引文
[1]Honda H,Masatsuka A.On the mechanisms of theearthquakes and the stresses producing them in Japan and itsvicinity.Ibid,1952,4:42-60.
[2]Honda H,Masatsuka A,Emura K.On the mechanism of theearthquakes and the stresses producing them in Japan and itsvicinity(second paper):Tohoku Univ.Sci.Rept.,Ser.5.Geophys.,1957,8:186-205.
[3]Nakamura K,Uyeda S.Stress gradient in arc-back arcregions and plate subduction.J.Geophys.Res.,1980,85(B11):6419-6428.
[4]Uyeda S,Kanamori H.Back-arc opening and the mode ofsubduction.J.Geophys.Res.,1979,84(B3):1049-1061.
[5]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 andstress state in the Japan Sea and the northeast China.Seismology and Geology(in Chinese),1987,9(2):49-61.
[6]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 therecent tectonic stress field in China and adjacent areas.Chinese J.Geophys.(in Chinese),2004,47(4):654-662.
[7]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 focalmechanism solutions and their quality evaluation.Chinese J.Geophys.(in Chinese),2009,52(5):1402-1411.
[8]Zheng X F,Yao Z X,Liang J H,et al.The role played andopportunities provided by IGP DMC of China national seismicnetwork in Wenchuan earthquake disaster relief and researches.Bull.Seism.Soc.Am.,2010,100(5B):2866-2872,doi:10.1785/0120090257.
[9]Obana K,Fujie G,Takahashi T,et al.Normal-faultingearthquakes beneath the outer slope of the Japan trench afterthe 2011 Tohoku earthquake:Implications for the stressregime in the incoming Pacific plate.Geophysical ResearchLetters,2012,39(7),doi:10.1029/2011GL050399.
[10]Ammon C J,Lay T,Kanamori H,et al.A rupture model ofthe 2011off the Pacific coast of Tohoku earthquake.EarthPlanets Space,2011,63(7):693-696.
[11]Fujii Y,Satake K,Sakai S,et al.Tsunami source of the2011off the Pacific coast of Tohoku earthquake.EarthPlanets Space,2011,63(7):815-820.
[12]Hayes G P.Rapid source characterization of the 2011 Mw9.0off the Pacific coast of Tohoku earthquake.Earth PlanetsSpace,2011,63(7):529-534.
[13]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 2011Tohoku-Oki earthquake in Japan on crustal deformation ofnortheastern region in China.Seismology and Geology(inChinese),2012,34(3):425-439.
[14]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 coseismicdisplacements associated with the 2011Tohoku-oki earthquake inJapan observed by Global Positioning System.Chinese Sci.Bull.,2011,56(23):2419-2424.
[15]王凡,沈正康,王阎昭等.2011年3月11日日本宫城Mw9.0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 March11,2011 Mw9.0Tohoku-oki earthquake on regional volcanicactivities.Chinese Sci.Bull.,2011,56(20):2077-2081.
[16]Lallemand S,Jolivet L.Japan Sea:apull-apart basin?Earthand Planetary Science Letters,1986,76(3-4):375-389.
[17]Nakamura K.Possible nascent trench along the eastern Japansea as the convergent boundary between Eurasian and NorthAmerican plates.Bull.Earthquake Res.Inst.Univ.Tokyo(in Japanese with English abstract),1983,58:721-732.
[18]Kobayashi Y.Incipient subduction of a lithospheric plateunder the eastern margin of the Japan Sea.The EarthMonthly(in Japanese),1983,5:510-514.
[19]Seno T.A consideration on the“Japan sea subductionhypothesis”seismic slip vector along the Japan trench.Jishin(J.Geol.Soc.Jpn.)(in Japanese),1983,36:227-273.
[20]Jolivet L,Tamaki K.Neogene kinematics in the Japan Searegion and volcanic activity of the northeast Japan arc.∥Proc.Ocean Drill.Program Sci.Results,1992,127-128:1311-1331.
[21]Tamaki K.Two modes of back-arc spreading.Geology,1985,13(7):475-478.
[22]Otofuji Y I,Matsuda T,Nohda S.Paleomagnetic evidencefor the Miocene counter-clockwise rotation of northeastJapan-rifting process of the Japan arc.Earth Planet.Sci.Lett.,1985,75(2-3):265-277.
[23]Tatsumi Y,Otofuji Y I,Matsuda T,et al.Opening of thesea of Japan back-arc basin by asthenospheric injection.Tectonophysics,1989,166(4):317-329.
[24]Liu J Q,Han J T,Fyfe W S.Cenozoic episodic volcanismand continental rifting in northeast China and possible link toJapan Sea development as revealed from K-Ar geochronology.Tectonophysics,2001,339(3-4):385-401.
[25]Nelson T H,Temple P G.Mainstream mantle convection:Ageologic analysis of plate motion.Amer.Assoc.Petrol.Geol.Bull.,1972,56(2):226-246.
[26]Minster J B,Jordan T H,Molnar P,et al.Numericalmodelling of instantaneous plate tectonics.Geophys.J.Int.,1974,36(3):541-576.
[27]Kanamori H.Seismic and aseismic slip along subductionzones and their tectonic implications.//Talwani M,PitmanW C eds.Island Arcs,Deep Sea Trenches and Back-ArcBasins.American Geophysical Union,Washington,D.C.1977,doi:10.1029/ME001p0163.
[28]Nishimura S.Why are there no back-arc basins around theeastern Pacific margin?Revista Mexicana de CienciasGeologicas,2002,19(3):170-174.
[29]Kimura G,Tamaki K.Collision,rotation and back-arcspreading in the region of the Okhotsk and Japan Seas.Tectonics,1986,5(3):389-401.
[30]Jolivet L,Huchon P,Ragin C.Tectonic setting of WesternPacific marginal basins.Tectonophysics,1989,160(1-4):23-47.
[31]Tamaki K,Honza E.Global tectonics and formation ofmarginal basins:role of the western Pacific.Episodes,1991,14(3):224-230.
[32]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 easternmargin of Eurasia plate:dextral pulling apart.Oil&GasGeology(in Chinese),1999,20(3):187-191.
[33]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 NorthwestPacific Ocean margin(1):comments on basin-formingmechanism.Oil&Gas Geology(in Chinese),2000,21(2):93-98.
[34]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 NorthwestPacific margin(2):linked dextral pull-apart basin system.Oil&Gas Geology(in Chinese),2000,21(3):185-190.
[35]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 NorthwestPacific margin(3):tectonic evlution of post rifting period.Oil&Gas Geology(in Chinese),2000,21(4):287-292.
[36]Karig D E.Origin and development of marginal basins in thewestern Pacific.Journal of Geophysical Research,1971,76(11):2542-2561.
[37]Maruyama S,Hasegawa A,Santosh M,et al.The dynamicsof Big Mantle Wedge,Magma Factory,and metamorphic-metasomatic factory in subduction zones.Gondwana Res.,2009,16(3-4):414-430.
[38]Grove T L,Till C B,Lev E,et al.Kinematic variables andwater transport control the formation and location of arcvolcanoes.Nature,2009,459(7247):694-697.