鲁西金岭地区含矿闪长岩体成因:来自锆石U-Pb年代学和地球化学证据

doi:10.13278/j.cnki.jjuese.201706112

吉林大学学报(地球科学版) ›› 2017, Vol. 47 ›› Issue (6): 1732-1745.doi: 10.13278/j.cnki.jjuese.201706112

鲁西金岭地区含矿闪长岩体成因:来自锆石U-Pb年代学和地球化学证据

张超¹, 崔芳华¹, 张照录¹, 耿瑞², 宋明春³

1. 山东理工大学资源与环境工程学院, 山东淄博 255049;
2. 山东黄金集团有限公司, 济南 255014;
3. 山东省地质矿产勘查开发局, 济南 255013

收稿日期:2017-03-07 出版日期:2017-11-26 发布日期:2017-11-26
通讯作者: 崔芳华(1986),女,讲师,主要从事矿物和岩石成因方面的研究,E-mail:shadow20052009@163.com E-mail:shadow20052009@163.com
作者简介:张超(1986),男,讲师,主要从事岩浆活动与构造运动方面的研究,E-mail:bosewell@163.com
基金资助:
山东省中青年科学家科研奖励基金项目（ZR2016DB08）；泰山学者工程专项经费（ts201511076）

Petrogenesis of Ore-Bearing Dioritic Pluton in Jinling Area in Western Shandong:Evidence from Zircon U-Pb Chronology and Petro-Geochemistry

Zhang Chao¹, Cui Fanghua¹, Zhang Zhaolu¹, Geng Rui², Song Mingchun³

1. School of Resources and Environmental Engineering, Shandong University of Technology, Zibo 255049, Shandong, China;
2. Shandong Gold Group Co. LTD, Jinan 255014, China;
3. Shandong Bureau of Geology and Mineral Resources Exploration and Development, Jinan 255013, China

Received:2017-03-07 Online:2017-11-26 Published:2017-11-26
Supported by:
Supported by the Young Scientists Fund of Shandong Province(ZR2016DB08) and Taishan Scholar Special Project Funds(ts201511076)

摘要/Abstract

摘要： 鲁西金岭闪长岩位于华北克拉通东南部，主要由辉石闪长岩-黑云母闪长岩组成。LA-ICP-MS锆石U-Pb定年测定闪长岩侵位年龄为（129.17±0.96）和（130.15±0.65） Ma，属于早白垩世岩浆活动的产物。闪长岩SiO₂和K₂O的质量分数较低，MgO、Na₂O、Fe₂O₃、MgO和Al₂O₃的质量分数较高，Mg^#为58.00~70.00。Na₂O/K₂O为1.08~2.96，相对富钠高铝，其里特曼指数为1.95~2.96，具有钙碱性系列的岩浆演化趋势。金岭闪长岩w（Ni）为99.00×10^-6~237.00×10^-6，w（Cr）为270.00×10^-6~600.00×10^-6，w（Co）为19.00×10^-6~44.00×10^-6，表明其具有幔源岩浆的属性。稀土元素球粒陨石标准化曲线表明样品具有富集轻稀土元素（LREE），亏损重稀土元素（HREE）以及弱Eu （δEu为0.91~1.12）异常的特征。所有样品富集大离子亲石元素（Ba、K、Sr）和高场强元素Nd，亏损高场强元素Rb、Nb、Ta、Zr。样品中约2.5 Ga古老锆石的存在证明岩浆源区受到古老下地壳物质的混染作用。鲁西金岭地区闪长岩应形成于太平洋板块俯冲后后撤引起的伸展环境，其岩浆源区是富集地幔起源的基性岩浆底侵华北古老下地壳并与下地壳熔融形成的壳源酸性岩浆混合过程的产物。

关键词: 岩石地球化学, 锆石U-Pb年代学, 闪长岩, 鲁西地区, 太平洋板块

Abstract: The Jinling dioritic pluton in west Shandong is mainly composed of pyroxene diorite and biotite diorite. The zircon U-Pb dating results reveal that the dioritic pluton was emplaced in Early Cretaceous(129.17±0.96) Ma and (130.15±0.65)Ma. The major element data show that the diorites contain low contents of SiO₂, K₂O, and high contents of Na₂O, Fe₂O₃, MgO, Mg^# and Al₂O₃. The Na₂O/K₂O ratios range from 1.08 to 2.96. The diorites are enriched relatively in sodium and alumina. The diorites have calc-alkaline characteristics according to the Ritttman index(1.95-2.96). The contents of Ni、Cr、Co are 99.00×10^-6-237.00×10^-6,270.00×10^-6-600.00×10^-6,19.00×10^-6-44.00×10^-6 respectively, similar to the contents of mantle magma. The chondrite standardized REE curves show that they are enriched in light REE, and depleted of heavy REE with weak Eu anomaly (0.91-1.12). The diorites are enriched in large ion lithophile element (LILE) Ba, K, Sr, and high field strength elements (HFSE) Nd, while depleted of high field strength elements (HFSE) Rb, Nb, Ta, and Zr. The residual ancient zircons (~2.5 Ga) in the sample (N₁) indicate a mix of ancient lower crust occurred in the source area. The Jinling pluton might be formed under a lithospheric extension related to the rollback of the subducted Pacific plate, and the magma was the mixing product of the siliceous crust melted through underplating of basaltic magma, and the mantle enriched basaltic magma.

Key words: petro-geochemistry, zircon U-Pb chronology, diorite, Luxi area, Pacific plate

中图分类号:

P588.12

张超, 崔芳华, 张照录, 耿瑞, 宋明春. 鲁西金岭地区含矿闪长岩体成因:来自锆石U-Pb年代学和地球化学证据[J]. 吉林大学学报(地球科学版), 2017, 47(6): 1732-1745.

Zhang Chao, Cui Fanghua, Zhang Zhaolu, Geng Rui, Song Mingchun. Petrogenesis of Ore-Bearing Dioritic Pluton in Jinling Area in Western Shandong:Evidence from Zircon U-Pb Chronology and Petro-Geochemistry[J]. Journal of Jilin University(Earth Science Edition), 2017, 47(6): 1732-1745.

参考文献

[1] 黄有德, 李绥远. 中国东部地区夕卡岩型铁矿成矿控制和富集条件[J]. 矿产与地质, 1983(3):129-142. Huang Youde, Li Suiyuan. Ore-Controlling and Enrichment Condition of Skarn Iron Deposit in Eastern China[J]. Journal of Mining and Geology, 1983(3):129-142.
[2] 赵一鸣. 中国主要富铁矿床类型及地质特征[J]. 矿床地质, 2013, 32(4):685-704. Zhao Yiming. Main Genetic Types and Geological Characteristics of Iron-Rich Ore Deposits in China[J]. Mineral Deposits, 2013, 32(4):685-704.
[3] 毛景文. 湖南柿竹园钨锡钼铋多金属矿床地质与地球化学[M]. 北京:地质出版社,1998:1-214. Mao Jingwen. Deposit Geology and Chemistry of the Polymetallic W Sn Mo Bi in Shizhuyuan, Hunan Province[M]. Beijing:Geological Publishing House, 1998:1-214.
[4] Kwak T A P. W-Sn Skarn Deposits and Related Metamorphic Skarns and Granitoids[J]. Elsevier, 1987, 52:559.
[5] 陈斌, 陈长健, 贺敬博,等. 华北东部中生代高镁埃达克质岩浆的起源:岩石学和Nd-Sr-Os同位素证据[J]. 科学通报, 2013,58(20):1941-1953. Chen Bin, Chen Changjian, He Jingbo, et al. Origin of Mesozoic High-Mg Adakitic Rocks from Northeastern China:Petrological and Nd-Sr-Os Isotopic Constraints[J].ChineseScience Bulletin, 2013, 58(20):1941-1953.
[6] 王浩, 徐兆文, 李海勇,等. 邹平雪山二长岩年代学和Sr-Nd同位素研究及成因探讨[J]. 南京大学学报(自然科学), 2015,51(1):73-86. Wang Hao, Xu Zhaowen, Li Haiyong, et al. Geochronology,Sr-Nd Isotope and Genesis of the Xueshan Monzonite,Zouping County,Shandong Province[J]. Journal of Nanjing University(Natural Sciences), 2015,51(1):73-86.
[7] 杨承海, 许文良, 杨德彬,等. 鲁西上峪辉长-闪长岩的成因:年代学与岩石地球化学证据[J]. 中国科学:地球科学, 2008, 31(1):44-55. Yang Chenghai, Xu Wenliang, Yang Debin, et al.Petrogenesis of Shangyu Gabbro-Diorites in Western Shandong:Evidence from Chronology and Petro-Geochemistry[J]. Chinese Science:Earth Science, 2008, 31(1):44-55.
[8] Guo F, Fan W M, Wang Y J, et al. Late Mesozoic Mafic Intrusive Complexes in North China Block:Constraints on the Nature of Subcontinental Lithospheric Mantle[J]. Physics & Chemistry of the Earth Part A Solid Earth & Geodesy, 2001, 26(9/10):759-771.
[9] Lan T G, Fan H R, Santosh M, et al.Crust-Mantle Interaction Beneath the Luxi Block,Eastern North China Craton:Evidence from Coexisting Mantle-and Crust-Derived Enclaves in a Quartz Monzonite Pluton[J]. Lithos, 2013, 177:1-16.
[10] Jin Z, Zhang Z, Hou T, et al. Genetic Relationship of High-Mg Dioritic Pluton to Iron Mineralization:A Case Study from the Jinling Skarn-Type Iron Deposit in the North China Craton[J]. Journal of Asian Earth Sciences, 2015, 113:957-979.
[11] Xie Q, Zhang Z, Hou T, et al. Petrogenesis of the Zhangmatun Gabbro in the Jinan Complex, North China Craton:Implications for Skarn-Type Iron Mineralization[J]. Journal of Asian Earth Sciences, 2015, 113:1197-1217.
[12] 许文良, 王冬艳, 高山,等. 鲁西中生代金岭闪长岩中纯橄岩和辉石岩包体的发现及其意义[J]. 科学通报, 2003, 48(8):790-797. Xu Wenliang, Wang Dongyan, Gao Shan, et al. The Discovery and Significance of Xenoliths of Dunite and Pyroxenite in Jinling Mesozoic Diorite in Western Shandong Province[J]. Chinese Science Bulletin, 2003, 48(8):790-797.
[13] 宁培松, 龙群, 程婷,等. 鲁西地块晚中生代中-基性岩地球化学和Sr-Nd-Pb同位素组成特征[J]. 地球科学与环境学报, 2013, 35(4):62-76. Ning Peisong, Long Qun, Cheng Ting, et al. Geochemistry and Sr-Nd-Pb Isotopic Composition of Late Mesozoic Intermediate-Basic Rock in Western Shandong Block[J]. Journal of Earth Sciences & Environment, 2013, 35(4):62-76.
[14] 王冬艳, 许文良, 兰翔,等. 鲁西中生代辉长-闪长岩中辉石岩捕虏体的岩石成因[J]. 吉林大学学报(地球科学版), 2004, 34(2):167-173. Wang Dongyan, Xu Wenliang, Lan Xiang, et al. Petrogenesis of Pyroxenite Xenoliths in Mesozoic Gabbro-Diorite from Western Shandong Province, China[J]. Journal of Jiling University(Earth Science Edition), 2004, 34(2):167-173.
[15] 巫祥阳, 徐义刚, 马金龙,等. 鲁西中生代高镁闪长岩的地球化学特征及其成因探讨[J]. 大地构造与成矿学, 2003, 27(3):228-236. Wu Xiangyang, Xu Yigang, Ma Jinlong, et al. Geochemistry and Petrogenesis of the Mesozoic High-Mg Diorites from Western Shandong[J]. Geotectonica et Metallogenia, 2003, 27(3):228-236.
[16] 杨承海, 许文良, 杨德彬,等. 鲁西中生代高Mg闪长岩的成因:年代学与岩石地球化学证据[J]. 地球科学:中国地质大学学报, 2006, 31(1):81-92. Yang Chenghai, Xu Wenliang, Yang Debin, et al. Petrogenesis of Mesozoic High-Mg Diorites in Western Shandong:Evidence from Chronology and Petro-Geochemistry[J]. Earth Science:Journal of China University of Geosciences, 2006, 31(1):81-92.
[17] Lan T G, Fan H R, Hu F F, et al. Multiple Crust-Mantle Interactions for the Destruction of the North China Craton:Geochemical and Sr-Nd-Pb-Hf Isotopic Evidence from the Longbaoshan Alkaline Complex[J]. Lithos, 2012, 122:87-106.
[18] Yang Q L, Zhao Z F, Zheng Y F. Slab-Mantle Inte-raction in Continental Subduction Channel:Geochemical Evidence from Mesozoic Gabbroic Intrusives in Southeastern North China[J]. Lithos, 2012, 155(1):442-460.
[19] Zhang H F, Sun M, Zhou X H, et al. Geochemical Constraints on the Origin of Mesozoic Alkaline Intrusive Complexes from the North China Craton and Tectonic Implications[J]. Lithos, 2005, 69(6):297-317.
[20] 郝兴中. 鲁西地区铁矿成矿规律与预测研究[D]. 北京:中国地质大学(北京), 2014. Hao Xingzhong. Study on Metallogenic Regularities and Prognosis of Iron Deposits in Western Shandong Province[D]. Beijing:China University of Geosciences(Beijing), 2014.
[21] Ludwig K R. Users Manual for Isoplot/Ex Rev. 2.49[M]. Berkeley:Berkeley Geochronology Centre Special Publication, 2001:1-56.
[22] S Mackenzie-W. TheInterpretation of Igneous Rocks[M]. London:Allen and Unwin, 1979:1-450.
[23] Rickwood P C. Boundary Lines with in Petrologic Diagrams Which Use Oxides of Major and Minor Elements[J]. Lithos, 1989, 22(4):247-263.
[24] Boynton W V. Geochemistry of the Rare Earth Elements:Meteorite Studies[M]//Henderson P.Rare Earth Element Geochemistry.Amsterdam:Elsevier, 1984:63-114.
[25] Sun S S, Mcdonough W F. Chemical and Isotopic Systematics of Oceanic Basalts; Implications for Mantle Composition and Processes[J]. Geological Society London Special Publications, 1989, 42(1):313-345.
[26] 刘永江, 刘宾强, 冯志强,等. 大兴安岭中北段老道口闪长岩锆石U-Pb年龄、地球化学特征及构造意义[J]. 吉林大学学报(地球科学版), 2016, 46(2):482-498. Liu Yongjiang, Liu Binqiang, Feng Zhiqiang, et al. SIMS Zircon U-Pb Age, Petrogeochemistry and Its Tectonic Implication of Laodaokou Diorite in the Mid-North Part of Great Xing'an Range[J]. Journal of Jilin University (Earth Science Edition), 2016, 46(2):482-498.
[27] Kelemen P B, Shimizu N, Dunn T. Relative Deple-tion of Niobium in Some Arc Magmas and the Continental Crust:Partitioning of K, Nb, La and Ce During Melt/Rock Reaction in the Upper Mantle[J]. Earth & Planetary Science Letters, 1993, 120(3/4):111-134.
[28] Rudnick R L, Fountain D M. Nature and Composi-tion of the Continental Crust:A Lower Crustal Perspective[J]. Reviews of Geophysics, 1995, 33(3):267-310.
[29] 郭锋, 范蔚茗, 王岳军,等. 大兴安岭南段晚中生代双峰式火山作用[J]. 岩石学报, 2001, 17(1):161-168. Guo Feng, Fan Weiming, Wang Yuejun, et al. Petrogenesis of the Late Mesozoic Bimodal Volcanic Rocks in the Southern Da Hinggan Mts, China.[J]. Acta Petrologica Sinica, 2001, 17(1):161-168.
[30] 张玉涛, 张连昌, 英基丰,等. 大兴安岭北段塔河地区早白垩世火山岩地球化学及源区特征[J]. 岩石学报, 2007, 23(11):2811-2822. Zhang Yutao, Zhang Lianchang, Ying Jifeng, et al. Geochemistry and Source Characteristics of Early Cretaceous Volcanic Rocks in Tahe, North Da Hinggan Mountain.[J]. Acta Petrologica Sinica, 2007, 23(11):2811-2822.
[31] 山东省地质矿产局第四地质研究院. 山东省区域地质[M]. 济南:山东省地图出版社, 2003:331-350. NO.4 Institute Of Geological Research Institute of Shandong Provincial Bureau of Geology and Mineral Resources.Regional Geology of Shandong Province[M]. Jinan:Map Publishing House of Shandong Province, 2003:331-350.
[32] 山东省地矿局地质综合研究队和实验室. 山东省岩浆岩研究报告[R].济南:山东省地图出版社, 1985:1-50. Comprehensive Geological Research Brigade and Laboratory of Shandong Provincial Bureau of Geology and Mineral Resources. The Report of Magmatic Rocks Study in Shandong Province[R].Jinan:Map Publishing House of Shandong Province, 1985:1-50.
[33] 陈立辉, 周新华. 鲁西中生代闪长岩中的深源超镁铁质岩捕虏体及其富硅交代特征[J]. 中国科学:地球科学, 2003, 33(8):734-744. Chen Lihui, Zhou Xinhua. The Characteristics of Silica Enrichment and Deep Source Ultramafic Rocks Xenoliths in Mesozoic Diorite from Western Shandong Province[J]. China Science:Earth Science, 2003, 33(8):734-744.
[34] 许文良, 王冬艳, 王清海,等. 鲁西中生代闪长岩中两类幔源捕虏体的岩石学和地球化学[J]. 岩石学报, 2003, 19(4):623-636. Xu Wenliang, Wang Dongyan, Wang Qinghai, et al. Petrology and Geochemistry of Two Types of Mantle-Derived Xenoliths in Mesozoic Diorite from Western Shandong Province[J]. Acta Petrologica Sinica, 2003, 19(4):623-636.
[35] Green T H. Significance of Nb/Ta as an Indicator of Geochemical Processes in the Crust-Mantle System[J]. Chemical Geology, 1995, 120(3):347-359.
[36] Ionov D A, Griffin W L, O'Reilly S Y. Volatile-Bearing Minerals and Lithophile Trace Elements in the Upper Mantle[J]. Chemical Geology, 1997, 141(3/4):153-184.
[37] Mcdonough W F, Sun S S. The Composition of the Earth[J]. Chemical Geology, 1995, 120(3/4):223-253.
[38] Adam J, Green T H, Sie S H. Proton Microprobe Determined Partitioning of Rb, Sr, Ba, Y, Zr, Nb and Ta Between Experimentally Produced Amphiboles and Silicate Melts with Variable F Content[J]. Chemical Geology, 1993, 109(1/2/3/4):29-49.
[39] Latourrette T, Hervig R L, Holloway J R. Trace Element Partitioning Between Amphibole, Phlogopite, and Basanite Melt[J]. Earth & Planetary Science Letters, 1995, 135(1/2/3/4):13-30.
[40] Vaughan A P M, Leat P T, Dean A A, et al. Crustal Thickening Along the West Antarctic Gondwana Margin During Mid-Cretaceous Deformation of the Triassic Intra-Oceanic Dyer Arc[J]. Lithos, 2012, 142/143(6):130-147.
[41] Yang C H, Xu W L, Yang D B, et al. Petrogenesis of Shangyu Gabbro-Diorites in Western Shandong:Geochronological and Geochemical Evidence[J].Science in China:Series D:Earth Sciences, 2008, 51(4):481-492.
[42] Defant M J, Drummond M S. Derivation of Some Modern arc Magmas by Melting of Young Subducted Lithosphere[J]. Nature, 1990, 347:662-665.
[43] Chen B, Jahn B M, Suzuki K. Petrological and Nd-Sr-Os Isotopic Constraints on the Origin of High-Mg Adakitic Rocks from the North China Craton:Tectonic Implications[J]. Geology, 2012, 41(1):91-94.
[44] Wang Y, Houseman G A, Lin G, et al. Mesozoic Lithospheric Deformation in the North China Block:Numerical Simulation of Evolution from Orogenic Belt to Extensional Basin System[J]. Tectonophysics, 2005, 405(1/2/3/4):47-63.
[45] Wang K, Burov E, Gumiaux C, et al. Formation of Metamorphic Core Complexes in Non-Over-Thickened Continental Crust:A Case Study of Liaodong Peninsula(East Asia)[J]. Lithos, 2015, 238:86-100.
[46] Yang L Q, Deng J, Wang Z L, et al. Thermochro-nologic Constraints on Evolution of the Linglong Metamorphic Core Complex and Implications for Gold Mineralization:A Case Study from the Xiadian Gold Deposit, Jiaodong Peninsula, Eastern China[J]. Ore Geology Reviews, 2016, 72:165-178.
[47] Ji M, Liu J, Hu L, et al. Evolving Magma Sources During Continental Lithospheric Extension:Insights from the Liaonan Metamorphic Core Complex, Eastern North China Craton[J]. Tectonophysics, 2015,647/648:48-62.
[48] Zhu G, Chen Y, Jiang D, et al. Rapid Change from Compression to Extension in the North China Craton During the Early Cretaceous:Evidence from the Yunmengshan Metamorphic Core Complex[J]. Tectonophysics, 2015, 656(1):91-110.
[49] 王德滋, 赵广涛, 邱检生. 中国东部晚中生代A型花岗岩的构造制约[J]. 高校地质学报, 1995(2):13-21. Wang Dezi, Zhao Guangtao, Qiu Jiansheng. The Tectonic Constraint on the Late Mesozoic A-Type Granitoids in Eastern China[J]. Geological Journal of Universitiesf, 1995(2):13-21.
[50] Yang Q L, Zhao Z F, Zheng Y F. Modification of Subcontinental Lithospheric Mantle Above Continental Subduction Zone:Constraints from Geochemistry of Mesozoic Gabbroic Rocks in Southeastern North China[J]. Lithos, 2012, 146/147(8):164-182.
[51] Kawamoto N, Smit J. Petrogenesis and Tectonic Implications of Late Jurassic Shoshonitic Lamprophyre Dikes from the Liaodong Peninsula, NE China[J]. Mineralogy and Petrology, 2010, 100(3):127-151.
[52] Ma L, Jiang S Y, Dai B Z, et al. Multiple Sources for the Origin of Late Jurassic Linglong Adakitic Granite in the Shandong Peninsula, Eastern China:Zircon U-Pb Geochronological, Geochemical and Sr-Nd-Hf Isotopic Evidence[J]. Lithos, 2013, 162(1):251-263.
[53] Liang C, Liu Y, Neubauer F, et al. Structures, Ki-nematic Analysis, Rheological Parameters and Temperature-Pressure Estimate of the Mesozoic Xingcheng-Taili Ductile Shear Zone in the North China Craton[J]. Journal of Structural Geology, 2015, 78:27-51.
[54] Liang C, Liu Y, Neubauer F, et al. Structural Cha-racteristics and LA-ICP-MS U-Pb Zircon Geochronology of the Deformed Granitic Rocks from the Mesozoic Xingcheng-Taili Ductile Shear Zone in the North China Craton[J]. Tectonophysics, 2015,650:80-103.

Metrics

Viewed

Full text

Abstract

Cited

Shared

Discussed

鲁西金岭地区含矿闪长岩体成因:来自锆石U-Pb年代学和地球化学证据

Petrogenesis of Ore-Bearing Dioritic Pluton in Jinling Area in Western Shandong:Evidence from Zircon U-Pb Chronology and Petro-Geochemistry

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]	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.
[2]	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.
[3]	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.
[4]	孙宁辰, 周建波, 李功宇, 辛中华, 陈卓, 王红燕. 东北中生代盆地演化及其对古太平洋板块俯冲的制约[J]. 吉林大学学报(地球科学版), 2026, 56(1): 66-88.
[5]	韩伟, 周建波, 陈志方, 冯志强. 那丹哈达地体增生序列与演化及其对古太平洋板块俯冲-增生历史的制约[J]. 吉林大学学报(地球科学版), 2026, 56(1): 131-148.
[6]	孙路华, 梁琛岳, 郑常青, 宋志伟, 周建波. 辽西医巫闾山地区晚中生代伸展变形事件识别及其构造意义[J]. 吉林大学学报(地球科学版), 2026, 56(1): 173-198.
[7]	许中杰, 冷龙, 朱占平, 段煜, 张芳霞, 徐大志. 渤海湾盆地歧口凹陷古近纪构造背景分析：来自碎屑锆石U-Pb年代学的证据[J]. 吉林大学学报(地球科学版), 2026, 56(1): 229-251.
[8]	尹志刚, 姜琦, 李萌萌, 吴子杰, 陈军典, 张凯强, 郭浩, 马岩. 辽东本溪地区新太古代晚期刘家堡子岩体成因及地质意义[J]. 吉林大学学报(地球科学版), 2025, 55(5): 1549-1563.
[9]	杨雨, 付文钊, 朱磊, 尹志刚, 马占才, 陈金勇, 高莲凤, 张振国, 巩磊. 辽西小孤山金矿床赋矿凝灰岩的年代学、岩石地球化学特征及其地质意义 [J]. 吉林大学学报(地球科学版), 2025, 55(4): 1120-1142.
[10]	董立帅, 郝俊杰, 侯建军, 张梓靖, 郑常青, 侯飞飞. 华北克拉通中部造山带河北良岗榴闪岩变质作用演化及其地质意义 [J]. 吉林大学学报(地球科学版), 2025, 55(4): 1181-1212.
[11]	赵佳奇, 宋志伟, 田志远, 王虞舜, 张猛, 杨宁, 梁琛岳. 辽西兴城娘娘顶地区花岗质片麻岩形成时代与变形样式[J]. 吉林大学学报(地球科学版), 2024, 54(3): 890-904.
[12]	尹志刚, 李萌萌, 吴子杰, 陈军典, 姜然, 张凯强, 姜琦, 郭浩. 辽宁本溪地区新太古代晚期钾质花岗岩的发现及其地质意义[J]. 吉林大学学报(地球科学版), 2024, 54(1): 125-139.
[13]	何军成, 刘军, 李小伟, 王晓彤, 孙鹏. 黑龙江省团结沟浅成低温热液金矿床成因——锆石U-Pb定年、元素地球化学和Hf-S-Pb-He同位素证据 [J]. 吉林大学学报(地球科学版), 2023, 53(5): 1437-1466.
[14]	牟芮霆, 裴福萍, 时玉芹, 魏敬洋. 吉林省伊通地区早二叠世火山岩成因：锆石U-Pb年代学和岩石地球化学证据[J]. 吉林大学学报(地球科学版), 2023, 53(4): 1117-1131.
[15]	李怡欣, 耿瑞, 肖风利, 柏城璘, 孙景贵. 黑龙江省老柞山金矿区花岗闪长岩成因及其对成矿的启示：锆石U-Pb同位素定年和岩石地球化学特征[J]. 吉林大学学报(地球科学版), 2023, 53(3): 809-821.