参考文献:Angelier J, Chang T-Y, Hu J-C, Chang C-P, Siame L, Lee J-C, Deffontaines B, Chu H-T, Lu C-Y (2009) Does extrusion occur at both tips of the Taiwan collision belt? Insights from active deformation studies in the ilan plain and pingtung plain regions. Tectonophysics 466:356–376CrossRef Brace WF, Kohlstedt DL (1980) Limits on lithospheric stress imposed by laboratory experiments. J Geophys Res 85(B11):6248–6252CrossRef Chang C-P, Angelier J, Huang C-Y (2000) Origin and evolution of a melange: the active plate boundary and suture zone of the longitudinal valley, Taiwan. Tectonophysics 325:43–62CrossRef Chang C-P, Chang T-Y, Angelier J, Kao H, Lee J-C, Yu S-B (2003) Strain and stress field in Taiwan oblique convergent system: constraints from gps observation and tectonic data. Earth Planet Sci Lett 214:115–127CrossRef Chen YR, Lai YC, Huang YL, Huang BS, Wen KL (2008) Investigation of source depths of the 2006 Pingtung earthquake sequence using a dense array at teleseismic distances. Terr Atmos Ocean Sci 19(6):579–588CrossRef Chi W-C, Reed DL, Moore G, Nguyen T, Liu C-S, Lundberg N (2003) Tectonic wedging along the rear of the offshore Taiwan accretionary prism. Tectonophysics 374:199–217CrossRef Ching K-E, Rau R-J, Lee J-C, Hu J-C (2007) Contemporary deformation of tectonic escape in sw Taiwan from gps observations, 1995-2005. Earth Planet Sci Lett 262:601–619CrossRef Coblentz DD, Richardson RM (1996) Analysis of the South American intraplate stress field. J Geophys Res 101(B4):8643–8657CrossRef Demets C, Gordon RG, Argus DF, Stein S (1994) Effect of recent revisions to the geomagnetic reversal time scale on estimates of current plate motions. Geophys Res Lett 21(20):2191–2194CrossRef England P, Houseman G (1986) Finite strain calculations of continental deformation 2. Comparison with the India-Asia collision zone. J Geophys Res 91(B3):3664–3676CrossRef England P, McKenzie D (1982) A thin viscous sheet model for continental deformation. Geophys J R Astron Soc 70(2):295–321CrossRef Houseman G, England P (1986) Finite strain calculations of continental deformation 1. Method and general results for convergent zones. J Geophys Res 91(B3):3651–3663CrossRef Hsu Y-J, Segall P, Yu S-B, Kuo L-C, Williams CA (2007) Temporal and spatial variations of post-seismic deformation following the 1999 Chi-Chi, Taiwan earthquake. Geophys J Int 169(2):367–379CrossRef Hu J-C, Angelier J, Lee J-C, Chu H-T, Byrne D (1996) Kinematics of convergence, deformation and stress distribution in the Taiwan collision area: 2-D finite-element numerical modeling. Tectonophysics 255:243–268CrossRef Hu J-C, Angelier J, Yu S-B (1997) An interpretation of the active deformation of southern Taiwan based on numerical simulation and gps studies. Tectonophysics 274:145–169CrossRef Hu JC, Yu SB, Angelier J, Chu HT (2001) Active deformation of Taiwan from gps measurements and numerical simulations. J Geophys Res 106(B2):2265–2280CrossRef Kao H, Shen SSJ, Ma K-F (1998) Transition from oblique subduction to collision: earthquakes in the southernmost Ryukyu arc-Taiwan region. J Geophys Res 103(B4):7211–7229CrossRef Kao H, Huang GC, Liu CS (2000) Transition from oblique subduction to collision in the northern Luzon arc-Taiwan region: constraints from bathymetry and seismic observations. J Geophys Res 105(B2):3059–3079CrossRef Kaus BJP, Liu YC, Becker TW, Yuen DA, Shi YL (2009) Lithospheric stress-states predicted from long-term tectonic models: influence of rheology and possible application to Taiwan. J Asian Earth Sci 36(1):119–134CrossRef Kim K-H, Chiu J-M, Pujol J, Chen K-C, Huang B-S, Yeh Y-H, Shen P (2005) Three-dimensional Vp and Vs structural models associated with the active subduction and collision tectonics in the Taiwan region. Geophys J Int 162(1):204–220CrossRef Kirby SH, Kronenberg AK (1987) Rheology of the lithosphere: selected topics. Rev Geophys 25(6):1219–1244CrossRef Kubo A, Fukuyama E (2003) Stress field along the Ryukyu Arc and the Okinawa Trough inferred from moment tensors of shallow earthquakes. Earth Planet Sci Lett 210:305–316CrossRef Kuo-Chen H, Wu FT, Roecker SW (2012) Three-dimensional P velocity structures of the lithosphere beneath Taiwan from the analysis of TAIGER and related seismic data sets. J Geophys Res 117(B6):B06306 Lacombe O, Mouthereau F, Angelier J, Deffotaines B (2001) Structural, geodetic and seismological evidence for tectonic escape in SW Taiwan. Tectonophysics 333:323–345CrossRef Lee SJ, Liang WT, Huang BS (2008) Source mechanisms and rupture processes of the 26 December 2006 Pingtung earthquake doublet as determined from the regional seismic records. Terr Atmos Oceanic Sci 19(6):555–566CrossRef Li Q, Liu M, Zhang H (2009) A 3-D viscoelastoplastic model for simulating long-term slip on non-planar faults. Geophys J Int 176:293–306CrossRef Lin C-H (2002) Active continental subduction and crustal exhumation: the Taiwan orogeny. Terra Nova 14(4):281–287CrossRef Liu M, Yang Y (2003) Extensional collapse of the Tibetan Plateau: results of three-dimensional finite element modeling. J Geophys Res 108(B8):2361CrossRef Liu M, Yang Y, Stein S, Zhu Y, Engeln J (2000) Crustal shortening in the andes: why do GPS rates differ from geological rates? Geophys Res Lett 27(18):3005–3008CrossRef Ma KF, Song TRA (2004) Thermo-mechanical structure beneath the young orogenic belt of Taiwan. Tectonophysics 388:21–31CrossRef Ma K-F, Lee C-T, Tsai Y-B, Shin T-C, Mori J (1999) The Chi-Chi, Taiwan earthquake: large surface displacements on an inland thrust fault. Eos Trans Am Geophys Union 80(50):605–611CrossRef Mouthereau F, Petit C (2003) Rheology and strength of the eurasian continental lithosphere in the foreland of the Taiwan collision belt: constraints from seismicity, flexure, and structural styles. J Geophys Res 108(B11):2512CrossRef Mouthereau F, Fillon C, Ma K-F (2009) Distribution of strain rates in the Taiwan orogenic wedge. Earth Planet Sci Lett 284:361–385CrossRef Richardson RM (1978) Finite element modeling of stress in the Nazca plate: driving forces and plate boundary earthquakes. Tectonophysics 50(2–3):223–248CrossRef Shi YL, Cao JL (2008) Effective viscosity of China continental lithosphere. Front Earth Sci 15(3):82–95CrossRef Shin TC, Kuo KW, Lee WHK, Teng TL, Tsai YB (2000) A preliminary report on the 1999 Chi-Chi (Taiwan) earthquake. Seismol Res Lett 71(1):24–30CrossRef Shiono K, Sugi N (1985) Life of and oceanic plate: cooling time and assimilation time. Tectonophysics 112:35–50CrossRef Sun Y, Zhang H, Shi Y (2011) Numerical investigation on the geodynamical mechanism of the first major shock of 2006 Pingtung M W 7.0 earthquake. Sci China Ser D 54(5):631–639CrossRef Sun Y, Dong S, Fan T, Zhang H, Shi Y (2013) 3D rheological structure of the continental lithosphere beneath china and adjacent regions. Chin J Geophys 56(9):2936–2946 Sun Y, Dong S, Zhang H, Shi Y (2014) Numerical investigation of the geodynamic mechanism for the late jurassic deformation of the ordos block and surrounding orogenic belts. J Asian Earth Sci. doi:10.1016/j.jseaes.2014.08.033 Tsai Y-B, Teng T-L, Chiu J-M, Liu H-L (1977) Tectonic implications of the seismicity in the Taiwan region. Mem Geol Soc China 2:13–41 Wang C-Y, Shin T-C (1998) Illustrating 100 years of Taiwan seismicity. Terr Atmos Ocean Sci 9(4):589–614 Wu FT, Rau R-J, Salzberg D (1997) Taiwan orogeny: thin-skinned or lithospheric collision? Tectonophysics 274:191–220CrossRef Wu Y-M, Chang C-H, Zhao L (2007) Seismic tomography of Taiwan: improved constraints from a dense network of strong motion stations. J Geophys Res 112:B08312 Wu YM, Zhao L, Chang CH, Hsiao NC, Chen YG, Hsu SK (2009) Relocation of the 2006 Pingtung earthquake sequence and seismotectonics in southern Taiwan. Tectonophysics 479:19–27CrossRef Yen H-Y, Liang W-T, Kuo B-Y, Yen Y-H, Liu C-S, Reed D, Lundberg N, Su F-C, Chung H-S (1995) A regional gravity map for the subduction-collision zone near Taiwan. Terr Atmos Ocean Sci 6(2):233–250 Yen HY, Yeh YH, Wu FT (1998) Two-dimensional crustal structures of Taiwan from gravity data. Tectonics 17(1):104–111CrossRef Yu SB, Kuo LC (2001) Present-day crustal motion along the longitudinal valley fault, eastern Taiwan. Tectonophysics 333:199–217CrossRef Yu SB, Chen HY, Kuo LC (1997) Velocity field of gps stations in the Taiwan area. Tectonophysics 274:41–59CrossRef Zhou D, Yu H-S, Xu H-H, Shi X-B, Chou Y-W (2003) Modeling of thermo-rheological structure of lithosphere under the foreland basin and mountain belt of Taiwan. Tectonophysics 374:115–134CrossRef
作者单位:Yujun Sun (1) Mian Liu (2) (3) Shuwen Dong (4) Huai Zhang (2) Yaolin Shi (2)
1. Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing, 100081, China 2. Key Laboratory of Computational Geodynamics, Chinese Academy of Sciences, Beijing, 100049, China 3. Department of Geological Sciences, University of Missouri, Columbia, MO, 65211, USA 4. Chinese Academy of Geological Sciences, Beijing, 100037, China
刊物主题:Geophysics/Geodesy;
出版者:Springer Berlin Heidelberg
ISSN:1867-8777
文摘
Taiwan is a young orogenic belt with complex spatial distributions of deformation and earthquakes. We have constructed a three-dimensional finite element model to explore how the interplays between lithospheric structure and plate boundary processes control the distribution of stress and strain rates in the Taiwan region. The model assumes a liberalized power-law rheology and incorporates main lithospheric structures; the model domain is loaded by the present-day crustal velocity applied at its boundaries. The model successfully reproduces the main features of the GPS-measured strain rate patterns and the earthquake-indicated stress states in the Taiwan region. The best fitting model requires the viscosity of the lower crust to be two orders of magnitude lower than that of the upper crust and lithospheric mantle. The calculated deviatoric stress is high in regions of thrust faulting and low in regions of extensional and strike-slip faulting, consistent with the spatial pattern of seismic intensity in Taiwan. Keywords Taiwan Stress Strain rate FEM model Earthquake