吉林大学学报(地球科学版) ›› 2017, Vol. 47 ›› Issue (5): 1405-1418.doi: 10.13278/j.cnki.jjuese.201705106

• 地质与资源 • 上一篇    下一篇

中条山篦子沟铜矿辉钼矿铼-锇同位素年龄及其地质意义

耿艳光1, 简伟2, 李洪英2, 叶会寿2, 毕珉烽2, 胡乔青2, 李超3, 范成龙1, 王梦琦2   

  1. 1. 中国地质大学(北京)地球科学与资源学院, 北京 100083;
    2. 中国地质科学院矿产资源研究所/国土资源部成矿作用与资源评价重点实验室, 北京 100037;
    3. 国家地质实验测试中心, 北京 100037
  • 收稿日期:2017-04-11 出版日期:2017-09-26 发布日期:2017-09-26
  • 通讯作者: 简伟(1985),男,助理研究员,博士,主要从事矿床学研究,E-mail:jianwei@cags.ac.cn E-mail:jianwei@cags.ac.cn
  • 作者简介:耿艳光(1988),男,研究生,主要从事地质工程方面研究,E-mail:476201034@qq.com
  • 基金资助:
    国家自然科学基金项目（41602074）；中国地质调查局项目（DD20160124）；中央级公益性科研院所基本科研业务专项（YYWF201510）

Re-Os Isotopic Dating of Molybdenite from Bizigou Cu Deposit in Zhongtiao Mountain and Its Implication

Geng Yanguang1, Jian Wei2, Li Hongying2, Ye Huishou2, Bi Minfeng2, Hu Qiaoqing2, Li Chao3, Fan Chenglong1, Wang Mengqi2   

  1. 1. School of Geosciences and Resources, China University of Geosciences, Beijing 100083, China;
    2. Institute of Mineral Resources, Chinese Academy of Geological Sciences/Key Laboratory of Metallogeny and Mineral Assessment, MRL, Beijing 100037, China;
    3. National Research Center for Geoanalysis, Beijing 100037, China
  • Received:2017-04-11 Online:2017-09-26 Published:2017-09-26
  • Supported by:
    Supported by National Natural Science Foundation of China(41602074),Project of China Geological Survey(DD20160124)and Special Fund for Basic Scientific Research Business of Central Public Research Institutes(YYWF201510)

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摘要： 篦子沟铜矿位于山西中条山胡-篦型铜矿田，矿体与地层产状一致，呈层状、似层状分布于中条群篦子沟组和余元下组中，经历了多期次多阶段成矿作用。为限定篦子沟铜矿后期热液脉状矿化的形成时代，对篦子沟铜矿区方解石-石英脉中与黄铜矿共生的辉钼矿样品进行了Re-Os同位素测定。结果表明，6件辉钼矿样品Re-Os同位素模式年龄为（1 539±26）~（1 616±26 ）Ma，加权平均年龄为（1 577±31）Ma（MSWD=5.5），等时线年龄为（1 522±180）Ma（MSWD= 9.6），表明热液脉状矿化形成于中元古代长城纪晚期。据此篦子沟铜矿的热液脉状矿化可分为3个成矿期次，分别为古元古代晚期发生的微细脉浸染状矿化期、脉状矿化期和中元古代早期热液脉状辉钼矿矿化期。此次事件可能为中元古代伸展-裂解事件岩浆侵位产生的热液对原来的篦子沟铜矿进行再次的矿化、富集。结合已有资料，证明篦子沟以及中条山地区在中元古代早期存在热液矿化事件。

关键词: Re-Os同位素年龄, 胡-篦型铜矿田, 脉状矿化, 中元古代矿化, 中条山篦子沟铜矿

Abstract: The Bizigou Cu deposit is located in the field of "Hu-Bi" type Cu ore district in Zhongtiao mountain in the southern edge of the North China craton, and it was formed through multiple mineralization events. The orebodies are consistent with the attitude of stratum, and are bedded in the Bizigou Formation and Yuyuanxia Formation. Molybdenite and chalcopyrite occur disseminated in the molybdenite-bearing calcite-quartz veins. Re-Os molybdenite model ages fall in the range from (1 539±26) to (1 616±26) Ma with an isochron age of (1 522±180) Ma (MSWD=9.6) and a weighted mean model age of (1 577±31) Ma (MSWD=5.5), suggesting its hydrothermal vein mineralization formation in the Mesoproterozoic. In the hydrothermal mineralization of the Bizigou deposit,three mineralization events were identified:Paleoproterozoic disseminated mineralization, Paleoproterozoic vein-type mineralization, and Mesoproterozoic vein-type mineralization. This study indicates the existence of a Mesoproterozoic hydrothermal Cu mineralization event in the Bizigou and Zhongtiao Mountain region combining with the existing data.

Key words: Re-Os dating, "Hu-Bi type" Cu deposits, vein-type mineralization, Mesoproterozoic mineralization, Bizigou Cu deposit,Zhongtiao Mountain

中图分类号: 

  • P618.41
[1] 姜玉航,牛贺才,严爽,等.中条山铜矿峪铜矿成矿机制初探[J]. 矿物学报,2013 (增刊2):390-391. Jiang Yuhang, Niu Hecai, Yan Shuang, et al. Copper Deposits in the Zhongtiao Mountains Valley Copper Metallogenic Mechanism[J]. Journal of minerals, 2013, (Sup.2):390-391.
[2] Chen W M, Zhang C X, Lu J R,et al. Polygenetic Mineralization of the Early Proterozoic Tongkuangyu Metaporphyry Copper Deposit in the Zhongtiao Mountains,Shanxi Province[J].Acta Geologica Sinica,1998,72 (2):154-168.
[3] 陈文明,李树屏. 中条山铜矿峪斑岩铜矿金属硫化物的铼-锇同位素年龄及地质意义[J]. 矿床地质,1998,17 (3):224-228. Chen Wenming, Li Shuping. Rhenium-Osmium Isotoric Ages of Sulfides from the Tongkuangyu Porphyry Copper Deposit in the Zhongtiao Mountain[J]. Mineral Deposits, 1998,17 (3):224-228.
[4] 许庆林.山西中条山铜矿峪铜矿矿床地质特征及成因研究[D].长春:吉林大学,2010:117. Xu Qinglin. Study on the Geological Characteristics and Ore Genesis of Tongkuangyu Copper Deosite in the Zhongtiaoshan Mountains,Shanxi Province.[D]. Changchun:Jilin University, 2010:117.
[5] 真允庆,姚长富.中条山区裂谷型层状铜矿床[J].桂林冶金地质学院学报, 1992,12(1):30-40. Zhen Yunqing, Yao Changfu. Stratiform Copper Deposts with in the Raft Valleys of Zhongtiaoshan Area.[J]. Journal of Guilin College of Geology, 1992,12(1):30-40.
[6] Jiang Yuhang, Zhao Yan, Niu Hecai.Paleoproterozoic Copper System in the Zhongtiaoshan Region, Southern Margin of the North China Craton:Ore Geology, Fluid Inclusion, and Isotopic Investigation[J].Main Tectonic Events and Metallogeny of the North China Craton, 2016,9(2):229-250.
[7] 徐文忻, 汪礼明, 李蘅,等. 中条山铜矿床同位素地球化学研究[J]. 地球学报, 2005, 26(增刊1):130-133. Xu Wenxin,Wang Liming,Li Heng,et al. Isotope Geochemist of Copper Dopsits in the Zhongtiao Mountain[J]. Acta Geoscientia Sinica, 2005, 26(Sup.1):130-133.
[8] 薛克勤.中条裂谷构造与成矿作用研究[D].北京:中国地质大学(北京),2006:111. Xue Keqin. Study on the Relation Between Sturcture and Metallogenesis in the Zhongtiao Rift[D]. Beijing:China University of Geoscienees,2006:111.
[9] 许庆林,孙丰月,张晗, 等. 山西中条山铜矿峪铜矿流体包裹体、锆石U-Pb年龄、Hf同位素及其地质意义[J]. 吉林大学学报(地球科学版),2012,42(增刊3):64-80. Xu Qinglin, Sun Fengyue, Zhang Han, et al. Fluid Inclusions,Zircon U-Pb Age and Hf Isotope of Tongkuangyu Copper Deposit in Zhongtiaoshan Mountains and Its Geological Significance,Shanxi Province,China[J]. Journal of Jilin University(Earth Science Edition),2012,42(Sup.3):64-80.
[10] 李宁波,罗勇,郭双龙,等.中条山铜矿峪变石英二长斑岩的锆石U-Pb年龄和Hf同位素特征及其地质意义[J].岩石学报, 2013,29(7):2416-2424. Li Ningbo, Luo Yong, Guo Shuanglong,et al. Zircon U-Pb Geochronology and Hf Isotope Geochemistry of Metamorphic Quartz-Monzonite Porphyry from Tongkuangyu Area,Zhongtiao Mountain and Its Geological Implications[J].Acta Petrologica Sinica,2013,29(7):2416-2424.
[11] 周雄.中条山铜矿峪铜矿区火山岩的地球化学特征及构造背景[J].四川地质学报,2013,33(2):240-243,246. Zhou Xiong. Geochemistry Characteristics of the Volcanic Rocks from Tongkuangyu, Zhongtiaoshan and Their Tectonic Implications[J]. Journal of Sichuan Geology,2013,33(2):240-243,246.
[12] 苗培森,赵凤清.中条山及其邻区古元古代地层对比研究[J].地层学杂志,2013, 37(4):639. Miao Peisen, Zhao Fengqing. Zhongtiao Mountains and Its Adjacent Regions Paleoproterozoic Stratigraphic Correlation Research[J]. Stratigraphy Magazine, 2013, 37(4):639.
[13] 姜玉航,罗勇,牛贺才, 等. 中条山落家河铜矿流体包裹体初步研究[J]. 岩石学报,2013,29(7):2583-2592. Jiang Yuhang, Luo Yong, Niu Hecai, et al. Study on Fluid Inclusions From the Luojiahe Copper Deposit in Zhongtiaoshan Region[J]. Acta Petrologica Sinica,2013, 29(7):2583-2592.
[14] 张晗. 山西中条山北段古元古代铜矿成矿作用[D].长春:吉林大学,2012. Zhang Han. Metallogenesis of Paleproterozoic Copper Deposites in the Northern Zhongtiaoshan Mountains,Shanxi Province[D]. Changchun:Jilin University,2012.
[15] 谭少华. 山西中条山胡-篦型铜矿床成矿地质条件与矿床成因[J]. 西南工学院学报,1997,12(2):60-63. Tan Shaohua. the Geological Factor of Mineralization and the Cause of Formation of the Hu-Bi Copper Deposit, Zhongtiao Mountains, Shanxi[J]. Journal of Southwest Institute of Technology,1997,12(2):60-63.
[16] 孙海田,葛朝华,冀树楷. 中条山地区前寒武纪地层同位素年龄及其意义[J]. 地质通报, 1990,3(3):237-248. Sun Haitian, Ge Chaohua, Ji Shukai. Isotopic Ages of Precambrian Strata in the Zhongtiao Mountains Area and Their Significance[J]. Geologcal Bulletin of China,1990,3(3):237-248.
[17] 庞雪娇. 山西中条山南和沟、老宝滩铜矿床矿化富集规律及矿床成因探讨[D].长春:吉林大学, 2010. Pang Xuejiao. Study on the Enrichment Regularities and Ore Genetic Rules of Nanhegou and Laobaotan Copper Deposits in the Zhongtiao Mountains,Shanxi Province[D]. Changchun:Jilin University, 2010.
[18] 薛昊日. 山西中条山桐木沟、篦子沟铜矿床地质特征及成矿模式研究[D]. 长春:吉林大学, 2010. Xue Haori. Study on the Geological Features and Metallogenic Models of Tongmugou and Bizigou Copper Deposites of Zhongtiaoshan in Shanxi Province[D]. Changchun:Jilin University, 2010.
[19] 黄维平,孙丰月,张晗,等. 山西中条山胡-篦型铜矿床岩石地球化学特征[J]. 世界地质,2013,32(2):212-220. Hang Weiping, Sun Fengyue, Zhang Han, et al. Petrology and Geochemistry Characteristic of Hu-Bi Copper Deposit in Zhongtiao Mountains of Shanxi Province[J]. Global Geology. 2013,32(2):212-220.
[20] Qiu Zhengjie, Fan Hongrui, Liu Xuan,et al. Mine-ralogy, Chalcopyrite Re-Os Geochronology and Sulfur Isotope of the Hujiayu Cu Deposit in the Zhongtiao Mountains, North China Craton:Implications for a Paleoproterozoic Metamorphogenic Copper Mineralization[J].Ore Geology Reviews,2016,78:252-267.
[21] 陆松年,李怀坤,李惠民. 成矿地质事件的同位素年代学研究[J]. 地学前缘,1999,6(2):142-149. Lu Songnian, Li Huaikun, Li Huimin. Research on Isotopic Geochronology of Mineralization Events[J]. Earth Science Frontiers,1999,6(2):142-149.
[22] 陶铨.中条山地区前寒武纪地层的时代[C]//天津地质矿产研究所.中国地质科学院天津地质矿产研究所文集.北京:地质出版社,1985:29-37. Tao Quan. Discussion on The Geochronology of Precambrian Mountain Area[C]//Tianjin Institute of Geology and Mineral Resources.The Chinese Academy of Geological Sciences, Tianjin Institute of Geology and Mineral Resources of Corpus. Beijing:Geological Publishing House,1985:29-37.
[23] 黄典豪,杜安道,吴澄宇, 等. 华北地台钼(铜)矿床成矿年代学研究:辉钼矿铼-锇年龄及其地质意义[J]. 矿床地质,1996,15(4):78-86. Huang Dianhao, Du Andao, Wu Chengyu, et al. Metallochronology of Molybdenum (-Copper) Deposits in the North China Platform:Re-Os Age of Molybdenite and Its Geological Significance[J]. Mineral Deposits,1996,15(4):78-86.
[24] 中条山铜矿地质编写组. 中条山铜矿地质[M]. 北京:地质出版社,1978:1-167. Copper Deposits Drafting Group of the Zhongtiao Mountains. Zhongtiao Mountains Copper Mine Geology[M].Beijing:Geological Publishing House,1978:1-167.
[25] 王子维. 中条地区胡家峪铜矿床地质特征及成矿动力学背景[D]. 长春:吉林大学, 2014. Wang Ziwei. Geological Characteristics and Metallogenic Geodynamics Background of the Hujiayu Copper Deposit in the Zhongtian Mountian[D]. Changchun:Jilin University, 2014.
[26] 马杏垣. 构造学研究现状与展望:参加 27 届国际地质大会侧记[J].地质科技情报,1985(1):2-4. Ma Xingyuan. Tectonics Research Present Situation and Prospect:In the 27th International Geological Congress Sidelights[J].Geological Science and Technology Intelligence, 1985(1):2-4.
[27] 郑超文. 论山西台块构造演化[J]. 山西地质,1986,5(1):25-26. Zheng Chaowen. Theory of Shanxi Block Tectonic Evolution[J]. Shanxi Geological, 1986,5(1):25-26.
[28] 孙大中,李惠民,林源贤,等. 中条山前寒武纪年代学、年代构造格架和年代地壳结构模式的研究[J]. 地质学报,1991,65(3):216-231. Sun Dazhong, Li Huimin, Lin Yuanxian, et al. Precambrian Geochronology Chronotectonic Framework and Model of Chronocrustal Structure of the Zhongtiao Mountains[J]. Acta Geologica Sinica,1991,65(3):216-231.
[29] 刘玄,范宏瑞,邱正杰. 中条山地区绛县群和中条群沉积时限:夹层斜长角闪岩SIMS锆石U-Pb年代学证据[J]. 岩石学报,2015,31(6):1564-1572. Liu Xuan, Fan Hongrui, Qiu Zhengjie. Formation Ages of the Jiangxian and Zhongtiao Groups in the Zhongtiao Mountain Region, North China Craton:Insights from SIMS U-Pb Dating on Zircons of Intercalated Plagioclase Amphibolites[J]. Acta Petrologica Sinica, 2015,31(6):1564 -1572.
[30] Liu C H, Zhao G C, Sun M,et al.U-Pb Geochro-nology and Hf Isotope Geochemistry of Detrital Zircons from the Zhongtiao Complex:Constraints on the Tectonic Evolution of the Trans-North China Orogen[J].Precambrian Research,2013,230(8):31-44.
[31] 宋文法. 篦子沟铜矿床的成矿地质条件及找矿方向[J]. 有色金属设计,2006,33(1):11-14. Song Wenfa. Mineralized Geological and Condition and Range of Reconnaissance of Bizigou Copper Ore Deposit[J]. Nonferrous Metals Design, 2006,33(1):11-14.
[32] 冯世军. 篦子沟铜矿床的背斜构造与控矿作用[J]. 山西冶金,2007,105 (1):24-26. Feng Shijun. The Bizigou Copper ore Deposit in the Anticline Structure and Ore-Controlling Role[J]. Shanxi Metallurgy, 2007, 105(1):24-26.
[33] 胡维兴. 关于中条山胡-篦型铜矿床成矿期和成矿时代问题[J]. 华北地质矿产杂志,1994,9(2):161-166. Hu Weixing. On Mineralization Period and Mentallogenic Epoch of the Hu-Bi Type Copper Deposits in Zhongtiao Mountians, North China[J]. Journal of Geology and Mineral Resources,1994,9(2):161-166.
[34] 杜安道,何红蓼,殷宁万,等.辉钼矿的铼-锇同位素地质年龄测定方法研究[J].地质学报,1994,68(4):339-347. Du Andao, He Hongliao, Yin Ningwan, et al. A Study on the Rhenium-Osmiu Geochronometry of Molybdenites[J]. Acta Geologica Sinica,1994,68(4):339-347.
[35] Du A D, Wu S Q, Sun D Z, et al. Preparation and Certification of Re-Os Dating Reference Materials:Molybdenite HLP and JDC[J].Geostandard and Geoanalytical Research, 2004,28 (1):41-52.
[36] Wieser M E. Atomic Weights of the Elements (Iupac Technical Report)[J].Pure and Applied Chemistry,2005,78(11):2051-2066.
[37] Bohlkea J K, De Laeter J R, De Bievre P, et al. Isotopic Compositions of the Elements[J]. Journal of Physical Chemical Reference Data,2005,34(1):57-67.
[38] Smoliar, Michael I, Walker, et al. Re-Os Ages of Group ⅡA, ⅢA, IVA, and IVB Iron Meteorites[J].Science Magazine, 1996, 271:1099-1102.
[39] Hu W X,Sun D Z. Mineralization and Evolution of the Early Proterozoic Copper Deposits in the Zhongtiao Mountains[J]. Acta Geologica Sinica,1987,61 (2):61-76.
[40] 翟明国. 华北克拉通的形成演化与成矿作用[J].矿床地质,2010,29 (1):24-36. Zhai Mingguo. Tectonic Evolution and Metallogenesis of North China Craton[J].Mineral Deposits,2010,29 (1):24-36.
[41] 郭红党.中条裂谷演化与成矿作用探讨J].矿产勘查,2010,1 (5):441-445. Guo Hongdang. Disscusion on the Relation Between Evolution and Metallogenesis in the Zhongtiao Rift[J]. Mineral Exploration,2010,1 (5):441-445.
[42] 李三忠,扬振升,刘永江.辽东早元古代造山带隆滑构造解析[J]. 长春地质学院学报, 1996,26(3):305-309. Li Sanzhong, Yang Zhensheng, Liu Yongjiang. Preliminary Analysis on Uplift Bedding Delamination Structure of the Palaeoproterozoic[J].Journal of Changchun University of Earth Sciences,1996, 26(3):305-309.
[43] 李三忠,韩宗珠,刘永江, 等. 辽河群区域变质特征及其大陆动力学意义[J]. 地质论评,2001,47(1):9-18. Li Sanzhong, Han Zongzhu, Liu Yongjiang, et al. Continental Dynamics and Regional Metamorphism of the Liaohe Group[J]. Geological Review,2001,47(1):9-18.
[44] 沈保丰,翟安民,杨春亮.古元古代:中国重要的成矿期[J]. 地质调查与研究,2010,33(4):241-256,308. Shen Baofeng, Zhai Anmin, Yang Chunliang. Paleoproterozoic:An Important Metallogenic Epoch in China[J]. Geological Survey and Research,2010,33(4):241-256,308.
[45] 耿元生, 杨崇辉,万渝生.吕梁地区古元古代花岗岩浆作用:来自同位素年代学的证据[J].岩石学报, 2006,22(2):305-314. Geng Yuansheng, Yang Chonghui, Wan Yusheng. Pleoproetrozoic Granitic Magmaitism in the Lüliang Area,North China Craton:Constraintform Isotopic Geochronology[J]. Aeate Potrlogicain Sica, 2006,22(2):305-314.
[46] 沈保丰,李俊建,翟安民, 等. 地壳演化和成矿耦合:以华北陆块北缘中段为例[J]. 前寒武纪研究进展,2001,24(1):9-16. Shen Baofeng, Li Junjian, Zhai Anmin, et al.The Coupling Between the Crustal Evolution and Mineralization:Example by the Middle North Margin of North China Craton[J]. Precambrian Research Progress,2001,24(1):9-16.
[47] 龚瑞君. 华北地台北缘中西段前寒武系重大成矿地质事件[D]. 成都:成都理工大学,2010. Gong Ruijun. Precambrian Important Tectonic Events in the Central and West Part of North Margin, North China Platform[D]. Chengdu:Chengdu University of Technology,2010.
[48] 白瑾,戴凤岩,颜耀阳. 中条山前寒武纪地壳演化[J]. 地学前缘,1997,4(3):285-286. Bai Jin, Dai Fengyan, Yan Yaoyang. Precambrian Crustal Evolution of the Zhongtiao Mountains[J]. Earth Science Frontiers, 1997,4(3):285-286.
[49] Peng P,Zhai M G, Guo J H.1.80-1.75 Ga Mafic Dyke Swarms in the Central North China Craton:Implications for a Plumerelated Break-Up Event in Hanski E, Mertanen S,Ram Tand Vuollo J:Dyke Swarms:Time Markers of Crustal Evolution[M].New York:Taylor & Francis Publisher,2006:1-2.
[50] Peng P, Zhai M G, Ernst R E,et al. A 1.78 Ga Large Igneous Province in the North China Craton:The Xiong'er Volcanic Province and the North China Dyke Swarm[J].Lithos,2008,101 (3/4):260-280.
[51] He Y H,Zhao G C,Sun M,et al. SHRIMP and LA-ICP-MS Zircon Geochronology of the Xiong'er Volcanic Rocks:Implications for the Paleo-Mesoproterozoic Evolution of the Southern Margin of the North China Craton[J].Precambrian Research,2009,168(3/4):213-222.
[52] 李海艳. 山西省运城市芦家坪铜矿地质特征及找矿标志[J]. 华北国土资源,2012(3):111-113,115. Li Haiyan. Lujiaping Copper Mine Geological Characteristics and Main Ore Guide of Shanxi Yuncheng[J].Huabei Land and Resources,2012(3):111-113,115.
[53] 张金星, 马春阳. 河南省济源市铜锣地区铜矿地质特征及成因解析[C]//段子清.河南地球科学通报.北京:中国大地出版社,2010:5. Zhang Jinxing, Ma Chunyang. Analyze on the Mineralization and Geological Characteristics of Tongluo Copper Deposition Jiyuan City of Henan Province[C]//Duan Ziqing.Henan Earth Science Bulletin. Beijing:The Earth Publishing House of China,2010:5.
[54] 葛桐孚,崔小军,刘纪峰. 济源铜锣铜矿区矿床成因及找矿方向探讨[J].科技创新导报,2010, 164 (20):116-117. Ge Tongfu, Cui Xiaojun, Liu Jifeng. The Genesis and Prospecting Direction of Jiyuan Tongluo Deposite[J]. Science and Technology Innovation Herald,2010,164(20):116-117.
[55] 崔小军,康顺福,刘家军, 等. 中条裂谷的递进演化与王屋山地区铜矿成矿地质条件分析[J]. 地质找矿论丛,2007,22(1):24-30. Cui Xiaojun, Kang Shunfu, Liu Jiajun, et al. Stepwise Evolution of Zhongtiao Rift and Analysis on Copper Mineralization Conditions in Wangwushan Region[J]. Contributions to Geology and Mineral Resources Research,2007,22(1):24-30.
[56] 刘亮明. 中条山地区地壳递进演化与胡-篦型铜矿床的成因[J]. 九江,1999,30(4):647-675. Liu Liangming. Progressive Evolution of Crust and Genesis of "Hu-Bi" Type Copper Deposits in Zhongtiaoshan District[J]. Jiujiang,1999,30(4):647-675.
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