引文
[1]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.Wang Q C,Sun S,Li J L,et al.The tectonic evolution of theQingling mountain belt[J].Acta Geologica Sinica(inChinese),1989,(2):129-142.
[2]刘福田,徐佩芬,刘劲松,等.大陆深俯冲带的地壳速度结构—东大别造山带深地震宽角反射/折射研究[J].地球物理学报,2003,46(3):366-372.Liu F T,Xu P F,Liu J S,et al.The crustal velocity structureof the continental deep subduction belt:study on the easternDaBie orogen by seismic wide-angle reflction/refraction[J].Chinese J.Geophys.(in Chinese),2003,46(3):5366-372.
[3]姚大全,张杰,沈小七.安徽霍山地区断层活动习性研究的新进展[J].地球物理学进展,2006,21(3):776-782.Yao D Q,Zhang H,Shen X Q.New advance of fault activebehavior research in Huoshan area Anhui province[J].Progress in Geophysics(in Chinese),2006,21(3):776-782.
[4]张杰,沈小七,王行舟,等.利用层析成像的结果探讨安徽及邻区中强地震深部构造背景[J].中国地质,2005,21(3):350-359.Zhang J,Shen X Q,Wang X Z,et al.Discussion on deeptectonic backgrounds of moderate-strong earthquake in Anhuiand its neighboring region by using results of seismictomography[J].Earthquake Research in China(in Chinese),2005,21(3):350-359.
[5]姚大全,刘家灿,李杰,等.六安-霍山地震危险区地震活动和地震构造[J].地震地质,2003,25(2):211-219.Yao D Q,Liu J C,Li J,et al.Seismic activities and structuresof the Luan-Huoshan seismic risk area[J].Seismology andGeology(in Chinese),2003,25(2):211-219.
[6]姚大全,汤有标,刘加灿,等.大别山东北部基岩区断裂活动习性的综合研究[J].地震地质,1999,21(1):63-68.Yao D Q,Li J.synthetical study on active behavior of fault inbed rock area of northeastern Dabie mountain[J].Seismologyand Geology(in Chinese),1999,21(1):63-68.
[7]闫素萍,张毅,张有林,等.东大别构造带地震地磁监测试验区岩石圈磁场特征分析[J].地球物理学进展,2010:1599-1604.Yan S P,Zhang Y,Zhang Y L,et al.Characteristics of thegeomagnetic field of lithosphere in the eastern Dabie orogen[J].Progress in Geophysics(in Chinese),2010:1599-1604.
[8]徐树桐,江来利,刘贻灿,等.大别山区(安徽部分)的构造格局和演化过程[J].地质学报,1992,66(1):1-15.Xu S T,Jiang L L,Liu Y C,et al.Tectonic framework andevolution of the DaBie mountains in Anhui,Eastern China[J].Acat Geologica Sinica(in Chinese),1992,66(1):1-15.
[9]王椿镛,张先康,陈布云,等.大别造山带的地壳结构研究[J].中国科学(D),1997,27(3):221-226.Wang C Y,Zhang X K,Chen B Y,et al.The researcher ofcrust structure in Dabie orogenic belt[J].Science in China(Series D)(in Chinese),1997,27(3):221-226.
[10]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):349-361.Dong S W,Wu X Z,Gao R,et al.On the crust velocitylevels and dynamics of the Dabieshan orogenci belt[J].Chinese J.Geophys.(in Chinese),1998,41(3):349-361.
[11]徐树桐,袁学诚,吴维平,等.大别山黄石六安反射地震剖面新的地质解释[J].地质通报,2008,27(1):19-26.Xu S T,Yu X C,Wu W P,et al.New geologicalinterpretation of the seismic reflection profile from Huangshito Liu’an across the Dabie Mountains,China[J].GeologicalBulletin of China(in Chinese),2008,27(1):19-26.
[12]徐佩芬,刘福田,王清晨,等.大别-苏鲁碰撞造山带的地震层析成像研究—岩石圈三维速度结构[J].地球物理学报,2000,43(3):377-385.Xu P F,Liu F T,Wang Q C,et al.Seismic tomographybeneath the Dabie-Sulu collision orogen-3Dvelocity structuresof lithosphere[J].Chinese J.Geophys.(in Chinese),2003,46(3):377-385.
[13]杨文采.东大别超高压变质带的深部构造[J].中国科学(D),2003,33(2):183-194.Yang W C.Deep structure of ultrahigh-pressure metamorphicbelt in eastern Dabieshan mountains[J].Science in China(Series D)(in Chinese),2003,33(2):183-194.
[14]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.Yang W C,Fang H,Chen Z Y,et al.Geophysicalinvestigation of northern SULU UHPM terrane in East China(Ⅱ):Non-seismic methods[J].Chinese J.Geophys.(inChinese),1999,42(4):508-519.
[15]肖骑彬,赵国泽,詹燕,等.大别山超高压编制带深部电性结构及其动力学意义初步研究[J].地球物理学报,2007,50(3):812-822.Xiao Q B,Zhao G Z,Zhan Y,et al.A preliminary study onelectrical structure and dynamic of ultral-high pressuremetamorphic belt beneath the Dabie Moutains[J].Chinese J.Geophys.(in Chinese),2007,50(3):812-822.
[16]张交东,杨晓勇,刘成斋,等.大别山北缘深部结构的高精度重磁电震解析[J].地球物理学报,2012,55(7):2292-2306.Zhang J D,Yang X Y,Liu C Z,et al.The file deep structureof the northern margin of the Dabie Orogenic Belt fromgravity-magnetic-eldctrical-seismic combination survey[J].Chinese J.Geophys.(in Chinese),2012,55(7):2292-2306.
[17]徐如刚,张毅,王雷,等.九江-瑞昌MS5.7地震前后地磁场水平分量异常追踪与分析[J].地球物理学进展,2010,25(4):1175-1179.Xu R G,Zhang Y,Wang L,et al.Tracing and analyzinganomalies of horizontal geomagnetic component before andafter the MS5.7Jiujiang-Ruichang earthquake[J].Progressin Geophysics(in Chinese),2010,25(4):1175-1179.
[18]管志宁,郝天珧,姚长利.21世纪重力与磁法勘探的展望[J].地球物理学进展,2002,17(2):237-244.Guan Z N,Hao T Y,Yao C L.Prospect of gravity andmagnetic exploration in the 21st century[J].Progress inGeophysics(in Chinese),2002,17(2):237-244.
[19]刘天佑.位场勘探数据处理新方法[M].北京:科学出版社,2007.Liu T Y.New Process Method of Source Field ProspectingData[M](in Chinese).Beijing:Science Press,2007.
[20]刘天佑.重磁勘探软件手册(GMS3.0)方法原理[D].武汉:中国地质大学,2009.Liu T Y.Handbook of Gravity and Magnetic ProspectingSoftware and Principles of GMS3.0[D](in Chinese).Wuhan:China University of Geosciences,2009.
[21]虎喜凤,刘明涛,赵丽,等.豫北地区居里面与地震关系的研究[J].华北地震科学,2000,18(3):26-31.Hu X F,Liu M T,Zhao L,et al.Study of the relationshipbetween curie surface and earthquakes in north Henan[J].North China Earthquake Sciences(in Chinese),2000,18(3):26-31.
[22]张先,刘敏,赵丽等.华北地区居里温度面与地震活动的再研究[J].物探与化探,2000,24(2):81-86.Zhang X,Liu M,Zhao L,et al.Restudy of curietemperature interface and seismicity in north China.[J].Geophysical&Geochemical Exploration(in Chinese),2000,24(2):81-86.
[23]黄兆熊,高德章.上海及其邻域居里面与地震活动趋势[J].地震学报,1992,14(3):363-365.Huang Z X,Gao D Z.Curie temperature interface andseismicity in Shanghai and its adjacent areas[J].Geophysical&Geochemical Exploration(in Chinese),1992,14(3):363-365.
[24]邵世德,严晓红.安徽省及邻区居里面的地质分析[J].合肥工业大学学报(自然科学版),1992,15(2):100-105.Shao S D,Yan X H.Geological analysis curie temperaturesurface in Anhui Province and its adjacent areas[J].Journalof Hefei University of Technology(Natural Science)(inChinese),1992,15(2):100-105.
[25]徐树桐,袁学诚,吴维平,等.大别山黄石-六安反射地震剖面新的地质解释[J].地质通报,2008,27(1):19-26.Xu S T,Yuan X C,Wu W P,et al.New geologicalinterpretation of the seismic reflection rofile from Huangshi toLiu’an across the Dabie Montains,China[J].GeologicalBulletin of China(in Chinese),2008,27(1):19-26.
[26]Blakely R J.Potential Theory in Gravity and Magnetic Applications[M].New York:Cambridge University Press,1995.
[27]潘永信,朱日祥.大别山超高压变质岩带的岩石磁学和磁组构研究及其地质意义[J].岩石学报,2005,21(4):1101-1108.Pan Y X,Zhu R X.Rock magnetism and magnetic fabricstudies of the ultrahigh-pressure(UHP)metamorphic rocksfrom the Dabie organic belt,East-central China:implicationsfor retrograde metamorphism[J].Acta Petrologica Sinica(inChinese),2005,21(4):1101-1108.
[28]徐海军,金振民,欧新功,等.超高压榴辉岩退变质作用对岩石磁化率的影响[J].地球科学-中国地质大学学报,2004,29(6):674-684.Xue H J,Jin Z M,Ou X G,et al.Effects of retrogression ofUltrahigh-Pressure eclogites on magnetic susceptibility andanisotropy[J].Earth Science-Journal of China University ofGeosciences(in Chinese),2004,29(6):674-684.