参考文献/References:
[1] Yin A,Harriso T M.The Tectonics of Asia[M].Cambridge:Cambridge University Press,1996:345-370.
[2] Harker B R,Ratschbacher L W,Webb L,et al.U-Pb zircon ages constrain the architecture of the ultrahigh pressure Qinling-Dabie orogen,China[J].Earth and Planetary Science Letters,1998,161(1/4):215-230.
[3] Liu X C,Jahn B M,Liu D Y,et al.SHRIMP U-Pb zircon dating of a metagabbro and eclogites from western Dabieshan(Hong’an Block),China,and its tectonic implications[J].Tectonophysics,2004,394(3/4):171-192.
[4] 杨泽强.河南商城县汤家坪钼矿辉钼矿铼-锇同位素年龄及地质意义[J].矿床地质,2007,26(3):289-295.
[5] 魏庆国,高昕宇,赵太平,等.大别北麓汤家坪花岗斑岩锆石LA-ICP-MS U-Pb定年和岩石地球化学特征及其对岩石成因的制约[J].岩石学报,2010,26(5):1550-1562.
[6] 李毅,李偌,杨永飞,等.大别山北麓钼矿床地质特征和地球动力学背景[J].岩石学报,2013,29(1):95-106.
[7] 陈红瑾,陈衍景,张静,等.安徽省金寨县沙坪沟钼矿含矿岩体锆石U-Pb年龄和Hf同位素特征及其地质意义[J].岩石学报,2013,29(1):131-145.
[8] 周泰禧,陈江峰,张巽,等.北淮阳花岗岩-正长岩带地球化学特征及其大地构造意义[J].地质论评,1995,41(2):144-151.
[9] 周泰禧,陈江峰,李学明,等.安徽舒霍正长岩带侵入体的40Ar/39Ar法同位素地质年龄[J].安徽地质,1992,2(1):4-11.
[10] 王根节,张怀东,项斌,等.北淮阳构造带东段中生代岩浆活动与多金属成矿作用[J].安徽地质,2010,20(4):267-272.
[11] 周伟伟,蔡剑辉,阎国翰,等.安徽金寨响洪甸碱性侵入岩年代学、岩石地球化学及其意义[J].矿床地质,2014,33(1):104-122.
[12] 彭智,杜建国,陈芳,等.北淮阳东段同兴寺碱性岩体地球化学特征、LA-ICP-MS锆石U-Pb年龄及其地质意义[J].地质学报,2015,89(4):701-714.
[13] 陈芳,彭智,董婷婷,等.北淮阳东段张冲闪长玢岩地球化学特征、LA-ICP-MS锆石U-Pb年龄及其地质意义[J].大地构造与成矿学,2016,40(6):1289-1298.
[14] 邱军强,彭智,陈芳,等.北淮阳东段杨家湾岩体地球化学特征、锆石U-Pb定年及地质意义[J].华东地质,2016,37(2):89-96.
[15] 鹿献章,周博文,彭智,等.北淮阳东段河棚岩体地球化学特征、LA-ICP-MS锆石U-Pb年龄及地质意义[J].华东地质,2017,38(2):81-90.
[16] 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):1-14.
[17] 徐树桐,刘贻灿,江来利,等.大别山的构造格局和演化[M].北京:科学出版社,1994:1-175.
[18] Li S G,Xiao Y,Liu D L,et al.Collision of the North China and Yangtze Blocks and formation of coesite-bearing eclogites: Timing and processes[J].Chemical Geology,1993,109(1/4):89-111.
[19] Cong B L,Wang Q C,Zhai M G,et al.Ultrahigh-pressure metamorphic rocks in the Dabie-Sulu region,China: Their formation and exhumation[J].Island Arc,1994,3(3):135-150.
[20] 张怀东,王波华,郝越进,等.安徽沙坪沟斑岩型钼矿床地质特征及综合找矿信息[J].矿床地质,2012,31(1):41-51.
[21] 彭智.北淮阳东段基础地质评述[J].安徽地质,2004,14(3):172-176.
[22] 杜建国.大别造山带中生代岩浆作用与成矿地球化学研究[D].合肥: 合肥工业大学,2000:1-176.
[23] 彭智,陆三明,徐晓春.北淮阳构造带东段金多金属矿床区域成矿规律[J].合肥工业大学学报(自然科学版),2005,28(4):364-368.
[24] 陆三明,徐晓春,彭智.北淮阳构造带东段隐爆角砾岩型多金属矿床的地质特征及成因[J].地质与勘探,2005,41(3):7-11.
[25] Benisek A,Dachs E,Kroll H.A ternary feldspar-mixing model based on calorimetric data:development and application[J].Contributions to Mineralogy and Petrology,2010,160(3):327-337.
[26] Liu Y S,Gao S,Hu Z C,et al.Continental and oceanic crust recycling-induced melt-peridotite interactions in the Trans-North China Orogen:U-Pb dating,Hf isotopes and trace elements in zircons from mantle xenoliths[J].Journal of Petrology,2009,51(1/2):537-571.
[27] 侯可军,李延河,田有荣.LA-MC-ICP-MS锆石微区原位U-Pb定年技术[J].矿床地质,2009,28(4):481-492.
[28] Sláma J,Kosler J,Condon D J,et al.Plesovice zircon-A new natural reference material for U-Pb and Hf isotopic microanalysis[J].Chemical Geology,2008,249(1/2):1-35.
[29] McDonough W F,Sun S S.The composition of the Earth[J].Chemical Geology,1995,120(3/4):223-253.
[30] Sun S S,McDonough W F.Chemical and isotopic systematics of oceanic basalts:implications for mantle composition and processes[J].Geological Society London Special Publications,1989,42(1):313-345.
[31] Tarney J,Jones C E.Trace element geochemistry of orogenic igneous rocks and crustal growth models[J].Journal of Geological Society of London,1994,151(5):855-868.
[32] 吴元宝,郑永飞.锆石成因矿物学研究及其对U-Pb年龄解释的制约[J].科学通报,2004,49(16):1589-1604.
[33] Belousova E,Griffin W,O’Reilly S Y,et al.Igneous zircon:trace element composition as an indicator of source rock type[J].Contributions to Mineralogy and Petrology,2002,143(5):602-622.
[34] 赵新福,李建威,马昌前,等.北淮阳古碑花岗闪长岩侵位时代及地球化学特征:对大别山中生代构造体制转换的启示[J].岩石学报,2007,23(6):1392-1402.
[35] Rapp R P,Watson E B.Dehydration melting of metabasalt at 8—32 kbar:Implications for continental growth and crust-mantle recycling[J].Journal of Petrology,1995,36(4):891-931.
[36] Sen C,Dunn T.Dehydration melting of a basaltic composition amphibolites at 1.5 and 2.0 GPa:implications for the origin of adakites[J].Contributions to Mineralogy and Petrology,1994,117(4):394-409.
[37] Fan W M,Guo F,Wang Y J,et al.Late Mesozoic Volcanism in the northern Huaiyang tectono-magmatic belt,central China:Partial melts from a lithospheric mantle with subducted continental crust relicts beneath the Dabie Orogen?[J].Chemical Geology,2004,209(1/2):27-48. [38] Pearce J A,Harris N B W,Tindle A G.Trace element discrimination diagrams for the tectonic interpretation of granitic rocks[J].Journal of Petrology,1984,25(4):956-983.
[39] Wilson M. Igneous petroge
nesis[M].London:Springer,1998.
[40] Jahn B M,Wu F Y,Loc C H,et al.Crust-mantle interaction induced by deep subduction of the continental crust:Geochemical and Sr-Nd isotopic evidence from post-collisional mafic-ultramafic intrusions of the northern Dabie complex,central China[J].Chemical Geology,1999,157(1/2):119-146.
[41] 李曙光,Hart S R,郑双根,等.中国华北、华南陆块碰撞时代的钐-钕同位素年龄证据[J].中国科学(B辑),1989,19(3):312-319.
[42] Li C,Chen Y J,He S D.Age,mechanism and direction of East Qinling-Dabieshan lithosphere delamination-Petrological evidence and stipulation[J].Acta Geochemistry,2001,20(1):59-72.
[43] 马昌前,杨坤光,明厚利,等.大别山中生代地壳从挤压转向伸展的时间:花岗岩的证据[J].中国科学(D辑),2003,33(9):817-827.
[44] Batchelor R A,Bowden P.Petrogenetic interpretation of granitoid rock series using multicationic paramet-ers[J].Chemical Geology,1985,48(1):43-55.
[45] Pearce J.Source and settings of granitic rocks[J].Episodes,1996,19(4):120-125.
[46] Hammarstrom J M,Zen E A. Aluminum in hornblende: An empirical igneous geobarometer[J].American Mineralogist,1986,71(11):1297-1313.
[47] 潘国强,陆现彩,于航波.北淮阳中生代adakite岩石地球化学特征及成因讨论[J].岩石学报,2001,17(4):541-550.
[48] 薛怀民,董树文,刘晓春.北大别东部白垩纪埃达克质火山岩及其锆石U-Pb年代学[J].地球化学,2002,31(5):455-463.
[49] Wang Y,Fan W,Peng T,et al.Nature of the Mesozoic lithospheric mantle and tectonic decoupling beneath the Dabie Orogen,Central China:Evidence from 40Ar/39Ar geochronology,elemental and Sr-Nd-Pb isotopic compositions of early Cretaceous mafic igneous rocks[J].Chemical Geology,2005,220(3/4):165-189.
相似文献/References:
[1]翁望飞,丁勇.德兴含铜埃达克质斑岩的地球化学特征、成因及地质意义[J].华东地质,2015,36(02):104.
[2]罗春林,刘高峰,左祖发.赣南坪市花岗岩体LA-ICP-MS锆石U-Pb年龄、地球化学特征及构造意义[J].华东地质,2016,37(02):79.[doi:10.16788/j.hddz.32-1865/P.2016.02.001]
LUO Chun-lin,LIU Gao-feng,ZUO Zu-fa.LA-ICP-MS zircon U-Pb ages and geochemical characteristics of the Pingshi granitic pluton in southern Jiangxi and their tectonic significance[J].East China Geology,2016,37(04):79.[doi:10.16788/j.hddz.32-1865/P.2016.02.001]
[3]王建中钱壮志,徐 刚,姜 超.西秦岭白马山“C”型埃达克岩成因:地球化学、Sr-Nd-Pb同位素制约[J].华东地质,2016,37(03):174.[doi:10.16788/j.hddz.32-1865/P.2016.03.003]
WANG Jian-zhong,QIAN Zhuang-zhi,XU Gang,et al.Petrogenesis of the Baimashan C-type adakite in Western Qinling: Constraints from their geochemistry and Sr-Nd-Pb isotopic compositions[J].East China Geology,2016,37(04):174.[doi:10.16788/j.hddz.32-1865/P.2016.03.003]
[4]孙建东,骆学全,张雪辉,等.江西省铅山县二叠纪海相火山岩锆石U-Pb年龄及Lu-Hf同位素组成[J].华东地质,2016,37(04):246.[doi:10.16788/j.hddz.32-1865/P.2016.04.002]
SUN Jian-dong,LUO Xue-quan,ZHANG Xue-hui,et al.Zircon U-Pb age and Lu-Hf isotopic compositions of the Permian marine volcanic rocks in Qianshan County, Jiangxi Province[J].East China Geology,2016,37(04):246.[doi:10.16788/j.hddz.32-1865/P.2016.04.002]
[5]赵志雄,许 海,贾元琴,等.内蒙古北山地区斑状花岗闪长岩地球化学、LA-ICP-MS锆石U-Pb年龄及地质意义[J].华东地质,2016,37(04):252.[doi:10.16788/j.hddz.32-1865/P.2016.04.003]
ZHAO Zhi-xiong,XU Hai,JIA Yuan-qin,et al.Geochemistry and LA-ICP-MS zircon U-Pb age of porphyritic granodiorite in the Beishan orogenic belt in Inner Mongolia and their geological significance[J].East China Geology,2016,37(04):252.[doi:10.16788/j.hddz.32-1865/P.2016.04.003]
[6]史洪峰,续琰祺,张 景,等.西藏赛卓花岗闪长岩锆石U-Pb年龄、地球化学特征及构造意义[J].华东地质,2018,39(02):90.[doi:10.16788/j.hddz.32-1865/P.2018.02.002]
SHI Hong-feng,XU Yan-qi,ZHANG Jing,et al.Geochemistry and zircon U-Pb dating of the Saizhuo granodiorite in Tibet and their tectonic significance[J].East China Geology,2018,39(04):90.[doi:10.16788/j.hddz.32-1865/P.2018.02.002]
[7]周琦忠,张 琪,宗德林,等.徐州贾汪地区暗色岩锆石U-Pb年龄及金刚石成因探讨[J].华东地质,2018,39(03):202.[doi:10.16788/j.hddz.32-1865/P.2018.03.006]
ZHOU Qi-zhong,Zhang Qi,ZONG De-lin,et al.Zircon U-Pb dating of dark rocks in the Jiawang area, Xuzhou, and diamond genesis analysis[J].East China Geology,2018,39(04):202.[doi:10.16788/j.hddz.32-1865/P.2018.03.006]
[8]肖 林,程招勋,都士卓,等.乌兰浩特地区中性火山岩LA-ICP-MS锆石U-Pb年龄、地球化学特征及成因探讨[J].华东地质,2019,40(04):253.[doi:10.16788/j.hddz.32-1865/P.2019.04.002]
XIAO Lin,CHENG Zhao-xun,DU Shi-zhuo,et al.LA-ICP-MS zircon U-Pb age, geochemistry and genesis of intermediate volcanic rocks in the Ulanhot area, Inner Mongolia[J].East China Geology,2019,40(04):253.[doi:10.16788/j.hddz.32-1865/P.2019.04.002]
[9]范飞鹏,陈乐柱,李海立,等.南岭东段枫树洞稀土矿中辉长质包体锆石U-Pb年代学、地球化学特征及其成岩作用[J].华东地质,2020,41(04):325.[doi:10.16788/j.hddz.32-1865/P.2020.04.003]
FAN Fei-peng,CHEN Le-zhu,LI Hai-li,et al.Zircons in the gabbro enclaves of Fengshudong REE deposit in Eastern Nanling Mountains: Chronology, geochemistry and diagenesis[J].East China Geology,2020,41(04):325.[doi:10.16788/j.hddz.32-1865/P.2020.04.003]
[10]于俊杰,刘平,林丰增,等.福建三沙湾90 ka以来沉积物来源及环境演变研究[J].华东地质,2022,43(01):30.[doi:10.16788/j.hddz.32-1865/P.2022.01.003]
YU Junjie,LIU Ping,LIN Fengzeng,et al.Sediment sources and environment evolution since 90 ka in Sansha Bay, Fujian Province[J].East China Geology,2022,43(04):30.[doi:10.16788/j.hddz.32-1865/P.2022.01.003]