冀东峪耳崖金矿区闪长岩脉地球化学特征及其地质意义

doi:10.13278/j.cnki.jjuese.20200069

吉林大学学报(地球科学版) ›› 2021, Vol. 51 ›› Issue (2): 416-428.doi: 10.13278/j.cnki.jjuese.20200069

冀东峪耳崖金矿区闪长岩脉地球化学特征及其地质意义

杨爱雪^1,2, 孙德有², 侯雪刚^2,3, 王久良¹, 张继林⁴, 李临位⁴

1. 河北省地质矿产勘查开发局第五地质大队, 河北唐山 063000;
2. 吉林大学地球科学学院, 长春 130061;
3. 河南省国土资源科学研究院, 郑州 450053;
4. 中国黄金集团有限公司, 北京 100010

收稿日期:2020-03-23 出版日期:2021-03-26 发布日期:2021-04-06
通讯作者: 孙德有(1965-),男,教授,博士生导师,主要从事火成岩及地球化学方面的研究,E-mail:sundy@jlu.edu.cn E-mail:sundy@jlu.edu.cn
作者简介:杨爱雪(1992-),女,硕士研究生,主要从事火成岩方面的研究,E-mail:337394871@qq.com
基金资助:
中国黄金集团有限公司科研项目（ZJ-DJ/2015-HBYEY）

Geochemical Characteristics and Geological Significance of Diorite of Yu'erya Gold Deposit Area in Eastern Hebei Province

Yang Aixue^1,2, Sun Deyou², Hou Xuegang^2,3, Wang Jiuliang¹, Zhang Jilin⁴, Li Linwei⁴

1. The Fifth Geology Company of Hebei Geology ﹠ Minerals Bureau, Tangshan 063000, Hebei, China;
2. College of Earth Sciences, Jilin University, Changchun 130061, China;
3. Henan Academy of Land and Resources Sciences, Zhengzhou 450053, China;
4. China National Gold Group Co., Ltd, Beijing 100010, China

Received:2020-03-23 Online:2021-03-26 Published:2021-04-06
Supported by:
Supported by the Scientific Research Projects of China National Gold Group Co., Ltd(ZJ-DJ/2015-HBYEY)

摘要/Abstract

摘要： 冀东地区位于华北板块北缘燕山造山带东部，矿产资源丰富，是中国金矿的主要产地之一，尤其是热液型金矿。峪耳崖金矿床是冀东众多热液型金矿床的典型代表，金矿主体赋存于侏罗纪峪耳崖花岗岩体内，少部分赋存于侵入花岗岩体的侏罗纪闪长岩脉中。闪长岩脉元素地球化学分析显示：w（SiO₂）为51.99%~61.88%、Mg^#值为0.37~0.64，w（Na₂O+K₂O）为5.07%~8.89%，A/NK为1.37~2.26，A/CNK为0.73~0.96，属准铝质高钾钙碱性系列；富集轻稀土元素和大离子亲石元素Rb、Ba、K、Sr，亏损重稀土元素和高场强元素Nb、Ta、Ti。锆石原位Hf同位素测试表明，ε_Hf（t）为负值，介于-16.5~-6.5之间。综合研究认为：峪耳崖金矿区侏罗纪闪长岩浆源于俯冲流体交代的富集岩石圈地幔，岩浆上侵过程中受到华北板块古老下地壳物质的有限混染；成矿期闪长岩浆为金成矿提供了部分物质来源；峪耳崖金矿区闪长岩脉形成于古太平洋板块向欧亚大陆俯冲的动力学背景。

关键词: 闪长岩脉, 地球化学, Hf同位素, 岩石成因, 峪耳崖金矿床

Abstract: Located in the eastern part of the Yanshan orogenic belt on the northern margin of the North China plate in eastern Hebei Province,Yu'erya is one of the main gold producing areas especially with hydrothermal gold deposits. The Yu'erya deposit is representative in eastern Hebei Province, which occurs mainly in the granite of the Jurassic Yu'erya pluton with a few orebodies in the Jurassic diorite that intruded into the granite. The geochemical data show that the w(SiO₂) of diorites is 51.99%-61.88% and w(Na₂O+K₂O) is 5.07%-8.89%, with Mg^# values between 0.37 to 0.64. They are high-potassium calc-alkaline and quasi-aluminum with A/CNK and A/NK values ranging from 0.73 to 0.96 and 1.37 to 2.26, respectively. All samples are rich in LREE and LILE including Rb, Ba, K,and Sr, and are depleted of HREE and HFSE such as Nb, Ta and Ti. The zircon Hf isotope studies show that the ε_Hf(t) values of the diorites range from -16.5 to -6.5. These data indicate that the Jurassic diorite magma originated from the enriched lithospheric mantle replaced by subduction fluids, and was contaminated limitedly by the ancient lower crust material of the North China plate during magma upwelling. In the ore-forming period,the diorite magma provided part of the material for the gold mineralization. Combined with other regional results, this study suggests that the magmatism is likely associated with the subduction of the paleo-Pacific plate beneath Eurasia.

Key words: diorite, geochemistry, Hf isotope, petrogenesis, Yu’erya gold deposit

中图分类号:

P588.13

杨爱雪, 孙德有, 侯雪刚, 王久良, 张继林, 李临位. 冀东峪耳崖金矿区闪长岩脉地球化学特征及其地质意义[J]. 吉林大学学报(地球科学版), 2021, 51(2): 416-428.

Yang Aixue, Sun Deyou, Hou Xuegang, Wang Jiuliang, Zhang Jilin, Li Linwei. Geochemical Characteristics and Geological Significance of Diorite of Yu'erya Gold Deposit Area in Eastern Hebei Province[J]. Journal of Jilin University(Earth Science Edition), 2021, 51(2): 416-428.

参考文献

[1] 尹业长,郝立波,赵玉岩,等.冀东高家店和蛇盘兔花岗岩体:年代学、地球化学及地质意义[J].吉林大学学报(地球科学版),2018,48(2):574-586. Yin Yechang,Hao Libo,Zhao Yuyan,et al. Gaojiadian Granite and Shepantu Granite in Eastern Hebei Province:Chronology,Geochemistry and Geological Significances[J].Journal of Jilin University(Earth Science Edition),2018,48(2):574-586.
[2] 龙天祥,何小虎,刘飞,等.长安金矿区碱性岩锆石U-Pb年代学、微量元素、Hf同位素特征及其地质意义[J].吉林大学学报(地球科学版),2019,49(6):1607-1627. Long Tianxiang,He Xiaohu,Liu Fei,et al.Zircon U-Pb Geochronology,Trace Element,Hf Isotope of Alkaline Rochs from Chang'an Gold Deposit and Its Geological Implication[J].Journal of Jilin University(Earth Science Edition),2019,49(6):1607-1627.
[3] 王建中,李建威,赵新福,等.铜陵地区朝山矽卡岩型金矿床及含矿岩体的成因:⁴⁰Ar/³⁹Ar年龄、元素地球化学及多元同位素证据[J].岩石学报,2008,24(8):1875-1888. Wang Jianzhong,Li Jianwei,Zhao Xinfu,et al. Genesis of the Chaoshan Gold Deposit and Its Host Intrusion,Tongling Area:Constraints from ⁴⁰Ar/³⁹Ar Ages and Elemental and Sr-Nd-O-C-S Isotope Geochemistry[J]. Acta Petrologica Sinica,2008,24(8):1875-1888.
[4] 谢建成,杨晓勇,肖益林,等.铜陵矿集区中生代侵入岩成因及成矿意义[J].地质学报,2012,86(3):423-459. Xie Jiancheng,Yang Xiaoyong,Xiao Yilin,et al.Petrogenesis of the Mesozoic Intrusive Rocks from the Tongling Ore Cluster Region:The Metallogenic Significance[J].Acta Geologica Sinica,2012,86(3):423-459.
[5] 施珂,杨晓勇,杜建国,等.安徽铜陵杨冲里金矿床成矿流体特征与成矿模式探讨[J].岩石学报,2019,35(12):3734-3748. Shi Ke,Yang Xiaoyong,Du Jianguo,et al.Study on Fluid Characteristics and Discussion on Its Metallogenic Model of Yangchongli Gold Deposit in the Tongling,Anhui Province[J].Acta Petrologica Sinica,2019,35(12):3734-3748.
[6] 杨爱雪,孙德有,张继林,等.冀东峪耳崖金矿区闪长岩脉的锆石U-Pb年龄测定[J].黄金,2016,37(8):14-18. Yang Aixue,Sun Deyou,Zhang Jilin,et al.Zircon U-Pb Dating of Diorite Dikes from Yu'erya Gold District in Eastern Hebei Province[J].Gold,2016,37(8):14-18.
[7] Song Y,Jiang S H,Bagas L,et al. The Geology and Geochemistry of Jinchangyu Gold Deposit,North China Craton:Implications for Metallogenesis and Geodynamic Setting[J].Ore Geology Reviews,2016,73:313-329.
[8] 杨付领,牛宝贵,任纪舜,等.马兰峪背斜核部中生代侵入岩体锆石U-Pb年龄、地球化学特征及其构造意义[J].地球学报,2015,36(4):445-465. Yang Fuling,Niu Baogui,Ren Jishun,et al. Zircon U-Pb Ages and Geochemical Characteristics of the Mesozoic Intrusive Bodies Along the Core of the Malanyu Anticline and Their Tectonic Significances[J]. Acta Geoscientica Sinica,2015,36(4):445-465.
[9] Xu P,Wu F Y,Xie L W,et al.Hf Isotopic Compositions of the Standard Zircons for U-Pb Dating[J].Chinese Science Bulletin,2004,49(15):1642-1648.
[10] Wu F Y,Yang Y H,Xie L W,et al.Hf Isotopic Compositions of the Standard Zircons and Baddeleyites Used in U-Pb Geochronology[J].Chemical Geology,2006,234(1/2):105-126.
[11] 彭头平,王岳军,范蔚茗,等.南太行山闪长岩的SHRIMP锆石U-Pb年龄及岩石成因研究[J].岩石学报,2004,20(5):1253-1262. Peng Touping,Wang Yuejun,Fan Weiming,et al.SHRIMP Zircon U-Pb Geochronology of the Giorites for Southern Taihang Mountains in the North China Interior and Its Petrogenesis[J].Acta Petrologica Sinica,2004,20(5):1253-1262.
[12] 陈艳,张招崇,朱江.河南省安林矽卡岩型铁矿的成岩时代和成矿物质来源探讨[J].岩石学报,2014,30(5):1307-1321. Chen Yan,Zhang Zhaochong,Zhu Jiang.Geochronology of the Anlin Iron Skarn Deposit,Henan Province and Insight into the Sources of Iron.[J].Acta Petrologica Sinica,2014,30(5):1307-1321.
[13] 钱青,钟孙霖,李通艺,等.八达岭基性岩和高Ba-Sr花岗岩地球化学特征及成因探讨:华北和大别-苏鲁造山带中生代岩浆岩的对比[J].岩石学报,2002,18(3):275-292. Qian Qing,Zhong Sunlin, Li Tongyi,et al.Geochemical Characteristics and Petrogenesis of the Badaling High Ba-Sr Granitoids:A Comparison of Igneous Rocks from North China and the Dabie-Sulu Orogen[J].Acta Petrologica Sinica,2002,18(3):275-292.
[14] Yang J H,Wu F Y,Chung S L,et al. A Hybrid Origin for the Qianshan A-Type Granite,Northeast China:Geochemical and Sr-Nd-Hf Isotopic Evidence[J]. Lithosphere,2006,89:89-106.
[15] 张旗,王焰,熊小林,等.埃达克岩和花岗岩:挑战与机遇[M].北京:中国大地出版社,2008. Zhang Qi,Wang Yan,Xiong Xiaolin,et al. Adakite and Granite:Challenges and Opportunities[M].Beijing:China Land Press,2008.
[16] 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):891-93l.
[17] 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,1999,157:119-146.
[18] Gill J B.Orogenic Andesites and Plate Tectonics[M].Berlin:Springer Verlag,1981:385.
[19] Mecdonald R,Rogers N W,Fitton J G.Plume Lithosphere Interactions in the Generation of the Basalts of the Kenys Rift,East Africa[J].Journal of Petrology,2001,42:877-900.
[20] Goswami T K.Subduction Related Magmatism:Constrainsfrom the REE Pattern in the Lohit Batholith,Arunachal Pradesh,India[J]. Geosciences,2013,3(4):128-141.
[21] Rottura A,Bargossi G M,Caggianelli A,et al. Origin and Significance of the Permian High-K Cale-Alkaline Magmatism in the Centrl-Eastern Southern Alps[J].Lithosphere,1998,45(1/2/3/4):345-348.
[22] 孙熠.河北邯邢地区早白垩世岩浆作用及成矿意义[D].武汉:中国地质大学(武汉),2016. Sun Yi.Petrogenesis and Mineralization of the Early Cretaceous Intrusive Rocks in Handan-Xingtai Area,Hebei Province,China[D].Wuhan:China University of Geosciences (Wuhan),2016.
[23] Louro V H A,Cawood P A,Mantovani M S M,et al.Tectonic Insights of the Southwest Amazon Craton from Geophysical,Geochemical and Mineralogical Data of Figueira Branca Mafic-Ultramafic Suite, Brazil[J]. Tectonophysics,2017,708:96-107.
[24] 陈绍聪,叶会寿,王义天,等.冀东峪耳崖金矿床辉钼矿Re-Os年龄及其地质意义[J].中国地质,2014,41(5):1565-1576. Chen Shaocong,Ye Huishou,Wang Yitian,et al. Re-Os Age of Molybdenite from the Yu'erya Au Deposit in Eastern Hebei Province and Its Geological Significance[J]. Geology in China,2014,41(5):1565-1576.
[25] 陈绍聪,叶会寿,王义天,等.冀东峪耳崖金矿床蚀变绢云母⁴⁰Ar-³⁹Ar年龄及其地质意义[J].矿床地质,2019,38(3):557-570. Chen Shaocong,Ye Huishou,Wang Yitian,et al.⁴⁰Ar-³⁹Ar Age of Altered Sericite from Yu'erya Au Deposit in Eastern Hebei Province and Its Geological Significance[J]. Mineral Deposits,2019,38(3):557-570.
[26] 姚凤良,孙丰月.矿床学教程[M].北京:地质出版社,2006. Yao Fengliang,Sun Fengyue. A Course in Mineralogy[M]. Beijing:Geological Publishing House,2006.
[27] 唐杰,许文良,王枫,等.古太平洋板块在欧亚大陆下的俯冲历史:东北亚陆缘中生代-古近纪岩浆记录[J].中国科学:地球科学,2018,48(5):549-583. Tang Jie,Xu Wenliang,Wang Feng,et al. Subduction History of the Paleo-Pacific Slab Beneath Eurasian Continent:Mesozoic-Paleogene Magmatic Records in Northeast Asia[J].Science China:Earth Sciences,2018,48(5):549-583.
[28] 马强.辽西三叠纪-侏罗纪火山岩:华北北缘东段下地壳再造与克拉通破坏[D].武汉:中国地质大学(武汉),2013. Ma Qiang.Triassic-Jurassic Volcanic Rocks in Western Liaoning Implications for Lower Crustal Reworking and Lithospheric Destruction in the North Part of Eastern North China Craton[D].Wuhan:China University of Geosciences (Wuhan),2013.
[29] 何泽宇,申俊峰,王来明,等.胶东宋家沟金矿中基性脉岩锆石U-Pb年代学、地球化学及其地质意义[J].世界地质,2020,39(3):509-527. He Zeyu,Shen Junfeng,Wang Laiming,et al.LA-ICP-MS U-Pb Dating,Geochemistry and Geological Implications of Intermediate-Mafic Dikes in Songjiagou Gold Deposit,Eastern Shandong Province[J]. Global Geology,2020,39(3):509-527.
[30] 李洪奎,李大鹏,耿科,等.胶东地区燕山期岩浆活动及其构造环境:来自单颗锆石SHRIMP年代学的记录[J].地质学报,2017,91(1):163-179. Li Hongkui,Li Dapeng,Geng Ke,et al. The Mesozoic Magmaticactivities Framework in Jiaodong Area:SHRIMP Chronology Recording of Single Particle Zircon[J].Acta Geologica Sinica,2017,91(1):163-179.

Metrics

Viewed

Full text

Abstract

Cited

Shared

Discussed

冀东峪耳崖金矿区闪长岩脉地球化学特征及其地质意义

Geochemical Characteristics and Geological Significance of Diorite of Yu'erya Gold Deposit Area in Eastern Hebei Province

PDF (PC)

摘要/Abstract

引用本文

使用本文

参考文献

相关文章 15

Metrics

本文评价

推荐阅读 10

[1]	任宪军, 石云倩. 松辽盆地南部下白垩统火石岭组钙碱性火山岩地球化学特征及成因[J]. 吉林大学学报(地球科学版), 2026, 56(3): 818-834.
[2]	王常东, 董小宇, 郝晓飞, 姜山, 于兵, 周舰, 王天奇. 广兴—芝瑞盆地上伙房地段流纹斑岩地球化学特征及其地质意义[J]. 吉林大学学报(地球科学版), 2026, 56(3): 835-851.
[3]	刘宇泰, 李碧乐, 陈晓琳, 李浩然, 史雨凡, 孙亚明. 东昆仑沟里地区瓦勒尕南矿区花岗闪长岩地球化学特征、锆石U-Pb年代学及其地质意义[J]. 吉林大学学报(地球科学版), 2026, 56(3): 875-895.
[4]	孙文博, 苟军, 王世成, 王常东, 王广婷, 孙家兴, 张铎, 田丽, 孙德有. 大兴安岭南部白音沙那盆地中生代火山岩年代学及岩石成因[J]. 吉林大学学报(地球科学版), 2026, 56(3): 852-874.
[5]	张海洪, 乔锦燃, 陈国强, 薛晓刚, 邓馨卉, 苗长盛, 李雪, 郜春生. 张广才岭南部早侏罗世两类I型花岗岩成因：年代学、地球化学和锆石Hf同位素证据[J]. 吉林大学学报(地球科学版), 2026, 56(3): 896-914.
[6]	赵振, 秦光雄, 闫佰忠, 马苗苗. 青海省互助土族自治县地热田水化学特征及成因机制[J]. 吉林大学学报(地球科学版), 2026, 56(3): 986-1001.
[7]	何天鑫, 柳蓉, 刘强浩, 宁婷, . 银额盆地下白垩统巴音戈壁组纤维状方解石脉成因机制——热水沉积与同位素证据[J]. 吉林大学学报(地球科学版), 2026, 56(2): 497-510.
[8]	李阳, 周文博, 王长虹, 刘娜, 苟军, 孙文博, 孙家兴, 孙德有. 海拉尔盆地克鲁伦凹陷赋铀地层沉积物源#br#[J]. 吉林大学学报(地球科学版), 2026, 56(2): 522-539.
[9]	徐骏, 高阳, 刘军, 王晓彤, . 大兴安岭北段三矿沟铁铜矿床成因——来自石榴子石U-Pb定年及元素地球化学证据[J]. 吉林大学学报(地球科学版), 2026, 56(2): 540-556.
[10]	张佳琦, 王志新, 梁琛岳, 郑常青, 刘永江. 吉中地区范家屯组变沉积岩碎屑锆石年代学与Hf同位素示踪——对古亚洲洋东段闭合的约束[J]. 吉林大学学报(地球科学版), 2026, 56(1): 149-172.
[11]	高心如, 梁琛岳, 郑常青, 刘永江, 周建波, 宋志伟, 贾祥鹤, 殷浚哲, 洪雨萱, 谭卓, 张佳琦. 蒙古—鄂霍茨克构造域东段晚中生代演化历史——来自岩浆岩和沉积岩的证据[J]. 吉林大学学报(地球科学版), 2026, 56(1): 36-65.
[12]	陈卓, 周建波, 李功宇, 辛中华, 王红燕, 孙宁辰. 北方造山带东段微陆块构造属性与超大陆重建[J]. 吉林大学学报(地球科学版), 2026, 56(1): 1-16.
[13]	柳蓉, 何天鑫, 张浩然, 刘强浩, 张苡铭. 中国典型含油气盆地热液作用及其对沉积环境的影响[J]. 吉林大学学报(地球科学版), 2025, 55(6): 1785-1805.
[14]	张万仁, 吴保祥, 韦枫, 杨维刚, 刘杰. 甘肃省宕昌—崖湾地区水系沉积物地球化学特征与锑找矿预测[J]. 吉林大学学报(地球科学版), 2025, 55(5): 1462-1480.
[15]	郑伟, 刘东宏, 吴晓东, 孙煜恒, 邢波. 粤西石菉Cu-Mo矿床石榴子石与符山石地球化学特征及其对成矿流体演化的制约[J]. 吉林大学学报(地球科学版), 2025, 55(5): 1481-1505.