Fujii Y, Satake K, Sakai S, et al. Tsunami source of the 2011 off the Pacific coast of Tohoku earthquake. Earth Planets Space, 2011, 63(7): 815-820.
[2]
Hayes G P. Rapid source characterization of the 2011 Mw9.0 off the Pacific coast of Tohoku earthquake. Earth Planets Space, 2011, 63(7): 529-534.
[3]
王凡, 沈正康, 王阎昭等. 2011年3月11日日本宫城Mw 9.0级地震对其周边地区火山活动的影响. 科学通报, 2011, 56(14): 1080-1083. Wang F, Shen Z K, Wang Y Z, et al. Influence of the March 11, 2011 Mw9.0 Tohoku-oki earthquake on regional volcanic activities. Chinese Sci. Bull., 2011, 56(20): 2077-2081.
[4]
Lallemand S, Jolivet L. Japan Sea: a pull-apart basin? Earth and Planetary Science Letters, 1986, 76(3-4): 375-389.
[5]
Nakamura K. Possible nascent trench along the eastern Japan sea as the convergent boundary between Eurasian and North American plates. Bull. Earthquake Res. Inst. Univ. Tokyo (in Japanese with English abstract), 1983, 58: 721-732.
[6]
Kobayashi Y. Incipient subduction of a lithospheric plate under the eastern margin of the Japan Sea. The Earth Monthly (in Japanese), 1983, 5:510-514.
[7]
Jolivet L, Tamaki K. Neogene kinematics in the Japan Sea region and volcanic activity of the northeast Japan arc.//Proc. Ocean Drill. Program Sci. Results, 1992, 127-128: 1311-1331.
[8]
Tamaki K. Two modes of back-arc spreading. Geology, 1985, 13(7): 475-478.
[9]
Otofuji Y I, Matsuda T, Nohda S. Paleomagnetic evidence for the Miocene counter-clockwise rotation of northeast Japan-rifting process of the Japan arc. Earth Planet. Sci. Lett., 1985, 75(2-3): 265-277.
[10]
Tatsumi Y, Otofuji Y I, Matsuda T, et al. Opening of the sea of Japan back-arc basin by asthenospheric injection. Tectonophysics, 1989, 166(4): 317-329.
[11]
Liu J Q, Han J T, Fyfe W S. Cenozoic episodic volcanism and continental rifting in northeast China and possible link to Japan Sea development as revealed from K-Ar geochronology. Tectonophysics, 2001, 339(3-4): 385-401.
[12]
Nelson T H, Temple P G. Mainstream mantle convection: A geologic analysis of plate motion. Amer. Assoc. Petrol. Geol. Bull., 1972, 56(2): 226-246.
[13]
Jolivet L, Huchon P, Ragin C. Tectonic setting of Western Pacific marginal basins. Tectonophysics, 1989, 160(1-4): 23-47.
[14]
Tamaki K, Honza E. Global tectonics and formation of marginal basins: role of the western Pacific. Episodes, 1991, 14(3): 224-230.
[15]
许浚远, 张凌云. 欧亚板块东缘新生代盆地成因: 右行剪切拉分作用. 石油与天然气地质, 1999, 20(3): 187-191. Xu J Y, Zhang L Y. Genesis of Cenozoic basins in the eastern margin of Eurasia plate: dextral pulling apart. Oil & Gas Geology (in Chinese), 1999, 20(3): 187-191.
[16]
许浚远, 张凌云. 西北太平洋边缘新生代盆地成因(上): 成盆机制述评. 石油与天然气地质, 2000, 21(2): 93-98. Xu J Y, Zhang L Y. Genesis of Cenozoic basins in Northwest Pacific Ocean margin(1): comments on basin-forming mechanism. Oil & Gas Geology (in Chinese), 2000, 21(2): 93-98.
[17]
许浚远, 张凌云. 西北太平洋边缘新生代盆地成因(中): 连锁右行拉分裂谷系统. 石油与天然气地质, 2000, 21(3): 185-190. Xu J Y, Zhang L Y. Genesis of Cenozoic basins in Northwest Pacific margin(2): linked dextral pull-apart basin system. Oil & Gas Geology (in Chinese), 2000, 21(3): 185-190.
[18]
许浚远, 张凌云. 西北太平洋边缘新生代盆地成因(下): 后裂谷期构造演化. 石油与天然气地质, 2000, 21(4): 287-292. Xu J Y, Zhang L Y. Genesis of cenozoic basins in Northwest Pacific margin(3): tectonic evlution of post rifting period. Oil & Gas Geology (in Chinese), 2000, 21(4): 287-292.
[19]
Karig D E. Origin and development of marginal basins in the western Pacific. Journal of Geophysical Research, 1971, 76(11): 2542-2561.
[20]
Maruyama S, Hasegawa A, Santosh M, et al. The dynamics of Big Mantle Wedge, Magma Factory, and metamorphic-metasomatic factory in subduction zones. Gondwana Res., 2009, 16(3-4): 414-430.
[21]
Honda H, Masatsuka A. On the mechanisms of the earthquakes and the stresses producing them in Japan and its vicinity. Ibid, 1952, 4: 42-60.
[22]
Honda H, Masatsuka A, Emura K. On the mechanism of the earthquakes and the stresses producing them in Japan and its vicinity (second paper): Tohoku Univ. Sci. Rept., Ser. 5. Geophys., 1957, 8: 186-205.
[23]
Nakamura K, Uyeda S. Stress gradient in arc-back arc regions and plate subduction. J. Geophys. Res., 1980, 85(B11): 6419-6428.
[24]
Uyeda S, Kanamori H. Back-arc opening and the mode of subduction. J. Geophys. Res., 1979, 84(B3): 1049-1061.
[25]
宁杰远, 臧绍先. 日本海及中国东北地震的深度分布及其应力状态. 地震地质, 1987, 9(2): 49-61. Ning J Y, Zang S X. The distribution of earthquakes and stress state in the Japan Sea and the northeast China. Seismology and Geology (in Chinese), 1987, 9(2): 49-61.
[26]
谢富仁, 崔效锋, 赵建涛等. 中国大陆及邻区现代构造应力场分区. 地球物理学报, 2004, 47(4): 654-662. Xie F R, Cui X F, Zhao J T, et al. Regional division of the recent tectonic stress field in China and adjacent areas. Chinese J. Geophys. (in Chinese), 2004, 47(4): 654-662.
[27]
俞春泉, 陶开, 崔效锋等. 用格点尝试法求解P波初动震源机制解及解的质量评价. 地球物理学报, 2009, 52(5): 1402-1411. Yu C Q, Tao K, Cui X F, et al. P-wave first-motion focal mechanism solutions and their quality evaluation. Chinese J. Geophys. (in Chinese), 2009, 52(5): 1402-1411.
[28]
Zheng X F, Yao Z X, Liang J H, et al. The role played and opportunities provided by IGP DMC of China national seismic network in Wenchuan earthquake disaster relief and researches. Bull. Seism. Soc. Am., 2010, 100(5B): 2866-2872, doi:10.1785/0120090257.
[29]
Obana K, Fujie G, Takahashi T, et al. Normal-faulting earthquakes beneath the outer slope of the Japan trench after the 2011 Tohoku earthquake: Implications for the stress regime in the incoming Pacific plate. Geophysical Research Letters, 2012, 39(7), doi:10.1029/2011GL050399.
[30]
Ammon C J, Lay T, Kanamori H, et al. A rupture model of the 2011 off the Pacific coast of Tohoku earthquake. Earth Planets Space, 2011, 63(7): 693-696.
[31]
陈为涛, 甘卫军, 肖根如等. 3·11日本大地震对中国东北部地区地壳形变态势的影响. 地震地质, 2012, 34(3): 425-439. Chen W T, Gan W J, Xiao G R, et al. The impact of 2011 Tohoku-Oki earthquake in Japan on crustal deformation of northeastern region in China. Seismology and Geology (in Chinese), 2012, 34(3): 425-439.
[32]
王敏, 李强, 王凡等. 全球定位系统测定的2011年日本宫城MW9. 0级地震远场同震位移. 科学通报, 2011, 56(20): 1593-1596. Wang M, Li Q, Wang F, et al. Far-field coseismic displacements associated with the 2011 Tohoku-oki earthquake in Japan observed by Global Positioning System. Chinese Sci. Bull., 2011, 56(23): 2419-2424.
[33]
Seno T. A consideration on the "Japan sea subduction hypothesis" seismic slip vector along the Japan trench. Jishin (J. Geol. Soc. Jpn.) (in Japanese), 1983, 36: 227-273.
[34]
Minster J B, Jordan T H, Molnar P, et al. Numerical modelling of instantaneous plate tectonics. Geophys. J. Int., 1974, 36(3): 541-576.
[35]
Kanamori H. Seismic and aseismic slip along subduction zones and their tectonic implications.//Talwani M, Pitman W C eds. Island Arcs, Deep Sea Trenches and Back-Arc Basins. American Geophysical Union, Washington, D. C. 1977,doi: 10.1029/ME001p0163.
[36]
Nishimura S. Why are there no back-arc basins around the eastern Pacific margin? Revista Mexicana de Ciencias Geologicas, 2002, 19(3): 170-174.
[37]
Kimura G, Tamaki K. Collision, rotation and back-arc spreading in the region of the Okhotsk and Japan Seas. Tectonics, 1986, 5(3): 389-401.
[38]
Grove T L, Till C B, Lev E, et al. Kinematic variables and water transport control the formation and location of arc volcanoes. Nature, 2009, 459(7247): 694-697.
