吉林大学学报(地球科学版) ›› 2019, Vol. 49 ›› Issue (6): 1628-1648.doi: 10.13278/j.cnki.jjuese.20190068

• 地质与资源 • 上一篇    下一篇

东昆仑五龙沟矿集区中三叠世辉绿岩脉的岩石成因:年代学、地球化学特征及其构造意义

程龙1, 丁清峰1, 邓元良2, 宋凯1, 张强1   

  1. 1. 吉林大学地球科学学院, 长春 130061;
    2. 青海省第六地质勘察院, 青海 海西 810001
  • 收稿日期:2019-04-02 发布日期:2019-11-30
  • 通讯作者: 丁清峰(1976-),男,教授,博士,主要从事矿床学方面的研究和教学工作,E-mail:dingqf@jlu.edu.cn E-mail:dingqf@jlu.edu.cn
  • 作者简介:程龙(1991-),男,研究生,主要从事矿产普查与勘探(固体方向)方向的研究,E-mail:773710523@qq.com
  • 基金资助:
    国家自然科学基金项目（41572056）

Petrogenesis of Middle Triassic Diabase Veins in Wulonggou Ore Concentrated Areas Within East Kunlun Orogen: Chronology, Geochemistry and Tectonic Significance

Cheng Long1, Ding Qingfeng1, Deng Yuanliang2, Song Kai1, Zhang Qiang1   

  1. 1. College of Earth Sciences, Jilin University, Changchun 130061, China;
    2. Qinghai Sixth Geological Exploration Istitute, Haixi 810001, Qinghai, China
  • Received:2019-04-02 Published:2019-11-30
  • Supported by:
    Supported by National Natural Science Foundation of China (41572056)

PDF (PC)

284

摘要： 本文对五龙沟矿集区4条辉绿岩脉中的锆石进行LA-ICP-MS U-Pb定年研究，发现其中大部分锆石为捕获锆石，而拥有最新年龄的锆石可代表岩浆结晶时的锆石，其加权平均年龄为（242.8±2.1）Ma，属于中三叠世。这些辉绿岩脉的w（SiO2）为42.82%~52.94%，w（Na2O）为1.98%~4.51%，w（K2O）为0.70%~2.04%，属于钙碱性和高钙碱性系列；4条岩脉中V、Cr、Ni等质量分数与MgO质量分数均呈正相关，且质量分数较小，表明其岩浆演化过程中经历了以橄榄石、辉石为主的分离结晶作用；其微量元素具有相对富集大离子亲石元素（Rb、Ba、Eu）和轻稀土元素，亏损高场强元素的特征，Nb/La为0.39~0.50，Nb/Ta为12.16~16.69，Zr/Hf为45.82~47.06，明显和亏损软流圈地幔来源的岩浆不同。综合分析认为，五龙沟矿集区的中三叠世辉绿岩脉大地构造背景为俯冲环境，是受俯冲板片流体改造的岩石圈地幔部分熔融的产物，并经受了一定的地壳混染。

关键词: 五龙沟矿集区, 辉绿岩脉, 中三叠世, 年代学, 地球化学, 岩石圈

Abstract: Through a LA-ICP-MS U-Pb dating of zircons from four diabase dykes in Wulonggou ore concentrated areas, we found that the most zircons are the inherited zircons. The zircons with the latest age represent those from the magmatic crystallization of diabase veins with an average age of (242.8±2.1) Ma (the Middle Triassic). The four diabase dykes are calc-alkaline -high calc-alkaline with w(SiO2) range of 42.82%-52.94%,w(Na2O) range of 1.98%-4.51% and w(K2O) range of 0.70%-2.04%. V, Cr, Ni and the other trace elements in the four dikes are positively correlated with MgO mass fraction, and the mass fraction is small. This results indicate that the fractional crystallizations of the olivine and pyroxene occurred during the magmatic process. The trace elements are characterized by relatively rich in LILE (Rb, Ba, Eu), LREE, depleted of HFSE, Nb/La is 0.39-0.50, Nb/Ta is 12.16-16.69, and Zr/Hf is 45.82-47.06. These features are quite different from those of the magma derived from the depleted asthenosphere mantle. In conclusion, the Middle Triassic diabase dikes in Wulonggou ore concentrated areas may be derived from the partial melting of the lithospheric mantle, reconstructed by the subduction plate fluids and contaminated by the crust.

Key words: Wulonggou ore concentrated areas, diabase dykes, Middle Triassic, chronology, geochemistry, lithospheric

中图分类号: 

  • P588.124
[1] 姜春发,杨经绥,冯秉贵,等. 昆仑开合构造[M]. 北京:地质出版社,1992. Jiang Chunfa, Yang Jingsui, Feng Binggui, et al. The Opening and Closing Structure of Kunlun Area[M].Beijing:Geological Publish House,1992.
[2] 潘桂棠,李兴振,王立全,等.青藏高原及邻区大地构造单元初步划分[J].地质通报, 2002, 21(11):701-707. Pan Guitang, Li Xingzhen, Wang Liquan, et al. The Preliminary Repartition of Tibetan Plateau andIts Adgacent Areas Tectonic Unit[J]. Geological Bulletin, 2002,21(11):701-707.
[3] 王艺龙,李艳军,魏俊浩,等.东昆仑五龙沟地区晚志留世A型花岗岩成因:U-Pb年代学、地球化学、Nd及Hf同位素制约[J]. 地球科学, 2018, 43(4):1219-1236. Wang Yilong, Li Yanjun, Wei Junhao, et al. Origin of Late Silurian A-Type Granite in Wulongou Area,East Kunlun Orogen:Zircon U-Pb Age, Geochemistry Nd and Hf Isotopic Constraints[J]. Earth Science, 2018, 43(4):1219-1236.
[4] 谌宏伟, 罗照华, 莫宣学,等.东昆仑造山带三叠纪岩浆混合成因花岗岩的岩浆底侵作用机制[J]. 中国地质, 2005,32(3):386-395. Chen Hongwei, Luo Zhaohua, Mo Xuanxue, et al. Magmatic Underplating Mechanism of Triassic Magmatic Mixed-Origin Granites in the East Kunlun Orogenic Belt[J]. Geology in China, 2005,32(3):386-395.
[5] Xiong Fuhao, Ma Changqian, Jiang Hong'an, et al. Geochronology and Geochemistry of Middle Devonian Mafic Dykes in the East Kunlun Orogenic Belt, Northern Tibet Plateau:Implications for the Transition from Prototethys to Paleotethys Orogeny[J]. Chemie der Erde, Geochemistry, Interdisciplinary Journal for Chemical Problems of the Geosciences and Geoecology, 2014, 74(2):225-235.
[6] 李瑞保, 裴先治, 李佐臣,等.东昆仑东段古特提斯洋俯冲作用:乌妥花岗岩体锆石U-Pb年代学和地球化学证据[J]. 岩石学报, 2018, 34(11):3399-3421. Li Ruibao, Pei Xianzhi, Li Zuochen, et al. Paleo-Tethys Ocean Subduction in Eastern Section of East Kunlun Orogen:Evidence from the Zircon U-Pb Geochronology and Geochemistry of the Wutuo Pluton[J]. Acta Petrologica Sinica, 2018, 34(11):3399-3421.
[7] 国显正,栗亚芝,贾群子,等.东昆仑五龙沟金多金属矿集区晚二叠世-三叠纪岩浆岩年代学、地球化学及其构造意义[J].岩石学报, 2017, 34(8):2359-2379. Guo Xianzheng, Li Yazhi, Jia Qunzi, et al. Geochronology and Geochemistry of the Wulonggou Orefield Related Granites in Late Permian-Triassic East-Kunlun:Implication for Metallogenic Tectonic[J]. Acta Petrologica Sinica, 2017, 34(8):2359-2379.
[8] Ding Qingfeng, Liu Fei, Yan Wei. Zircon U-Pb Geochronology and Hf Isotopic Constraints on the Petrogenesis of Early Triassic Granites in the Wulonggou Area of the Eastern Kunlun Orogen, Northwest China[J]. International Geology Review, 2015, 57(13):1735-1752.
[9] 陈国超,裴先治,李瑞保,等.东昆仑古特提斯后碰撞阶段伸展作用:来自晚三叠世岩浆岩的证据[J].地学前缘,2019,26(4):192-208. Chen Guochao, Pei Xianzhi, Li Ruibao, et al. Post-Collisional Extension of the Paleo-Tethys in East Kunlun:Evidence from Late Triassic Magmatic Rocks[J]. Earth Science Frontiers,2019, 26(4):192-208.
[10] Lingeois G P.Preface-Some Words on the Post-Collisional Magmatism[J].Lithos,1998,45(1/2/3/4):XV-XVII.
[11] 秦社彩,范蔚茗,郭锋,等.浙闽晚中生代辉绿岩脉的岩石成因:年代学与地球化学制约[J].岩石学报, 2010, 26(11):3295-3306. Qin Shecai, Fan Weiming, Guo Feng, et al. Petrogenesis of Late Mesozoic Diabase Dikes in Zhejiang-Fujian Provinces:Constraints from Ar-Ar Dating and Geochemistry[J]. Acta Petrologica Sinica, 2010, 26(11):3295-3306.
[12] 莫宣学,罗照华,邓晋福,等.东昆仑造山带花岗岩及地壳生长[J].高校地质学报,2007,13(3):403-414. Mo Xuanxue, Luo Zhaohua, Deng Jinfu, et al.Granitoids and Crustal Growth in the East Kunlun Orogenic Belt[J]. Geological Journal of China Universities, 2007,13(3):403-414.
[13] 严威,邱殿明,丁清峰,等.东昆仑五龙沟地区猴头沟二长花岗岩年龄、成因、源区及其构造意义[J].吉林大学学报(地球科学版),2016,46(2):443-460. Yan Wei,Qiu Dianming, Ding Qingfeng,et al.Geochronology, Petrogenesis, Source and Its Structural Significance of Houtougou Monzogranite of Wulonggou Area East Kunlun Orogen[J]. Journal of Jilin University (Earth Science Edition), 2016,46(2):443-460.
[14] 李厚民,沈远超,胡正国,等.青海东昆仑五龙沟金矿床成矿条件及成矿机理[J].地质与勘探,2001,37(1):65-69. Li Houmin,Shen Yuanchao, Hu Zhengguo,et al. Minerogenetic Mechanism and Condition of Wulonggou Gold Deposit in East Kunlun Mountains,Qinghai Province[J]. Geology and Prospecting, 2001,37(1):65-69.
[15] Yuan Chao, Zhou Meifu, Sun Min, et al.Triassic Granitoids in the Eastern Songpan Ganzi Fold Belt, SW China:Magmatic Response to Geodynamics of the Deep Lithosphere[J]. Earth and Planetary Science Letters, 2010, 290(3/4):481-492.
[16] 许志琴. 造山的高原:青藏高原的地体拼合、碰撞造山及隆升机制[M].北京:地质出版社,2007. Xun Zhiqin. Orogenic Plateau:Terrain Assemblage, Collision Orogeny and Uplift Mechanism of the Qinghai-Tibet Plateau[M]. Beijing:Geological Publishing House,2007.
[17] 郭正府,邓晋福,许志琴,等.青藏东昆仑晚古生代末-中生代中酸性火成岩与陆内造山过程[J].现代地质,1998,12(3):51-59. Guo Zhengfu, Deng Jinfu, Xu Zhiqin, et al. Late Paleozoic-Mesozoic Intermediate-Acid Igneous Rocks and Intracontinental Orogeny in Eastern Kunlun, Qinghai-Tibet[J]. Modern Geology, 1998,12(3):51-59.
[18] 丰成友. 青海东昆仑地区的复合造山过程及造山型金矿床成矿作用[D].北京:中国地质科学院,2002. Feng Chengyou. Multiple Orogenic Processes and Mineralization of Orogenic Deposits in Eastern Kunlun Orogen,Qinghai Province[D]. Beijing:Chinese Academy of Geological Science Physics,2002.
[19] 张德全,张慧,丰成友,等.柴北缘-东昆仑地区造山型金矿床的流体包裹体研究[J].中国地质,2007,34(5):843-854. Zhang Dequan,Zhang Hui, Feng Chengyou,et al.Fluid Inclusions in Orogenic Gold Deposits in the Northern Qaidammargin East Kunlun Region[J].Geology in China, 2007,34(5):843-854.
[20] 青海省第一地质矿产勘察院.青海省都兰县五龙沟地区红旗沟-深水潭金矿区详查报告[R].平安:青海省第一地质矿产勘察院,2010. First Geology and Mineral Exploration Istitute of Qinghai Province. The Detailsed Investigation Report of Gold Deposit in Hongqigou-Shenshuitan,Wulonggou,Qinghai Province[R]. Ping'an:First Geology and Mineral Exploration Istitute of Qinghai Province,2010.
[21] Liu Yongsheng, Gao Shan, Hu Zhaochu, 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.
[22] Liu Yongsheng, Hu Zhaochu, Gao Shan, et al. In Situ, Analysis of Major and Trace Elements of Anhydrous Minerals by LA-ICP-MS Without Applying an Internal Standard[J]. Chemical Geology, 2008, 257(1):34-43.
[23] Ludwig K R. User's Manual for Isoplot 3.00:A Geochronological Toolkit for Microsoft Excel[M]. Berkeley:Berkeley Geochronlogical Center Special Publication,2003:1-70.
[24] Ding Qingfeng, Jiang Shaoyong, Sun Fengyue. Zircon U-Pb Geochronology, Geochemical and Sr-Nd-Hf Isotopic Compositions of the Triassic Granite and Diorite Dikes from the Wulonggou Mining Area in the Eastern Kunlun Orogen, NW China:Petrogenesis and Tectonic Implications[J]. Lithos, 2014, 205(9):266-283.
[25] Gou Jun, Sun Deyou, Ren Yunsheng, et al. Petrogenesis and Geodynamic Setting of Neoproterozoic and Late Paleozoic Magmatism in the Manzhouli-Erguna Area of Inner Mongolia, China:Geochronological, Geochemical and Hf Isotopic Evidence[J]. Journal of Asian Earth Sciences, 2013, 67/68:114-137.
[26] Hoskin P W O, Black L P. Metamorphic Zircon Formation by Solid-State Recrystallization of Trotolith Igneous Zircon[J]. Journal of Metamorphic Geology, 2010, 18(4):423-439.
[27] Belousova E, Griffin W, Suzanne Y, et al. Igneous Zircon:Trace Element Composition as an Indicator of Source Rock Type[J]. Contributions to Mineralogy and Petrology, 2002, 143(5):602-622.
[28] Bas M J L, Maitre R W L, Streckeisen A, et al. A Chemical Classification of Volcanic Rocks Based on the Total Alkali-Silica Diagram[J]. Jour Petrol, 1986, 27(3):745-750.
[29] Sun S S, Mcdonough W F. Chemical and Isotopic Iystematics of Oceanic Basalts:Implications for Mantle Composition and Processes[J]. Geological Society London Special Publications, 1989, 42(1):313-345.
[30] Boynton W V. Chapter 3-Cosmochemistry of the Rare Earth Elements:Meteorite Studies[J]. Developments in Geochemistry, 1984, 2(2):63-114.
[31] Meschede M. A Method of Discriminating Between Different Types of Mid-Ocean Ridge Basalts and Continental Tholeiites with the Nb-Zr-Y Diagram[J]. Chemical Geology, 1986, 56(3/4):207-218.
[32] Wood D A. The Application of a Th-Hf-Ta Diagram to Problems of Tectonomagmatic Classification and to Establishing the Nature of Crustal Contamination of Basaltic Lavas of the British Tertiary Volcanic Province[J]. Earth and Planetary Science Letters,1980, 50(1):11-30.
[33] 赵忠华, 孙德有, 苟军,等. 满洲里南部塔木兰沟组火山岩年代学与地球化学[J]. 吉林大学学报(地球科学版), 2011, 41(6):1865-1880. Zhao Zhonghua, Sun Deyou, Gou Jun,et al.Chronology and Geochemistry of Vocanic Rock in Tamulangou Formation from Southern Manchuria Inner-Mongolia[J]. Journal of Jilin University (Earth Science Edition), 2011, 41(6):1865-1880.
[34] Paces J B, Bell K. Non-Depleted Sub-Continental Mantle Beneath the Superior Province of the Canadian Shield:Nd-Sr Isotopic and Trace Element Evidence from Midcontinent Rift Basalts[J]. Geochimica et Cosmochimica Acta, 1989, 53(8):2023-2035.
[35] Rudnick R L, Fountain D M. Nature and Composition of the Continental Crust:A Lower Crustal Perspective[J]. Reviews of Geophysics, 1995, 33(3):267.
[36] Barth M G, Mcdonough W F, Rudnick R L. Tracking the Budget of Nb and Ta in the Continental Crust[J]. Chemical Geology, 2000, 165(3/4):197-213.
[37] 夏林圻,夏祖春,徐学义,等. 中国中西部及邻区大陆板内火山作用[M]. 北京:科学出版社, 2013. Xia Linyin,Xia Zuchun,Xu Xueyi, et al. Intracontinental Volcanism in Central and Western China and Its Adjacent Areas[M].Beijing:Science Press, 2013.
[38] 曹建劲,胡瑞忠,谢桂青,等.广东沿海地区基性岩脉地球化学及成因[J].岩石学报,2009,25(4):984-1000. Cao Jianjin, Hu Ruizhong, Xie Guiqing, et al.Geochemistry and Genesis of Mamic Dikes from the Coastal Area of Guangdong Province,China[J]. Acta Petrologica Sinica, 2009,25(4):984-1000.
[39] Weaver B L. The Origin of Ocean Island Basalt End-Member Compositions:Trace Element and Isotopic Constraints[J]. Earth & Planetary Science Letters, 1991, 104(2/3/4):381-397.
[40] Zhao Zhenhua, Bao Zhiwei, Zhang Boyou. Geochemistry of the Mesozoic Basaltic Rocks in Southern Hunan Province[J]. Science in China:Series D:Earth Sciences,1998,41(Sup1):102-112.
[41] Wilson M, Downes H. Tertiary-Quaternary Extension-Related Alkaline Magmatism in Western and Central Europe[J]. Journal of Petrology, 1991, 32(4):811-849.
[42] Arndt N T, Czamanske G K, Wooden J L, et al. Mantle and Crustal Contributions to Continental Flood Volcanism[J]. Tectonophysics, 1993, 223(1/2):39-52.
[43] Hooper P R, Hawkesworth C J. Isotopic and Geochemical Constraints on the Origin and Evolution of the Columbia River Basalt[J]. Journal of Petrology, 1993, 6(6):1203-1246.
[44] Gallagher K, Hawkesworth C. Dehydration Melting and the Generation of Continental Flood Basalts[J]. Nature, 1992, 358:57-59.
[45] Hawkesworth C, Turner S, Gallagher K, et al. Calc-Alkaline Magmatism, Lithospheric Thinning and Extension in the Basin and Range[J]. Journal of Geophysical Research:Solid Earth, 1995, 100(6):10271-10286.
[46] Macdonald R, Rogers N W, Fitton J G, et al. Plume-Lithosphere Interactions in the Generation of the Basalts of the Kenya Rift, East Africa[J]. Journal of Petrology, 2001, 42(5):877-900.
[47] 杨锡铭, 孙丰月, 赵拓飞,等. 东昆仑阿克楚克塞地区辉长岩地球化学特征、锆石U-Pb年龄及其构造意义[J]. 地质通报, 2018, 37(10):76-86. Yang Ximing, Sun Fengyue, Zhao Tuofei, et al. Zircon U-Pb Dating, Geochemistry and Tectonic Implications of Akechukesai Gabbro in East Kunlun Orogenic Belt[J]. Geological Bulletin of China, 2018, 37(10):76-86.
[48] Chen Nengsong, Sun Min, Wang Qingyan, et al. EMP Chemical Ages of Monazites from Central Zone of the Eastern Kunlun Orogen:Records of Multi-Tectonometamorphic Events[J].Chinese Science Bulletin,2007,52(16):2252-2263.
[49] Yang Jingsui, Robinson P T, Jiang Chunfa, et al. Ophiolites of the Kunlun Mountains, China and Their Tectonic Implication[J]. Tectonophysics, 1996, 258(1):215-231.
[50] Yang Jingsui, Shi Rendeng, Wu Cailai, et al. Dur'ngoi Ophiolite in East Kunlun, Northeast Tibetan Plateau:Evidence for Paleo-Tethyan Suture in Northwest China[J].Journal of Earth Science,2009,20(2):303-331.
[51] Bonin B. Do Coeval Mafic and Felsic Magmas in Post-Collisional to Within-Plate Regimes Necessarily Imply Two Contrasting, Mantle and Crustal, Sources? A Review[J]. Lithos, 2004, 78(1-2):1-24.
[52] Sengor A M C. Tectonics of the Tethysides:Orogenic Collage Development in a Collisional Setting[J]. Annual Review of Earth & Planetary Sciences, 2003, 15(1):213-244.
[53] Yin An, Harrison T M.Geologic Evolution of the Himalayan-Tibetan Orogen[J]. Annual Review of Earth and Planetary Sciences,2000, 28(1):211-280.
[54] Roger F, Arnaud N, Gilder S, et al. Geochronological and Geochemical Constraints on Mesozoic Suturing in East Central Tibet[J]. Tectonics, 2003, 22(4):1037-1057.
[55] 栗亚芝,孔会磊,李金超,等.青海五龙沟矿区月亮湾斜长花岗岩地球化学特征及U-Pb年代学研究[J].矿物岩石地球化学通报,2015,34(2):401-409. Li Yazhi, Kong Huilei, Li Jinchao,et al.Geochemistry and Zircon U-Pb Geochronology of the Yueliangwan Plagiogranite in the Wulonggou Gold Deposit, Qinghai Province[J]. Bulletin of Mineralogy, 2015,34(2):401-409.
[56] 马昌前, 熊富浩, 尹烁,等. 造山带岩浆作用的强度和旋回性:以东昆仑古特提斯花岗岩类岩基为例[J]. 岩石学报, 2015, 31(12):3555-3568. Ma Changqian,Xiong Fuhao,Yin Shuo,et al. Magmatism Strength and Cyclicity in Orogenic Belt:A Case Study of Paleo-Tethyan Granitoid Base in East Kunlun[J]. Acta Petrologica Sinica, 2015, 31(12):3555-3568.
[57] 袁万明,莫宣学.东昆仑印支期区域构造背景的花岗岩记录[J].地质论评, 2000, 46(2):203-211. Yuan Wanming, Mo Xuanxue. Granite Record of the Ido-Chinese-Epoch Regional Tectonic Background in East Kunlun[J]. Geological Review, 2000, 46(2):203-211.
[58] 刘成东,莫宣学,罗照华,等.东昆仑造山带花岗岩类Pb-Sr-Nd-O同位素特征[J].地球学报,2003, 24(6):584-588. Liu Chengdong, Mo Xuanxue, Luo Zhaohua,et al. Pb-Sr-Nd-O Isotope Characteristics of Granitoids in East Kunlun Orogenic Belt[J]. Acta Geoscientica Sinica, 2003, 24(6):584-588.
[59] Yuan Chao, Sun Min, Xiao Wenjiao, et al. Garnet-Bearing Tonalitic Porphyry from East Kunlun, Northeast Tibetan Plateau:Implications for Adakite and Magmas from the MASH Zone[J]. International Journal of Earth Sciences, 2009, 98(6):1489-1510.
[60] Liu Chengdong, Mo Xuanxue, Luo Zhaohua,et al.Mixing Events Between the Crust- and Mantle-Derived Magmas in Eastern Kunlun:Evidence from Zircon Shrimp Ⅱ Chronology[J].Chinese Science Bulletin,2004(8):828-834.
[61] Chen Guochao, Pei Xianzhi, Li Ruibao, et al. Late Triassic Magma Mixing in the East Kunlun Orogenic Belt:A Case Study of Helegang Xilikete Granodiorites[J]. Geology in China, 2013, 40(4):1044-1065.
[1] 雷如雄, 赵同阳, 李平, 董连慧, 李基宏, 吴昌志. 北阿尔金地区大平沟金矿H-O-S-Pb同位素地球化学特征对金矿成因的启示[J]. 吉林大学学报(地球科学版), 2019, 49(6): 1578-1590.
[2] 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.
[3] 曾文人, 孟庆涛, 刘招君, 徐银波, 孙平昌, 王克兵. 柴北缘团鱼山地区中侏罗统石门沟组油页岩有机地球化学特征及古湖泊条件[J]. 吉林大学学报(地球科学版), 2019, 49(5): 1270-1284.
[4] 陈庆松, 杨润柏, 刘德民, 陶兰初. 滇东北会泽灯影组硅质岩成因及沉积环境——来自岩石学和地球化学证据[J]. 吉林大学学报(地球科学版), 2019, 49(5): 1327-1337.
[5] 牛海青, 韩小锋, 肖波, 魏建设, 张慧元, 王宝文. 中口子盆地侏罗系煤系烃源岩地球化学特征及生烃潜力评价[J]. 吉林大学学报(地球科学版), 2019, 49(4): 970-981.
[6] 周翔. 松辽盆地北部营城组火山岩地球化学特征及地质意义[J]. 吉林大学学报(地球科学版), 2019, 49(4): 1001-1014.
[7] 于介禄, 于介江, 杨万志, 张元厚, 郭秀玮. 东天山觉罗塔格带东段早志留世中酸性侵入岩的年代学、地球化学及构造意义[J]. 吉林大学学报(地球科学版), 2019, 49(3): 690-708.
[8] 王春光, 董晓杰, 徐仲元, 任云伟, 王文龙, 陈煜嵩. 内蒙古红山子地区新太古代变质侵入岩年代学及地球化学特征[J]. 吉林大学学报(地球科学版), 2019, 49(3): 709-726.
[9] 单玄龙, 蔡壮, 郝国丽, 邹欣彤, 赵容生. 地球化学温标估算长白山地热系统热储温度[J]. 吉林大学学报(地球科学版), 2019, 49(3): 662-672.
[10] 鲁倩, 孙景贵, 安久海, 韩吉龙, 褚小磊. 吉林敦化松江河地区中生代似斑状花岗岩成因和形成环境:元素、Hf同位素和锆石U-Pb年代学证据[J]. 吉林大学学报(地球科学版), 2019, 49(3): 673-689.
[11] 单承恒, 王政, 史长浩. 基于综合等级划分方法的土地质量地球化学评价——以吉林省乌拉街镇为例[J]. 吉林大学学报(地球科学版), 2019, 49(3): 817-829.
[12] 严克涛, 郭清海, 刘明亮. 西藏搭格架高温热泉中砷的地球化学异常及其存在形态[J]. 吉林大学学报(地球科学版), 2019, 49(2): 548-558.
[13] 张治波, 朱志军, 王文锋, 徐颖, 李丽荣. 滇西兰坪盆地中-新生代蒸发岩元素地球化学特征及其形成环境[J]. 吉林大学学报(地球科学版), 2019, 49(2): 356-379.
[14] 吴永涛, 韩润生. 滇东北矿集区茂租铅锌矿床地球化学特征[J]. 吉林大学学报(地球科学版), 2019, 49(2): 400-413.
[15] 秦亚, 杨启军, 李程, 周叔齐, 许浩天. 广西佛子冲铅锌矿田火成岩的时空序列及其对成矿时限的约束[J]. 吉林大学学报(地球科学版), 2019, 49(2): 425-444.
Viewed
Full text


Abstract

Cited
  Shared   
  Discussed   
[1] 曲亚军,朱大岗,孟宪刚,邵兆刚,余 佳,韩建恩,孟庆伟. 西藏纳木错地区116 ka以来的湖相沉积及其环境演化与气候变迁[J]. J4, 2006, 36(02): 187 -0193 .
[2] 胡克,陈兵,Hiroyuki Kitagawa,介冬梅,赵奎涛. 松嫩平原西部碱尘气溶胶的元素特征分析[J]. J4, 2006, 36(03): 417 -423 .
[3] 邹新宁，孙 卫，张盟勃,万玉君. 地震属性分析在岩性气藏描述中的应用[J]. J4, 2006, 36(02): 289 -0294 .
[4] 马艳梅,崔启良,周强,黄伟军,刘冶,彭刚,邹广田. 橄榄石原位高温拉曼光谱研究[J]. J4, 2006, 36(03): 342 -345 .
[5] 祝洪臣,王海坡,张炯飞. 内蒙古苏尼特左旗两种不同成因类型金矿[J]. J4, 2006, 36(05): 759 -766 .
[6] 何朋朋，姚磊华，刘立鹏，陈庆. 地下水位随机性影响下的边坡可靠性分析[J]. J4, 2009, 39(2): 288 -0293 .
[7] 何满潮,王建,李启民,乾增珍. 地层新能源利用的系统化设计[J]. J4, 2007, 37(1): 125 -0128 .
[8] 康春莉,隋海清,高红杰,郭 晶,郭 平，于宏兵,林学钰. UV/H2O2法降解乙酸影响因素的研究[J]. J4, 2007, 37(2): 371 -374 .
[9] 张 艳，王璞珺，陈文礼，刘万洙，唐华风. 低程度勘探区有效烃源岩的识别与平面成图--以塔里木盆地孔雀河地区为例[J]. J4, 2007, 37(3): 463 -0468 .
[10] 杨双玲，刘万洙，于世泉，王国军，黄玉龙. 松辽盆地火山岩储层储集空间特征及其成因[J]. J4, 2007, 37(3): 506 -0512 .
版权所有 © 《吉林大学学报(地球科学版)》编辑部
地址：长春市西民主大街938号(130026)　电话：+86-431-88502374；13756165364　E-mail: xuebao1956@jlu.edu.cn
本系统由北京玛格泰克科技发展有限公司设计开发