| Citation: |
ZANG SHAOXIAN, NING JIEYUAN, XU LIZHONGcom sh advance. 1989: THE DISTRIBUTION OF EARTHQUAKES, BEHAVIOR OF THE SUBDUCTION ZONE AND STRESS STATE IN THE RYUKYU ISLAND ARC. Acta Seismologica Sinica, 11(2): 113-123.
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[1] Katsumata,M.and 1969. Seismicity tectonics of the western Pacific:Izu——Mariana——Caroline and Ryukyu——Taiwan regions. J. Geophys. Res., 74, 5923——5948.
[2] Wu, F. T., 1970.Focal mechanism and tectonics in the vicinity of Taiwan. Bull. Seism. Soc., Am., 60,2045——2056. [3] Fitch, L, 1972. Plate convergence, transcurrent faults and internal deformation adjacent Asia and the wes——tern Pacific. J. Geophys. Res., 77, 4432——4460. [4] Shiono, K., T. Mikumo, and Y. Ishikawa, 1980. Tectonics of the Kyushu——Ryukyuarc as evidenced frorra seismicity and focal mechanism of shallow to intermediate——depth earthquakes. J. Phys. Earth, 28, 17——43. [5] lchikawa, M,1971. Reanalyses of mechanism of earthquakes which occured in and near Japan, and sta——tistical studies on the modal plane solutions obtained, 1928——1968. Gaophys. bfag., 35. 207——274. [6] Isacks, B. and P, Molnar, 1971. Distribution of stresses in the descending lithosphere from a global survey of focal mechanism solutions of mantal earthquakes. Pcv. Geaphys. Space Phys., 9, 103——174. [7] Wageman, J. M., T. W. C. Hilde, and K. O. Emery, 1970. Structural framework of east China sea and Yellow sca. Amer. Assoc. Petrol. Genl., 54, 1611——1643 [8] Lee, Chao——Shing, G. G. Jr. Shor, L. D. Bibee, R. S. Lu, and T. W. C. Hilde, 1980. Okinawa trough:Origin of a back——are basin. Marine Geol., 35, 219——241. [9] Eguchi, T, and S. Uyeda, 1983. Seismotectonics of the Okinawa trough and Ryukyu arc. Memoir of Geol.Soc. of China, 5, L89——210. [10] Konishi, K., 1965. Geotectonic framewor!t of tire Ryukyu island (Nansei shoto). J. Geol. Soc. Japan, 71,437——457. [11] 减绍先,1981,地震断裂和应力场.地震地质,3,37——46, [12] 减绍先,1987,缅甸山脉地区Benioff带的形态及其应力状态.地球物理学报,30,144——158, [13] Kizaki, K., 1978. Tectonics of the Ryukyu. islandarc. J. Phys. Earth, 26, Suppl., s301——s307 [14] Letouzey, J. and M. Kimura, 1985. Okinawa trough genesis: structure and evolution of a backare basin developed in a continent. Marine and Pexrol. Geol., 2. 111——130. [15] Uyeda, S, and H. Kanamori, 1979. Back——arc opening and the mode of subduction. J. Geophyr. Res., 84, 1049——1062. [16] Seno, T., 1977. The instantaneous rotation vector of the Philipping sea plate relative to the Eurasian plate Tectonophysics, 42, 209——226.
[1] Katsumata,M.and 1969. Seismicity tectonics of the western Pacific:Izu——Mariana——Caroline and Ryukyu——Taiwan regions. J. Geophys. Res., 74, 5923——5948.
[2] Wu, F. T., 1970.Focal mechanism and tectonics in the vicinity of Taiwan. Bull. Seism. Soc., Am., 60,2045——2056. [3] Fitch, L, 1972. Plate convergence, transcurrent faults and internal deformation adjacent Asia and the wes——tern Pacific. J. Geophys. Res., 77, 4432——4460. [4] Shiono, K., T. Mikumo, and Y. Ishikawa, 1980. Tectonics of the Kyushu——Ryukyuarc as evidenced frorra seismicity and focal mechanism of shallow to intermediate——depth earthquakes. J. Phys. Earth, 28, 17——43. [5] lchikawa, M,1971. Reanalyses of mechanism of earthquakes which occured in and near Japan, and sta——tistical studies on the modal plane solutions obtained, 1928——1968. Gaophys. bfag., 35. 207——274. [6] Isacks, B. and P, Molnar, 1971. Distribution of stresses in the descending lithosphere from a global survey of focal mechanism solutions of mantal earthquakes. Pcv. Geaphys. Space Phys., 9, 103——174. [7] Wageman, J. M., T. W. C. Hilde, and K. O. Emery, 1970. Structural framework of east China sea and Yellow sca. Amer. Assoc. Petrol. Genl., 54, 1611——1643 [8] Lee, Chao——Shing, G. G. Jr. Shor, L. D. Bibee, R. S. Lu, and T. W. C. Hilde, 1980. Okinawa trough:Origin of a back——are basin. Marine Geol., 35, 219——241. [9] Eguchi, T, and S. Uyeda, 1983. Seismotectonics of the Okinawa trough and Ryukyu arc. Memoir of Geol.Soc. of China, 5, L89——210. [10] Konishi, K., 1965. Geotectonic framewor!t of tire Ryukyu island (Nansei shoto). J. Geol. Soc. Japan, 71,437——457. [11] 减绍先,1981,地震断裂和应力场.地震地质,3,37——46, [12] 减绍先,1987,缅甸山脉地区Benioff带的形态及其应力状态.地球物理学报,30,144——158, [13] Kizaki, K., 1978. Tectonics of the Ryukyu. islandarc. J. Phys. Earth, 26, Suppl., s301——s307 [14] Letouzey, J. and M. Kimura, 1985. Okinawa trough genesis: structure and evolution of a backare basin developed in a continent. Marine and Pexrol. Geol., 2. 111——130. [15] Uyeda, S, and H. Kanamori, 1979. Back——arc opening and the mode of subduction. J. Geophyr. Res., 84, 1049——1062. [16] Seno, T., 1977. The instantaneous rotation vector of the Philipping sea plate relative to the Eurasian plate Tectonophysics, 42, 209——226. |
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