吉林大学学报(地球科学版) ›› 2020, Vol. 50 ›› Issue (5): 1418-1432.doi: 10.13278/j.cnki.jjuese.20190293
• 整装勘查区矿床成因与成矿作用研究专辑 • 上一篇 下一篇
康凯1, 杜泽忠2,3, 于晓飞2,3, 李永胜2,3, 吕鑫2,3, 孙海瑞2,3, 杜轶伦2,3
Kang Kai1, Du Zezhong2,3, Yu Xiaofei2,3, Li Yongsheng2,3, Lü Xin2,3, Sun Hairui2,3, Du Yilun2,3
摘要: 天山—北山铅锌成矿带位于中亚造山带、塔里木板块和华北板块的交汇地带,是我国西北地区重要的金属资源产地之一。花牛山铅锌矿是天山—北山地区具典型成因意义的铅锌矿床,矿床成因机制一直存在争议。本文通过LA-ICP-MS对其闪锌矿微量组成进行分析,结果表明:该矿床闪锌矿形成于中—高温环境,以富集Fe、Mn、In、Cd、Cu等元素,贫Ga、Ge、Ni等元素为特征,其中Fe、Mn、In、Cd、Cu以类质同象的形式赋存于闪锌矿中,Ag、Pb以显微包裹体的形式赋存于闪锌矿中;其微量元素组成与岩浆热液为主导的矿床(都龙、黄岗梁、孟恩陶勒盖、赤土店)类似,除此之外,闪锌矿Tl元素质量分数以及Cd/Fe和Cd/Mn值均显示岩浆热液属性,在微量元素判别图中样品也落入岩浆热液区域。野外调研发现,矿体底部未见角砾状和网脉状矿体,矿体均发育在岩性界面及层间破碎带中。结合矿床地质特征、闪锌矿微量元素地球化学特征,认为花牛山铅锌矿床成因类型属于中高温岩浆热液型。
中图分类号:
[1] 聂凤军. 北山地区金属矿床成矿规律及找矿方向[M]. 北京:地质出版社,2002. Nie Fengjun. Metallogenic Regularity and Prospecting Direction of Metal Deposits in Beishan Area[M]. Beijing:Geological Publishing House, 2002. [2] 曹亮,陕亮,张雨莲. 北山地区铅锌矿成矿类型及找矿方向[J]. 资源环境与工程, 2008,22(1):26-31. Cao Liang, Shan Liang, Zhang Yulian. Metallogenetic Types of Lead-Zinc Deposit and Prospecting Direction in Beishan Area[J]. Resources Environment and Engineering, 2008,22(1):26-31. [3] 丁建华,程松林,陈兴华,等. 新疆东天山铅锌矿成矿规律及区域预测[J]. 地质通报,2010, 29(10):1504-1511. Ding Jianhua, Cheng Songlin, Chen Xinghua, et al. Metallogenic Rules and Regional Prediction of Lead-Zinc in Eastern Tianshan Area, China[J]. Geological Bulletin of China, 2010, 29(10):1504-1511. [4] 何智祖. 甘肃北山花牛山一带铅锌金矿床地质特征及找矿思路[J]. 甘肃科技,2015, 31(15):19-22, 71. He Zhizu. Geological Characteristics and Prospecting Ideas of Lead-Zinc Gold Deposit in Huaniushan Area, North Gansu Province[J]. Gansu Science and Technology, 2015, 31(15):19-22, 71. [5] 代文军. 甘肃北山花牛山金银铅锌矿床成因探讨[J]. 华南地质与矿产,2010(3):25-34. Dai Wenjun.Metallogenic Study of Huaniushan Au-Ag-Pb-Zn Deposit, Beishan Area, Gansu Province[J]. Geology and Mineral Resources of South China, 2010(3):25-34. [6] 杨建国,翟金元,杨宏武,等. 甘肃北山地区花牛山铅锌矿区玄武岩锆石LA-ICP-MS U-Pb定年及其地质意义[J]. 地质通报,2010, 29(7):1017-1023. Yang Jianguo, Zhai Jinyuan, Yang Hongwu, et al. LA-ICP-MS Zircon U-Pb Dating of Basalt and Its Geological Significance in Huaniushan Pb-Zn Deposit, Beishan Area, Gansu, China[J]. Geological Bulletin of China, 2010, 29(7):1017-1023. [7] 杨建国,翟金元,杨宏武,等. 甘肃花牛山喷流沉积型金银铅锌矿床控矿因素与找矿前景分析[J]. 大地构造与成矿学,2010, 34(2):246-254. Yang Jianguo, Zhai Jinyuan, Yang Hongwu, et al. Metallotectonics and Prospection of the Huaniushan Exhalogene Gold-Silver-Lead-Zinc Deposit in Beishan, Gansu Province[J]. Geotectonica et Metallogenia, 2010, 34(2):246-254. [8] 朱江,吕新彪,曹晓峰,等. 甘肃花牛山铅锌金矿床地质特征及成矿物质来源[J]. 矿床地质,2010, 29(增刊1):1033-1034. Zhu Jiang,Lü Xinbiao, Cao Xiaofeng, et al. Geological Characteristics and Metallogenic Material Sources of Lead-Zinc Gold Deposit in Huaniushan Gansu Province[J]. Mineral Deposits, 2010, 29(Sup.1):1033-1034. [9] 朱江. 北山造山带南带构造-岩浆建造与金多金属成矿[D]. 武汉:中国地质大学,2013. Zhu Jiang. Tectono-Magmatic Formation and Gold-Polymetallic Mineralization in South Beishan Area, NW China[D]. Wuhan:China University of Geosciences, 2013. [10] 李增达. 甘肃花牛山铅锌银多金属矿田岩浆成矿作用与找矿[D]. 北京:中国地质大学(北京),2018. Li Zengda. Magmatic Mineralization and Prospecting of the Huaniushan Lead-Zinc-Silver Polymetallic Ore Field in Gansu Province, China[D]. Beijing:China University of Geosciences (Beijing), 2018. [11] Ute M, Norbert B, Peter H. Mineralogical and Geochemical Features of Sulfide Chimneys from the MESO Zone, Central Indian Ridge[J]. Chemical Geology, 1999, 155(1):29-44. [12] Yang Xueming, Lentz D R, Sylvester P J. Gold Contents of Sulfide Minerals in Granitoids from Southwestern New Brunswick, Canada[J]. Mineralium Deposita, 2006, 41(4):369-386. [13] Zhang Q. Trace Elements in Galena and Sphalerite and Their Geochemical Significance in Distinguishing the Genetic Types of Pb-Zn Ore Deposits[J]. Chinese Journal of Geochemistry, 1987, 6:177-190. [14] Huston D L, Sie S H, Suter G F, et al. Trace Elements in Sulfide Minerals from Eastern Australian Volcanic-Hosted Massive Sulfide Deposits:Part I:Proton Microprobe Analyses of Pyrite, Chalcopyrite, and Sphalerite, and Part II:Selenium Levels in Pyrite; Comparison with δ34S Values and Implications for the Source of Sulfur in Volcanogenic Hydrothermal Systems[J]. Economic Geology, 1995, 90:1167-1196. [15] Beaudoin G. Acicular Sphalerite Enriched in Ag, Sb, and Cu Embedded Within Colour Banded Sphalerite from the Kokanee Range, BC[J]. Canadian Mineralogist, 2000, 38:1387-1398. [16] 涂光炽,高振敏,胡瑞忠. 分散元素地球化学及成矿机制[M]. 北京:地质出版社, 2003:1-424. Tu Guangchi, Gao Zhenmin, Hu Ruizhong, et al. Geochemistry and Mineralization Mechanism of Dispersed Elements[M]. Beijing:Geological Publishing House, 2003:1-424. [17] 邹志超,胡瑞忠,毕献武,等. 滇西北兰坪盆地李子坪铅锌矿床微量元素地球化学特征[J].地球化学,2012, 41(5):482-496. Zou Zhichao, Hu Ruizhong, Bi Xianwu, et al. Trace Element Geochemistry of the Liziping Pb-Zn Deposit, the Lanping Basin, Northwest Yunnan Province, China[J]. Geochimica, 2012, 41(5):482-496. [18] 李珍立,叶霖,黄智龙,等. 贵州天桥铅锌矿床闪锌矿微量元素组成初探[J]. 矿物学报,2016, 36(2):183-188. Li Zhenli, Ye Lin, Huang Zhilong, et al. Primary Research on Trace Elements in Sphalerite from Tianqiao Pb-Zn Deposit, Northwestern Guizhou Province, China[J]. Acta Mineralogica Sinica, 2016, 36(2):183-188. [19] 陈翠华,宋志娇,杨玉龙,等. 贵州习水洞子沟铅锌矿床闪锌矿微量元素特征与成因[J]. 矿物学报, 2019(5):485-493. Chen Cuihua, Song Zhijiao, Yang Yulong, et al. The Trace Elements Characteristics of Sphalerite and Genetic Analysis of Dongzigou Lead-Zinc Deposit in Xishui County, Guizhou Province[J]. Acta Mineralogica Sinica, 2019(5):485-493. [20] Cook N J, Ciobanu C L,Pring A, et al. Trace and Minor Elements in Sphalerite:A LA-ICPMS Study[J]. Geochimica et Cosmochimica Acta, 2009, 73(16):4761-4791. [21] Cook N J, Ciobanu C L, Williams T. The Mineralogy and Mineral Chemistry of Indium in Sulphide Deposits and Implications for Mineral Processing[J]. Hydrometallurgy, 2011, 108(3/4):226-228. [22] Cook N J, Sundblad K, Valkama M, et al. Indium Mineralisation in A-Type Granites in Southeastern Finland:Insights into Mineralogy and Partitioning Between Coexisting Minerals[J]. Chemical Geology, 2011, 284(1/2):62-73. [23] Ye L, Cook N J, Ciobanu C L, et al. Trace and Minor Elements in Sphalerite from Base Metal Deposits in South China:A LA-ICPMS Study[J]. Ore Geology Reviews, 2011, 39(4):188-217. [24] 周涛发,张乐骏,袁峰,等. 安徽铜陵新桥Cu-Au-S矿床黄铁矿微量元素LA-ICP-MS原位测定及其对矿床成因的制约[J]. 地学前缘,2010, 17(2):306-319. Zhou Taofa, Zhang Lejun, Yuan Feng, et al. LA-ICP-MS in Situtrace Element Analysis of Pyrite from the Xinqiao Cu-Au-S Deposit in Tongling, Anhui, and Its Constraints on the Ore Genesis[J]. Earth Science Frontiers, 2010, 17(2):306-319. [25] 叶霖,杨玉龙,鲍谈. 不同类型铅锌矿床中闪锌矿微量元素组成特征:以LA-ICPMS分析测试为例[J].矿床地质,2012,31(增刊1):985-986. Ye Lin, Yang Yulong, Bao Tan, et al. Geological Characteristics and Metallogenic Material Composition Characteristics of Sphalerite in Different Types of Lead-Zinc Deposits:A Case Study of LA-ICPMS Analysis and Test[J]. Mineral Deposits, 2012, 31(Sup.1):985-986. [26] 叶霖,高伟,杨玉龙,等. 云南澜沧老厂铅锌多金属矿床闪锌矿微量元素组成[J]. 岩石学报,2012,28(5):1362-1372. Ye Lin, Gao Wei, Yang Yulong, et al. Trace Elements in Sphalerite in Laochang Pb-Zn Polymetallic Deposit, Lancang, Yunnan Province[J]. Acta Petrologica Sinica, 2012, 28(5):1362-1372. [27] 叶霖,李珍立,胡宇思,等. 四川天宝山铅锌矿床硫化物微量元素组成:LA-ICPMS研究[J].岩石学报,2016,32(11):3377-3393. Ye Lin,Li Zhenli,Hu Yusi, et al. Trace Elements in Sulfide from the Tianbaoshan Pb-Zn Deposit,Sichuan Province, China:A LA-ICPMS Study[J]. Acta Petrologica Sinica, 2016, 32(11):3377-3393. [28] 胡鹏,吴越,张长青,等. 扬子板块北缘马元铅锌矿床闪锌矿LA-ICP-MS微量元素特征与指示意义[J]. 矿物学报,2014, 34(4):461-468. Hu Peng, Wu Yue, Zhang Changqing, et al. Trace and Minor Elements in Sphalerite from the Mayuan Lead-Zinc Deposit, Northern Margin of the Yangtze Plate:Implications from LA-ICP-MS Analysis[J]. Acta Mineralogica Sinica, 2014, 34(4):461-468. [29] 张乐骏,周涛发. 矿物原位LA-ICPMS微量元素分析及其在矿床成因和预测研究中的应用进展[J]. 岩石学报,2017, 33(11):3437-3452. Zhang Lejun, Zhou Taofa. Minerals In-Situ LA-ICPMS Trace Elements Study and the Applications in Ore Deposit Genesis and Exploration[J]. Acta Petrologica Sinica, 2017, 33(11):3437-3452. [30] 徐卓彬,邵拥军,杨自安,等.内蒙古黄岗梁铁锡矿床闪锌矿LA-ICP-MS微量元素组成及其指示意义[J]. 岩石矿物学杂志,2017, 36(3):360-370. Xu Zhuobin, Shao Yongjun, Yang Zi'an, et al. LA-ICP-MS Analysis of Trace Elements in Sphalerite from the Huanggangliang Fe-Sn Deposit, Inner Mongolia, and Its Implications[J]. Acta Petrologica et Mineralogica, 2017, 36(3):360-370. [31] 冷成彪,齐有强. 闪锌矿与方铅矿的LA-ICPMS微量元素地球化学对江西冷水坑银铅锌矿田的成因制约[J]. 地质学报,2017, 91(10):2256-2272. Leng Chengbiao, Qi Youqiang. Genesis of the Lengshuikeng Ag-Pb-Zn Orefield in Jiangxi:Constraint from In-Situ LA-ICPMS Analyses of Minor and Trace Elements in Sphalerite and Galena[J]. Acta Geologica Sinica, 2017, 91(10):2256-2272. [32] 张辉善,李艳广,全守村,等. 阿尔金喀腊达坂铅锌矿床金属硫化物元素地球化学特征及其对成矿作用的制约[J]. 岩石学报,2018, 34(8):2295-2311. Zhang Huishan, Li Yanguang, Quan Shoucun, et al. Geochemical Characteristics of Metallic Sulfides from the Kaladaban Deposit in Xinjiang and Its Implications for Pb-Zn Ore-Forming Mechanism[J]. Acta Petrologica Sinica, 2018, 34(8):2295-2311. [33] 毛启贵. 北山及邻区古生代-早中生代增生与碰撞大地构造格局[D]. 北京:中国科学院大学,2008. Mao Qigui. Paleozoic to Early Mesozoic Accretionary and Collisional Tectonics of the Beishan and Adjacent Area Northwest China[D]. Beijing:University of Chinese Academy of Sciences, 2008. [34] 张洲远. 甘肃北山花牛山金矿地质特征和成矿类型研究[D]. 西安:长安大学,2016. Zhang Zhouyuan. Geological Characteristics and Metallogenic Type Research of Huaniushan Gold Deposit in Beishan Area Gansu Province[D]. Xi'an:Chang'an University, 2016. [35] Zong K Q, Klemd R, Yuan Y, et al. The Assembly of Rodinia:The Correlation of Early Neoproterozoic (ca 900 Ma) High-Grade Metamorphism and Continental Arc Formation in the Southern Beishan Orogen, Southern Central Asian Orogenic Belt (CAOB)[J]. Precambrian Research, 2017, 290:32-48. [36] Hu Z C, Zhang W, Liu Y S, et al. "Wave" Signal Smoothing and Mercury Removing Device for Laser Ablation Quadrupole and Multiple Collector ICP-MS Analysis:Application to Lead Isotope Analysis[J]. Analytical Chemistry, 2015, 87:1152-1157. [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 Internalstandard[J]. Chemical Geology, 2008, 257:34-43. [38] Maslennikov V V, Maslennikova S P, Large R R, et al. Study of Trace Element Zonation Invent Chimneys from the Silurian Yaman-Kasy Volcanic-Hosted Massive Sulfide Deposit (Southern Urals, Russia) Using Laser Ablation-Inductively Coupled Plasma Mass Spectrometry (LA-ICPMS)[J]. Economic Geology, 2009,104(8):1111-1141. [39] Maydagán L, Franchini M B, Lentz D, et al. Sulfide Composition and Isotopic Signature of the Altar Cu-Au Deposit, Argentina:Constraints on the Evolution of the Porphyryepithermal System[J]. The Canadian Mineralogist, 2013,51(6):813-840. [40] 刘英俊,曹励明,李兆嶙,等. 元素地球化学[M]. 北京:科学出版社,1984:187-193. Liu Yingjun, Cao Liming, Li Zhaolin, et al. Element Geochemistry[M]. Beijing:Science Press,1984:187-193. [41] 韩照信. 秦岭泥盆系铅锌成矿带中闪锌矿的标型特征[J]. 西安工程学院学报,1994(1):12-17. Han Zhaoxin. The Typomorphic Characteristic of the Sphalerite in the Qinling Devonian System Lead-Zinc Metallogenic Belt[J]. Journal of Xi'an Engineering University, 1994(1):12-17. [42] 刘锦康,邓明国,李余华,等.滇西勐兴铅锌矿床闪锌矿ICP-MS微量元素特征及其地质意义[J]. 矿物岩石地球化学通报,2020, 39(1):133-143. Liu Jinkang, Deng Mingguo, Li Yuhua,et al. The ICP-MS Trace Element Characteristics of Sphalerites from the Mengxing Pb-Zn Deposit, Western Yunnan and Their Geological Significances[J]. Bulletin of Mineralogy, Petrology and Geochemistry, 2020, 39(1):50-59. [43] 曹华文,张寿庭,郑硌,等. 河南栾川矿集区中鱼库(铅)锌矿床闪锌矿微量元素地球化学特征[J]. 矿物岩石,2014, 34(3):50-59. Cao Huawen, Zhang Shouting, Zheng Luo, et al. Geochemical Characteristics of Trace Element of Sphalerite in the Zhongyuku (Pb)-Zn Deposit of the Luanchuan,Southwest of China[J]. Journal of Mineralogy and Petrology, 2014, 34(3):50-59. [44] 朱赖民,袁海华,栾世伟. 金阳底苏会东大梁子铅锌矿床内闪锌矿微量元素标型特征及其研究意义[J]. 四川地质学报,1995, 1:49-55. Zhu Laimin, Yuan Haihua, Luan Shiwei, et al. Trace Element Type Characteristics of Sphalerite in Dongdaliangzi Lead-Zinc Deposit in Jinyang Disuhui and Its Research Significance[J]. Acta Geologica Sichuan, 1995, 1:49-55. [45] 杨敏之. 闪锌矿的颜色及其对寻找分散元素的意义[J]. 地质月刊,1958(4):22-29. Yang Minzhi. The Color of Sphalerite and Its Significance for the Search for Dispersed Elements Geology in China, 1958(4):22-29. [46] 张铭杰,梁收运,吴茂炳. 花牛山铅锌矿床成因的矿物学研究[J]. 甘肃地质学报,1998, 7(2):93-98. Zhang Mingjie, Liang Shouyun, Wu Maobing. A Mineralogical Study on the Genesis of Huaniushan Lead-Zinc Deposit[J]. Gansu Geology, 1998, 7(2):93-98. [47] 张乾. 利用方铅矿、闪锌矿的微量元素图解法区分铅锌矿床的成因类型[J]. 地质地球化学,1987(9):64-66. Zhang Qian. Distinguish the Genetic Type of Lead-Zinc Deposits by Trace-Element Diagrams of Galena and Sphalerite[J]. Geology and Geochemistry, 1987(9):64-66. [48] 金露英,秦克章,李光明,等. 大兴安岭北段岔路口斑岩Mo-热液脉状Zn-Pb成矿系统硫化物微量元素的分布、起源及其勘探指示[J]. 岩石学报, 2014, 31(8):2417-2434. Jin Luying,Qin Kezhang,Li Guangming, et al. Trace Element Distribution in Sulfides from the Chalukou Porphyry Mo-Vein-Type Zn-Pb System, Northern Great Xing'an Range, China:Implications for Metal Source and Ore Exploration[J]. Acta Petrologica Sinica, 2014, 31(8):2417-2434. [49] 叶霖,刘玉平,张乾,等. 云南都龙超大型锡锌多金属矿床中闪锌矿微量及稀土元素地球化学特征[J]. 吉林大学学报(地球科学版), 2017, 47(3):734-750. Ye Lin, Liu Yuping, Zhang Qian, et al. Trace and Rare Earth Elements Characteristics of Sphalerite in Dulong Super Large Sn-Zn Polymetallic Ore Deposit, Yunnan Province[J]. Journal of Jilin University (Earth Science Edtion), 2017, 47(3):734-750. [50] 张乾,刘志浩,战新志,等. 内蒙古孟恩陶勒盖银铅锌铟矿床的微量元素地球化学[J]. 矿物学报, 2004, 24(1):40-48. Zhang Qian, Liu Zhihao, Zhan Xinzhi, et al. Trace Element Geochemistry of Meng'entaolegai Ag-Pb-Zn-In Deposit, Inner Mongolia, China[J]. Acta Mineralogica Sinica, 2004, 24(1):40-48. [51] 田浩浩,张寿庭,曹华文,等. 豫西赤土店铅锌矿床闪锌矿微量元素地球化学特征[J]. 矿物岩石地球化学通报,2015, 34(2):334-342. Tian Haohao, Zhang Shouting, Cao Huawen, et al. Geochemical Characteristics of Trace Elements of Sphalerite in the Chitudian Pb-Zn Deposit, West Henan Province[J]. Bulletin of Mineralogy, Petrology and Geochemistry, 2015, 34(2):334-342. [52] 叶霖,刘铁庚. 富镉锌矿成矿流体地球化学研究:以贵州都匀牛角塘富镉锌矿为例[J]. 地球化学, 2000(6):597-603. Ye Lin, Liu Tiegeng. Geochemical Study on the Metallogenic Fluid of Cadmium-Rich Zinc Deposits:A Case Study of the Niujiaotang Cadmium-Rich Zinc Deposits in Duyun, Guizhou[J]. Geochimica, 2000(6):597-603. [53] 谢文安. 湖南层控与岩浆型铅锌矿床中闪锌矿的标型特征及其地质意义[J]. 地质地球化学,1982(2):57-60. Xie Wen'an. Sphalerite in Stratabound and Magmatic Lead-Zinc Deposits in Hunan Province[J]. Geology and Geochemistry, 1982(2):57-60. |
[1] | 范飞鹏, 肖惠良, 陈乐柱, 李海立, 刘建雄, 邓中林, 康丛轩, 林耿伟, 陈凯. 粤东莲花山地区多期岩浆锆石年代学、Hf同位素组成及其成矿作用[J]. 吉林大学学报(地球科学版), 2020, 50(5): 1462-1490. |
[2] | 郝宇杰, 商青青, 任云生, 刘小禾, 陈聪. LA-ICP-MS原位分析白钨矿稀土元素[J]. 吉林大学学报(地球科学版), 2020, 50(4): 1029-1041. |
[3] | 曹星星, 吴攀, 周少奇, 谢峰, 荣嵘. 酸性矿山排水影响的水库沉积物微量元素地球化学特征[J]. 吉林大学学报(地球科学版), 2020, 50(4): 1112-1126. |
[4] | 龙天祥, 何小虎, 刘飞, 李宗勇, 王玉朝, 赵俊, 李云飞, 王长兵, 曹原. 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. |
[5] | 杨帆, 汪岩, 那幅超, 付俊彧, 张广宇, 孙巍, 庞雪娇, 陈井胜, 刘淼, 李斌. 内蒙古白音诺尔铅锌矿床成矿时代及其地质意义——来自侵入岩地球化学及年代学的制约[J]. 吉林大学学报(地球科学版), 2018, 48(6): 1696-1710. |
[6] | 叶霖, 刘玉平, 张乾, 鲍谈, 何芳, 王小娟, 王大鹏, 蓝江波. 云南都龙超大型锡锌多金属矿床中闪锌矿微量及稀土元素地球化学特征[J]. 吉林大学学报(地球科学版), 2017, 47(3): 734-750. |
[7] | 张艳, 韩润生, 魏平堂, 邱文龙. 云南会泽矿山厂铅锌矿床流体包裹体特征及成矿物理化学条件[J]. 吉林大学学报(地球科学版), 2017, 47(3): 719-733. |
[8] | 刘锦, 刘正宏, 赵辰, 彭游博, 王楚杰, 杨仲杰, 豆世勇. 辽宁清河断裂以北新太古代变质表壳岩的发现及其地质意义[J]. 吉林大学学报(地球科学版), 2017, 47(2): 497-510. |
[9] | 张朋, 杨宏智, 李斌, 寇林林, 杨凤超. 辽东青城子矿集区姚家沟钼矿床成矿物质来源、成矿年代及成矿动力学背景[J]. 吉林大学学报(地球科学版), 2016, 46(6): 1684-1696. |
[10] | 孙珍军, 孙国胜, 于赫楠, 向柱, 田毅, 刘彤, 陈旭, 李杨. 赤峰撰山子花岗岩年代学、地球化学特征及其成岩动力学背景[J]. 吉林大学学报(地球科学版), 2016, 46(6): 1740-1753. |
[11] | 陈斌, 李壮, 王家林, 张璐, 鄢雪龙. 辽东半岛~2.2 Ga岩浆事件及其地质意义[J]. 吉林大学学报(地球科学版), 2016, 46(2): 303-320. |
[12] | 韩润生, 李波, 倪培, 邱文龙, 王旭东, 王天刚. 闪锌矿流体包裹体显微红外测温及其矿床成因意义——以云南会泽超大型富锗银铅锌矿床为例[J]. 吉林大学学报(地球科学版), 2016, 46(1): 91-104. |
[13] | 田陟贤, 李永军, 田猛, 杨高学, 向坤鹏, 佟丽莉. 西准噶尔恰达地区哈尔加乌组火山岩锆石U-Pb年代学、地球化学及地质意义[J]. 吉林大学学报(地球科学版), 2016, 46(1): 135-145. |
[14] | 秦亚, 张青伟, 康志强, 李赛赛, 冯佐海, 杨启军, 庞保成, 白令安, 谢永彬, 叶鸣. 桂东大瑶山成矿带花岗岩类岩石年代学格架的厘定[J]. 吉林大学学报(地球科学版), 2015, 45(6): 1735-1756. |
[15] | 宋樾, 王建, 刘金霖, 包真艳. 西昆仑慕士塔格—公格尔印支期侵入岩岩石与锆石地球化学特征及研究意义[J]. 吉林大学学报(地球科学版), 2015, 45(5): 1418-1435. |
|