必须声明标量变量 "@Script_ID"。 安徽南陵—宣城地区岩浆岩锆石U-Pb年龄及元素地球化学特征-《地球科学与环境学报》
|本期目录/Table of Contents|

[1]徐晓春,安昱华,许心悦,等.安徽南陵—宣城地区岩浆岩锆石U-Pb年龄及元素地球化学特征[J].地球科学与环境学报,2020,42(01):15-35.[doi:10.19814/j.jese.2019.05023]
 XU Xiao-chun,AN Yu-hua,XU Xin-yue,et al.Zircon U-Pb Ages and Element Geochemistry Characteristics of Magmatic Rocks in Nanling-Xuancheng Area of Anhui, China[J].Journal of Earth Sciences and Environment,2020,42(01):15-35.[doi:10.19814/j.jese.2019.05023]
点击复制

安徽南陵—宣城地区岩浆岩锆石U-Pb年龄及元素地球化学特征(PDF)
分享到:

《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

卷:
第42卷
期数:
2020年第01期
页码:
15-35
栏目:
基础地质与矿产地质
出版日期:
2020-01-15

文章信息/Info

Title:
Zircon U-Pb Ages and Element Geochemistry Characteristics of Magmatic Rocks in Nanling-Xuancheng Area of Anhui, China
文章编号:
1672-6561(2020)01-0015-21
作者:
徐晓春安昱华许心悦傅仲阳
(合肥工业大学 资源与环境工程学院,安徽 合肥 230009)
Author(s):
XU Xiao-chun AN Yu-hua XU Xin-yue FU Zhong-yang
(School of Resources and Environmental Engineering, Hefei University of Technology, Hefei 230009, Anhui, China)
关键词:
岩浆岩 锆石U-Pb年龄 元素地球化学 岩石成因 火山岩 侵入岩 成岩成矿关系 安徽
Keywords:
magmatic rock zircon U-Pb age element geochemistry petrogenesis volcanic rock intrusive rock relationship between magmatism and mineralization Anhui
分类号:
P588.1; P59
DOI:
10.19814/j.jese.2019.05023
文献标志码:
A
摘要:
安徽南陵—宣城地区是一个中—新生代火山-沉积盆地,位于长江中下游构造-岩浆-成矿带东北段的东南翼。对该区发育的岩浆岩开展了较为系统的LA-ICP-MS锆石U-Pb定年及岩石主量、微量和稀土元素分析,并与长江中下游构造-岩浆-成矿带其他地区岩浆岩进行对比,旨在确定岩浆岩的成岩时代、探讨岩浆岩成因及其与成矿的关系。南陵—宣城地区岩浆岩一部分侵入于盆地基底中,另一部分喷发形成盆地盖层,还有一部分产于盆地之上的推覆构造(体)中。侵入岩的岩性主要为花岗岩、花岗闪长岩、石英闪长岩、辉石闪长岩等,火山岩主要为英安质火山碎屑岩和熔岩。获得的侵入岩锆石U-Pb年龄主要为138~135 Ma,火山岩年龄均小于134 Ma,表明岩浆作用发生于晚中生代(燕山晚期)早白垩世。岩浆岩主量元素显示高Si、K的特征,为亚碱性高钾钙碱性系列岩石; 微量元素组成显示岩浆岩富集Rb、Th、U、K等大离子亲石元素,亏损Nb、Ta、Ti等高场强元素,火山岩比侵入岩较为亏损Sr和P; 球粒陨石标准化稀土元素配分模式均表现为富集轻稀土元素的右倾模式和较弱的Eu负异常。元素地球化学特征指示区内岩浆岩具有壳幔混源且以幔源为主的特征。南陵—宣城地区既发育与长江中下游构造-岩浆-成矿带隆起区(如铜陵地区)同位素地质年龄和地球化学特征基本一致的侵入岩,又发育与凹陷区(如庐枞、宁芜等盆地)同位素地质年龄和地球化学特征基本一致的火山—次火山岩,显示该区晚中生代岩浆作用具有长江中下游构造-岩浆-成矿带隆起区和凹陷区的双重特征。岩浆作用的双重特征暗示与其有关的成矿作用也可能具有双重性,即既可能发育与隆起区侵入岩浆作用有关的斑岩型、矽卡岩型和脉型铜金等多金属矿床,也可能发育与凹陷区火山—次火山岩有关的玢岩型铁(硫)矿床。
Abstract:
The Nanling-Xuancheng area of Anhui, which is a Meso-Cenozoic volcanic-sedimentary basin, is located in the southeastern limb of the northeastern part of middle-lower Yangtze river valley tectonic-magmatic-metallogenic belt. Zircon U-Pb dating, and major, trace and rare earth elements of the magmatic rocks in Nanling-Xuancheng area were focused, and compared with those of the magmatic rocks in other areas of middle-lower Yangtze river valley tectonic-magmatic-metallogenic belt, for determining the age, and discussing the petrogenesis of the magmatic rocks and the relationship between the magmatism and mineralization. In Nanling-Xuancheng area, a part of the magmatic rocks intruded into the basement of the basin or erupted as the cover rocks of the basin, and the other part of the magmatic rocks occurred in the nappe above the basin. The intrusive rocks are mainly granite, granodiorite, quartz diorite and pyroxene diorite, and the volcanic rocks are dacitic pyroclastic rocks and lavas. The results show that the zircon U-Pb ages of the intrusive rocks are between 138 Ma and 135 Ma, and the ages of the volcanic rocks are all less than 134 Ma, suggesting that the magmatism occurred in Early Cretaceous of Late Mesozoic(Late Yanshanian). The characteristics of major elements show that the magmatic rocks are high for Si and K, belonging to sub-alkaline and high-K calc-alkaline series; the characteristics of trace elements show that the magmatic rocks are rich in Rb, Th, U and K, and poor in Ti, Nb and Ta, the volcanic rocks are more deficient from intrusive rocks in Sr and P; the chondrite-normalized REE patterns show that the magmatic rocks are rich in LREE and have weak negative Eu anomalies. The element geochemical characteristics indicate that the magmatic rocks have the characteristics of crust-mantle mixed and mainly mantle-derived. Zircon U-Pb dating, and geological and geochemical characteristics of the magmatic rocks in Nanling-Xuancheng area indicate that the Late Mesozoic magmatism in the area has the dual characteristics of those in upwelling areas and depression areas of the middle-lower Yangtze river valley tectonic-magmatic-metallogenic belt, that is, the study area not only develops intrusive rocks in the upwelling area(such as Tongling area), but also develops volcanic rocks in the depression area(such as Luzong and Ningwu basins). The duality of magmatism may imply the duality of mineralization, that is, the study area may develop hydrothermal porphyry-type, skarn-type and vein-type Cu-Au and other polymetallic deposits related to intrusive magmatism, also porphyry-type Fe(S)deposits associated with volcanic-subvolcanic rocks.

参考文献/References:

[1] 常印佛,刘湘培,吴言昌.长江中下游铜铁成矿带[M].北京:地质出版社,1991. CHANG Yin-fo,LIU Xiang-pei,WU Yan-chang.The Copper-iron Belt of the Lower and Middle Reaches of the Changjiang River[M].Beijing:Geological Publishing House,1991.
[2] 周涛发,范 裕,袁 峰,等.长江中下游成矿带火山岩盆地的成岩成矿作用[J].地质学报,2011,85(5):712-730. ZHOU Tao-fa,FAN Yu,YUAN Feng,et al.Petrogensis and Metallogeny Study of the Volcanic Basins in the Middle and Lower Yangtze Metallogenic Belt[J].Acta Geologica Sinica,2011,85(5):712-730.
[3] 韩克从,陈玉忠,陈思松,等.茅山地区的推覆构造及其地质意义[J].大地构造与成矿学,1985,9(1):57-68. HAN Ke-cong,CHEN Yu-zhong,CHEN Si-song,et al.Nappe Structure in the Maoshan Area and Its Geologi-cal Significance[J].Geotectonica et Metallogenia,1985,9(1):57-68.
[4] 徐学思,胡连英.江苏茅山构造-滑覆反序叠置造山[J].中国区域地质,2001,20(3):280-285. XU Xue-si,HU Lian-ying.Maoshan Structure in Jiangsu-sliding-reversed Stacking Orogeny[J].Regional Geo-logy of China,2001,20(3):280-285.
[5] 黄润生,曹建忠.江苏茅山推覆构造带的分析与研究[J].地质学刊,2010,34(1):6-9. HUANG Run-sheng,CAO Jian-zhong.Analysis and Study on Maoshan Nappe Tectonic Zone in Jiangsu[J].Journal of Geology,2010,34(1):6-9.
[6] 李海滨,贾 东,武 龙,等.下扬子地区中—新生代的挤压变形与伸展改造及其油气勘探意义[J].岩石学报,2011,27(3):770-778. LI Hai-bin,JIA Dong,WU Long,et al.The Mesozoic-Cenozoic Compressional Deformation,Extensional Modification and Their Significance for Hydrocarbon Exploration in Lower Yangtze Region[J].Acta Petrologica Sinica,2011,27(3):770-778.
[7] LIU Y S,HU Z C,ZONG K Q,et al.Reappraisement and Refinement of Zircon U-Pb Isotope and Trace Ele-ment Analyses by LA-ICP-MS[J].Chinese Science Bulletin,2010,55(15):1535-1546.
[8] LUDWIG K R.User's Manual for Isoplot 3.00:A Geo-chronological Toolkit for Microsoft Excel[R].Berkeley:Berkeley Geochronology Center,2003.
[9] QI L,HU J,GREGOGIRE D C.Determination of Trace Elements in Granites by Inductively Coupled Plasma Mass Spectrometry[J].Talanta,2000,51(3):507-513.
[10] HERMANN J,RUBATTO D,KORSAKOV A.Multiple Zircon Growth During Fast Exhumation of Diamondiferous,Deeply Subducted Continental Crust(Kokc-hetav Massif,Kazakhstan)[J].Contributions to Mineralogy and Petrology,2001,141(1):66-82.
[11] MIDDLEMOST E A K.Naming Materials in the Magma/Igneous Rock System[J].Earth-science Reviews,1994,37(3/4):215-224.
[12] PECCERILLO A,TAYLOR S R.Geochemistry of Eocene Calc-alkaline Volcanic Rocks from the Kastomonon Area,Northern Turkey[J].Contributions to Mineralogy and Petrology,1976,58(1):63-81.
[13] 周涛发,范 裕,王世伟,等.长江中下游成矿带成矿规律和成矿模式[J].岩石学报,2017,33(11):3353-3372. ZHOU Tao-fa,FAN Yu,WANG Shi-wei,et al.Meta-llogenic Regularity and Metallogenic Model of the Middle-lower Yangtze River Valley Metallogenic Belt[J].Acta Petrologica Sinica,2017,33(11):3353-3372.
[14] 徐晓春,左 续,何 俊,等.安徽铜陵地区晚中生代早、晚两期侵入岩的地质和地球化学特征[J].高校地质学报,2018,23(4):325-339. XU Xiao-chun,ZUO Xu,HE Jun,et al.Geological and Geochemical Characteristics of the Intrusive Rocks of Early and Late Stages During Late Mesozoic in Tong-ling District,Anhui Province[J].Geological Journal of China Universities,2018,23(4):325-339.
[15] 江 峰.安徽宣城茶亭铜金矿区岩浆岩特征及成因[D].合肥:合肥工业大学,2017. JIANG Feng.Characteristics and Genesis of Magmatic Rocks in the Chating Cu-Au Ore District,Xuancheng City,Anhui Province[D].Hefei:Hefei University of Technology,2017.
[16] 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,1989,42:313-345.
[17] BOYNTON W V.Cosmochemistry of the Rare Earth Elements:Meteorite Studies[J].Developments in Geo-chemistry,1984,2:63-114.
[18] 郭维民,陆建军,蒋少涌,等.安徽铜陵狮子山矿田岩浆岩年代学、Hf同位素、地球化学及岩石成因[J].中国科学:地球科学,2013,43(8):1268-1286. GUO Wei-min,LU Jian-jun,JIANG Shao-yong,et al.Chronology,Hf Isotopes,Geochemistry,and Petrogenesis of the Magmatic Rocks in the Shizishan Ore Field of Tongling,Anhui Province[J].Science China:Earth Sciences,2013,43(8):1268-1286.
[19] YAN J,LIU J M,LI Q Z,et al.In-situ Zircon Hf-O Isotopic Analyses of Late Mesozoic Magmatic Rocks in the Lower Yangtze River Belt,Central Eastern China:Implications for Petrogenesis and Geodynamic Evolution[J].Lithos,2015,227:57-76.
[20] CHEN M,SUN M,BUSLOV M M,et al.Crustal Melting and Magma Mixing in a Continental Arc Setting:Evidence from the Yaloman Intrusive Complex in the Gorny Altai Terrane,Central Asian Orogenic Belt[J].Lithos,2016,252/253:76-91.
[21] LI S,YANG X Y,HUANG Y,et al.Petrogenesis and Mineralization of the Fenghuangshan Skarn Cu-Au Deposit,Tongling Ore Cluster Field,Lower Yangtze Metallogenic Belt[J].Ore Geology Reviews,2014,58(3):148-162.
[22] 任康绪,阎国翰,牟保磊,等.阿拉善断块富碱侵入岩岩石地球化学和Nd、Sr、Pb同位素特征及其意义[J].地学前缘,2005,12(2):294-304. REN Kang-xu,YAN Guo-han,MU Bao-lei,et al.Geo-chemistry and Nd,Sr,Pb Isotopic Characteristics of the Alkali-rich Intrusive Rocks in Alxa Fault Block,Western Inner Mongolia and Their Implications[J].Earth Science Frontiers,2005,12(2):294-304.
[23] JAHN B M,WU F Y,LO 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.
[24] 薛怀民,马 芳,曹光跃.长江中下游地区晚中生代橄榄玄粗岩系列火山岩:年代学格架、地球化学特征及成因讨论[J].地质学报,2015,89(8):1380-1401. XUE Huai-min,MA Fang,CAO Guang-yue.Late Mesozoic Shoshonotic Volcanic Rocks in the Middle and Lower Yangtze River Reaches:Ages,Geochemical and Genesis[J].Acta Geologica Sinica,2015,89(8):1380-1401.
[25] 陈 龙.长江中下游地区晚中生代火山岩地球化学研究[D].合肥:中国科学技术大学,2016. CHEN Long.A Geochemical Study of Late Mesozoic Volcanics from the Middle-lower Yangtze Valley[D].Hefei:University of Science and Technology of China,2016.
[26] 高晓峰,郭 锋,李超文,等.溧水盆地两类晚中生代中酸性火山岩的岩石成因[J].岩石矿物学杂志,2007,26(1):1-12. GAO Xiao-feng,GUO Feng,LI Chao-wen,et al.The Genesis of Two Types of Late Mesozoic Intermediate-felsic Volcanic Rocks in Lishui Basin,Lower Yangtze Valley[J].Acta Petrologica et Mineralogica,2007,26(1):1-12.
[27] 瞿泓滢,王浩琳,裴荣富,等.鄂东南地区与铁山和金山店铁矿有关的花岗质岩体锆石LA-ICP-MS年龄和Hf同位素组成及其地质意义[J].岩石学报,2011,28(1):147-165. QU Hong-ying,WANG Hao-lin,PEI Rong-fu,et al.Zircon U-Pb Geochronological and Hf Isotopic Constraints on Petrogenesis of Tieshan and Jinshandian Plutons in the Southeastern Hubei Province[J].Acta Petrologica Sinica,2011,28(1):147-165.
[28] 颜代蓉,邓晓东,胡 浩,等.鄂东南地区阮家湾和犀牛山花岗闪长岩的时代、成因及成矿和找矿意义[J].岩石学报,2012,28(10):3373-3388. YAN Dai-rong,DENG Xiao-dong,HU Hao,et al.U-Pb Age and Petrogenesis of the Ruanjiawan Granodiorite Pluton and Xiniushan Granodiorite Porphyry,Southeast Hubei Province:Implication for Cu-Mo Mineralization[J].Acta Petrologica Sinica,2012,28(10):3373-3388.
[29] 黄圭成,夏金龙,丁丽雪,等.鄂东南地区铜绿山岩体的侵入期次和物源:锆石U-Pb年龄和Hf同位素证据[J].中国地质,2013,40(5):1392-1408. HUANG Gui-cheng,XIA Jin-long,DING Li-xue,et al.Stage Division and Origin of Tonglushan Pluton in Southeast Hubei Province:Evidence from Zircon U-Pb Ages and Hf Isotopes[J].Geology in China,2013,40(5):1392-1408.
[30] 王 建,谢桂青,姚 磊,等.鄂东南鸡笼山矽卡岩型金矿床花岗闪长斑岩的成因:地球化学和锆石U-Pb年代学约束[J].矿床地质,2014,33(1):137-152. WANG Jian,XIE Gui-qing,YAO Lei,et al.Petrogene-sis of Granodiorite Porphyry in Jilongshan Skarn Au Deposit of Southeast Hubei Province:Geochemical and Zircon U-Pb Dating Constraints[J].Mineral Deposits,2014,33(1):137-152.
[31] 丁丽雪,黄圭成,夏金龙.鄂东南地区殷祖岩体的成因及其地质意义:年代学、地球化学和Sr-Nd-Hf同位素证据[J].地质学报,2017,91(2):362-383. DING Li-xue,HUANG Gui-cheng,XIA Jin-long.Petrogenesis and Implications of the Yinzu Pluton in Southeast Hubei Province:Evidence from Geochronology,Geochemistry and Sr-Nd-Hf Isotopes[J].Acta Geologica Sinica,2017,91(2):362-383.
[32] 张智宇,杜杨松,张 静,等.安徽贵池铜山岩体SHRIMP锆石U-Pb年代学与岩石地球化学特征研究[J].地质论评,2011,57(3):366-378. ZHANG Zhi-yu,DU Yang-song,ZHANG Jing,et al.SHRIMP Zircon U-Pb Geochronology,Petrochemical and Geochemical Characteristics of Tongshan Intrusion in Guichi,Anhui Province[J].Geological Review,2011,57(3):366-378.
[33] 段留安,杨晓勇,汪方跃,等.长江中下游成矿带贵池抛刀岭金矿含矿岩体年代学及地球化学研究[J].岩石学报,2012,28(10):3241-3254. DUAN Liu-an,YANG Xiao-yong,WANG Fang-yue,et al.Geochemistry and Zircon U-Pb Age of Ore-bearing Porphyry in the Paodaoling Gold Deposit in Guichi,Middle-lower Yangtze Metallogenic Belt[J].Acta Petrologica Sinica,2012,28(10):3241-3254.
[34] 刘园园,马昌前,吕昭英,等.长江中下游贵池矿集区燕山期岩浆作用及其地质意义:年代学、地球化学及Sr-Nd-Hf同位素证据[J].岩石学报,2012,28(10):3287-3305. LIU Yuan-yuan,MA Chang-qian,LU Zhao-ying,et al.Zircon U-Pb Age,Element and Sr-Nd-Hf Isotopic Geo-chemistry of Late Mesozoic Magmatism from the Guichi Metallogenic District in the Middle and Lower Reaches of the Yangtze River Region[J].Acta Petrologica Sinica,2012,28(10):3287-3305.
[35] 刘一男,范 裕,严四华,等.长江中下游成矿带安庆—贵池矿集区五横岩体的成岩年代和区域岩浆活动演化研究[J].岩石学报,2013,30(4):1117-1129. LIU Yi-nan,FAN Yu,YAN Si-hua,et al.Petrogensis Chronology and Evolution of Regional Magmatic Activity Study of Anqing-Guichi Ore Deposit Concentrated Area in the Middle-lower Reaches of Yangtze River Metallogenic Belt[J].Acta Petrologica Sinica,2013,30(4):1117-1129.
[36] 陈志洪,邢光福,郭坤一,等.长江中下游成矿带九瑞矿集区(北部)含矿岩体的锆石U-Pb定年及其地质意义[J].地质学报,2011,85(7):1146-1158. CHEN Zhi-hong,XING Guang-fu,GUO Kun-yi,et al.Zircon U-Pb Ages of Ore-bearing Granitic Bodies in Northern Jiujiang-Ruichang Metallogenic District of the Mineralization Belt of the Middle-lower Reaches of the Yangtze River,and Its Geological Significance[J].Acta Geologica Sinica,2011,85(7):1146-1158.
[37] 徐耀明,蒋少涌,朱志勇,等.九瑞矿集区山上湾矿区石英闪长玢岩和花岗闪长斑岩的年代学、地球化学及成矿意义[J].岩石学报,2012,28(10):3306-3324. XU Yao-ming,JIANG Shao-yong,ZHU Zhi-yong,et al.Geochronology,Geochemistry and Mineralization of the Quartz Diorite-porphyrite and Granodiorite Porphyry in the Shanshangwan Area of the Jiurui Ore District,Jiangxi Province[J].Acta Petrologica Sinica,2012,28(10):3306-3324.
[38] 徐耀明,蒋少涌,朱志勇,等.江西九瑞矿集区成矿与未成矿中酸性侵入岩年代学、岩石化学、矿物化学特征的异同及地质意义[J].岩石学报,2013,29(12):4291-4310. XU Yao-ming,JIANG Shao-yong,ZHU Zhi-yong,et al.Geochronology,Geochemistry and Mineralogy of Ore-bearing and Ore-barren Intermediate-acid Intrusive Rocks from the Jiurui Ore District,Jiangxi Province and Their Geological Implications[J].Acta Petrologica Sinica,2013,29(12):4291-4310.
[39] 赵 玲,李 亮,匡福祥,等.江西九瑞矿集区鸡笼山Cu-Au-Mo矿床含矿岩体的年代学及地球化学研究[J].矿物岩石,2013,33(4):68-75. ZHAO Ling,LI Liang,KUANG Fu-xiang,et al.Zircon U-Pb Age and Geochemistry of the Ore-bearing Granitic Body from the Jilongshan Cu-Au-Mo Depo-sit,Jiujiang-Ruichang Metallogenic District of Jiangxi Province[J].Journal of Mineralogy and Petrology,2013,33(4):68-75.
[40] 徐夕生,范钦成,O'REILLY S Y,等.安徽铜官山石英闪长岩及其包体锆石U-Pb定年与成因探讨[J].科学通报,2004,49(18):1883-1890. XU Xi-sheng,FAN Qin-cheng,O'REILLY S Y,et al.U-Pb Dating of Zircons from Quartz Diorite and Its Enclaves at Tongguanshan in Anhui and Its Petrogenetic Implication[J].Chinese Science Bulletin,2004,49(18):1883-1890.
[41] 陈江峰,喻 钢,杨 刚,等.安徽沿江江南晚中生代岩浆-成矿年代学格架[J].安徽地质,2005,15(3):161-170. CHEN Jiang-feng,YU Gang,YANG Gang,et al.A Geochronological Framework of Late Mesozoic Magmatism and Metallogenesis in the Lower Yangtze Valley,Anhui Province[J].Geology of Anhui,2005,15(3):161-170.
[42] 谢建成.安徽铜陵地区中生代岩浆岩成岩和成矿作用研究[D].合肥:中国科学技术大学,2008. XIE Jian-cheng.The Diagenesis and Metallogenesis Research of Mesozoic Magmatic Rocks in Tongling Region,Anhui Province[D].Hefei:University of Science and Technology of China,2008.
[43] 吴才来,董树文,国和平,等.铜陵狮子山地区中酸性侵入岩锆石SHRIMP U-Pb定年及岩浆作用的深部过程[J].岩石学报,2008,24(8):1801-1812. WU Cai-lai,DONG Shu-wen,GUO He-ping,et al.Zircon SHRIMP U-Pb Dating of Intermediate-acid Intrusive Rocks from Shizishan,Tongling and the Deep Processes of Magmatism[J].Acta Petrologica Sinica,2008,24(8):1801-1812.
[44] 吴才来,高前明,国和平,等.铜陵中酸性侵入岩成因及锆石SHRIMP U-Pb定年[J].岩石学报,2010,26(8):2630-2652. WU Cai-lai,GAO Qian-ming,GUO He-ping,et al.Petrogenesis of the Intermediate-acid Intrusive Rocks and Zircon SHRIMP Dating in Tongling,Anhui,China[J].Acta Petrologica Sinica,2010,26(8):2630-2652.
[45] 徐晓春,陆三明,谢巧勤,等.铜陵狮子山矿田岩浆岩锆石SHRIMP定年及其成因意义[J].地质学报,2008,82(4):500-510. XU Xiao-chun,LU San-ming,XIE Qiao-qin,et al.SHRIMP Zircon U-Pb Dating for the Magmatic Rocks in Shizishan Ore-field of Tongling,Anhui Province,and Its Geological Implications[J].Acta Geologica Sinica,2008,82(4):500-510.
[46] 赖小东,杨晓勇,孙卫东,等.铜陵舒家店矿床年代学、岩石地球化学特征及成矿意义[J].地质学报,2012,86(3):470-485. LAI Xiao-dong,YANG Xiao-yong,SUN Wei-dong,et al.Chronological-geochemical Characteristics of the Shujiadian Intrusion,Tongling Ore Cluster Field:Its Significance to Metallogenesis[J].Acta Geologica Sinica,2012,86(3):470-485.
[47] 雷 敏,吴才来,秦海鹏,等.安徽铜陵地区虎山岩体矿物成分特征及其锆石U-Pb年代学[J].中国地质,2015,42(5):1274-1292. LEI Min,WU Cai-lai,QIN Hai-peng,et al.Mineral Composition and Zircon U-Pb Dating of the Hushan Intrusion in Tongling Area,Anhui Province[J].Geo-logy in China,2015,42(5):1274-1292.
[48] 孙 洋,马昌前,刘园园.长江中下游燕山期最新的成岩成矿事件:来自宁镇地区的证据[J].科学通报,2014,59(8):668-678. SUN Yang,MA Chang-qian,LIU Yuan-yuan.The Latest Yanshanian Magmatic and Metallogenic Events in the Middle-lower Yangtze River Belt:Evidences from the Ningzhen Region[J].Chinese Science Bulletin,2014,59(8):668-678.
[49] 关俊朋,韦福彪,孙国曦,等.宁镇中段中酸性侵入岩锆石U-Pb年龄及其成岩成矿指示意义[J].大地构造与成矿学,2015,39(2):344-354. GUAN Jun-peng,WEI Fu-biao,SUN Guo-xi,et al.Zircon U-Pb Dating of Intermediate-acid Intrusive Rocks in the Middle Section of Ningzhen District and Their Metallogenic Implications[J].Geotectonica et Metallogenia,2015,39(2):344-354.
[50] 张明超,陈仁义,叶天竺,等.宁镇矿集区安基山花岗闪长斑岩和韦岗花岗闪长岩的锆石U-Pb年龄、Hf同位素特征及其地质意义[J].地质学报,2018,92(11):84-104. ZHANG Ming-chao,CHEN Ren-yi,YE Tian-zhu,et al.Zircon U-Pb Dating and Hf Isotopic Compositions of the Anjishan Granodiorite Porphyry and Weigang Granodiorite in the Ningzhen Ore Cluster Area and Their Geological Implications[J].Acta Geologica Sini-ca,2018,92(11):84-104.
[51] 周涛发,宋明义,范 裕,等.安徽庐枞盆地中巴家滩岩体的年代学研究及其意义[J].岩石学报,2007,23(10):2379-2386. ZHOU Tao-fa,SONG Ming-yi,FAN Yu,et al.Chronology of the Bajiatan Intrusion in the Luzong Basin,Anhui,and Its Significance[J].Acta Petrologica Sinica,2007,23(10):2379-2386.
[52] 周涛发,范 裕,袁 峰,等.安徽庐枞(庐江—枞阳)盆地火山岩的年代学及其意义[J].中国科学:D辑,地球科学,2008,38(11):1342-1353. ZHOU Tao-fa,FAN Yu,YUAN Feng,et al.Geochronology of the Volcanic Rocks in the Luzong Basin and Its Significance[J].Science in China:Series D,Earth Sciences,2008,38(11):1342-1353.
[53] 周涛发,范 裕,袁 峰,等.庐枞盆地侵入岩的时空格架及其对成矿的制约[J].岩石学报,2010,26(9):2694-2714. ZHOU Tao-fa,FAN Yu,YUAN Feng,et al.Temporal-spatial Framework of Magmatic Intrusions in Luzong Volcanic Basin in East China and Their Constrain to Mineralizations[J].Acta Petrologica Sinica,2010,26(9):2694-2714.
[54] 曾键年,覃永军,郭坤一,等.安徽庐枞地区含矿岩浆岩锆石U-Pb年龄及其对成矿时限的约束[J].地质学报,2010,84(4):466-478. ZENG Jian-nian,QIN Yong-jun,GUO Kun-yi,et al.Zircon U-Pb Dating of Ore-bearing Magmatic Rocks and Its Constraint on the Formation Time of the Ore Deposits in Luzong Basin,Anhui Province[J].Acta Geologica Sinica,2010,84(4):466-478.
[55] 张乐骏,周涛发,范 裕,等.安徽庐枞盆地井边铜矿床的成矿时代及其找矿指示意义[J].岩石学报,2010,26(9):2729-2738. ZHANG Le-jun,ZHOU Tao-fa,FAN Yu,et al.Dating of Copper Mineralization in Jingbian Deposit and Its Prospecting Significance in Luzong Basin,Anhui Province[J].Acta Petrologica Sinica,2010,26(9):2729-2738.
[56] 薛怀民,董树文,马 芳.长江中下游庐枞盆地火山岩的SHRIMP锆石U-Pb年龄:对扬子克拉通东部晚中生代岩石圈减薄机制的约束[J].地质学报,2012,86(10):1569-1583. XUE Huai-min,DONG Shu-wen,MA Fang.Zircon SHRIMP U-Pb Ages of Volcanic Rocks in the Luzong Basin,Middle and Lower Yangtze River Reaches:Constraints on the Model of Late Mesozoic Lithospheric Thinning of the Eastern Yangtze Craton[J].Acta Geologica Sinica,2012,86(10):1569-1583.
[57] 薛怀民,马 芳,曹光跃,等.长江中下游庐枞火山岩盆地南侧钾质侵入岩带的成因[J].地质学报,2016,90(9):2233-2257. XUE Huai-min,MA Fang,CAO Guang-yue,et al.Petrogenesis of Potassic Intrusive Rocks Along the Southern Margin of the Luzong Volcanic Basin,Middle and Lower Yangtze River Reaches,China[J].Acta Geologica Sinica,2016,90(9):2233-2257.
[58] 范 裕,刘一男,周涛发,等.安徽庐枞盆地泥河铁矿床年代学研究及其意义[J].岩石学报,2014,30(5):1369-1381. FAN Yu,LIU Yi-nan,ZHOU Tao-fa,et al.Geochronology of the Nihe Deposit and in the Luzong Basin and Its Metallogenic Significances[J].Acta Petrologica Sinica,2014,30(5):1369-1381.
[59] 范 裕,邱 宏,张乐骏.安徽庐枞盆地南部花岗岩的成岩时代及其意义[J].地质科学,2014,49(2):631-650. FAN Yu,QIU Hong,ZHANG Le-jun,et al.Diagenetic Age of the Intrusions in Southern Part of the Luzong Basin and Its Significance[J].Chinese Journal of Geo-logy,2014,49(2):631-650.
[60] 范 裕,邱 宏,周涛发,等.安徽庐枞盆地隐伏侵入岩的LA-ICP MS定年及其构造意义[J].地质学报,2014,88(4):532-546. FAN Yu,QIU Hong,ZHOU Tao-fa,et al.LA-ICP MS Zircon U-Pb Dating for the Hidden Intrusions in the Luzong Basin and Its Tectonic Significance[J].Acta Geologica Sinica,2014,88(4):532-546.
[61] 贾丽琼,徐文艺,吕庆田,等.庐枞盆地砖桥地区科学深钻岩浆岩LA-MC-ICP MS锆石U-Pb年代学和岩石地球化学特征[J].岩石学报,2014,30(4):995-1016. JIA Li-qiong,XU Wen-yi,LU Qing-tian,et al.LA-MC-ICP MS Zircon U-Pb Geochronology and Petrological Geochemistry of Scientific Deep Drilling in Zhuanqiao,Lujiang-Zongyang Volcanic Basin[J].Acta Petrologica Sinica,2014,30(4):995-1016.
[62] 王继强,孙维安,袁 峰,等.庐枞盆地大倪庄铜矿床地质特征、成岩时代及成因探讨[J].中国地质,2017,44(1):86-100. WANG Ji-qiang,SUN Wei-an,YUAN Feng,et al.Geo-logical Characteristics,Rock-forming Epoch and Gene-sis of the Danizhuang Cu Deposit in Luzong Basin[J].Geology in China,2017,44(1):86-100.
[63] 张 旗,简 平,刘敦一,等.宁芜火山岩的锆石SHRIMP定年及其意义[J].中国科学:D辑,地球科学,2003,33(4):309-314. ZHANG Qi,JIAN Ping,LIU Dun-yi,et al.SHRIMP Dating of Volcanic Rocks from Ningwu Area and Its Geological Implications[J].Science in China:Series D,Earth Sciences,2003,33(4):309-314.
[64] 闫 峻,俞永飞,陈江峰.宁芜地区娘娘山组火山岩Rb-Sr同位素定年及其意义[J].地质论评,2009,55(1):121-125. YAN Jun,YU Yong-fei,CHEN Jiang-feng.Rb-Sr Isotopic Dating of Volcanic Rocks from the Niangniangshan Formation in the Nanjing-Wuhu Area and Its Geological Implications[J].Geological Review,2009,55(1):121-125.
[65] 范 裕,周涛发,袁 峰,等.宁芜盆地闪长玢岩的形成时代及对成矿的指示意义[J].岩石学报,2010,26(9):2715-2728. FAN Yu,ZHOU Tao-fa,YUAN Feng,et al.Geochronology of the Diorite Porphyrites in Ningwu Basin and Their Metallogenic Significance[J].Acta Petrologica Sinica,2010,26(9):2715-2728.
[66] 胡劲平,蒋少涌.宁芜盆地浅成侵入岩的锆石U-Pb年代学和Hf同位素研究及其地质意义[J].高校地质学报,2010,16(3):294-308. HU Jin-ping,JIANG Shao-yong.Zircon U-Pb Dating and Hf Isotopic Compositions of Porphyrites from the Ningwu Basin and Their Geological Implications[J].Geological Journal of China Universities,2010,16(3):294-308.
[67] 侯可军,袁顺达.宁芜盆地火山—次火山岩的锆石U-Pb年龄、Hf同位素组成及其地质意义[J].岩石学报,2010,26(3):888-902. HOU Ke-jun,YUAN Shun-da.Zircon U-Pb Age and Hf Isotopic Composition of the Volcanic and Sub-volcanic Rocks in the Ningwu Basin and Their Geological Implications[J].Acta Petrologica Sinica,2010,26(3):888-902.
[68] 段 超,李延河,毛景文.宁芜矿集区成岩成矿作用:来自花岗闪长斑岩锆石U-Pb年龄的证据[J].矿物学报,2011,31(增1):574-575. DUAN Chao,LI Yan-he,MAO Jing-wen.Diagenesis and Mineralization in Ningwu District:Evidence from Zircon U-Pb Age of Granodiorite Porphyry[J].Acta Mineralogica Sinica,2011,31(S1):574-575.
[69] 袁 峰,周涛发,范 裕,等.宁芜盆地花岗岩类的锆石U-Pb年龄、同位素特征及其意义[J].地质学报,2011,85(5):821-833. YUAN Feng,ZHOU Tao-fa,FAN Yu,et al.Zircon U-Pb Ages and Isotopic Characteristics of the Grani-toids in the Ningwu Basin,China,and Their Significance[J].Acta Geologica Sinica,2011,85(5):821-833.
[70] 周涛发,范 裕,袁 峰,等.宁芜(南京—芜湖)盆地火山岩的年代学及其意义[J].中国科学:地球科学,2011,41(7):960-971. ZHOU Tao-fa,FAN Yu,YUAN feng,et al.Geochronology and Significance of Volcanic Rocks in the Ning-Wu Basin of China[J].Science China:Earth Sciences,2011,41(7):960-971.
[71] 李锦伟,陈津华,曾键年,等.宁芜盆地吉山铁矿床辉长闪长玢岩SHRIMP锆石U-Pb定年及其地质意义[J].矿床地质,2012,31(6):1227-1236. LI Jin-wei,CHEN Jin-hua,ZENG Jian-nian,et al.SHRIMP Zircon U-Pb Dating of Gabbro-diorite Porphyrite in Jishan Iron Ore Deposit of Ningwu Basin and Its Geological Significance[J].Mineral Deposits,2012,31(6):1227-1236.
[72] 陈志洪,郭坤一,赵 玲.宁芜盆地火山基底侵入岩的锆石U-Pb定年和铪同位素研究[J].矿物岩石地球化学通报,2013,32(6):704-712. CHEN Zhi-hong,GUO Kun-yi,ZHAO Ling.Zircon U-Pb Dating and Hf Isotopic Study on Granitic Intrusions in the Basement of the Ningwu Basin[J].Bulletin of Mineralogy,Petrology and Geochemistry,2013,32(6):704-712.
[73] 王丽娟,王汝成,于津海,等.宁芜盆地火山-侵入岩的时代、地球化学特征及其地质意义[J].地质学报,2014,88(7):1247-1272. WANG Li-juan,WANG Ru-cheng,YU Jin-hai,et al.Geochronology,Geochemistry of Volcanic-intrusive Rocks in the Ningwu Basin and Its Geological Implications[J].Acta Geologica Sinica,2014,88(7):1247-1272.
[74] 杨颍鹤,王丽娟,张少琴.宁芜盆地火山作用峰期锆石U-Pb定年和Lu-Hf同位素研究[J].地质学刊,2015,39(4):556-566. YANG Yin-he,WANG Li-juan,ZHANG Shao-qin.Zircon U-Pb Dating and Lu-Hf Isotopic Analysis of Volcanic Rocks from the Nanjing-Wuhu Basin in Volcanism Peak Period[J].Journal of Geology,2015,39(4):556-566.
[75] 陈长健,陈 斌,王志强.宁芜地区中生代富钾和富钠火山岩的源区特征:岩石学和地球化学证据[J].岩石学报,2017,33(2):415-439. CHEN Chang-jian,CHEN bin,WANG Zhi-qiang.Petrology of the Mesozoic Magmatic Rocks in Ningwu Area:Insights from In-situ Zircon Hf Isotope and Nd-Sr Isotopes,East China[J].Acta Petrologica Sinica,2017,33(2):415-439.
[76] 禹 尧,徐夕生.长江中下游地区白垩纪富碱火山岩浆作用[J].地球科学,2009,34(1):105-116. YU Yao,XU Xi-sheng.Cretaceous Alkali-rich Magmatism in the Middle and Lower Reaches of the Yang-tze River[J].Earth Science,2009,34(1):105-116.
[77] 闫 峻,刘海泉,宋传中,等.长江中下游繁昌—宁芜火山盆地火山岩锆石U-Pb年代学及其地质意义[J].科学通报,2009,54(12):1716-1724. YAN Jun,LIU Hai-quan,SONG Chuan-zhong,et al.Zircon U-Pb Geochronology of the Volcanic Rocks from Fanchang-Ningwu Volcanic Basins in the Lower Yangtze Region and Its Geological Implications[J].Chinese Science Bulletin,2009,54(12):1716-1724.
[78] 袁 峰,周涛发,范 裕,等.安徽繁昌盆地中生代火山岩锆石LA-ICPMS U-Pb年龄及其意义[J].岩石学报,2010,26(9):2805-2817. YUAN Feng,ZHOU Tao-fa,FAN Yu,et al.LA-ICPMS U-Pb Ages of Zircons from Mesozoic Volcanic Rocks and Their Significance in Fanchang Basin[J].Acta Petrologica Sinica,2010,26(9):2805-2817.
[79] 刘建敏,闫 峻,陈丹丹,等.长江中下游地区繁昌盆地火山岩成因:锆石Hf-O同位素制约[J].岩石学报,2014,32(2):289-302. LIU Jian-min,YAN Jun,CHEN Dan-dan,et al.Petrogenesis of the Volcanic Rocks in Fanchang Basin,the Middle-lower Yangtze River Belt:Zircon Hf-O Isoto-pic Constraints[J].Acta Petrologica Sinica,2014,32(2):289-302.

相似文献/References:

[1]解小龙,牛漫兰,吴齐,等.秦祁昆结合部三叠纪岩浆岩岩石学特征及其构造环境[J].地球科学与环境学报,2015,37(06):72.
 XIE Xiao-long,NIU Man-lan,WU Qi,et al.Petrological Characteristics of Triassic Magmatic Rocks from the Conjunction of Qinling, Qilian and Kunlun Orogens and Their Tectonic Environment[J].Journal of Earth Sciences and Environment,2015,37(01):72.
[2]杨晓勇,古黄玲,严志忠,等.安徽贵池地区燕山期岩浆岩与铜金钼成矿关系:来自地质-地球化学-地球物理证据[J].地球科学与环境学报,2016,38(04):444.
 YANG Xiao-yong,GU Huang-ling,YAN Zhi-zhong,et al.Metallogenic Relationship Between Yanshanian Magmatic Rocks and Cu-Au-Mo Deposits in Guichi Area of Anhui: Evidences from Geological-geochemical-geophysical Characteristics[J].Journal of Earth Sciences and Environment,2016,38(01):444.
[3]余吉远,钱壮志,闫海卿,等.新疆天山冰达坂一带岩体地质特征及其分布[J].地球科学与环境学报,2006,28(01):13.
 YU Ji-yuan,QIAN Zhuang-zhi,YAN Hai-qing,et al.Geological Feature and Distribution of Bingdaban Magmatic Rocks in West Tianshan,Xinjiang Province[J].Journal of Earth Sciences and Environment,2006,28(01):13.
[4]李注苍,等.西秦岭糜署岭岩浆混合花岗岩 地球化学特征及构造意义[J].地球科学与环境学报,2005,27(02):12.
 LI Zhu-cang,LI Yong-jun,ZENG Jun-jie,et al.Geochemical features of Mishuling hybrid magma granite and its tectonic significance in Western Qinling[J].Journal of Earth Sciences and Environment,2005,27(01):12.
[5]杨航,赖绍聪*,张志华,等.北秦岭晚三叠世关山岩体地球化学特征及成因机制[J].地球科学与环境学报,2019,41(02):170.
 YANG Hang,LAI Shao-cong*,ZHANG Zhi-hua,et al.Geochemical Characteristics and Forming Mechanism of Late Triassic Guanshan Pluton in North Qinling, China[J].Journal of Earth Sciences and Environment,2019,41(01):170.
[6]李强,杨富全*,杨成栋.新疆阿尔泰大喀拉苏花岗岩年代学、地球化学特征及其构造意义[J].地球科学与环境学报,2019,41(04):396.
 LI Qiang,YANG Fu-quan*,YANG Cheng-dong.Geochronology and Geochemical Characteristics of Dakalasu Granite in Altay of Xinjiang, China and Their Tectonic Significance[J].Journal of Earth Sciences and Environment,2019,41(01):396.
[7]张忠利,杨成栋*,张斌,等.新疆阿尔泰克兰盆地泥盆纪花岗岩年代学特征及其地质意义[J].地球科学与环境学报,2019,41(04):414.
 ZHANG Zhong-li,YANG Cheng-dong*,ZHANG Bin,et al.Geochronological Characteristics of Devonian Granitoids in Kelan Basin of Altay, Xinjiang, China and Their Geological Implications[J].Journal of Earth Sciences and Environment,2019,41(01):414.
[8]史少飞,肖渊甫*,袁浩为,等.西藏冈底斯带北缘波果日则地区A型花岗岩年代学、地球化学特征及其地质意义[J].地球科学与环境学报,2019,41(06):644.
 SHI Shao-fei,XIAO Yuan-fu*,YUAN Hao-wei,et al.Geochronology and Geochemical Characteristics of A-type Granites in Boguorize Area, the Northern Margin of Gangdese Belt, Tibet, China and Their Geological Significance[J].Journal of Earth Sciences and Environment,2019,41(01):644.
[9]张晗,黄虎*,侯明才.四川广元地区朝天剖面上二叠统吴家坪组凝灰岩成因及其地质意义[J].地球科学与环境学报,2020,42(01):36.[doi:10.19814/j.jese.2019.08010]
 ZHANG Han,HUANG Hu*,HOU Ming-cai.Origin of Tuffs from Upper Permian Wujiaping Formation in Chaotian Section of Guangyuan Area, Sichuan, China and Its Geological Significance[J].Journal of Earth Sciences and Environment,2020,42(01):36.[doi:10.19814/j.jese.2019.08010]
[10]丁建刚,杨成栋*,杨富全,等.新疆阿尔泰别也萨麻斯稀有金属矿床含矿伟晶岩与花岗岩围岩成因关系[J].地球科学与环境学报,2020,42(01):71.[doi:10.19814/j.jese.2019.07021]
 DING Jian-gang,YANG Cheng-dong*,YANG Fu-quan,et al.Genetic Relationship Between Ore-bearing Pegmatite and the Surrounding Granite of Bieyesamasi Rare Metal Deposit in Altay of Xinjiang, China[J].Journal of Earth Sciences and Environment,2020,42(01):71.[doi:10.19814/j.jese.2019.07021]

备注/Memo

备注/Memo:
收稿日期:2019-05-15; 修回日期:2019-09-02; 网络首发日期:2019-11-07投稿网址:http:∥jese.chd.edu.cn/
基金项目:国家重点研发计划项目(2016YFC0600209)
作者简介:徐晓春(1961-),男,安徽潜山人,教授,博士研究生导师,理学博士,E-mail:xuxiaoch@sina.com。
更新日期/Last Update: 2020-01-07