吉林大学学报(地球科学版) ›› 2021, Vol. 51 ›› Issue (1): 107-125.doi: 10.13278/j.cnki.jjuese.20190260

• 地质与资源 • 上一篇    

小兴安岭平顶山一带早侏罗世花岗岩类年代学、地球化学特征及其地质意义

尹志刚1, 宫兆民1, 王春生2, 刘松杰2, 张圣听1, 王冠群1, 周小刚1, 张志浩1   

  1. 1. 辽宁工程技术大学矿业学院, 辽宁 阜新 123000;
    2. 黑龙江省生态地质调查研究总院, 哈尔滨 150036
  • 收稿日期:2019-12-05 发布日期:2021-02-02
  • 作者简介:尹志刚(1962-),男,教授,博士,主要从事区域矿产资源方面的研究,E-mail:yzg63@163.com
  • 基金资助:
    中国地质调查局项目(1212011220435);辽宁工程技术大学学科创新团队资助项目(LNTU20TD-14)

Chronological, Geochemical Characteristics and Geological Significance of Early Jurassic Granites in Pingdingshan Area of Lesser Xing'an Range

Yin Zhigang1, Gong Zhaomin1, Wang Chunsheng2, Liu Songjie2, Zhang Shengting1, Wang Guanqun1, Zhou Xiaogang1, Zhang Zhihao1   

  1. 1. College of Mining Engineering, Liaoning Technical University, Fuxin 123000, Liaoning, China;
    2. Heilongjiang General Institute of Ecological Geological Survey and Research, Harbin 150036, China
  • Received:2019-12-05 Published:2021-02-02
  • Supported by:
    Supported by the Project of China Geological Survey(1212011220435) and the Project Supported by Discipline Innovation Team of Liaoning Technical University(LNTU20TD-14)

摘要: 小兴安岭平顶山大地构造位于兴蒙造山带东段,隶属松嫩地块。本文对小兴安岭平顶山一带碱长花岗岩和正长花岗岩进行了锆石U-Pb年代学和岩石地球化学研究,以确定其形成时代、岩石成因及大地构造背景。结果显示:碱长花岗岩形成于(189±3) Ma,正长花岗岩形成于(191±3) Ma,同为早侏罗世岩浆事件演化的产物;岩石具有高硅(w(SiO2)为75.00%~77.60%)、富碱(w(K2O+Na2O)为7.13%~9.00%)、贫镁(w(MgO)为0.05%~0.45%)、贫钙(w(CaO)为0.17%~1.10%)、低磷钛(w(P2O5)为0.01%~0.07%,w(TiO2)为0.09%~0.23%)的特点,A/CNK值为0.94~1.17,属于准铝质-弱过铝质、高钾钙碱性系列岩石;亏损高场强元素Nb、P、Ti、Ta和大离子亲石元素Ba、Sr,Rb、K、Th、Hf等元素具有明显的正异常;稀土元素总量(w(ΣREE))为(38.76~297.13)×10-6,稀土配分曲线显示为轻稀土略微富集、重稀土较为平坦缓向倾斜的右倾型,具明显的负Eu异常。锆石饱和温度值及地球化学特征等多种证据显示,岩石为高分异的I型花岗岩。结合小兴安岭区域构造演化特征分析,研究区早侏罗世花岗岩类为松嫩地块与佳木斯地块沿嘉荫—牡丹江缝合带碰撞拼合后伸展环境下的产物,岩浆起源于下地壳火成岩物质的部分熔融。

关键词: 花岗岩类, I型花岗岩, 锆石U-Pb年代学, 岩石地球化学, 小兴安岭

Abstract: Lesser Xing'an Range is located in the eastern section of Xing-Meng orogenic belt, and belongs to Songnen block. The zircon U-Pb geochronology and rock geochemistry of the alkali feldspar granite and syenite granite in Pingdingshan area of Lesser Xing'an Range were studied to determine their formation age, rock genesis, and tectonic setting. The dating data show that the alkali feldspar granite was formed in (189±3) Ma,and the syenite granite was formed in (191±3) Ma, which is the product of the evolution of the Early Jurassic magmatic event. The geochemical results show that the rocks are characterized by high silicon (75.00%-77.60%), rich alkali(7.13%-9.00%), poor magnesium (0.05%-0.45%), poor calcium (0.17%-1.10%), low phosphorus (0.01%-0.07%) and titanium (0.09%-0.23%), and A/CNK (0.94-1.17), belonging to metal aluminous-weak peraluminous high-K calcium-alkaline series. The rocks are poor in high field strength elements Nb, P, Ti, Ta and large ion-lithophile elements Ba, Sr, while rich in Rb, K, Th, Hf and other elements. The total amount of rare earth elements is (38.76-297.13)×10-6. The REEs distribution curve shows that the light rare earth elements are slightly enriched, and the heavy rare earth elements are gently inclined to the right with obvious negative Eu anomaly. The zircon saturation temperature and geochemical characteristics show that the rocks are highly differentiated Type I granites. Based on the tectonic evolution characteristics of Lesser Xing'an Range, the Early Jurassic granites in the study area are the products the collision and amalgamation of Songnen block and Jiamusi block along the Jiayin-Mudanjiang suture zone, and the magma was originated from the partial melting of igneous material in the lower crust.

Key words: granite rock, Type I granite, zircon U-Pb chronology, rock geochemistry, Lesser Xing’an Range

中图分类号: 

  • P581.12
[1] 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.
[2] 唐杰,许文良,王枫,等. 东北亚早中生代火成岩组合的时空变异:对古太平洋板块俯冲开始时间的制约[J].矿物岩石地球化学通报,2016,35(6):1181-1194. Tang Jie, Xu Wenliang, Wang Feng, et al. Rock Associations and Their Spatial-Temporal Variations of the Early Mesozoic Igneous Rocks in the NE Asia:Constraints on the Initial Subduction Timing of the Paleo-Pacific Plate[J]. Bulletin of Mineralogy,Petrology and Geochemistry,2016,35(6):1181-1194.
[3] 邵济安,牟保磊,何国琦,等.华北北部在古亚洲域与古太平洋域构造叠加过程中的地质作用[J].中国科学:D辑,1997,27(5):390-394. Shao Ji'an,Mou Baolei,He Guoqi,et al. Geological Roles of Northern China in the Process of Structural Superposition of Paleo-Asian and Paleo-Pacific Regions[J]. Science in China:Series D,1997,27(5):390-394.
[4] 杨言辰,韩世炯,孙德有,等.小兴安岭-张广才岭成矿带斑岩型钼矿床岩石地球化学特征及其年代学研究[J].岩石学报,2012,28(2):379-390. Yang Yanchen,Han Shijiong,Sun Deyou, et al. Geological and Geochemical Features and Geochronology of Porphyry Molybdenum Deposits in the Lesser Xing'an Range-Zhangguangcai Range Metallogenic Belt[J]. Acta Petrologica Sinica,2012,28(2):379-390.
[5] Xu M J,Xu W L,Wang F, et al. Age,Association and Provenance of the "Neoproterozoic" Fengshuigouhe Group in the Northwestern Lesser Xing'an Range,NE China:Constraints from Zircon U-Pb Geochronology[J]. Journal of Earth Science,2012,23(6):786-801.
[6] 许文良,王枫,裴福萍,等.中国东北中生代构造体制与区域成矿背景:来自中生代火山岩组合时空变化的制约[J].岩石学报,2013,29(2):339-353. Xu Wenliang, Wang Feng,Pei Fuping, et al. Mesozoic Tectonic Regimes and Regional Ore-Forming Background in NE China:Constraints from Spatial and Temporal Variations of Mesozoic Volcanic Rock Associations[J]. Acta Petrologica Sinica,2013,29(2):339-353.
[7] 仲米山,王海鹏,张呈彬,等.黑龙江省东南部张广才岭群新兴组的形成时代及物源[J]. 地质学报,2018,92(11):2318-2330. Zhong Mishan, Wang Haipeng, Zhang Chengbin, et al. Formation Time and Provenance of the Xinxing Formation of Zhangguangcailing Group in Southeastern Heilongjiang Province[J]. Acta Geological Sinica.2018,92(11):2318-2330.
[8] 鲁倩,孙景贵,安久海,等.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. Lu Qian, SunJinggui, An Jiuhai, et al. Petrogenesis and Forming Environment of Mesozoic Porphyritic Granite in Songjianghe Region of Dunhua,Jilin Province:Evidences from Element Geochemistry Hf Isotope and U-Pb[J]. Journal of Jilin University (Earth Science Edition),2019,49(3):673-689.
[9] 刘亚洲,申维,李姗,等.小兴安岭-张广才岭地区成矿金属元素分布特征及找矿靶区预测[J].矿物岩石地球化学通报,2018,37(5):922-931. Liu Yazhou, Shen Wei, Li Shan, et al. Ore-Metal Distribution and Target Prediction of Exploration Target Area in the Xiaoxing'anling-Zhangguang-cailing Region[J]. Bulletin of Mineralogy,Petrology and Geochemistry,2018,37(5):922-931.
[10] 孙德有,吴福元,高山,等.小兴安岭东部清水岩体的锆石激光探针U-Pb年龄测定[J].地球学报,2004,10(2):213-218. Sun Deyou, Wu Fuyuan, Gao Shan, et al. LA-ICP MS Zircon U-Pb Age of the Qingshui Pluton in the East Xiao Hinggan Mountains[J]. Acta Geoscientica Sinica,2004,10(2):213-218.
[11] 王广婷,孙德有,孙如江,等.张广才岭南部横道河子岩体地球化学特征及其成因[J].世界地质,2015,34(2):321-329. Wang Guangting,Sun Deyou,Sun Rujiang,et al.Geochemistry of Hengdaohezi Pluton from Southern Zhangguangcai Range and Its Petrogenesis[J]. Global Geology,2015,34(2):321-329.
[12] 杨小鹏,王长兵,李文庆.大兴安岭北段索图罕地区碱长花岗岩成因及形成构造背景[J].吉林大学学报(地球科学版),2019,49(5):1338-1349. Yang Xiaopeng, Wang Changbing, Li Wenqing. Petrogenesis and Tectonic Setting of Moyite in Sotuhan Area, Northern Great Xing'an Range[J]. Journal of Jilin University (Earth Science Edition),2019,49(5):1338-1349.
[13] 袁洪林,吴福元,高山,等.东北地区新生代侵入体的锆石激光探针U-Pb年龄测定与稀土元素成分分析[J].科学通报,2003,6(14):1511-1520. Yuan Honglin, Wu Fuyuan, Gao Shan, et al. U-Pb Age Determination and Rare Earth Element Composition Analysis of Cenozoic Intrusions in Northeast China[J]. Chinese Science Bulletin,2003,6(14):1511-1520.
[14] Liu Y S, Hu Z C, Gao S, et al.Insitu Analysis of Major and Trace Elements of Anhydrous Minerals By LA-ICP-MS Without Applying an Internal Standard[J]. Chemical Geology, 2008, 257(1/2):34-43.
[15] Liu Y S, Gao S, Hu Z C, 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.
[16] Liu Y S, Hu Z C, Zong K Q, et al. Reappraisement and Refinement of Zircon U-Pb Isotope and Trace Element Analyses by LAICP-MS[J]. Chinese Science Bulletin, 2010, 55(15):1535-1546.
[17] Anderson T. Correction of Common Lead in U-Pb Analyses that Do Not Report 204Pb[J]. Chemical Geology,2002,192(1/2):59-79.
[18] Chen F K,Hegner E, Todt W. Zircon Ages and Nd Isotopic and Chemical Compositions of Orthogneisses from the Black Forest, Germany:Evidence for a Cambrian Magmatic Arc[J]. International Journal of Earth Sciences, 2000,88(4):791-802.
[19] Chen F K, Siebel W, Satir M, et al. Geochronology of the Karadere Basement (NW Turkey) and Implications for the Geological Evolution of the Istanbul Zone[J]. International Journal of Earth Sciences, 2002,91(3):469-481.
[20] Yan M, Chi Q. The Chemical Compositions of the Continental Crustand Rocks in the Eastern Part of China[M]. Beijing:Science Press, 2005.
[21] 吴福元,李献华,杨进辉,等.花岗岩成因研究的若干问题[J].岩石学报,2007,18(6):1217-1238. Wu Fuyuan,Li Xianhua,Yang Jinhui,et al.Disscussions on the Petrogenesis of Granites[J]. Acta Petrologica Sinica,2007,18(6):1217-1238.
[22] 张旗,王焰,李承东,等.花岗岩的Sr-Yb分类及其地质意义[J].岩石学报,2006,18(9):2249-2269. Zhang Qi, Wang Yan, Li Chengdong, et al.Granite Classification on the Basis of Sr and Yb Contents and Its Implications[J]. Acta Petrologica Sinica,2006,18(9):2249-2269.
[23] 陈佩嘉,戴朝成,黄成,等.乌拉山地区古元古代S型花岗岩岩石地球化学、锆石U-Pb年代学及其地质意义[J].中国地质,2017,44(5):959-973. Chen Peijia, Dai Chaocheng, Huang Cheng, et al. Geochemical Characteristics and Zircon U-Pb Age of the Paleoproterozic S-Type Granite in Wulashan Region and Its Geological Significance[J]. Geology in China,2017,44(5):959-973.
[24] David C,Robert J. The Geochemical and Sr-Nd Isotopic Characteristics of Paleozoic Fractionated S-Types Granites of North Queensland:Implications for S-Type Granite Petrogenesis[J]. Lithos,2013,162/163:37-56.
[25] 纪政,葛文春,杨浩,等.大兴安岭中段塔尔气地区早白垩世花岗岩成因及形成构造环境[J].世界地质,2016,35(2):283-296. Ji Zheng,Ge Wenchun,Yang Hao, et al. Petrogenesis of Early Cretaceous Granites in Taerqi Area of Central Great Xing' an Range and Its Tectonic Setting[J]. Global Geology,2016,35(2):283-296.
[26] 王强,赵振华,熊小林,等.桐柏-大别造山带燕山晚期A型花岗岩的厘定[J].岩石矿物学杂志,2000,16(4):297-306. Wang Qiang,Zhao Zhenhua,Xiong Xiaolin,et al. The Ascertainment of Late-Yanshanian A-Type Granite in Tongbai-Dabie Orogenic Belt[J]. Acta Petrologica et Mineralogica,2000,16(4):297-306.
[27] 邱检生,肖娥,胡建,等.福建北东沿海高分异I型花岗岩的成因:锆石U-Pb年代学、地球化学和Nd-Hf同位素制约[J].岩石学报,2008,24(11):2468-2484. Qiu Jiansheng, Xiao E, Hu Jian, et al. Petrogenesis of Highly Fractionated I-Type Granites in the Coastal Area of Northeastern Fujian Province:Constraints from Zircon U-Pb Geochronology, Geochemistry and Nd-Hf Isotopes[J]. Acta Petrologica Sinica,2008, 24(11):2468-2484.
[28] 邱检生,胡建,王孝磊,等.广东河源白石冈岩体:一个高分异的I型花岗岩[J].地质学报,2005,20(4):503-514. Qiu Jiansheng, Hu Jian, Wang Xiaolei, et al. The Baishigang Pluton in Heyuan, Guangdong Province:A Highly Fractionated I-Type Granite[J]. Acta Geologica Sinica,2005,20(4):503-514.
[29] Wu Fuyuan,Sun Deyou,Jahn B,et al. A Jurassic Garnet-Bearing Granitic Pluton from NE China Showing Tetrad REE Patterns[J]. Journal of Asian Earth Sciences,2004,23(5):731-744.
[30] 罗兰,蒋少涌,杨水源,等.江西彭山锡多金属矿集区隐伏花岗岩体的岩石地球化学、锆石U-Pb年代学和Hf同位素组成[J].岩石学报,2010,26(9):2818-2834. Luo Lan, Jiang Shaoyong, Yang Shuiyuan, et al. Petrochemistry, Zircon U-Pb Dating and Hf Isotopic Composition of the Granitic Pluton in the Pengshan Sn-Polymetallic Orefield, Jiangxi Province[J]. Acta Petrologica Sinica,2010,26(9):2818-2834.
[31] Bau M. Controls on the Fractionation of Isovalene Trace Elements in Magmatic and Aqueous Systems:Evidence from Y/Ho,Zr/Hf,and Lanthanide Tetrad Effect[J]. Contributions to Mineralogy and Petrology,1996,123(3):323-333.
[32] 贾小辉,王强,唐功建,等.A型花岗岩的研究进展及意义[J].大地构造与成矿学,2009,33(3):465-480. Jia Xiaohui,Wang Qiang,Tang Gongjian,et al. A-Type Granites:Research Progress and Implications[J]. Geotectonica et Metallogenia,2009,33(3):465-480.
[33] 王珍珍,刘栋,赵志丹,等.冈底斯带南部桑日高分异I型花岗岩的岩石成因及其动力学意义[J].岩石学报,2017,33(8):2479-2493. Wang Zhenzhen, Liu Dong, Zhao Zhidan, et al. The Sangri Highly Fractionated I-Type Granites in Southern Gangdese:Petrogenesis and Dynamic Implication[J]. Acta Petrologica Sinica, 2017, 33(8):2479-2493.
[34] 王文佳,易涛,任文秀,等.内蒙古中部莫花以力更高分异I型花岗岩体地球化学特征及其构造环境[J].兰州大学学报(自然科学版),2018,54(5):586-596. Wang Wenjia, Yi Tao, Ren Wenxiu, et al. Geochemical Characteristics of the Mohuayiligeng Highly Fractionated I-Type Granitoids in Middle lnner Mongolia and Its Tectonic Setting[J].Journal of Lanzhou University(Natural Science),2018,54(5):586-596.
[35] 肖中军,王振强,赵春勇,等.内蒙古苏尼特左旗北部阿登锡勒大队一带早石炭世高分异I型花岗岩的发现及地质意义[J].地质论评,2015,61(4):777-786. Xiao Zhongjun, Wang Zhenqiang, Zhao Chunyong, et al. The Discovery of Monzogranite and Its Geologic Implication in Adenxile,Sonid Zuoqi, Innner Mongolia[J]. Geological Review,2015,61(4):777-786.
[36] 吴福元,刘小驰,纪伟强,等.高分异花岗岩的识别与研究[J].中国科学:地球科学,2017,47(7):745-765. Wu Fuyuan, Liu Xiaochi, Ji Weiqiang, et al. Highly Fractionated Granites:Recognition and Research[J]. Science China:Earth Sciences,2017,47(7):745-765.
[37] 陈璟元,杨进辉.佛冈高分异I型花岗岩的成因:来自Nb-Ta-Zr-Hf等元素的制约[J].岩石学报,2015,31,(3):846-854. Chen Jingyuan, Yang Jinhui. Petrogenesis of the Fogang Highly Fractionated I-Type Granitoids:Constraints from Nb,Ta,Zr and Hf[J]. Acta Petrologica Sinica, 2015, 31, (3):846-854.
[38] 彭智,杜建国,陈芳,等.北淮阳东段同兴寺碱性岩体地球化学特征, LA-ICP-MS锆石U-Pb年龄及其地质意义[J].地质学报, 2015, 89(4):701-714. Peng Zhi, Du Jianguo, Chen Fang, et al.Geochemical Characteristics and LA-ICP-MS Zircon U-Pb Geochronology Study of Tongxingsi Alkaline Intrusion in the East Part of North Huaiyang and Their Geological Significance[J]. Acta Geologica Sinica, 2015, 89(4):701-714.
[39] 李高杰,潘硕,侯宇.新疆准噶尔北塔山地区晚石炭世侵入岩地球化学特征及构造环境[J]. 地质科技情报, 2015, 34(5):46-52. Li Gaojie, Pan Shuo, Hou Yu. Geochemical Characteristics and Tectonic Settings of Late Carboniferous Intrusive Rocks from North Tashan Area in Junggar, Xinjiang[J]. Geological Science and Technology Information, 2015, 34(5):46-52.
[40] Xu WL,Ji W Q,Pei F P,et al.Triassic Volcanism in Eastern Heilongjiang and Jilin Provinces,NE China:Chronology, Geochemistry,and Tectonic Implications[J]. Journal of Asian Earth Sciences,2009,34(3):1-24.
[41] 肖庆辉,邓晋福,马大铨,等.花岗岩研究思维与方法[M].北京:地质出版社,2002. Xiao Qinghui, Deng Jinfu, Ma Dashuan, et al. Research and Methods of Granite Research[M]. Beijing:Geological Publishing House, 2002.
[42] 韩振哲,赵海玲,李娟娟,等.小兴安岭东南伊春一带早中生代花岗岩与多金属成矿作用[J].中国地质,2010, 37(1):74-87. Han Zhenzhe,Zhao Hailing,Li Juanjuan,et al. Early Mesozoic Granites and Polymetallic Mineralization in Southeastern Yichun Area, of Xiao Hinggan Mountains[J]. Geology in China,2010, 37(1):74-87.
[43] 徐美君,许文良,王枫,等.小兴安岭中部早侏罗世花岗质岩石的年代学与地球化学及其构造意义[J].岩石学报,2013,29(2):354-368. Xu Meijun,Xu Wenliang,Wang Feng,et al. Chronology and Geochemistry of the Early Jurassic Granitoids in the Central Lesser Xing'an Range,NE China and Its Tectonic Implications[J]. Acta Petrologica Sinica,2013,29(2):354-368.
[44] Yu J J,Wang F,Xu W L,et al. Early Jurassic Mafic Magmatism in the Lesser Xing'an-Zhangguangcai Range,NE China,and Its Tectonic Implications:Constraints from Zircon U-Pb Chronology and Geochemistry[J]. Lithos,2012, 142/143:256-266.
[45] 刘翠,邓晋福,许立权,等.大兴安岭-小兴安岭地区中生代岩浆-构造-钼成矿地质事件序列的初步框架[J].地学前缘,2011,18(3):166-178. Liu Cui,Deng Jinfu,Xu Liquan,et al. A Preliminary Frame of Magma-Tectonic-Mo Metallogenic Events of Mesozoic Era in Da Hinggan Mountains and Xiao Hinggan Mountains Areas[J]. Earth Science Frontiers,2011,18(3):166-178.
[46] Kravchinsky V A,Cogné J P,Harbert W P,et al. Evolution of the Mongol-Okhotsk Ocean as Constrained by New Palaeom Agnetic Data from the Mongol-Okhotsk Suture Zone,Siberia[J]. Geophysical Journal of the Royal Astronomical Society,2010,148(1):34-57.
[47] Kelty T K,An Y,Dash B,et al. Detrita-Zircon Geochronology of Paleozoic Sedimentary Rocks in the Hangay-Hentey Basin,North-Central Mongolia:Implications for the Tectonic Evolution of the Mongo-Okhotsk Ocean in Central Asia[J]. Tectonophysics,2008,451(1):290-311.
[48] Zorin Y. Geodynamics of the Western Part of the Mongolia-Okhotsk Collisional Belt,Trans-Baikal Region (Russia) and Mongolia[J].Tectonophysics,1999,306(1):45-67.
[49] Xu W L,Pei F P,Wang F,et al. Spatial-Temporal Relationships of Mesozoic Volcanic Rrocks in NE China:Constraints on Tectonic Overprinting and Transformations Between Multiple Tectonic Regimes[J]. Journal of Asian Earth Sciences, 2013,74(4):167-193.
[50] 孟恩,许文良,杨德彬,等.满洲里地区灵泉盆地中生代火山岩的锆石U-Pb年代学、地球化学及其地质意义[J].岩石学报,2011,27(4):1209-1226. Meng En,Xu Wenliang,Yang Debin,et al. Zircon U-Pb Chronology,Geochemistry of Mesozoic Volcanic Rocks from the Lingquan Basin in Manzhouli Area,and Its Tectonic Implications[J]. Acta Petrologica Sinica,2011,27(4):1209-1226.
[51] 徐文喜.小兴安岭-张广才岭成矿带钼矿床岩石地球化学特征及地球动力学研究[J].吉林地质,2018,37(1):38-44. Xu Wenxi. Lithogeochemical Characteristics and Geodynamics of the Molybdenum Deposits in Xiao Hinggan Mountains-Zhangguangcai Range Metallogenic Belt[J]. Jilin Geology, 2018,37(1):38-44.
[52] 裴福萍,许文良,孟恩.等.古太平洋俯冲作用的开始:来自吉黑东部早-中侏罗世火山岩的年代学及地球化学证据[J].矿物岩石地球化学通报,2008,27(增刊1):268. Pei Fuping, Xu Wenliang, Meng En. et al. The Beginning of Paleo-Pacific Subduction:Evidence from Chronology and Geochemistry of the Early-Middle Jurassic Volcanic Rocks in Eastern Jihei[J]. Bulletin of Mineralogy,Petrology and Geochemistry, 2008, 27(Sup.1):268.
[53] Zhou J B,Wilde S A,Zhao G C,et al. New SHRIMP U-Pb Zircon Ages from the Heilongjiang High-Pressure Belt:Constraints on the Mesozoic Evolution of NE China[J]. American Journal of Science,2010,310(9):1024-1053.
[54] 周建波,蒲先刚,侯贺晟,等.东北中生代增生杂岩及对古太平洋向欧亚大陆俯冲历史的制约[J].岩石学报,2018, 34(10):2845-2856. Zhou Jianbo, Pu Xiangang, Hou Hesheng, et al. The Mesozoic Accretionary Complex in NE China and Its Tectonic Implications for the Subduction of the Paleo-Pacific Plate Beneath the Eurasia[J]. Acta Petrologica Sinica, 2018, 34(10):2845-2856.
[55] 王五力,李永飞,郭胜哲,等.中国东北地块群及其构造演化[J].地质与资源,2014,23(1):4-24. Wang Wuli,Li Yongfei,Guo Shengzhe,et al.The Northeast Block Group and Its Tectonic Evolution[J].Geology and Resources,2014,23(1):4-24.
[56] 葛文春,吴福元,周长勇,等.兴蒙造山带东段斑岩型Cu,Mo矿床成矿时代及其地球动力学意义[J].科学通报, 2007,57(20):2407-2417. Ge Wenchun, Wu Fuyuan, Zhou Changyong, et al. The Metallogenic Age and Geodynamic Significance of Porphyry Cu and Mo Deposits in the Eastern Segment of the Xingmeng Orogenic Belt[J].Chinese Science Bulletin, 2007,57(20):2407-2417.
[57] 孙德有,吴福元,高山,等.吉林中部晚三叠世和早侏罗世两期铝质A型花岗岩的厘定及对吉黑东部构造格局的制约[J].地学前缘,2005,12(2):263-275. Sun Deyou, Wu Fuyuan, Gao Shan, et al. Confirmation of Two Episodes of A-Type Granite Emplacement During Late Triassic and Early Jurassic in the Central Jilin Province, and Their Constraints on the Structural Pattern of Eastern Jilin-Heilongjiang Area,China[J]. Earth Science Frontiers, 2005,12(2):263-275.
[58] 周建波,曾维顺,曹嘉麟,等.中国东北地区的构造格局与演化:从500 Ma到180 Ma[J].吉林大学学报(地球科学版),2012,42(5):1298-1316. Zhou Jianbo,Zeng Weishun,Cao Jialin, et al. The Tectonic Framework and Evolution of the NE China:From~500 Ma to~180 Ma[J]. Journal of Jilin University(Earth Science Edition),2012,42(5):1298-1316.
[1] 余振东, 项新葵, 谭荣, 孙德明, 张斯. 赣北大湖塘平苗矿段白云母花岗岩锆石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), 2020, 50(5): 1505-1517.
[2] 赵亚云, 刘晓峰, 刘远超, 次琼, 郑常云, 杨春四, 李莉, 付海龙. 西藏昂仁县多仁则—桑阿卡地区铜多金属矿点含矿岩体成因及成矿意义[J]. 吉林大学学报(地球科学版), 2020, 50(5): 1323-1339.
[3] 贺根文, 路思明, 彭琳琳, 于长琦, 李伟, 刘翠辉. 赣南狮吼山硫铁多金属矿区花岗岩地球化学、年代学特征及其成因[J]. 吉林大学学报(地球科学版), 2020, 50(5): 1491-1504.
[4] 孙海瑞, 吕志成, 于晓飞, 李永胜, 杜泽忠, 吕鑫, 公凡影. 甘肃柳园地区早二叠世正长花岗斑岩脉锆石U-Pb年代学、岩石地球化学特征——对北山造山带晚古生代构造背景的指示[J]. 吉林大学学报(地球科学版), 2020, 50(5): 1433-1449.
[5] 任文恺, 王生云, 陈礼标, 吴少锋, 张海青. 青海同仁兰采地区花岗闪长岩LA-ICP-MS锆石U-Pb年代学、地球化学特征及其地质意义[J]. 吉林大学学报(地球科学版), 2020, 50(4): 1059-1074.
[6] 蔡永丰, 刘风雷, 冯佐海, 周云, 曾长育. 桂东北姑婆山岩体矿物学和年代学特征及其成岩成矿意义[J]. 吉林大学学报(地球科学版), 2020, 50(3): 842-856.
[7] 陈会军, 于宏斌, 马永非, 陈井胜, 钱程, 刘世伟, 崔天日, 钟辉. 吉东南地区五女峰岩体锆石U-Pb年代学、岩石地球化学特征及其构造意义[J]. 吉林大学学报(地球科学版), 2020, 50(2): 531-541.
[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] 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.
[10] 张超, 吴新伟, 张渝金, 郭威, 权京玉. 龙江盆地中生代火山岩锆石U-Pb年代学及其对基底性质的制约[J]. 吉林大学学报(地球科学版), 2019, 49(2): 460-476.
[11] 尹志刚, 李海娜, 张海, 郝科, 庞学昌, 宫兆民, 李敏, 张圣听. 大兴安岭加格达奇东北部花岗岩类形成时代、地球化学特征及成因[J]. 吉林大学学报(地球科学版), 2018, 48(6): 1741-1755.
[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.
[13] 付俊彧, 汪岩, 钟辉, 宋维民, 孙巍, 那福超, 钱程, 杨雅军, 庞雪娇, 江山. 内蒙古突泉县牤牛海地区超镁铁质岩地球化学及源区特征[J]. 吉林大学学报(地球科学版), 2017, 47(4): 1172-1186.
[14] 赵院冬, 车继英, 吴大天, 许逢明, 赵君, 李士超. 小兴安岭西北部早—中侏罗世TTG花岗岩年代学、地球化学特征及构造意义[J]. 吉林大学学报(地球科学版), 2017, 47(4): 1119-1137.
[15] 张立敏, 王岳军, 张玉芝, 刘汇川, 张新昌. 海南岛北部古生界时代:碎屑锆石U-Pb年代学约束[J]. 吉林大学学报(地球科学版), 2017, 47(4): 1187-1206.
Viewed
Full text


Abstract

Cited

  Shared   
  Discussed   
No Suggested Reading articles found!