«上一篇/Previous Article|本期目录/Table of Contents|下一篇/Next Article»

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

卷:

第43卷

期数:

2021年第04期

页码:

686-709

栏目:

基础地质与矿产地质

出版日期:

2021-07-15

文章信息/Info

Title:

Neoproterozoic Continental Arc Magmatism in Bikou Micro-block, the Northwestern Margin of Yangtze Plate, China: Evidence from Zircon U-Pb Dating, Hf Isotope and Geochemistry

文章编号:

1672-6561(2021)04-0686-24

作者:

秦 利¹; 裴先治¹; 2*; 李佐臣¹; 2; 李瑞保¹; 2; 裴 磊¹; 2; 刘成军¹; 2; 周 海¹; 2; 王 盟¹; 2; 赵少伟¹; 2; 陈有炘¹; 2; 高 峰¹; 2

(1. 长安大学 地球科学与资源学院,陕西 西安 710054; 2. 长安大学 西部矿产资源与地质工程教育部重点实验室,陕西 西安 710054)

Author(s):

QIN Li¹;  PEI Xian-zhi¹; 2*;  LI Zuo-chen¹; 2;  LI Rui-bao¹; 2;  PEI Lei¹; 2;  LIU Cheng-jun¹; 2;  ZHOU Hai¹; 2;  WANG Meng¹; 2;  ZHAO Shao-wei¹; 2;  CHEN You-xin¹; 2;  GAO Feng¹; 2

(1. School of Earth Science and Resources, Chang'an University, Xi'an 710054, Shaanxi, China; 2. Key Laboratory of Western China's Mineral Resources and Geological Engineering of Ministry of Education, Chang'an University, Xi'an 710054, Shaanxi, China)

关键词:

花岗闪长岩;  锆石U-Pb年龄;  Hf同位素;  地球化学;  岩石成因;  俯冲;  新元古代;  碧口微地块

Keywords:

granodiorite;  zircon U-Pb age;  Hf isotope;  geochemistry;  petrogenesis;  subduction;  Neoproterozoic;  Bikou micro-block

分类号:

P597

DOI:

10.19814/j.jese.2020.10032

文献标志码:

A

摘要:

扬子板块西北缘碧口微地块内部发育有较多的新元古代基性—中酸性侵入岩体。对碧口微地块勉略宁地区出露的新元古代二里坝花岗闪长岩进行了岩石学、地球化学、锆石U-Pb年代学、Hf同位素研究。结果表明:二里坝花岗闪长岩2件样品的²⁰⁶Pb/²³⁸U加权平均年龄分别为(821.3±5.5)Ma和(822.6±5.8)Ma; 二里坝花岗闪长岩主体为准铝质—弱过铝质、钙碱性系列岩石,富集轻稀土元素和大离子亲石元素,亏损高场强元素Ti、Nb、Ta等,为I型花岗岩; 稀土元素总含量(质量分数)为(81.5～147.3)×10^-6,球粒陨石标准化稀土元素配分模式呈右倾型,具弱的正Eu异常(0.92～1.26); 锆石ε_Hf(t)为-14.06～-7.38,二阶段Hf模式年龄为2.25～1.90 Ga。结合区域地质资料认为,二里坝花岗闪长岩主要是由下地壳变基性岩部分熔融形成,是与俯冲相关的新元古代大陆弧环境下的产物。

Abstract:

The Bikou micro-block in the northwestern margin of Yangtze plate develops more Neoproterozoic basic and intermediate-acid intrusions. The petrology, geochemistry, zircon U-Pb dating and Hf isotope of Neoproterozoic Erliba granodiorites in Mianxian-Lueyang-Ningqiang area of Bikou micro-block were systematic studied. The results show that Erliba granodiorites are mainly in Early Neoproterozoic with ²⁰⁶Pb/²³⁸U weighted mean ages of(821.3±5.5)Ma and(822.6±5.8)Ma; Erliba granodiorites belong to metaluminous to weak peraluminous and calc-alkaline series, and are enriched in LREEs and LILEs, depleted in HFSEs(e.g. Ti, Nb, and Ta), indicating I-type granite affinity; the total contents of REE are(81.5-147.3)×10^-6, and the chondrite-normalized REE pattern shows right-sloping type with weak positive Eu anomalies(0.92-1.26); the values of zircon ε_Hf(t)range from -14.06 to -7.38 with the corresponding two-stage Hf model age of 2.25-1.90 Ga. The above features indicate that the source rocks probably derive from the ancient crust. Combined with regional geological data, it is suggested that Erliba granodiorites are formed by partial melting of metabasic rocks in the lower crust, and the products under Neoproterozoic continental arc environment related to subduction.

参考文献/References:

[1] LI Z X,ZHANG L,POWELL C M.South China in Rodinia:Part of the Missing Link Between Australia-East Antarctica and Laurentia?[J].Geology,1995,23(5):407-410. [2] 裴先治,张国伟,赖绍聪,等.西秦岭南缘勉略构造带主要地质特征[J].地质通报,2002,21(2):486-494. PEI Xian-zhi,ZHANG Guo-wei,LAI Shao-cong,et al.Main Geological Feature of the Mianlue Tectonic Belt on the Southern Margin of the West Qinling[J].Geological Bulletin of China,2002,21(2):486-494. [3] 闫全人,王宗起,闫 臻,等.碧口群火山岩的时代:SHRIMP锆石U-Pb测年结果[J].地质通报,2003,22(6):456-459. YAN Quan-ren,WANG Zong-qi,YAN Zhen,et al.Geochronology of the Bikou Group Volcanic Rocks:Newest Results from SHRIMP Zircon U-Pb Dating[J].Geological Bulletin of China,2003,22(6):456-459. [4] DRUSCHKE P A,HANSON A D,YAN Q R,et al.Stratigraphic and SHRIMP Detrital Zircon Evidence for a Neoproterozoic Continental Arc,Central China:Rodinia Implications[J].The Journal of Geology,2006,114(5):627-636. [5] 李永飞,赖绍聪.碧口洋岛型火山岩的厘定及其构造意义[J].西北地质,2006,39(4):1-9. LI Yong-fei,LAI Shao-cong.Discrimination of OIB Volcanic Rocks of Bikou Group and Their Tectonic Implication[J].Northwestern Geology,2006,39(4):1-9. [6] 夏林圻,夏祖春,徐学义,等.碧口群火山岩岩石成因研究[J].地学前缘,2007,14(3):84-101. XIA Lin-qi,XIA Zu-chun,XU Xue-yi,et al.Petrogene-sis of the Bikou Group Volcanic Rocks[J].Earth Science Frontiers,2007,14(3):84-101. [7] 李佐臣,裴先治,丁仨平,等.川西北平武地区南一里花岗岩体地球化学特征及其构造环境[J].地质学报,2009,83(2):260-271. LI Zuo-chen,PEI Xian-zhi,DING Sa-ping,et al.Geochemical Features and Tectonic Setting of the Nanyili Granite in the Pingwu Area,Northwestern Sichuan[J].Acta Geologica Sinica,2009,83(2):260-271. [8] 李佐臣,裴先治,丁仨平,等.川西北碧口地块老河沟岩体和筛子岩岩体地球化学特征及其构造环境[J].地质学报,2010,84(3):343-356. LI Zuo-chen,PEI Xian-zhi,DING Sa-ping,et al.Geochemical Features and Tectonic Setting of the Laohegou Granite and the Shaiziyan Granite in Bikou Block,in Northwest Sichuan[J].Acta Geologica Sinica,2010,84(3):343-356. [9] WANG W,LIU S W,FENG Y G,et al.Chronology,Petrogenesis and Tectonic Setting of the Neoproterozoic Tongchang Dioritic Pluton at the Northwestern Margin of the Yangtze Block:Constraints from Geochemistry and Zircon U-Pb-Hf Isotopic Systematics[J].Gondwana Research,2012,22(2):699-716. [10] 赖绍聪,李永飞,秦江锋.碧口群西段董家河蛇绿岩地球化学及LA-ICP-MS锆石U-Pb定年[J].中国科学:D辑,地球科学,2007,37(增1):262-270. LAI Shao-cong,LI Yong-fei,QIN Jiang-feng.Geochemistry and LA-ICP-MS Zircon U-Pb Dating of the Dongjiahe Ophiolite Complex from the Western Bikou Terrane[J].Science in China:Series D,Earth Sciences,2007,37(S1):262-270. [11] 裴先治,李佐臣,丁仨平,等.扬子地块西北缘轿子顶新元古代过铝质花岗岩:锆石SHRIMP U-Pb年龄和岩石地球化学及其构造意义[J].地学前缘,2009,16(3):231-249. PEI Xian-zhi,LI Zuo-chen,DING Sa-ping,et al.Neoproterozoic Jiaoziding Peraluminous Granite in the Northwestern Margin of Yangtze Block:Zircon SHR-IMP U-Pb Age and Geochemistry and Their Tectonic Significance[J].Earth Science Frontiers,2009,16(3):231-249. [12] 李佐臣,裴先治,李瑞保,等.扬子地块西北缘刘家坪地区大滩花岗岩体年代学、地球化学及其构造环境[J].地质论评,2013,59(5):869-884. LI Zuo-chen,PEI Xian-zhi,LI Rui-bao,et al.Geochronological and Geochemical Study on Datan Gra-nite in Liujiaping Area,Northwest Yangtze Block and Its Tectonic Setting[J].Geological Review,2013,59(5):869-884. [13] 汪新伟,沃玉进,张荣强.扬子克拉通南华纪—早古生代的构造-沉积旋回[J].现代地质,2008,22(4):525-533. WANG Xin-wei,WO Yu-jin,ZHANG Rong-qiang.Tectonic-sedimentary Cycle of the Yangtze Craton from Nanhuaan to the Early Palaeozoic[J].Geoscience,2008,22(4):525-533. [14] 李佐臣.扬子地块西北缘后龙门山造山带(北段)物质组成、构造特征及其形成演化[D].西安:长安大学,2009. LI Zuo-chen.Composition,Structural Characteristics and Evolution of Back-Longmenshan Orogen(North Section)in the Northwest Margin of Yangtze Block[D].Xi'an:Chang'an University,2009. [15] 李曙光,孙卫东,张国伟,等.南秦岭勉略构造带黑沟峡变质火山岩的年代学和地球化学:古生代洋盆及其闭合时代的证据[J].中国科学:D辑,地球科学,1996,26(3):223-230. LI Shu-guang,SUN Wei-dong,ZHANG Guo-wei,et al.Chronology and Geochemistry of Metavolcanic Rocks from Heigouxia Valley in Mian-Lue Tectonic Belt,South Qinling:Evidence for a Paleozoic Oceanic Basin and Its Close Time[J].Science in China:Series D,Earth Sciences,1996,26(3):223-230. [16] 张成立,王 涛,王晓霞.秦岭造山带早中生代花岗岩成因及其构造环境[J].高校地质学报,2008,14(3):304-316. ZHANG Cheng-li,WANG Tao,WANG Xiao-xia.Origin and Tectonic Setting of the Early Mesozoic Grani-toids in Qinling Orogenic Belt[J].Geological Journal of China Universities,2008,14(3):304-316. [17] 裴先治.南秦岭碧口群岩石组合特征及其构造意义[J].西安地质学院学报,1989,11(2):46-56. PEI Xian-zhi.The Feature and the Tectonic Significance of Rock Assemblage in the Bikou Group,Southern Qinling[J].Journal of Xi'an College of Geology,1989,11(2):46-56. [18] DONG Y P,LIU X M,SANTOSH M,et al.Neopro-terozoic Accretionary Tectonics Along the Northwestern Margin of the Yangtze Block,China:Constraints from Zircon U-Pb Geochronology and Geochemistry[J].Precambrian Research,2012,196/197:274-274. [19] 夏林圻,夏祖春,徐学义.南秦岭中—晚元古代火山岩性质与前寒武纪大陆裂解[J].中国科学:D辑,地球科学,1996,26(3):237-243. XIA Lin-qi,XIA Zu-chun,XU Xue-yi.Properties of Middle-Late Proterozoic Volcanic Rocks in South Qinling and the Precambrian Continental Break-up[J].Science in China:Series D,Earth Sciences,1996,26(3):237-243. [20] 夏林圻,夏祖春,徐学义.南秦岭元古宙西乡群大陆溢流玄武岩的确定及其地质意义[J].地质论评,1996,42(6):513-522. XIA Lin-qi,XIA Zu-chun,XU Xue-yi.The Confirmation of Continental Flood Basalt of the Proterozoic Xixiang Group in the South Qinling Mountains,and Its Geological Implications[J].Geological Review,1996,42(6):513-522. [21] 徐学义,夏祖春,夏林圻.南秦岭元古宙板内火山作用特征及构造意义[J].岩石矿物学杂志,2001,20(3):255-262. XU Xue-yi,XIA Zu-chun,XIA Lin-qi.Proterozoic Intraplate Volcanic Rocks in South Qinling Mountains and Their Tectonic Implications[J].Acta Petrologica et Mineralogica,2001,20(3):255-262. [22] 张二朋,牛道韫,霍有光,等.秦巴及邻区地质构造特征概论[M].北京:地质出版社,1993. ZHANG Er-peng,NIU Dao-yun,HUO You-guang,et al.Geologic Tectonic Features of Qinling-Dabashan and Adjacent Regions[M].Beijing:Geological Publishing House,1993. [23] 刘国惠,张寿广,游振东,等.秦岭造山带主要变质岩群及变质演化[M].北京:地质出版社,1993. LIU Guo-hui,ZHANG Shou-guang,YOU Zhen-dong,et al.Major Metamorphic Groups and Their Evolu-tions in the Qinling Orogenic Belt[M].Beijing:Geological Publishing House,1993. [24] 莫宣学.岩浆与岩浆岩:地球深部“探针”与演化记录[J].自然杂志,2011,33(5):255-259,313. MO Xuan-xue.Magma and Magmatic/Igneous Rocks:A Lithoprobe into the Deep Earth and Records of the Earth's Evolution[J].Chinese Journal of Nature,2011,33(5):255-259,313. [25] 张国伟,孟庆任,于在平,等.秦岭造山带的造山过程及其动力学特征[J].中国科学:D辑,地球科学,1996,26(3):193-200. ZHANG Guo-wei,MENG Qing-ren,YU Zai-ping,et al.Orogenesis and Dynamic of Qinling Orogen[J].Science in China:Series D,Earth Sciences,1996,26(3):193-200. [26] 徐学义,陈隽璐,闫 臻,等.秦岭及邻区地质图(1:500 000)[M].西安:西安地图出版社,2014. XU Xue-yi,CHEN Jun-lu,YAN Zhen,et al.Geologi-cal Map(1:500 000)of Qinling and Adjacent Areas[M].Xi'an:Xi'an Cartographic Publishing House,2014. [27] 陕西省地质矿产勘查开发局区域地质调查队.中华人民共和国1:50 000地质图及区域地质报告(徐家坪、两河口、张家河、略阳县、何家岩幅)[R].西安:陕西省地质矿产勘查开发局区域地质调查队,1995. Regional Geological Survey Team,Shaanxi Provincial Bureau of Geology and Mineral Exploration and Development.1:50 000 Geological Map and Regional Geological Report of the People's Republic of China(Xujiaping,Lianghekou,Zhangjiahe,Lueyang and Hejiayan Sheets)[R].Xi'an:Regional Geological Survey Team,Shaanxi Provincial Bureau of Geology and Mi-neral Exploration and Development,1995. [28] 张宗清,张国伟,唐索寒,等.鱼洞子群变质岩年龄及秦岭造山带太古宙基底[J].地质学报,2001,75(2):198-204. ZHANG Zong-qing,ZHANG Guo-wei,TANG Suo-han,et al.On the Age of Metamorphic Rocks of the Yudongzi Group and the Archean Crystalline Basement of the Qinling Orogen[J].Acta Geologica Sinica,2001,75(2):198-204. [29] 张 欣,徐学义,宋公社,等.西秦岭略阳地区鱼洞子杂岩变形花岗岩锆石LA-ICP-MS U-Pb测年及地质意义[J].地质通报,2010,29(4):510-517. ZHANG Xin,XU Xue-yi,SONG Gong-she,et al.Zircon LA-ICP-MS U-Pb Dating and Significance of Yudongzi Group Deformation Granite from Lueyang Area,Western Qinling,China[J].Geological Bulletin of China,2010,29(4):510-517. [30] HUI B,DONG Y P,CHENG C,et al.Zircon U-Pb Chronology,Hf Isotope Analysis and Whole-rock Geochemistry for the Neoarchean-Paleoproterozoic Yu-dongzi Complex,Northwestern Margin of the Yangtze Craton,China[J].Precambrian Research,2017,301:65-85. [31] XIAO L,ZHANG H F,NI P Z,et al.LA-ICP-MS U-Pb Zircon Geochronology of Early Neoproterozoic Mafic-intermediate Intrusions from NW Margin of the Yangtze Block,South China:Implication for Tectonic Evolution[J].Precambrian Research,2007,154(3/4):221-235. [32] 叶 霖,程增涛,陆丽娜,等.陕南勉略宁地区铜厂闪长岩岩石地球化学及SHRIMP锆石U-Pb同位素年代学[J].岩石学报,2009,25(11):2866-2876. YE Lin,CHENG Zeng-tao,LU Li-na,et al.Petrological Geochronology and Zircon SHRIMP U-Pb of Tong-chang Diorites,Mianluening Area,Southern Shaanxi Pro-vince,China[J].Acta Petrologica Sinica,2009,25(11):2866-2876. [33] 平先权,郑建平,熊 庆,等.扬子西北缘碧口块体花岗质岩体锆石U-Pb年龄、Hf同位素特征及其地质意义[J].吉林大学学报(地球科学版),2014,44(4):1200-1218. PING Xian-quan,ZHENG Jian-ping,XIONG Qing,et al.Zircon U-Pb Ages and Hf Isotope Characteristics of the Granitic Plutons in Bikou Terrane,Northwestern Yangtze Block and Their Geological Significance[J].Journal of Jilin University(Earth Science Edition),2014,44(4):1200-1218. [34] 游 军,张小明,杨运军,等.略阳白雀寺—石瓮子双峰式侵入岩锆石U-Pb定年、地球化学特征及意义[J].矿产勘查,2018,9(12):2365-2377. YOU Jun,ZHANG Xiao-ming,YANG Yun-jun,et al.Zircon U-Pb Geochronology and Geochemistry of Baiquesi-Shiwengzi Bimodal Intrusive Rocks in Lue-yang,and Their Significance[J].Mineral Exploration,2018,9(12):2365-2377. [35] 秦江锋,赖绍聪,李永飞.扬子板块北缘碧口地区阳坝花岗闪长岩体成因研究及其地质意义[J].岩石学报,2005,21(3):697-710. QIN Jiang-feng,LAI Shao-cong,LI Yong-fei.Petrogenesis and Geological Significance of Yangba Granodiorites from Bikou Area,Northern Margin of Yang-tze Plate[J].Acta Petrologica Sinica,2005,21(3):697-710. [36] 李佐臣,裴先治,丁仨平,等.川西北平武地区南一里花岗闪长岩锆石U-Pb定年及其地质意义[J].中国地质,2007,34(6):1003-1012. LI Zuo-chen,PEI Xian-zhi,DING Sa-ping,et al.Zircon U-Pb Dating of the Nanyili Granodiorite in the Pingwu Area,Northwestern Sichuan,and Its Geolo-gical Significance[J].Geology in China,2007,34(6):1003-1012. [37] LIU Y S,HU Z C, GAO S,et al.In-situ Analysis of Major and Trace Elements of Anhydrous Minerals by LA-ICP-MS Without Applying an Internal Standard[J].Chemical Geology,2008,257(1):34-43. [38] LIU Y S,GAO S,GAO C G,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,2010,51(1/2):537-571. [39] LUDWIG K R.User's Manual for Isoplot 3.00:A Geochronological Toolkit for Microsoft Excel[R].Berkeley:Berkeley Geochronology Center,2003. [40] SÖDERLUND U,PATCHETT P J,VERVOORT J D,et al.The ¹⁷⁶Lu Decay Constant Determined by Lu-Hf and U-Pb Isotope Systematics of Precambrian Mafic Intrusions[J].Earth and Planetary Science Letters,2004,219(3/4):311-324. [41] BLICHERT-TOFT J,CHAUVEL C,ALBARÈDE F.Separation of Hf and Lu for High-precision Isotope Analysis of Rock Samples by Magnetic Sector-multiple Collector ICP-MS[J].Contributions to Mineralogy and Petrology,1997,127(3):248-260. [42] VERVOORT J D,PATCHETT P J.Behavior of Hafnium and Neodymium Isotopes in the Crust:Constraints from Precambrian Crustally Derived Granites[J].Geochimica et Cosmochimica Acta,1996,60(19):3717-3733. [43] CORFU F,HANCHAR J M,HOSKIN P W O,et al.Atlas of Zircon Textures[J].Reviews in Mineralogy and Geochemistry,2003,53(1):469-500. [44] HOSKIN P W O.The Composition of Zircon and Igneous and Metamorphic Petrogenesis[J].Reviews in Mineralogy and Geochemistry,2003,53(1):27-62. [45] GREEN T H,PEARSON N J.An Experimental Study of Nb and Ta Partitioning Between Ti-rich Minerals and Silicate Liquids at High Pressure and Temperature[J].Geochimica et Cosmochimica Acta,1987,51(1):55-62. [46] GREEN T H.Significance of Nb/Ta as an Indicator of Geochemical Processes in the Crust-mantle System[J].Chemical Geology,1995,120(3/4):347-359. [47] BARTH M G,MCDONOUGH W F,RUDNICK R L.Tracking the Budget of Nb and Ta in the Continental Crust[J].Chemical Geology,2000,165(3/4):197-213. [48] RICKWOOD P C.Boundary Lines Within Petrologic Diagrams Which Use Oxides of Major and Minor Elements[J].Lithos,1989,22(4):247-263. [49] MANIAR P D,PICCOLI P M.Tectonic Discrimination of Granitoids[J].GSA Bulletin,1989,101(5):635-643. [50] 闫全人,王宗起,HANSON A D,等.南秦岭横丹浊积岩系:晚古生代发育于扬子板块被动陆缘上的弧前盆地充填物[J].地质通报,2002,21(8/9):495-500. YAN Quan-ren,WANG Zong-qi,HANSON A D,et al.Hengdan Turbidite Terrain:Fillings in a Late Paleozoic Forearc Basin Developed on the Passive Margin of the Yangtze Plate[J].Geological Bulletin of China,2002,21(8/9):495-500. [51] 闫全人,王宗起,闫 臻,等.秦岭勉略构造混杂带康县—勉县段蛇绿岩块-铁镁质岩块的SHRIMP年代及其意义[J].地质论评,2007,53(6):755-764. YAN Quan-ren,WANG Zong-qi,YAN Zhen,et al.SHRIMP Analyses for Ophiolitic-mafic Blocks in the Kangxian-Mianxian Section of the Mianxian-Lueyang Melange:Their Geological Implications[J].Geological Review,2007,53(6):755-764. [52] SUN S S,MCDONOUGH W F.Chemical and Isoto-pic Systematics of Oceanic Basalts:Implications for Mantle Composition and Processes[J].Geological Society,London,Special Publications,1989,42:313-345. [53] 夏林圻,夏祖春,马中平,等.南秦岭中段西乡群火山岩岩石成因[J].西北地质,2009,42(2):1-37. XIA Lin-qi,XIA Zu-chun,MA Zhong-ping,et al.Petrogenesis of Volcanic Rocks from Xixiang Group in Middle Part of South Qinling Mountains[J].Northwestern Geology,2009,42(2):1-37. [54] TAYLOR S R,MCLENNAN S M.The Geochemical Evolution of the Continental Crust[J].Reviews of Geophysics,1995,33(2):241-265. [55] 赵振华,熊小林,王 强,等.铌与钽的某些地球化学问题[J].地球化学,2008,37(4):304-320. ZHAO Zhen-hua,XIONG Xiao-lin,WANG Qiang,et al.Some Aspects on Geochemistry of Nb and Ta[J].Geochimica,2008,37(4):304-320. [56] HOFMANN A W.Chemical Differentiation of the Earth:The Relationship Between Mantle,Continental Crust,and Oceanic Crust[J].Earth and Planetary Science Letters,1988,90(3):297-314. [57] COLLINS W J,BEAMS S D,WHITE A J R,et al.Nature and Origin of A-type Granites with Particular Reference to Southeastern Australia[J].Contributions to Mineralogy and Petrology,1982,80:189-200. [58] 吴福元,李献华,郑永飞,等.Lu-Hf同位素体系及其岩石学应用[J].岩石学报,2007,23(2):185-220. WU Fu-yuan,LI Xian-hua,ZHENG Yong-fei,et al.Lu-Hf Isotopic Systematics and Their Applications in Petrology[J].Acta Petrologica Sinica,2007,23(2):185-220. [59] WOLF M B,WYLLIE P J.The Formation of Tonali-tic Liquids During the Vapo-absent Partial Melting of Amphibolite at 10 kbar[J].Eos,1989,70:506-518. [60] BEARD J S,LOFGREN G E.Dehydration Melting and Water-saturated Melting of Basaltic and Andesitic Greenstones and Amphibolites at 1.3 and 6.9 kbar[J].Journal of Petrology,1991,32(2):365-402. [61] JOHANNES W,EHLERS C,KRIEGSMAN L M,et al.The Link Between Migmatites and S-type Granites in the Turku Area,Southern Finland[J].Lithos,2003.68(3/4):69-90. [62] SISSON T W,RATAJESKI K,HANKINS W B,et al.Voluminous Granitic Magmas from Common Basaltic Sources[J].Contributions to Mineralogy and Petrology,2005,148(6):635-661. [63] ALTHERR R,HOLL A,HEGNER E,et al.High-potassium,Calc-alkaline I-type Plutonism in the European Variscides:Northern Vosges(France)and Northern Schwarzwald(Germany)[J].Lithos,2000,50(1/2/3):51-73. [64] 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. [65] 闫全人,HANSON A D,王宗起,等.扬子板块北缘碧口群火山岩的地球化学特征及其构造环境[J].岩石矿物学杂志,2004,23(1):1-11. YAN Quan-ren,HANSON A D,WANG Zong-qi,et al.Geochemistry and Tectonic Setting of the Bikou Volcanic Terrane on the Northern Margin of the Yangtze Plate[J].Acta Petrologica et Mineralogica,2004,23(1):1-11. [66] PITCHER W S.The Nature and Origin of Granite[M].Dordrecht:Chapman and Hall,1997. [67] DEFANT M J,DRUMMOND M S.Derivation of Some Modern Arc Magmas by Melting of Young Subducted Lithosphere[J].Nature,1990,347:662-665. [68] GAO F,PEI X Z,LI R B,et al.Provenance and Depositional Mechanism Analyses of the Yangtianba Formation,Northwestern Margin of the Yangtze Block,Southwestern China[J].Journal of Geodynamics,2020,138:101750. [69] GAO F,PEI X Z,LI R B,et al.Further Constraints on a Neoproterozoic Active Continental Margin from Sandstones of the Hengdan Group in the Bikou Terrane,Northwestern Margin of the Yangtze Block,South China[J].Journal of Asian Earth Sciences,2020,203:104514. [70] GAO F,PEI X Z,LI R B,et al.Neoproterozoic Tectonic Evolution of the Northwestern Margin of the Yangtze Block(Southwestern China):Evidence from Sandstone Geochemistry and Detrital Zircon U-Pb Ages of the Hengdan Group[J].Precambrian Research,2020,344:105737. [71] AO W H,ZHAO Y,ZHANG Y K,et al.The Neopro-terozoic Magmatism in the Northern Margin of the Yangtze Block:Insights from Neoproterozoic(950-706 Ma)Gabbroic-granitoid Rocks of the Hannan Complex[J].Precambrian Research,2019,333:105442. [72] LUO B J,LIU R,ZHANG H F,et al.Neoproterozoic Continental Back-arc Rift Development in the Northwestern Yangtze Block:Evidence from the Hannan Intrusive Magmatism[J].Gondwana Research,2018,59:27-42. [73] DU L L,GUO J H,NUTMAN A P,et al.Implications for Rodinia Reconstructions for the Initiation of Neoproterozoic Subduction at ～860 Ma on the Western Margin of the Yangtze Block:Evidence from the Guandaoshan Pluton[J].Lithos,2014,196/197:67-82. [74] SUN W H,ZHOU M F.The ～860 Ma,Cordilleran-type Guandaoshan Dioritic Pluton in the Yangtze Block,SW China:Implications for the Origin of Neoproterozoic Magmatism[J].The Journal of Geology,2008,116(3):238-253. [75] ZHU Y,LAI S C,QIN J F,et al.Petrogenesis and Geo-dynamic Implications of Neoproterozoic Gabbro-diorites,Adakitic Granites,and A-type Granites in the Southwestern Margin of the Yangtze Block,South China[J].Journal of Asian Earth Sciences,2019,183:103977. [76] XU Y,YANG K G,POLAT A,et al.The Similar to 860 Ma Mafic Dikes and Granitoids from the Northern Margin of the Yangtze Block,China:A Record of Oceanic Subduction in the Early Neoproterozoic[J].Precambrian Research,2016,275:310-331. [77] ALLEGRE C J,MINSTER J F.Quantitative Models of Trace Element Behavior in Magmatic Processes[J].Earth and Planetary Science Letters,1978,38(1):1-25. [78] 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. [79] BATCHELOR R A,BOWDEN P.Petrogenetic Interpretation of Granitoid Rocks Series Using Multicationic Parameters[J].Chemical Geology,1985,48(1/2/3/4):43-45. [80] 马永旺,王国芝,胡新伟.“彭灌杂岩”推覆体的构造变形特征[J].四川地质学报,1996,16(2):110-114. MA Yong-wang,WANG Guo-zhi,HU Xin-wei.Tectonic Deformation of Pengguan Complex as a Nappe[J].Acta Geologica Sichuan,1996,16(2):110-114. [81] 张宗清,张国伟,唐索寒,等.汉南侵入杂岩年龄及其快速冷凝原因[J].科学通报,2000,45(23):2566-2571. ZHANG Zong-qing,ZHANG Guo-wei,TANG Suo-han,et al.Geochronology of the Hannan Intrusive Complex to Adjoin the Qinling Orogen and Its Rapid Cooling Reason[J].Chinese Science Bulletin,2000,45(23):2566-2571. [82] YAN Q R,WANG Z Q,HANSON A D,et al.SHRIMP Age and Geochemistry of the Bikou Volcanic Terrane:Implications for Neoproterozoic Tectonics on the Northern Margin of the Yangtze Craton[J].Acta Geologica Sinica,2003,77(4):479-490. [83] 凌文黎,高 山,欧阳建平,等.西乡群的时代与构造背景:同位素年代学及地球化学制约[J].中国科学:D辑,地球科学,2002,32(2):101-112. LING Wen-li,GAO Shan,OUYANG Jian-ping,et al.Time and Tectonic Setting of the Xixiang Group:Constraints from Zircon U-Pb Geochronology and Geochemistry[J].Science in China:Series D,Earth Sciences,2002,32(2):101-112. [84] 赵凤清,赵文平,左义成,等.陕南汉中地区新元古代岩浆岩U-Pb年代学[J].地质通报,2006,25(3):383-388. ZHAO Feng-qing,ZHAO Wen-ping,ZUO Yi-cheng,et al.U-Pb Geochronology of Neoproterozoic Magmatic Rocks in Hanzhong,Southern Shaanxi,China[J].Geological Bulletin of China,2006,25(3):383-388. [85] 张 沛,周祖翼,许长海,等.川西龙门山彭灌杂岩地球化学特征:岩石成因与构造意义[J].大地构造与成矿学,2008,32(1):105-116. ZHANG Pei,ZHOU Zu-yi,XU Chang-hai,et al.Geochemistry of Pengguan Complex in the Longmenshan Region,Western Sichuan Province,SW China:Petrogenesis and Tectonic Implications[J].Geotectonica et Metallogenia,2008,32(1):105-116. [86] 马润则,肖渊甫,魏显贵,等.米仓山地区岩浆活动与构造演化[J].矿物岩石,1997,17(增1):79-85. MA Run-ze,XIAO Yuan-fu,WEI Xian-gui,et al.The Magmatic Activity and Tectonic Evolution in the Micangshan Area,China[J].Journal of Mineralogy and Petrology,1997,17(S1):79-85. [87] 肖渊甫,马润则,何政伟,等.米仓山碱性杂岩单元特征及构造环境分析[J].矿物岩石,1997,17(增1):62-69. XIAO Yuan-fu,MA Run-ze,HE Zheng-wei,et al.The Units Characteristics and Tectonic Settings of the Alkalic Complex in Micangshan[J].Journal of Mineralogy and Petrology,1997,17(S1):62-69. [88] 程建萍,凌文黎.米仓山新元古代岩浆岩省:一个潜在的Rodinia重建方案验证地区[J].地质科技情报,2000,19(3):12-16. CHENG Jian-ping,LING Wen-li.Michangshan Neoproterozoic Igneous Province in Northwest Yangtze Block,South China:A Potential Testee in Rodinia Supercontinent Reconstruction[J].Geological Science and Technology Information,2000,19(3):12-16. [89] 陆松年,李怀坤,陈志宏,等.秦岭中—新元古代地质演化及对Rodinia超级大陆事件的响应[M].北京:地质出版社,2003. LU Song-nian,LI Huai-kun,CHEN Zhi-hong,et al.Meso-Neoproterozoic Geological Evolution in the Qinling Orogeny and Its Response to the Supercontinent Events of Rodinia[M].Beijing:Geological Publishing House,2003. [90] 李瑞保,裴先治,丁仨平,等.西秦岭南缘勉略带琵琶寺基性火山岩LA-ICP-MS锆石U-Pb年龄及其构造意义[J].地质学报,2009,83(11):1612-1623. LI Rui-bao,PEI Xian-zhi,DING Sa-ping,et al.LA-ICP-MS Zircon U-Pb Dating of the Pipasi Basic Volcanic Rocks Within the Mian-Lue Tectonic Zone in the Southern Margin of West Qinling and Its Geolo-gical Implication[J].Acta Geologica Sinica,2009,83(11):1612-1623. [91] 敖文昊,张宇昆,张瑞英,等.新元古代扬子北缘地壳增生事件:来自汉南祖师店奥长花岗岩地球化学、锆石LA-ICP-MS U-Pb年代学和Hf同位素证据[J].地质论评,2014,60(6):1393-1408. AO Wen-hao,ZHANG Yu-kun,ZHANG Rui-ying,et al.Neoproterozoic Crustal Accretion of the Northern Margin of Yangtze Plate:Constrains from Geochemical Characteristics,LA-ICP-MS Zircon U-Pb Chronology and Hf Isotopic Compositions of Trondh-jemite from Zushidian Area,Hannan Region[J].Geological Review,2014,60(6):1393-1408. [92] 徐 通.勉略构造带三岔子—横现河地区蛇绿岩与相关火山岩地球化学、年代学及构造演化[D].西安:长安大学,2014. XU Tong.Geochemistry and Geochronology of Ophiolite and Related Volcanic Rocks in Sanchazi-Heng-xianhe Area,Mianlue Tectonic Zone and Regional Tectonic Evolution[D].Xi'an:Chang'an University,2014. [93] 甘保平,赖绍聪,秦江锋.米仓山坪河新元古代二长花岗岩成因及其地质意义[J].地质论评,2016,62(4):929-944. GAN Bao-ping,LAI Shao-cong,QIN Jiang-feng.Petrogenesis and Implications for the Neoproterzoic Monzogranite in Pinghe,Micang Mountain[J].Geological Review,2016,62(4):929-944. [94] LI J Y,WANG X L,GU Z D.Early Neoproterozoic Arc Magmatism of the Tongmuliang Group on the Northwestern Margin of the Yangtze Block:Implications for Rodinia Assembly[J].Precambrian Research,2018,309:181-197. [95] 崔建堂,韩芳林,张拴厚,等.南秦岭西乡群锆石SHRIMP U-Pb年龄及其构造地质意义[J].陕西地质,2010,28(2):53-58. CUI Jian-tang,HAN Fang-lin,ZHANG Shuan-hou,et al.Zircon SHRIMP U-Pb Dating and the Tectonic Significance of the Xixiang Group in Southern Qinling[J].Geology of Shaanxi,2010,28(2):53-58. [96] LING W L,GAO S,ZHANG B R,et al.Neoproterozoic Tectonic Evolution of the Northwestern Yangtze Craton,South China:Implications for Amalgamation and Break-up of the Rodinia Supercontinent[J].Precambrian Research,2003,122(1/2/3/4):111-140. [97] ZHAO J H,ZHOU M F.Secular Evolution of the Neoproterozoic Lithospheric Mantle Underneath the Northern Margin of the Yangtze Block,SouthChina[J].Lithos,2009,107(3):152-168. [98] 凌文黎,高 山,程建萍,等.扬子陆核与陆缘新元古代岩浆事件对比及其构造意义:来自黄陵和汉南侵入杂岩ELA-ICPMS锆石U-Pb同位素年代学的约束[J].岩石学报,2006,22(2):387-396. LING Wen-li,GAO Shan,CHENG Jian-ping,et al.Neoproterozoic Magmatic Events Within the Yangtze Continental Interior and Along Its Northern Margin and Their Tectonic Implication:Constraint from the ELA-ICPMS U-Pb Geochronology of Zircons from the Huangling and Hannan Complexes[J].Acta Pe-trologica Sinica,2006,22(2):387-396. [99] ZHAO J H,ZHOU M F,ZHENG J P,et al.Neopro-terozoic Crustal Growth and Reworking of the Northwestern Yangtze Block:Constraints from the Xixiang Dioritic Intrusion,South China[J].Lithos,2010,120(3/4):439-452. [100] 耿英英.扬子地块北缘花岗岩SHRIMP锆石U-Pb定年及地球化学特征研究[D].北京:中国地质大学,2010. GENG Ying-ying.SHRIMP U-Pb Zircon Geochrono-logy and Geochemistry Study of Neoproterozoic Gra-nites in the Northern Margin of Yangtze Continental[D].Beijing:China University of Geosciences,2010. [101] ZHOU M F,KENNEDY A K,SUN M,et al.Neoproterozoic Arc-related Mafic Intrusions Along the Northern Margin of South China:Implications for the Accretion of Rodinia[J].The Journal of Geology,2002,110(5):611-618. [102] DONG Y P,LIU X M,SANTOSH M,et al.Neopro-terozoic Subduction Tectonics of the Northwestern Yangtze Block in South China:Constrains from Zircon U-Pb Geochronology and Geochemistry of Mafic Intrusions in the Hannan Massif[J].Precambrian Research,2011,189(1/2):66-90. [103] DONG Y P,ZHANG G W,NEUBAUER F,et al.Tectonic Evolution of the Qinling Orogen,China:Review and Synthesis[J].Journal of Asian Earth Sciences,2011,41(3):213-237. [104] 林振文,秦 艳,周振菊,等.南秦岭勉略带铧厂沟火山岩锆石U-Pb年代学及地球化学研究[J].岩石学报,2013,29(1):85-96. LIN Zhen-wen,QIN Yan,ZHOU Zhen-ju,et al.Zircon U-Pb Dating and Geochemistry of the Volcanic Rocks at Huachanggou Area,Mian-Lue Suture,South Qinling[J].Acta Petrologica Sinica,2013,29(1):85-96. [105] 李献华,李武显,何 斌.华南陆块的形成与Rodinia超大陆聚合-裂解:观察、解释与检验[J].矿物岩石地球化学通报,2012,31(6):543-559. LI Xian-hua,LI Wu-xian,HE Bin.Building of the South China Block and Its Relevance to Assembly and Breakup of Rodinia Supercontinent:Observations,Interpretations and Tests[J].Bulletin of Mineralogy,Petrology and Geochemistry,2012,31(6):543-559. [106] 陆松年.新元古时期Rodinia超大陆研究进展述评[J].地质论评,1998,44(5):489-495. LU Song-nian.A Review of Advance in the Research on the Neoproterozoic Rodinia Supercontinent[J].Geological Review,1998,44(5):489-495.

相似文献/References:

[1]徐多勋,杨拴海,李瑞保,等.西秦岭西段塔洞花岗闪长岩体年代学、地球化学特征及其地质意义[J].地球科学与环境学报,2015,37(03):22.
　XU Duo-xun,YANG Shuan-hai,LI Rui-bao,et al.Geochronological, Geochemical Characteristics and Geological Significance of Tadong Granodiorite Pluton in the Western Section of West Qinling[J].Journal of Earth Sciences and Environment,2015,37(04):22.
[2]王鑫,董国臣,董亮琼.东昆仑东段早泥盆世花岗岩成因：来自龙漠卡岩体的证据[J].地球科学与环境学报,2018,40(04):414.
　WANG Xin,DONG Guo-chen,DONG Liang-qiong.Genesis of Early Devonian Granitoid in East Segment of East Kunlun: Evidences from Longmoka Pluton[J].Journal of Earth Sciences and Environment,2018,40(04):414.
[3]闫盼盼,梁婷*,徐生发,等.皖南竹溪岭花岗闪长岩的岩浆源区:来自矿物学、地球化学证据[J].地球科学与环境学报,2019,41(02):141.
　YAN Pan-pan,LIANG Ting*,XU Sheng-fa,et al.Tracer Origin of Zhuxiling Granodiorite in the Southern Anhui, China: Evidence from Mineralogical and Geochemical Characteristics[J].Journal of Earth Sciences and Environment,2019,41(04):141.
[4]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(04):170.
[5]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(04):396.
[6]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(04):414.
[7]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(04):644.
[8]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.[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(04):15.[doi:10.19814/j.jese.2019.05023]
[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(04):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(04):71.[doi:10.19814/j.jese.2019.07021]
[11]李君阳,薛春纪*,王 斌,等.东昆仑五龙沟金矿田平台岩体岩相学、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,2023,45(05):1176.[doi:10.19814/j.jese.2022.10046]
　LI Jun-yang,XUE Chun-ji*,WANG Bin,et al.Petrography, Geochronology, Geochemical Characteristics of Pingtai Pluton in Wulonggou Gold Orefield, East Kunlun Orogen, China and Their Tectonic Significance[J].Journal of Earth Sciences and Environment,2023,45(04):1176.[doi:10.19814/j.jese.2022.10046]

备注/Memo

备注/Memo:

收稿日期:2020-10-22; 修回日期:2020-12-15
基金项目:国家自然科学基金项目(41872233,41872235,41802234,41902046); 陕西省自然科学基础研究计划项目(2019JM-312); 中央高校基本科研业务费专项资金项目(300102270202,300102279108,300103183081,300104282717,201810710233); 陕西省自然科学基金项目(2020JQ-353); 国家留学基金委员会项目(201806565026)
作者简介:秦 利(1995-),男,安徽六安人,理学硕士研究生,E-mail:qinlichd@163.com。
*通讯作者:裴先治(1963-),男,新疆哈密人,教授,博士研究生导师,理学博士,E-mail:peixzh@chd.edu.cn。

常用功能

更新日期/Last Update: 2021-04-20