引文
[1]刘庆生,高山,郑建平.大陆地壳磁性结构及其研究意义[J].科学通报,1998,43(12):1 246-1 252.
[2]Liu Qingsheng,Gao Shan,Liu Yongsheng.Magnetic structureof the continental crustal cross-section in central North ChinaCraton[J].Journal of Geodynamics,2000,29(1/2):1-13.
[3]Liu Qingsheng,Gao Shan.Magnetic petrology of high-gradeterrains in the Archean shield areas:Window into deep crustalstructure and geodynamic processes[J].Journal of China Uni-versity of Geosciences,1998,9(1):81-85.
[4]Liu Qingsheng,Gao Shan,Xu Qingdong,et al.Magnetic struc-ture of Archean Kongling Group from Yangtze Craton,SouthChina[J].Journal of China University of Geosciences,1998,9(2):144-151.
[5]金振民,余日东,杨文采,等.江苏东海县幔源橄榄岩包体及其深部构造意义[J].地质学报,2003,77(4):452-459.
[6]Fountain D M,Salisbury M H.Exposed cross sections throughthe continental crust:Implications for crustal structure,petrol-ogy and evolution[J].Earth Planetary Science Letters,1981,5:263-277.
[7]Shive P N,Blakely R J,Frost B R,et al.Magnetic properties ofthe lower continental crust[M]∥Fountain D M.Continentallower crust.New York:Elsevier,1992:145-177.
[8]刘庆生,高山,刘勇胜.华北克拉通中部大陆地壳断面磁性结构研究及意义[J].地球物理学报.2000,43(1):64-72.
[9]McEnroe S A,Langenhorst F,Robinson P,et al.What is mag-netic in the lower crust?[J].Earth Planetary Science Letters,2004,226:175-192.
[10]张国伟,张本仁,袁学诚,等.秦岭造山带与大陆动力学[M].北京:科学出版社,2004.
[11]董树文,孙先知,张勇,等.大别山碰撞造山带基本结构[M].科学通报,1993,38(6):542-545.
[12]董树文,吴宣志,高锐,等.大别造山带地壳速度结构与动力学[J].地球物理学报,1998,41(3):349-360.
[13]刘建华,刘福田,孙若昧,等.秦岭—大别造山带及其南北缘地震层析成像[J].地球物理学报,1995,38(1):46-54.
[14]Okay A I,Sengoer A M C,Satn M.Tectonics of an ultrahigh-pressure metamorphic terran:The Dabie shan/Tongbai Shanorogen,China[J].Tectonics,1993,12(6):1 320-1 334.
[15]王清晨,孙枢,李继亮,等.秦岭的大地构造演化[J].地质科学,1989,2:129-142.
[16]刘景波,游振东.秦岭群中条带状混合岩质量等比线分析[J].岩石学报,1997,13(3):427-438.
[17]索书田,钟增球,游振东.大别苏鲁超高压—高压变质带伸展构造格架及其动力学意义[J].地质学报,2001,75(1):14-24.
[18]Xu S T,Okay A,Ji S,et al.Diamond from the Dabie Shan met-amorphic rocks and its implication for tectonic setting[J].Sci-ences,1992,256:80-82.
[19]王椿镛,张先康,陈步云,等.大别造山带的地壳结构研究[J].中国科学:D辑,1997,27(3):221-226.
[20]袁学诚,任纪舜,徐明才,等.东秦岭邓县—南漳反射地震剖面及其构造意义[J].中国地质,2002,29(1):14-19.
[21]杨文采,余长青.根据地球物理资料分析大别—苏鲁超高压变质带演化的运动学与动力学[J].地球物理学报,2001,44(3):61-75.
[22]杨文采,程振炎,张春贺.中国科学深钻选址地球物理调查与大别—苏鲁岩石圈[J].地球学报,2003,24(5):391-404.
[23]杨文采,杨午阳,程振炎.中国大陆科学钻探主孔区三维地震资料的初步解释[J].岩石学报,2004,20(1):128-134.
[24]王有学,姜枚,韩国华.中国大陆科学钻探场址区的地壳速度结构特征[J].地球科学:中国地质大学学报,2004,29(6):667-672.
[25]徐纪人,赵志新.苏鲁造山带区域地壳山根结构特征[J].岩石学报,2004,20(1):149-156.
[26]杨文采,程振炎,陈国九,等.苏鲁超高压变质带北部地球物理调查(Ι)——深反射地震[J].地球物理学报,1999,42(1):41-52.
[27]杨文采,胡振远,程振炎,等.郯城—涟水综合地球物理剖面[J].地球物理学报,1999,42(2):206-217.
[28]杨文采,方慧,程振炎,等.苏鲁超高压变质带北部地球物理调查(Ⅱ):非地震方法[J].地球物理学报,1999,42(4):508-519.
[29]吴其反,路凤香,刘庆生,等.苏鲁地区地壳深部太古代残留岩片:来自航磁资料的证据[J].科学通报,2003,48(4):395-399.
[30]余钦范,姚长利,孟小红,等.苏北大陆科学钻探靶区重磁异常反演解释[J].地球物理学报,2001,44(6):825-832.
[31]余钦范,郭友钊,孟小红,等.苏北大陆科学钻探靶区岩石物理性质[J].地球物理学报,2002,45(1):93-100.
[32]多而特曼H B.岩石和矿物的物理性质[M].蒋宏耀译.北京:科学出版社,1985.
[33]Liu Qingsheng,Gao Shan.Magnetic structure of the continen-tal crust:Implications for crustal structure and evolution[J].Journal of China University of Geosciences,2000,11(3):356-360.
[34]胥颐.北天山地震带的航磁异常与深部构造[J].内陆地震,1996,10(4):304-310.
[35]Fausto F,Franco C,Emanuele B,et al.Rifted(?)crust at theEast Antarctic Craton margin:Gravity and magnetic interpre-tation along a traverse across the Wilkes Subglacial Basin re-gion[J].Earth Planetary Science Letters,2001,192:407-421.
[36]Mark P,John A P.Relating crustal magnetization and satellite-altitude magnetic anomalies in the Ungava Peninsula,northenQuebec,Canada[J].Earth Planetary Science Letters,2001,194:127-133.
[37]Brown D,Carbonell R,Kukkonen I,et al.Compositon of theUralide crust from seismic velocity(vp,vs),heat flow,gravity,and magnetic data[J].Earth Planetary Science Letters,2003,210:333-349.
[38]戴明刚.东海及邻域的两条剖面地球物理反演与综合解释[J].地球物理学进展,2004,19(2):331-340.
[39]Qiao Qingqing,Liu Qingsheng.Curie point depth investigationof the Dabie-Sulu UPH metamorphic belt[J].Tectonophysics,2007.
[40]张家声,劳秋元.航磁异常的构造解释和华北—塔南—扬子超陆块演化[J].地学前缘,1999,6(4):379-390.
[41]徐海军.中国大陆科学钻探工程主孔(100~2 000 m)岩芯及周边地区岩石的磁化率研究[D].武汉:中国地质大学,2005.
[42]路凤香,王春阳,胡宝群,等.南秦岭下地壳组成及岩石圈的拆离俯冲作用[J].中国地质,2005,30(2):113-119.
[43]李曙光.大别山超高压变质岩折返机制与华北华南陆块碰撞过程[J].地学前缘,2004,11(3):63-70.