发震带试验（SEIZE）

doi:10.11867/j.issn.1001-8166.2005.08.0823

对发震带试验计划(SEIZE)以及南海（Nankai）海槽的发震带钻探计划（NanTroSEIZE）进行了综述。SEIZE作为大陆边缘计划(MARGINS)的重要研究内容和综合大洋钻探计划（IODP）的优先研究领域，重点对世界主要俯冲发震带进行研究。SEIZE的主要研究内容包括：①凸凹体的物理性质；②在地震周期里，应力、应变和孔隙流体成分随时间的变化；③在俯冲逆冲断层上，发震带上界和下界的确定；④引起海啸的发震带的特征；⑤大型逆冲带地震在物质转换过程中所起的作用。NanTroSEIZE将成为IODP第一个基于立管钻探的计划，也是科学大洋钻探历史上第一个分期实施的复合钻探计划；钻入发震带的复合钻探计划将最终验证关于发震带的各种假说。 

关键词: 流体, 南海（Nankai）海槽, 综合大洋钻探计划（IODP）, 发震带试验(SEIZE), 俯冲带

This paper gives a brief introduction to the Seimogenic Zone Experiment (SEIZE) and Nankai Trough Seismogenic Zone Experiment (NanTroSEIZE). As one of major initiatives of the NSF-MARGINS Program and Integrated Ocean Drilling Program (IODP), SEIZE focuses its research on major subduction seismogenic belts in the world. The main study areas of SEIZE include: (1)physical nature of asperity; (2)temporal relationships among stress, strain, and pore fluid pressure throughout the earthquake cycle; (3)controls on the updip and downdip limits of the seismogenic zone of subduction thrusts; (4)nature of tsunamigenic earthquake zones; (5)role of large thrust earthquake in mass flux. As the first riser drilling proposal, NanTroSEIZE was highly ranked. It is also the first complex drilling proposal in the history of scientific ocean drilling program. Drilling through the seismogenic zone based on this complex drilling proposal will provide evidences to validate many hypotheses of the seismogenic zone.

Key words: Seismogenic Zone Experiment (SEIZE), Subduction zone, Fluid, Nankai Trough, Integrated Ocean Drilling Program (IODP). 

中图分类号:

P315

[1] IPSC. Earth, Ocean and life-Integrated Ocean Drilling Program, Initial Science Plan, 2003-2013 [M].Earth Sciences Division of NSFC translate.Shanghai: Tongji University Press,2003. [IODP科学规划委员会编著.IODP初始科学计划2003—2013 [M].国家自然科学基金委员会地球科学部等译.上海: 同济大学出版社, 2003.]
[2] Margins Steering Committee. The Seismogenic Zone Experiment (SEIZE): Science Plan [EB/OL]. http://www.geo.ua.edu/AMG/OldMargins/SEIZE_sci_plan.html#, 2004-10-10.
[3] Liu Xinyue , Wang Qing , Zhou Zuyi . IODP in Japan [J]. Advances in Earth Science, 2004, 19 (4):552-557. [刘新月, 王清, 周祖翼.日本的综合大洋钻探计划（IODP）[J]. 地球科学进展, 2004, 19 (4):552-557.]
[4] Lay T, Astiz L, Kanamori H, et al. Temporal variation of large intraplate earthquakes in coupled subduction Zone[J]. Physics of the Earth and Planetary Interiors, 1989, 54: 258-312.
[5] The Margins Office at Lamont-Doherty Earth Observatory of Columbia University. NSF MARGINS Program-Science Plan.2004 [M/OL]. http://www.margins.wustl.edu/Publications/SciencePlans/MARGINS_SciencePlans2004.pdf, 2004-10-02.
[6] Protti M, Mcnally K, Pacheco J, et al. The March 25, 1990 (M (W) =7.0 M (L) =6.8), earthquake at the entrance of the Nicoya Gulf, Costa-Rica-Its prior activity, foreshocks, and triggered seismicity [J]. Journal of Geophysical Research-Solid Earth, 1995, 100(B10): 20 345-20 358. 
[7] Bilek S L, Schwartz S Y, Deshon H R, et al. Control of seafloor roughness on earthquake rupture behavior[J].Geology,2003, 31: 455-458. 
[8] Ruff L J. Asperity Distributions and large Earthquake occurrence in subduction zones[J]. Tectonophysics, 1992, 211: 61-83. 
[9] McCaffrey R. Statistical significance of the seismic coupling coefficient[J]. Bulletin of the Seismological Society of America, 1997, 87:1 069-1 073. 
[10] Heki K, Miyazake S I, Tsuji H, et al. Silent fault slip following an interplate thrust earthquake at the Japan Trench[J]. Nature, 1997, .386: 595-598. 
[11] Hirose H, Hirahara K, Kimata F, et al. A slow thrust slip event following the two 1996 hyuganada earthquakes beneath the Bungo channel, Southwest Japan[J]. Geophysical Research Letters, 1999, 26: 3 237-3 240. 
[12] Ozawa S, Murakami M, Tada T, et al. Time-dependent inversion study of the slow thrust event in the Nankai Trough Subduction Zone, Southwestern Japan[J]. Journal of Geophysical Research-Solid Earth, 2001, 106: 787-802. 
[13] Burgmann R, Kogan M G, Levin V E, et al. Rapid Aseismic Moment Release Following the 5 December, 1997 Kronotsky, Kamchatka, Earthquake[J]. Geophysical Research Letters, 2001, 28: 213-234. 
[14] Dragert G, Wang K, James T S, et al. A silent slip event on the deeper Cascadia subduction interface[J]. Science, 2001, 292:1 225-1 528.
[15] Linde A T, Silver P G. Elevation changes and the great 1960 chilean earthquake-support for Aseismic Slip[J]. Geophusical Research Letters, 1989,16:1 305-1 308. 
[16] Geller R J, Jackson D D, Kagan Y Y, et al. Geoscience-earthquakes cannot be predicted[J]. Science, 1997,275:1 616-1 617.
[17] Masterlark T, DeMets C, Wang H F, et al. Homogeneous vs heterogeneous subduction zone models: Coseismic and postseismic deformation[J]. Geophysical Research Letters, 2001, 28: 4 047-4 050. 
[18] Hyndman R D, Wang K. Thermal constraints on the zone of major thrust earthquake failure—The Cascadia Subduction Zone[J]. Journal of Geophysical Research-Solid Earth, 1993, 98: 2 039-2 060.
[19] Hyndman R D, Wang K, Yamano M. Thermal constraints on the seismogenic portion of the southwestern Japan subduction thrust[J]. Journal of Geophysical Research-Solid Earth, 1995, 100: 15 373-15 392. 
[20] Fisher D, Byrne Tim. The character and distribution of mineralized fractures in the Kodiak formation, Alaska-implications for fluid-flow in an underthrust sequence[J]. Journal of Geophysical Research-Solid Earth and Planets, 1990, 95: 9 069-9 080.
[21] Moore J C, Saffer D. Updip limit of the seismogenic zone beneath the accretionary Prism of southwest Japan: An Effect of diagenetic to low-grade metamorphic processes and increasing effective stress[J].Geology, 2001, 29: 183-186. 
[22] Ujiie K. Evolution and kinematics of an ancient decollement zone, melange in the Shimanto accretionary complex of Okinawa Island, Ryukyu Arc[J]. Journal of Structural Geology, 2002, 24: 937-952. 
[23] Tsunami Earthquakes [EB/OL]. http://www.sciencemag.org/cgi/content/full/278/5338/598, 2005-02-12.
[24] Bilek S L, Lay, et al. Tsunami earthquakes possibly widespread manifestations of frictional conditional stability[J]. Geophysical Research Letters, 2002, 29: art. no.-1673.
[25] Hickman S, Sibson R, Bruhn R. Introduction to Special Section-Mechanical Involvement of Fluids in Faulting[J]. Journal of Geophysical Research-Solid Earth, 1995, 100: 12 831-12 840.
[26] Raleigh C B, Healy J H, Bredehoeft J D. Experiment in an earthquake control at Rangely, Colorado[J]. Science, 1976,191:1 230-1 237.
[27] Johnson P A, Mcevilly T V. Parkfield seismicity-fluid-driven[J]. Journal of Geophysical Research-Solid Earth, 1995,100:12 937-12 950. 
[28] Hubbert M K, Rubey M K, Rubey W W. Role of fluid pressure in the mechanics of overthrust faulting I: Mechanics of fluid-filled porous solids and its application to overthrust Faulting[J]. GSA Bulletin, 1959, 70: 115-166. 
[29] Davis D, Suppe J, Dahlen F A. Mechanics of Fold-and-Thrust Belts and Accretionary Wedges[J]. Journal of Geophysical Research, 1983, 88: 1 153-1 172.
[30] Scholz C H. Earthquakes and friction laws[J]. Nature, 1998, 391: 37-42.
[31] Saffer D M, Bekins B A. Hydrologic Controls on the Morphology and Mechanics of Accretionary Wedges[J]. Geology, 2002, 30: 271-274. 
[32] Revil A, Cathles L M. Fluid Transport by Solitary Waves Along Growing Faults-A Field Example from the South Eugene Island Basin, Gulf of Mexico[J]. Earth and Planetary Science Letters, 2002, 202(2): 321-335.
[33] Song Haibin, Matsuba Y O, Kuramot S. A summary of gas hydrate researches in adjacent sea regions around Japan especially the Nankai Trough[J]. Progress in Geophysics, 2001, 16(2): 88-98. [宋海斌,松林修,仓本真一.日本Nankai海槽天然气水合物研究现状[J].地球物理学进展,2001, 16(2): 88-98.][34] Xu Jiren, Zhao Zhixin, Kono Y, et al. Regional characteristics of stress field and its dynamics in and around the Nankai trough, Japan[J]. Chinese Journal of Geophysics, 2003, 46: 488-495. [徐纪人,赵志新,河野芳辉,等.日本南海海槽地震区域应力场及其板块构造动力学特征[J].地球物理学报, 2003, 46: 488-495.]
[35] Gaku Kimura, Harold Tobin, the NanTroSEIZE Working Group. NanTroSEIZE: The Nankai Trough seismogenic zone experiment Complex Drilling Project [EB/OL]. IODP Complex Drilling Project (CDP) proposal (603). http://www.ees.nmt.edu/NanTroSEIZE/603-CDP-REV3_pub.pdf, 2004-12-07.

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摘要

THE SEISMOGENIC ZONE EXPERIMENT(SEIZE)