Seismic slip propagation to the updip end of plate boundary subduction interface faults: Vitrinite reflectance geothermometry on integrated ocean drilling program nantro SEIZE cores

Geology

Volumn 39, Issue 4, 2011, Pages 395-398

  Sakaguchi, Arito ^a   Chester, Frederick ^b   Curewitz, Daniel ^c   Fabbri, Olivier ^d   Goldsby, David ^e   Kimura, Gaku ^f   Li, Chun Feng ^g   Masaki, Yuka ^h   Screaton, Elizabeth J ⁱ   Tsutsumi, Akito ^j   Ujiie, Kohtaro ^k   Yamaguchi, Asuka ^h  

^a JAPAN AGENCY FOR MARINE EARTH SCIENCE AND TECHNOLOGY   (Japan)

^b TEXAS A AND M UNIVERSITY   (United States)

^c SYRACUSE UNIVERSITY   (United States)

^d UNIVERSITÉ DE FRANCHE COMTÉ   (France)

^e BROWN UNIVERSITY   (United States)

^f UNIVERSITY OF TOKYO   (Japan)

^g TONGJI UNIVERSITY   (China)

^h KOCHI UNIVERSITY   (Japan)

ⁱ UNIVERSITY OF FLORIDA   (United States)

^j KYOTO UNIVERSITY   (Japan)

^k UNIVERSITY OF TSUKUBA   (Japan)

more..

Author keywords

[No Author keywords available]

Indexed keywords

ACCRETIONARY WEDGE; COSEISMIC SLIPS; FAULT ZONE; FRICTIONAL HEATING; GEOTHERMOMETRY; LOCALIZED TEMPERATURE; OCEAN DRILLING PROGRAMS; PLATE BOUNDARIES; SEA FLOOR; SEISMIC FAULTING; SEISMIC SLIPS; SEISMOGENIC ZONES; SUBDUCTION INTERFACE; VITRINITE REFLECTANCE;

EARTHQUAKES; OFFSHORE DRILLING; REFLECTION; TECTONICS; TSUNAMIS;

OFFSHORE OIL WELLS;

ACCRETIONARY PRISM; COSEISMIC PROCESS; DECOLLEMENT; DIP-SLIP FAULT; EARTHQUAKE MECHANISM; FAULT ZONE; GEOTHERMOMETRY; INTEGRATED APPROACH; OCEAN DRILLING PROGRAM; PLATE BOUNDARY; SEAFLOOR; SEISMICITY; SLIP RATE; SUBDUCTION ZONE; TSUNAMI; VITRINITE REFLECTANCE; WAVE PROPAGATION;

NANKAI TROUGH; PACIFIC OCEAN;

EID: 79954626808     PISSN: 00917613     EISSN: 00917613     Source Type: Journal    
DOI: 10.1130/G31642.1     Document Type: Article

References (19)

1. Ando, M., 1975, Source mechanisms and tectonic significance of historical earthquakes along the Nankai trough, Japan: Tectonophysics, v. 27, p. 119-140, doi: 10.1016/0040-1951(75)90102-X.
2. Baba, T., and Cummins, P.R., 2005, Contiguous rupture areas of two Nankai Trough earthquakes revealed by high-resolution tsunami waveform inversion: Geophysical Research Letters, v. 32, L08305, doi: 10.1029/2004GL022320.
3. Byrne, D., Davis, D., and Sykes, L., 1988, Loci and maximum size of thrust earthquakes and the mechanics of the shallow region of subduction zones: Tectonics, v. 7, p. 833-857, doi: 10.1029/TC007i004p00833.
4. Hirono, T., Ujiie, K., Ishikawa, T., Mishima, T., Hamada, Y., Tanimizu, M., Soh, W., and Kinoshita, M., 2009, Estimation of temperature rise in a shallow slip zone of the megasplay fault in the Nankai Trough: Tectonophysics, v. 478, p. 215-220, doi: 10.1016/j.tecto.2009.08.001.
5. Ichinose, G.A., Thio, H.K., Somerville, P.G., Sato, T., and Ishii, T., 2003, Rupture process of the 1944 Tonankai earthquake (Ms 8.1) from the inversion of teleseismic and regional seismograms: Journal of Geophysical Research, v. 108, no. B10, 2497, doi: 10.1029/2003JB002393.
6. Kanamori, H., 1977, The energy release in great earthquakes: Journal of Geophysical Research, v. 82, p. 2981-2987, doi: 10.1029/JB082i020p02981.
7. Kikuchi, M., Nakamura, M., and Yoshikawa, K., 2003, Source rupture processes of the 1944 Tonankai earthquake and the 1945 Mikawa earthquake derived from low-gain seismograms: Earth, Planets and Space, v. 55, p. 159-172.
8. Kimura, G., Screaton, E.J., and Curewitz, D., and the Expedition 316 Scientists, 2008, Nan-TroSEIZE Stage 1A: NanTroSEIZE shallow megasplay and frontal thrusts: Integrated Ocean Drilling Program Preliminary Report, v. 316, doi: 10.2204/iodp.pr.316.2008.
9. Kinoshita, M., Tobin, H., Ashi, J., Kimura, G., Lallemant, S., Screaton, E.J., Curewitz, D., Masago, H., and Moe, K.T., and the Expedition 314/315/316 Scientists, 2009, Proceedings of the Integrated Ocean Drilling Program, Volume 314/315/316: Washington, D.C, Integrated Ocean Drilling Program Management International, Inc., doi: 10.2204/iodp. proc.314315316.133.2009.
10. Mase, C.W., and Smith, L., 1987, Effects of frictional heating on the thermal, hydrological, and mechanical response of a fault: Journal of Geophysical Research, v. 92, p. 6249-6272, doi: 10.1029/JB092iB07p06249.
11. Moore, G.F., Bangs, N.L., Taira, A., Kuramoto, S., Pangborn, E., and Tobin, H.J., 2007, Threedimensional splay fault geometry and implications for tsunami generation: Science, v. 318, p. 1128-1131, doi: 10.1126/science.1147195.
12. O'Hara, K., Mizoguchi, K., Shimamoto, T., and Hower, J.C., 2006, Experimental frictional heating of coal gouge at seismic slip rates: Evidence for devolatilization and thermal pressurization of gouge fluids: Tectonophysics, v. 424, p. 109-118, doi: 10.1016/j.tecto.2006.07.007.
13. Park, J.-O., Tsuru, T., Kodaira, S., Cummins, P.R., and Kaneda, Y., 2002, Splay fault branching along the Nankai subduction zone: Science, v. 297, p. 1157-1160, doi: 10.1126/science.1074111.
14. Saffer, D., and Marone, C., 2003, Comparison of smectite- and illite-rich gouge frictional properties: Application to the updip limit of the seismogenic zone along subduction megathrusts: Earth and Planetary Science Letters, v. 215, p. 219- 235, doi: 10.1016/S0012-821X(03)00424-2.
15. Sibson, R.H., 1975, Generation of pseudotachylyte by ancient seismic faulting: Royal Astronomical Society Geophysical Journal, v. 43, p. 775-794, doi: 10.1111/j.1365-246X.1975.tb06195.x.
16. Sweeney, J.J., and Burnham, A.K., 1990, Evaluation of a simple model of vitrinite reflectance based on chemical kinetics: American Association of Petroleum Geologists Bulletin, v. 74, p. 1559-1570.
17. Tanioka, Y., and Satake, K., 2001, Detailed coseismic slip distribution of the 1944 Tonankai earthquake estimated from tsunami waveforms: Geophysical Research Letters, v. 28, p. 1075-1078, doi: 10.1029/2000GL012284.
18. Wang, K., and Hu, Y., 2006, Accretionary prisms in subduction earthquake cycles: The theory of dynamic Coulomb wedge: Journal of Geophysical Research, v. 111, B06410, doi: 10.1029/ 2005JB004094.
19. Yonekura, N., 1975, Quaternary tectonic movements in the outer arc on southwest Japan with special reference to seismic crustal deformation: Bulletin of Department of Geography, University of Tokyo, v. 7, p. 19-71.