引文
[1]黄宝春,周烑秀,朱日祥.从古地磁研究看中国大陆形成与演化过程[J].地学前缘,2008,15(3):348-359.[HUANG Bao-chun,ZHOU Yaoxiu,ZHU Rixiang.Discussions on phanero-zoic evolution and formation of continental China,based on pa-leomagnetic studies[J].Earth Science Frontiers,2008,15(3):348-359.]
[2]Zhang R Y,Liou J G,Ernst W G.The Dabie-Sulu continentalcollision zone:A comprehensive review[J].Gondwana Re-search,2009:1-26.
[3]Yokoyama M,Liu Y,Halim N,et al.Paleomagnetic study ofUpper Jurassic rocks from the Sichuan basin:tectonic aspectsfor the collision between the Yangtze Block and the North Chi-na Block[J].Earth and Planetary Science Letters,2001,193:273-285.
[4]许志琴.深俯冲和折返动力学——来自中国大陆科学钻探主孔及苏鲁超高压变质带的制约[J].岩石学报,2007,23(12):3041-3053.[XU Zhiqin.Contiental deep subduction and exhu-mation dynamics:Evidence from the main hole of the ChineseContinental Scientific Drilling and Sulu HP-UHP metamorphicterrane[J].Acta Petrologica Sinica,2007,23(12):3041-3053.]
[5]刘福来,许志琴,杨经绥,等.南苏鲁超高压带和高压带边界的准确限定——来自变质岩锆石中矿物包体的证据[J].岩石学矿物杂志,2005,24(1):32-46.[LIU Fulai,XU Zhiqin,YANGJinsuo.Tracing The boundary between UHP and HP meta-morphic belts in southwestern Sulu terrane,eastern China:Evidence from mineral inclusions in zircons from metamorphicrocks[J].Acta Petrologica et Mineralogica,2005,24(1):32-46.]
[6]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):346-359.[YANG Wencai,YU Changqing.Kinetics anddynamics of development of the Dabie-Sulu UHPM terranesbased on geophysical evidence[J].Chinese J.Geophys.,2001,44(3):346-359.]
[7]蔡乾忠.横贯黄海的中朝造山带与北-南黄海成盆成烃关系[J].石油与天然气地质,2005,26(2):185-196.[CAIQianzhong.Relationship between Sino-Korean orogenic belt traversing Yellow Sea and basin evolution and hydrocarbongeneration in North and South Yellow Sea basins[J].Oil&Gas Geology,2005,26(2):185-196.]
[8]陈建文.南黄海盆地区域地质背景[R].2009.[CHEN Jian-wen.Regional Geological Setting of South Yellow Sea Basin[R].2009.]
[9]任纪舜.南黄海盆地区域地质特征及其演化[R].2009.[RENJishun.Regional Geological Characteristics and DevelopmentProcesses of South Yellow Sea Basin[R].2009.]
[10]Faure M,Lin W,Le N.Where is the North China-South Chi-na block boundary in eastern China[J].Geology,2001,29(2):119-122.
[11]郝天珧,Mancheol S,徐亚,等.黄海地球物理场与深部构造——关于中朝与扬子块体边界结合带在海区位置的讨论[R].2008.[HAO Tianyao,Suh Mancheol,XU Ya,et al.Geophysical field and deep structure in Yellow Sea-where isthe Combined belt between North China craton and Yangtzeblocks[R].2008.]
[12]万天丰.中国大地构造学纲要[M].北京:地质出版社,2004.[WAN Tianfeng.The Summary of Tectonics in China[M].Geological Publishing House,2004.]
[13]王志才,晁洪太,杜宪宋,等.南黄海北部千里岩断裂活动性初探[J].地震地质,2008,30(1):176-186.[WANG Zhicai,CHAO Hongtai,DU Xiansong,et al.Preliminary survey onthe quaternary activities of the Qianliyan fault in the northernpart of the South Yellow Sea[J].Seismology and Geology,30(1):176-186.]
[14]韩宗珠,肖莹,于航,等.南黄海千里岩岛榴辉岩的矿物化学及成因探讨[J].海洋湖沼通报,2007(1):83-87.[HAN Zong-zhu,XIAO Ying,YU Hang,et al.A study on the mineralchemistry and genesis of the eclogite from Qianliyan island,the Southern Huanghai Sea[J].Transactions of Oceanologyand Limnonlgy,2007(1):83-87.]
[15]陈宣华,王小凤,张青,等.郯庐断裂带形成演化的年代学研究[J].长春科技大学学报,2000,30(3):215-220.[CHEN Xu-anhua,WANG Xiaofeng,ZHANG Qing.Geochronologicstudy on the formation and evolution of Tan-Lu Fault[J].Journal of Changchun University of Science and Technology,2000,30(3):215-220.]
[16]胡望水.郯庐断裂带及其周缘中新生代盆地发育特征[J].海洋地质与第四纪地质,2003,23(4):51-58.[HU Wangshui.Characteristics of Tan-Lu Fault zone and development ofMesozoic and Cenozoic basins along it[J].Marine Geologyand Quaternary Geology,2003,23(4):51-58.]
[17]龙汉春.关于郯庐断裂巨大平移问题的商榷[J].华东地质学院学报,1987,10(1):15-23.[LONG Hanchun.Discussionon the huge slip displacement of Tan-Lu Fault[J].Journal ofEast China Geological Institute,1987,10(1):15-23.]
[18]乔秀夫,张安棣.华北块体——胶辽朝块体与郯庐断裂[J].中国地质,2002,29(2):337-345.[QIAO Xiufu,ZHANG An-di.North China block,Jiao-Liao-Korea block and Tanlu fault[J].Geology in China,2002,29(2):337-345.]
[19]唐新功,陈永顺,唐哲.应用布格重力异常研究郯庐断裂构造[J].地震学报,2006,28(6):603-610.[TANG Xingong,CHEN Yongshun,TANG Zhe.Bouguer gravity study of mid-dle section of Tanlu Fault[J].Acta Seismologica Sinica,2006,28(6):603-610.]
[20]王小民,夏木林,Liou J G.中国东部的含科石英榴辉岩带的发现——郯庐断裂平移作用的证据[J].中国区域地质,1992(1):88-91.[WANG Xiaomin,XIA Mulin,LIOU J G.Thediscovery of coesite-bearing eclogite belt in eastern China[J].Regional Geology of China,1992(1):88-91.]
[21]徐嘉炜,马国锋.郯庐断裂带研究的十年回顾[J].地质论评,1992,38(4):316-322.[XU Jiawei,MA Goufeng.Review often years of research on the Tan-Lu fault[J].Geological Re-view,1992,38(4):316-322.]
[22]朱光,王勇生,刘国生,等.华北与华南板块的碰撞过程—郯庐断裂带周边的指示[R].2008.[ZHU Guang,WANG Yong-sheng,LIU Guosheng,et al.The collision processes betweenthe North and South China blocks-Evidences from adjacentarea of Tan-Lu Fault[R].2008.]
[23]朱光,徐嘉炜,刘国生,等.下扬子地区沿江前陆盆地形成的构造控制[J].地质论评,1998,44(2):120-129.[ZHU Guang,XU Jiawei,LIU Guosheng,et al.Tectonic control on devel-opment of the foreland basin along the Yangtze River in theLower Yangtze River region[J].Geological Review,1998,44(2):120-129.]
[24]许志琴,曾令森,梁凤华,等.大陆板片多重性俯冲与折返的动力学模式——苏鲁高压超高压变质地体的折返年龄限定[J].岩石矿物学杂志,2005,24(5):357-368.[XU Zhiqin,ZENGLingsen,LIANG Fenghua.A dynamic model for sequentialsubduction and exhumation of a continental slab:Age con-straints on the timing of exhumation of the Sulu HP-UHPmetamorphic terrane[J].Acta Petrologica et Mineralogical,2005,24(5):357-368.]
[25]赵志新,徐纪人,许志琴.上地幔三维S波速度结构与大别苏鲁超高压变质带俯冲折返机制探讨[J].岩石学报,2004,20(1):157-164.[ZHAO Zhixin,XU Jiren,XU Zhiqin.3DSwave velocity structure in the upper mantle and the mecha-nism investigation for the ultrahigh-pressure metamorphosedbelt in the Dabie-Sulu region[J].Acta Petrologica Sinica,2004,20(1):157-164.]
[26]Zhang K,Cai J,Zhu J.North China and South China collisioninsights from analogue modeling[J].Journal of Geodynam-ics,2006,42:38-51.
[27]张训华.中国海域构造地质学[M].北京:海洋出版社,2008.[ZHANG Xunhua.Marine Tectonic Geology in China[M].Beijing:Ocean Press,2008.]
[28]李金良.胶莱盆地沉积分析及构造演化[D].中国地质科学院,2006.[LI Jinliang.Analysis of sedimentary and TectonicEvolution of the Jiaolai Basin[D].Chinese Academy of Geo-sciences,2006.]
[29]姜同海.胶莱盆地构造特征及演化[D].山东科技大学,2005.[JIANG Tonghai.The Structural Characteristics and Evolu-tion of Jiaolai Basin[D].Shandong University of Science andTechnology,2005.]
[30]佟彦明.胶莱盆地构造演化研究[D].中国地质大学,2007.[TONG Yanming.Tectonic Evolution of Jiaolai Basin[D].China University of Geosciences,2007.]
[31]张岳桥,李金良,张田,等.胶莱盆地及其邻区白垩纪—古新世沉积构造演化历史及其区域动力学意义[J].地质学报,2008,82(9):1229-1257.[ZHANG Yueqiao,LI Jinliang,ZHANGTian,et al.Cretaceous to Paleocene tectonic sedimentary evo-lution of the Jiaolai Basin and the contiguous areas of theShandong Peninsula(north China)and its geodynamic impli-cations[J].Acta Geologica Sinica,2008,82(9):1229-1257.]
[32]翟慎德.胶莱盆地形成演化与油气形成条件[D].中国科学院广州地球化学研究所,2003.[ZHAI Shende.Formation andEvolution of Jiaolai Basin and Formation Condition of Combi-nation Gas[D].Guangzhou Institute of Geochemistry,Chi-nese Academy of Sciences,2003.]
[33]Xu Z,Yang W,Ji S,et al.Deep root of a continent-continentcollision belt:Evidence from the Chinese continental scientificdrilling(CCSD)deep borehole in the Sulu ultrahigh-pressure(HP-UHP)metamorphic terrane,China[J].Tectonophys-ics,2009,475:204-219.
[34]江苏省地质矿产局.江苏及上海区域地质志[M].北京:地质出版社,1984.[Jiangsu Bureau of Geology and Mineral Re-sources.Regional Geological Report in Jiangsu and Shanghai[M].Geological Publishing House,1984.]
[35]郭玉贵,李延成,许东禹,等.黄东海大陆架及邻域大地构造演化史[J].海洋地质与第四地质,1997,17(1):1-12.[GUOYugui,LI Yancheng,XU Dongyu,et al.Tectonic evolutionof Yellow Sea,East China Sea and continental shelf and adja-cent areas[J].Marine Geology and Quaternary Geology,1997,17(1):1-12.]
[36]马兆同,刘慧勤,马兆祥.胶南造山带及邻近地区的重磁场特征及地质解释[J].山东地质,1997,13(1):92-102.[MAZhaotong,LIU Huiqin,MA Zhaoxiang.Features of gravityand magnetic fields and geological explanation of the Jiaonanorogenic belt and its neighbor areas[J].Geology of Shan-dong,1997,13(1):92-102.]
[37]冯志强,陈春峰,姚永坚,等.南黄海北部前陆盆地的构造演化与油气突破[J].地学前缘,2008,15(6):219-231.[FENGZhiqiang,CHEN Chunfeng,YAO Yongjian,et al.Tectonicevolution and exploration target of the northern foreland ba-sin of the South Yellow Sea[J].Earth Science Frontiers,2008,15(6):219-231.]
[38]张泽明,许志琴,刘福来,等.南苏鲁造山带根部的物质组成及变质作用[J].地质通报,2002,21(10):609-616.[ZHANGZeming,XU Zhiqin,LIU Fulai,et al.Composition and meta-morphism of the root of the southern Sulu orogen[J].Geolog-ical Bulletin of China,2002,21(10):609-616.]
[39]翟明国,郭敬辉,王清晨,等.苏鲁变质带北部的岩石构造单元及结晶块体推覆构造[J].地质科学,2000,35(1):16-26.[ZHAI Mingguo,GUO Jinghui,WANG,Qingchen,et al.Di-vision of petrological-tectonic units in the northern Sulu ultra-high pressure zone:an example of thick-skin thrust of crys-talline units[J].Scientia Geologica Sinica,2000,35(1):16-26.]
[40]苏文,从柏林,游振东,等.石榴石塑性变形的机制:水解弱化[J].中国科学D辑,2001,31(12):999-1004.[SU Wen,CONG Bailin,YOU Zhendong,et al.Ductile deformationmechanism of garnet:hydrolysis weaken[J].Science in Chi-na(Series D),2001,31(12):999-1004.]
[41]许志琴,戚学祥,杨经绥,等.苏鲁高压—超高压变质地体的陆—陆碰撞深俯冲剥蚀模式[J].地球科学,2006,31(4):427-436.[XU Zhiqin,QI Xuxiang,YANG Jingsui,et al.Deep subduction erosion model for continent collision of theSulu HP-UHP metamorphic terrain[J].Earth Science,2006,31(4):427-436.]
[42]从柏林,王清晨.大别山-苏鲁超高压变质带研究的最新进展[J].科学通报.1999,44(11):1127-1141.[CONG Bailin,WANG Qingchen.The advanced progress of Dabie-Sulu UHPmetamorphism terrain[J].Chinese Science Bulletin,1999,44(11):1127-1141.]
[43]刘良,杨家喜,章军锋,等.超高压岩石中矿物显微出溶结构研究进展——面临问题与挑战[J].科学通报,2009,54(10):1387-1400.[LIU Liang,YANG Jiaxi,ZHANG Junfeng,etal.Exsolution microstructures in ultrahigh-pressure rocks:Progress,controversies and challenges[J].Chinese ScienceBulletin,2009,54(10):1387-1400.]
[44]杨经绥,李天福,梁凤华,等.中国大陆科学钻探主孔(CCSD-MH)石榴石橄榄岩:一个经历了深俯冲作用的古生代超镁铁质侵入体[J].岩石学报,2007,23(12):3153-3170.[YANGJingsui,LI Tianfu,LIANG Fenghua,et al.Garnet peridotitein CCSD-MH in the Sulu UHPM belt:A deep subductedPlaeozoic ultramafic intrusion[J].Acta Petrologica Sinica.2007,23(12):3153-3170.]
[45]周永胜,何昌荣,杨晓松.中地壳韧性剪切带中的水与变形机制[J].中国科学D辑,2008,38(7):819-832.[ZHOU Yong-sheng,HE Changrong,YANG Xiaosong.Water in the mid-dle crust ductile shear zone and its deformation mechanism[J].Science in China(Series D),2008,38(7):819-832.]
[46]嵇少丞,王茜,王勤,等.苏鲁—大别超高压变质岩的弹性力学性质与密度的关系[J].岩石学报,2007,23(12):3054-3064.[JI Shaocheng,WANG Qian,WANG Qin,et al.Correlationbetween elastic properties and density for Sulu-Dabie UHPmetamorphic rocks[J].Acta Petrologica Sinica,2007,23(12):3054-3064.]
[47]许志琴,李廷栋,杨经绥,等.大陆动力学的过去、现在和未来——理论与应用[J].岩石学报,2008,24(7):1433-1444.[XU Zhiqin,LI Tingdong,YANG Jingsui,et al.Advancesand prospective of continental dynamics:Theory and applica-tion[J].Acta Petrologica Sinica,2008,24(7):1433-1444.]
[48]许志琴,杨经绥,李海兵,等.中央造山带早古生代地体构架与高压/超高压变质带的形成[J].地质学报,2006,80(12):1793-1806.[XU Zhiqin,YANG Jingsui,LI Haibing,et al.The early Palaeozoic terrene framework and the formation ofthe pressure(HP)and ultra-high pressure(UHP)metamorphicbelts at the central orogenic belt(COB)[J].Acta GeologicaSinica,2006,80(12):1793-1806.]
[49]杨经绥,许志琴,张建新,等.中国主要的高压—超高压变质带构造背景[J].岩石学报,2009,25(7):1529-1560.[YANGJingsui,XU Zhiqin,ZHANG Jianxin,et al.Tectonic settingof main high-and ultrahigh-pressure metamorphic belts inChina and adjacent region and discussion on their subductionand exhumation mechanism[J].Acta Petrologica Sinica,2009,25(7):1529-1560.]
[50]张建新,杨天南,许志琴,等.胶南地区的伸展作用——以胶南—诸城一带为例[J].地球学报,1997,18(2):122-128.[ZHANG Jianxin,YANG Tiannan,XU Zhiqin,et al.Exten-sion of Jiaonan area in Shandong[J].Acta Geoscientica Sini-ca,1997,18(2):122-128.]