吉林大学学报(地球科学版) ›› 2017, Vol. 47 ›› Issue (6): 1746-1762.doi: 10.13278/j.cnki.jjuese.201706113
施珂1,2, 张达玉1, 丁宁2, 王德恩3, 陈雪锋1
Shi Ke1,2, Zhang Dayu1, Ding Ning2, Wang Deen3, Chen Xuefeng1
摘要: 皖南绩溪县逍遥岩体侵位于新元古界南华系、震旦系和下古生界海相沉积盖层中,岩性为花岗闪长岩。测得该岩体LA-ICP-MS锆石U-Pb同位素加权平均值年龄为(149.3±2.3)和(148.6±1.9) Ma,表明:岩体侵位于晚侏罗世。逍遥花岗闪长岩体的电子探针分析显示其黑云母为镁质黑云母。岩石地球化学研究表明:其为高钾钙碱性系列,准铝质-过铝质,属于I型花岗岩;微量元素特征显示其富集轻稀土而亏损重稀土元素,富集Ba、Sr等大离子亲石元素。综合地质、年代学、电子探针和岩石主微量元素分析,逍遥岩体形成于晚侏罗世,其岩浆来源于有幔源物质加入的下地壳,在形成过程中经历了较强的部分熔融作用,该岩体具有火山弧花岗岩特点。
中图分类号:
[1] Wu F Y, Ji W Q, Sun D H, et al. Zircon U-Pb Geo-chronology and Hf Isotopic Compositions of the Mesozoic Granites in Southern Anhui Province[J]. Lithos, 2012, 150:6-25. [2] 薛怀民, 汪应庚, 马芳, 等. 高度演化的黄山A型花岗岩:对扬子克拉通东南部中生代岩石圈减薄的约束[J]. 地质学报, 2009,83(2):247-259. Xue Huaimin, Wang Yinggeng, Ma Fang,et al. The Huangshan A-Type Granites with Tetrad REE:Constraints on Mesozoic Lithospheric Thinning of the Southeastern Yangtze Craton[J]. Acta Geologica Sinica, 2009, 83(2):247-259. [3] 周涛发, 袁峰, 侯明金, 等. 江南隆起带东段皖赣相邻区燕山期花岗岩类的成因及形成的地球动力学背景[J]. 矿物岩石, 2004, 24(3):65-71. Zhou Taofa, Yuan Feng, Hou Mingjin, et al. Genesis and Geodynamic Background of Yanshanian Granitoids in the Eastern Jiangnan Uplift in the Adjacent Area of Anhui and Jiangxi Provinces China[J]. Journal of Mineralogy and Petrology, 2004, 24(3):65-71. [4] 安徽省地质调查院. 安徽省钨矿资源潜力评价成果报告[R]. 合肥:安徽省地质调查院, 2011. Geological Survey of Anhui Province. Anhui Tungsten Resources Potential Evaluation Results Report[R]. Hefei:Geological Survey of Anhui Province,2011. [5] Song G X, Qin K Z, Li J M, et al. Mesozoic Mag-matism and Metallogeny in the Chizhou Area,Middle-Lower Yangtze Valley, SE China:Constrained Bypetrochemistry, Geochemistry and Geochronology[J]. Journal of Asian Earth Sciences, 2014, 91:137-153. [6] 范羽. 安徽青阳地区钨钼成矿作用研究[D].合肥:合肥工业大学, 2015:1-144. Fan Yu. Study on Tungsten-Molybdenum Mineralization in Qingyang Area, Anhui Province[D]. Hefei:Hefei University of Technology, 2015:1-144. [7] 秦燕, 王登红, 吴礼彬, 等. 安徽东源钨矿含矿斑岩中的锆石SHRIMP U-Pb年龄及其地质意义[J]. 地质学报, 2010,84(4):479-484. Qin Yan, Wang Denghong, Wu Libin,et al. Zircon SHRIMP U-Pb Dating of the Mineralized Porphyry in the DongyuanW Deposit in Anhui Province and Its Geological Significance[J]. Acta Geologica Sinica, 2010,84(4):479-484. [8] Song G X, Qin K Z, Li G M, et al. Geochronologic and Isotope Geochemical Constraints on Magmatism and Associated W-Mo Mineralization of the Jitoushan W-Mo Deposit, Middle-Lower Yangtze Valley[J]. Int Geol Rev, 2012, 54(13):1532-1547. [9] Song G X, Qin K Z, Li G M, et al. Geochronology and Ore-Formingfluids of the Baizhangyan W-Mo Deposit in the Chizhou Area, Middle-LowerYangtze Valley[J]. SE-China Resour Geol, 2013, 63(1):57-71. [10] 陈芳, 王登红, 杜建国, 等. 安徽绩溪伏岭花岗岩LA-ICP-MS锆石U-Pb年龄的精确测定及其地质意义[J]. 岩矿测试, 2013, 32(6):970-977. Chen Fang, Wang Denghong,Du Jianguo,et al. New Dating of the Fuling Granite Body with LA-ICP-MS Zircon U-Pb in Jixi,Anhui Province and Their Geological Significance[J]. Rock and Mineral Analysis, 2013,32(6):970-977. [11] 丁宁. 安徽省钨矿成矿规律[D]. 合肥:合肥工业大学, 2012:1-154. Ding Ning. Metallogenic Regularity of Tungsten Deposits in Anhui Province[D]. Hefei:Hefei University of Technology, 2012:1-154. [12] 周翔, 余心起, 杨赫鸣, 等. 皖南绩溪县靠背尖高Ba-Sr花岗闪长斑岩年代学及其成因[J]. 岩石学报, 2012, 28(10):3403-3417. Zhou Xiang, Yu Xinqi, Yang Heming, et al. Petrogenesis and Geochronology of the High Ba-Sr Kaobeijian Granodiorite Porphyry,Jixi County,South Anhui Province[J]. Acta Petrologica Sinica, 2012, 28(10):3403-3417. [13] 杜玉雕, 刘家军, 余心起, 等. 安徽逍遥钨-多金属矿床成矿物质来源与成矿:碳、硫和铅同位素证据[J]. 中国地质, 2014, 40(2):566-579. Du Yudiao, Liu Jiajun, Yu Xinqi,et al. TheSources of Metallogenic Materials and Mineralization of the Xiaoyao W-polymetallic Deposit in Anhui Province:Evidence from Carbon, Sulfur and Lead Isotopes[J]. Geology in China, 2014,40(2):566-579. [14] 汤金来, 程伟斌, 陈富荣, 等. 安徽绩溪逍遥钨-多金属矿床成矿地质条件与成矿潜力[J]. 合肥工业大学学报(自然科学版), 2014, 37(6):745-750. Tang Jinlai, Cheng Weibin, Chen Furong, et al. Ore-Forming Geological Conditions and Mineralization Potentiality of Xiaoyao WPolymetallic Deposit in Xiaoyao Village,Jixi County,Anhui Province[J]. Journal of Hefei University of Technology(Natural Science Edition), 2014, 37(6):745-750. [15] 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, 1991:1-397. Chang Yinfo, Liu Xiangpei, Wu Yanchang. The Middle and Lower Reaches of the Yangtze River Copper Iron Metallogenic Belt[M]. Beijing Geological Publishing House, 1991:1-397. [16] 袁峰, 周涛发, 范裕, 等. 皖赣相邻区燕山期花岗岩类构造背景及其意义[J]. 合肥工业大学学报(自然科学版), 2005, 28(9):1130-1134. Yuan Feng, Zhou Taofa, Fan Yu,et al. Tectonic Setting of Granitoids of Yanshanian Stage in the Adjoiningregion of Anhui and Jiangxi Province and Its Significance[J].Journal of Hefei University of Technology(Natural Science Edition),2005, 28(9):1130-1134. [17] 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, 2010, 51(1/2):537-571. [18] Liu Y S, Hu, Z C, Zong K Q, et al. Reappraisement and Refinement of Zircon U-Pb Isotope and Trace Element Analyses by LA-ICP-MS[J]. Chinese Science Bulletin, 2010, 55(15):1535-1546. [19] 李伟, 谢桂青, 姚磊, 等. 鄂东南地区程潮大型矽卡岩型铁矿区岩体成因探讨[J]. 吉林大学学报(地球科学版), 2014, 44(6):1827-1855. Li Wei, Xie Guiqing, Yao Lei, et al. Genesis of the Intrusive Rocks in the Chengchao Large Skarn Iron Deposit, Southeastern Hubei Province[J]. Journal of Jilin University (Earth Science Edition), 2014, 44(6):1827-1855. [20] 安徽省地质调查院. 浙赣皖相邻区综合找矿预测[R]. 合肥:安徽省地质调查院, 2012. Geological Survey of Anhui Province. The Comprehensive Prospecting Prediction of Zhejiang,Jiangxi and Anhui[R]. Hefei:Geological Survey of Anhui Province, 2012. [21] Cliff R A. Isotopic Dating in Metamorphic Belts[J]. Journal of the Geological Society, 1985, 142(1):97-110. [22] Nam T N, Sano Y, Terada K, et al. First SHRIMP U-Pb Zircon Dating of Granulites from the Kontum Massif (Vietnam) and Tectonothermal Implications[J]. Journalof Asian Earth Sciences,2011, 19(1/2):77-84. [23] Hourigan J K, Solov'ev A S, Ledneva G V, et al. Timing of Syenite Intrusions on the Eastern Slopeof the Sredinnyi Range, Kamchatka:Rate of Accretionary Structureexhumation[J]. Geochemistry International, 2004, 42(2):97-105. [24] Hirt W H. Petrology of the Mount Whitney Intrusive Suite, Eastern Sierra Nevada, California:Implications for the Emplacement and Differentiation of Composite Felsic Intrusions.[J]. Geological Society of America Bulletin, 2007, 119(9/10):1185-1200. [25] 陈江峰, 谢智, 郑永飞,等. 皖东侵入岩矿物Rb-Sr和Ar-Ar年代学及其与氧同位素平衡之间的关系[J]. 高校地质学报, 2003, 9(2):172-183. Chen Jiangfeng, Xie Zhi, Zheng Yongfei,et al. The Relation Between Rb-Sr, Ar-Ar Geochronometers and Oxygen Isotopic Equilibrium of Intrusions from Eastern Anhui Province, China[J]. Geological Journal of China Universities, 2003,9(2):172-183. [26] 汪雅菲. 安徽城安岩体地球化学特征及成因研究[D]. 合肥:合肥工业大学, 2015:1-114. Wang Yafei. The Geochemical Characteristics and Diagenesis Research of Cheng'an Composite Pluton,Anhui Province[D]. Hefei:Hefei University of Technology, 2015:1-114. [27] Su Y P, Zheng J P, Griffin W L, et al. Petrogenesis and Geochronology of Cretaceous Adakitic, I-and A-Type Granitoids in the NE Yangtze Block:Constraints on the Eastern Subsurface Boundary Between the North and South China Blocks[J]. Lithos, 2013,175/176:333-350. [28] Loiselle M C, Wones D R. Characteristics and Origin of Anorogenic Granites[J]. Geological Society of America Abstracts with Programs. 1979, 11(7):468. [29] Whalen, Chappell. Opaque Mineralogy and Mafic Mi-neral Chemistry of I-and S-Type Granites of Lachlan Fold Belt[J].Southeast Australia, American Mineralogist, 1988, 73(3):281-296. [30] 刘春花, 吴才来, 雷敏, 等. 秦岭东江口和柞水花岗岩的矿物成分特征及其形成的温压条件[J]. 岩石矿物学杂志, 2013, 32(3):341-354. Liu Chunhua, Wu Cailai, Lei Min,et al. Mineral Composition and Temperature-Pressure Conditions of Dongjiangkou and Zhashui Granites in the Qinling Mountains[J]. Acta Petrologica Et Mineralogica, 2013,32(3):341-354. [31] 谢建成, 夏冬梅, 方德, 等. 皖南晚中生代花岗闪长岩地球化学:成岩成矿制约[J]. 岩石学报, 2016, 32(2):439-455. Xie Jiancheng, Xia Dongmei, Fang De, et al. Geochemistry of Late Mesozioc Granodiorites Insouthern Anhui Province:Constraints for Rock and Ore-Forming[J]. Acta Petrologica Sinica, 2016, 32(2):439-455. [32] Rapp R P, Watson E B. Dehydration Melting of Me-tabasalt at 8-32 kbar; Implications for Continental Growth and Crust-Mantle Recycling[J]. Journal of Petrology, 1995, 36:891-931. [33] 丁孝石. 西藏中南部各类花岗岩中黑云母标型特征及其地质意义[J]. 中国地质科学院矿床地质研究所所刊, 1988(1):33-50. Ding Xiaoshi. Study of Typomorphic Characteristics of Micasfrom Granitoids in Central-Southern Xizang and Their Geological Significance[J]. Bulletin of the Institute of Mineral Deposits Chinese Academy of Geological Sciences, 1988(1):33-50. [34] Zhang D Y, Zhou T F, Yuan F, et al. Petrogenesis and Mineralization Potential of a Granite Porphyry Intrusion Beneath the Baishan Mo Deposit, Eastern Tianshan, NW China[J]. Journal of Asian Earth Sciences,2015,113:254-265. [35] 朱光, 刘国生. 皖南江南陆内造山带的基本特征与中生代造山过程[J]. 大地构造与成矿学, 2000,24(2):103-111. Zhu Guang, Liu Guosheng. Basic Characteristics and Mesozoic Orogenic Process of the Jiannan Intracontinental Orogenic Belt in Southern Anhui[J]. Geotectonica et Metallogenia, 2000, 24(2):103-111. [36] 周涛发, 袁峰, 岳书仓, 等. 安徽月山矿田硅、氦、氖同位素地球化学研究[J]. 矿物岩石地球化学通报, 2001, 20(4):385-387. Zhou Taofa, Yuan Feng, Yue Shucang,et al. Silicon, Helium and Neon Isotope Geochemistry of Cu, Au Ore Deposist in the Yueshan Orefield, Anhui Province[J]. Bulletin of Mineralogy, Petrology and Geochemistry, 2001, 20(4):385-387. [37] Zhou M F, Yan D P, Wang C L, et al. Subduction-Related Origin of the 750 Ma Xuelongbao Adakitic Complex (Sichuan Province, China);Implications for the Tectonic Setting of the Giant Neoproterozoic Magmatic Event in South China[J]. Earth and Planetary Science Letters, 2006,248:286-300. [38] Sun W D, Ding X, Hu Y H, et al. The Golden Tra-nsformation of the Cretaceous Plate Subduction in the West Pacific[J]. Earth and Planetary Science Letters, 2007, 262:533-542. [39] Li Z X, Li X H. Formation of the 1300-km-Wide Intracontinental Orogen and Postorogenic Magmatic Province in Mesozoic South China;A Flat-Slab Subduction Mode[J]. Geology, 2007, 35:179-182. [40] Li H, Ling M X, Li C Y, et al. A-type Granite Belts of Two Chemical Subgroups in Central Eastern China:Indication of Ridge Subduction[J]. Lithos, 2012, 150:26-36. [41] Li H, Zhang H, Ling M X, et al. Geochemical and Zircon U-Pb Study of the Huangmeijian A-Type Granite:Implications for Geological Evolution of the Lower Yangtze River Belt[J]. International Geology Review, 2011, 53(5/6):499-525. [42] 翁望飞, 曹诚, 支利赓, 等. 皖南燕山期高钾钙碱性埃达克岩厘定及岩石成因[J].地质与勘探, 2011,47(6):967-981. Weng Wangfei, Cao Cheng, Zhi Ligeng, et al. Geochemical Characteristics and Petrogenesis of High-K Calc-Alkaline Adakite of the Yanshanianepoch in South Anhui[J]. Geology and Exploration, 2011, 47(6):967-981. [43] 邓晋福, 吴宗絮. 下扬子克拉通岩石圈减薄时间与长江中下游Cu-Fe成矿带[J]. 安徽地质, 2001, 11(2):86-91. Deng Jinfu, Wu Zongxu. Lithospheric Thinning Event in the Lower Yangtze Craton and Cu-Fe Metallogenic Belt in the Middle and Lower Yangtze River Reaches[J]. Geology of Anhui, 2001, 11(2):86-91. [44] 汪洋, 邓晋福, 姬广义. 长江中下游地区早白垩世埃达克质岩的大地构造背景及其成矿意义[J].岩石学报, 2004, 20(2):297-314. Wang Yang, Deng Jinfu, Ji Guangyi. A Perspective on the Geotectonic Setting of Early Cretaceous Adakite-Like Rocks in the Lower Reaches of Yangtze River and Its Significance for Copper-Gold Mineralization[J]. Acta Perologica Sinica, 2004, 20(2):297-314. [45] 毛景文, 谢桂清, 张作衡, 等. 中国北方中生代大规模成矿作用的期次及地球动力学背景[J]. 岩石学报, 2005, 21(1):169-188. Mao Jingwen, Xie Guiqing, Zhang Zuoheng, et al. Mesozoic Large-Scale Metallogenic Pulses in North China and Corresponging Geodynamic Settings[J]. Acta Perologica Sinica, 2005, 21(1):169-188. [46] 郭令智, 卢华复, 施央申,等.江南中、新元古代岛弧的运动学和动力学[J]. 高校地质学报, 1996, 2(1):1-13. Guo Lingzhi, Lu Huafu, Shi Yangshen, et al. On the Meso-Neoproterozoic Jiangnan Island ARC:Its Kinematics and Dynamics[J]. Geological Journal of China Universities, 1996, 2(1):1-13. [47] 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 Zhenhua, Xiong Xiaolin, Wang Qiang, et al. Some Aspects on Geochemistry of Nb and Ta[J]. Geochemistry, 2008, 37(4):304-320. [48] 张虹, 戴圣潜, 管运财, 等. 皖南绩溪伏岭岩体岩石地球化学特征[J]. 中国地质, 2005, 32(3):411-416. Zhang Hong, Dai Shengqian, Guan Yuncai, et al. Petrology and Geochemistry of the Fuling Mass in Jixi, Southern Anhui[J]. Geology in China, 2005, 32(3):411-416. [49] Shi C Y, Yan M C, Chi Q H.Abundances of Chemical Elementsin Granitoids of Different Geological Ages and Their Characteristics in China[J]. Geoscience Frontiers, 2011, 2(2):261-275. [50] 杜玉雕. 安徽东源钨钼矿床流体特征与成矿机制[D]. 北京:中国地质大学, 2012:1-94. Du Yudiao. Fluid Characteristics and Metallogcnic Mechanism in the Dongyuan W-Mo Deposit in Anhui Province,China[D]. Beijing:China University of Geosciences, 2012:1-94. [51] 李斌. 宁国市大坞尖钨钼矿床地质特征及成因研究[D]. 合肥:合肥工业大学, 2014:1-84. Li Bin. A Study on the Characteristics and Genesis of W-Mo Polymetallic Deposits, Ningguo[D]. Hefei:Hefei University of Technology, 2014:1-84. [52] 王强, 赵振华, 简平, 等. 德兴花岗闪长斑岩SHRIMP锆石U-Pb年代学和Nd-Sr同位素地球化学[J]. 岩石学报, 2004, 20(2):315-324. Wang Qiang, Zhao Zhenhua, Jian Ping, et al. SHRIMP Zircon Geochronology and Nb-Sr Isotopic Geochemistry of the Dexing Granodiorite Porphyries[J]. Acta Perologica Sinica, 2004, 20(2):315-324. [53] 邱骏挺, 余心起, 张德会, 等. 浙西开北化区桐村花岗斑岩LA-ICPMS锆石U-Pb年代学及其地质意义[J]. 地质通报, 2011, 30(9):1360-1368. Qiu Junting, Yu Xinqi, Zhang Dehui, et al. LA-ICP-MS Zircon U-Pb Dating of the Tongcun Porphyry in Kaihua County, Western Zhejiang Province, and Its Geological Significance[J]. Geological Bulletin of China, 2011, 30(9):1360-1368. [54] 杨昔林, 曹殿华, 李以科, 等. 江西德兴孔家银山火山盆地的时代归属:锆石U-Pb年代学证据[J]. 中国地质, 2011, 38(1):86-93. Yang Xilin, Cao Dianhua, Li Yike, et al. Age of Kongjia-Yinshan Volcanic Basin in Dexing, Jiangxi Province:Evidence from Zircon U-Pb Chronology[J]. Geology in China, 2011, 38(1):86-93. [55] 王德恩, 周翔, 余心起, 等. 皖南祁门地区东源钨钼矿区花岗闪长斑岩SHRIMP锆石U-Pb年龄和Hf同位素特征[J]. 地质通报, 2011, 30(10):36-51. Wang Deen, Zhou Xiang, Yu Xinqi, et al. SHRIMP Zircon U-Pb Dating and Characteristics of Hf Isotopes of the Granodiorite Porphyries in the Dongyuan W -MoOre District, Qimen Area, Southern Anhui[J]. Geological Bulletin of China, 2011, 30(10):36-51. [56] 陈帅奇, 余心起, 张德会, 等. 浙西开化桐村花岗斑岩地球化学特征及找矿潜力[J]. 金属矿山, 2011(3):108-111. Chen Shuaiqi, Yu Xinqi, Zhang Dehui, et al. Geochemical Characteristics of Kaihua Tongcun Granitic Porphyry In Western Zhejiang and Ore-Prospecting Potential[J]. Metal Mine, 2011(3):108-111. |
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