downstream pore pressure. Friction constitutive behavior was determined using slide-hold-slide tests in which hold times ranged from 1 to 1000 s. Frictional healing rates range from approximately 0.003 to 0.008 per decade, with slightly higher rates measured for samples from Site C0004 than from Site C0007. Both sites exhibit similar compaction rates of approximately 0.002-0.007 per decade during holds. Both frictional healing and compaction correlate very well with the logarithm of hold time, with R (super 2) > 0.95. For Site C0004 samples, compressibility was found to be approximately 1-4 GPa (super -1) . At Site C0004, compaction rates and compressibility are elevated in the vicinity of the fault zone. At Site C0007, healing rates decrease, and compaction rates increase, with increasing depth.
Language:
English
Genre:
Serial
Rights:
URL:
http://publications.iodp.org/proceedings/314_315_316/ERR/CHAPTERS/314315316_219.PDF
Coverage:
Geographic coordinates:
North:33.1300
West:136.4300
East: 136.4757
South:33.0114
Keywords:
Engineering geology; Asia; boreholes; compaction; compressibility; continental margin; cores; elastic constants; Expedition 316; experimental studies; Far East; friction; Honshu; Integrated Ocean Drilling Program; IODP Site C0004; IODP Site C0007; Japan; Kii Peninsula; laboratory studies; marine sediments; mechanical properties; Nankai Trough; NanTroSEIZE; North Pacific; Northwest Pacific; Pacific Ocean; rates; sediments; shear stress; shear tests; soil mechanics; West Pacific; Young's modulus;
.
Copyright © 2006-2007 IODP-MI