吉林大学学报(地球科学版) ›› 2017, Vol. 47 ›› Issue (6): 1763-1783.doi: 10.13278/j.cnki.jjuese.201706114

• 地质与资源 • 上一篇    下一篇

滇东南猛洞岩群斜长角闪岩成因及其构造意义

谭洪旗1,2, 刘玉平3   

  1. 1. 中国地质科学院矿产综合利用研究所, 成都 610041;
    2. 成都理工大学地球科学学院, 成都 610059;
    3. 中国科学院地球化学研究所/矿床地球化学国家重点实验室, 贵阳 550002
  • 收稿日期:2017-03-06 出版日期:2017-11-26 发布日期:2017-11-26
  • 通讯作者: 刘玉平(1971),男,研究员,博士,主要从事矿床学、同位素年代学方面的研究,E-mail:liuyuping@vip.gyig.ac.cn E-mail:liuyuping@vip.gyig.ac.cn
  • 作者简介:谭洪旗(1984),男,工程师,主要从事区域地质调查方面的研究,E-mail:hongqitan@163.com
  • 基金资助:
    国家重点基础研究发展计划（"973"计划）项目（G2007CB411408）；国家自然科学基金项目（41603034，40972129）

Genesis of Amphibolite in Mengdong Group-Complex in Southeastern Yunnan and Its Tectonic Significance

Tan Hongqi1,2, Liu Yuping3   

  1. 1. Institute of Multipurpose Utilization of Mineral Resources, CAGS, Chengdu 610041, China;
    2. College of Earth Science, Chengdu University of Technology, Chengdu 610059, China;
    3. Institute of Geochemistry/State Key Laboratory of Ore Deposit Geochemistry, Chinese Academy of Sciences, Guiyang 550002, China
  • Received:2017-03-06 Online:2017-11-26 Published:2017-11-26
  • Supported by:
    Supported by National Key Basic Research Program of China(G2007CB411408) and National Natural Science Foundation of China(41603034,40972129)

PDF (PC)

411

摘要： 滇东南老君山地区发育猛洞岩群前寒武系斜长角闪岩，呈港湾状分布在片岩、片麻岩中，并为后期变质-变形作用叠加改造。斜长角闪岩SiO2质量分数为47.0%~50.4%，西蒙尼图解、DF及A-K图解均显示其原岩为正变质岩，因此推测为一套变质基性岩。斜长角闪岩地球化学特征显示，稀土总量w（ΣREE）=（214~267）×10-6，高于洋岛玄武岩，其配分模式与洋岛玄武岩相似，为轻稀土富集的右倾曲线；蛛网图显示Ba、Zr、Hf、Y元素亏损，富集Rb、Th、Ta、Nb、Ce、Sm元素，与板内碱性玄武岩特征类似；Zr/TiO2-Nb/Y、TiO2-10MnO-10P2O5、La/10-Nb/8-Y/15、Th/Zr-Nb/Zr、Th/Hf-Ta/Hf等判别图解显示，原岩为一套亚碱性-碱性玄武岩岩浆系列，其形成可能与大陆裂谷环境有关。角闪石及斜长石内部指示的（亚）显微结构较为发育，主要有自由位错、位错列，偶见位错环或位错偶极，与角闪石-斜长石矿物对获得的平均温度和压力（646℃、0.88 GPa）一致，最高变质程度达低角闪岩相；同时，前人获得榍石U-Pb年代学及南温河片麻岩状花岗岩变质增生锆石均为230 Ma左右，代表印支期构造-热事件，此时老君山变质核杂岩雏形开始形成。

关键词: 斜长角闪岩, 地球化学, 构造意义, 滇东南, 猛洞岩群

Abstract: Existingin schist and gneiss in Mengdong Group-Complex,the amphibolite belongs to Precambrian Formation in Laojunshan area of southeastern Yunnan, on which metamorphism and deformation superposed. The content of SiO2 ranges from 47.0% to 50.4%. In the discrimination diagrams of Simonen,DF and A-K,it falls in the series of orthometamorphite derived from meta-basite rock. Its geochemical characters show that the total REE contents of amphibolite (w(ΣREE)=(214-267)×10-6) exceed those of oceanic island basalt, while its distribution pattern is similar to that of oceanic island basalt in steep right-dipping with light REE enrichment. The spider diagram shows that it is enriched in Rb,Th,Ta,Nb,Ce and Sm,while depleted of Ba,Zr,Hf and Y, similar to the characteristics of the alkaline basalts within plate. The discrimination diagrams of Zr/TiO2-Nb/Y, TiO2-10MnO-10P2O5,La/10-Nb/8-Y/15,Th/Zr-Nb/Zr,and Th/Hf-Ta/Hf suggest that their protolith should be of alkaline basalt magma series in a continental rift environment. The microstructures of amphibole and plagioclase indicate that the microstructure is relatively free, with free dislocations and dislocation columns, occasionally dislocation rings or dislocation dipoles,which is in accordance with the average pressure and temperature of hornblende-plagioclase minerals of 0.88 GPa and 646℃ respectively, confirming that the highest metamorphic grade is of low amphibolite facies. According to the U-Pb dating of sphenes in plagiogneiss and metamorphic overgrowth zircon in Nanwenhe gneissic granite (230 Ma),the deformation conditions were related to the Indosinian tectono-thermal events, and during this period, the embryo of Laojunshan complex began to form.

Key words: amphibolite, geochemical, tectonic significances, southeastern Yunnan, Mengdong Group-Complex

中图分类号: 

  • P588.3
[1] 肖玲玲,卢俊生,王国栋,等. 赞皇变质杂岩区西南部斜长角闪岩的地球化学、变质演化研究及其构造意义[J]. 岩石学报,2012,28(9):2807-2818. Xiao Lingling, Lu Junsheng, Wang Guodong, et al. Geochemistry, Metamorphic Evolution and Its Tectonic Implications of Amphibolites in the Southwest Area of the Zanhuang Complex[J].Acta Petrologica Sinica, 2012, 28(9):2807-2818.
[2] 王金荣,王廷印,高军平,等. 甘肃金塔南山斜长角闪岩的地球化学特征及其构造意义[J]. 岩石学报,2002,18(2):231-237. Wang Jinrong, Wang Tingyin, Gao Junping, et al. Geochemistry of the Amphibolites from Jinta Nanshan, Gansu Province:Implications for the Tectonic Setting[J]. Acta Petrological Sinica, 2002, 18(2):231-237.
[3] 王忠梅,肖文交,韩春明,等. 甘肃敦煌红柳峡地区石榴石斜长角闪岩的变质特征、锆石U-Pb年龄及地质意义[J]. 岩石学报,2013,29(5):1685-1697. Wang Zhongmei, Xiao Wenjiao, Han Chunming, et al. Metamorphism, Zircon U-Pb Dating and Tectonic Implications of Garnet Amphibolites from Hongliuxia, Dunhuang, Gansu Province[J]. Acta Petrologica Sinica, 2013, 29(5):1685-1697.
[4] Cao S Y, Liu J L, Leiss B. Orientation-Related Defor-mation Mechanisms of Naturally Deformed Amphibole in Amphibolite Mylonites from the Diancang Shan, SW Yunnan, China[J]. Journal of Structural Geology, 2010, 32:606-622.
[5] 曹淑云,刘俊来,胡玲. 角闪石高温脆-韧性转变变形的显微与亚微构造证据:以滇西点苍山深变质剪切糜棱岩为例[J]. 中国科学:D辑,2007,37(8):1004-1013. Cao Shuyun, Liu Junlai, Hu Ling. Micro-and Submicrostructural Evidence for High-Temperature Brittle-Ductile Transition Deformation of Hornblende:Case Study of High-Grade Mylonites from Diancangshan, Western Yunnan[J].Science in China:Series D, 2007, 50(10):1459-1470.
[6] 关会梅,刘俊来,赵胜金. 变形角闪质岩石流动变形及其意义:以辽东古元古宙褶皱带变形斜长角闪岩为例[J]. 吉林大学学报(地球科学版),2008,38(5):777-783. Guan Huimei, Liu Junlai, Zhao Shengjin. Flow and Deformation Mechanisms of Hornblende Rocks:Example of Deformed Amphibolites from the Paleoproterozoic Fold Belt in Liaodong Peninsula[J]. Journal of Jilin University(Earth Science Edition), 2008, 38(5):777-783.
[7] 胡玲. 显微构造地质学概论[M]. 北京:地质出版社,1998:1-158. Hu Ling. An Introduction to Microstructural Geology[M]. Beijing:Geological Publishing House, 1998:1-158.
[8] Tullis J. Deformation of Feldspars[J]. Mineral Soc Am Rev Mineral, 1983, 2:297-323.
[9] 纪沫,胡玲,刘俊来,等. 主要造岩矿物动态重结晶作用及其变质条件[J]. 地学前缘,2008,15(3):226-233. Ji Mo, Hu Ling, Liu Junlai, et al. Dynamic Recrystallization and Metamorphic Conditions of Main Rock-Forming Minerals[J]. Earth Science Frontiers, 2008, 15(3):226-233.
[10] 丁星妤,戴塔根,刘晓玮. 滇东南南部多金属成矿带找矿潜力分析[J]. 吉林大学学报(地球科学版),2012,42(6):1730-1739. Ding Xingyu, Dai Tagen, Liu Xiaowei. Ore Prospecting Potential of the Polymetallic Metallogenic Belt in the South of SE Yunnan[J]. Journal of Jilin University(Earth Science Edition), 2012, 42(6):1730-1739.
[11] 贾福聚,燕永锋,伍伟,等. 云南老君山锡多金属成矿区硫、铅、氢、氧同位素地球化学[J]. 吉林大学学报(地球科学版),2016,46(1):105-118. Jia Fuju, Yan Yongfeng, Wu Wei, et al. S, Pb, H and O Isotopic Geochemistry of Laojunshan Tin-Metallic Metallogenic Region, Southeastern Yunnan Province, China[J]. Journal of Jilin University(Earth Science Edition), 2016, 46(1):105-118.
[12] 刘玉平, 李正祥, 叶霖, 等. 滇东南老君山矿集区钨成矿作用Ar-Ar年代学[J]. 矿物学报,2011,33(增刊1):617-618. Liu Yuping, Li Zhengxiang, Ye Lin, et al. Ar-Ar Geochronology of Tungsten Mineralization in the Laojunshan Ore Concentration Area, Yunnan Province[J]. Acta Mineralogica Sinica, 2011, 31(Sup. 1):617-618.
[13] 谭洪旗,刘玉平,叶霖,等. 滇东南南秧田钨锡矿床金云母40Ar-39Ar定年及意义[J]. 矿物学报,2011,31(增刊1):639-640. Tan Hongqi, Liu Yuping, Ye Lin, et al. 40Ar-39Ar Dating of Phlogopite from W-Sn Deposits in the Nanyangtian, Southeastern Yunnan, and Its Implication[J]. Acta Mineralogica Sinica, 2011, 31(Sup. 1):639-640.
[14] 刘玉平,李朝阳,叶霖,等. 滇东南老君山变质核杂岩成矿特征及找矿方向[J]. 矿物岩石地球化学通报,2004,25(增刊1):130. Liu Yuping, Li Chaoyang, Ye Lin, et al. Metallogenic Characteristics and Prospecting Direction of Laojunshan Metamorphic Core Complex in Southeastern Yunnan Province[J]. Bulletin of Mineralogy, Petrology and Geochemistry, 2004, 25(Sup. 1):130.
[15] 李东旭,许顺山. 变质核杂岩的旋扭成因:滇东南老君山变质岩的构造解析[J]. 地质论评,2000,46(2):113-119. Li Dongxu, Xu Shunshan. Rotation-Shearing Genesis of Metamorphic Core Complex:Structural Analysis of Metamorphic Core Complex in Laojunshan, Southeastern Yunnan Province[J]. Geological Review, 2000, 46(2):113-119.
[16] 郭利果. 滇东南老君山变质核杂岩地球化学和年代学初步研究[D]. 贵阳:中国科学院地球化学研究所,2006:1-120. Guo Liguo. Primary Research on Geochemistry and Geochronology of the Laojunshan Metamorphic Core Complex, Southeastern Yunnan[D].Guiyang:Institute of Geochemistry, Chinese Academy of Sciences, 2006:1-120.
[17] 张世涛,冯明刚,吕伟. 滇东南南温河变质核杂岩解析[J]. 中国区域地质,1998,17(4):390-397. Zhang Shitao, Feng Minggang, Lü Wei. Analysis of the Nanwenhe Metamorphic Core Complex in Southeastern Yunnan[J]. Regional Geology of China, 1998, 17(4):390-397.
[18] Liu Y P, Ye L, Li C Y, et al. Laojunshan-Song Chay Metamorphic Core Complex and Its Structure Significance[J]. Geochimica et Cosmochimica Acta, 2003, 67(18):A259.
[19] 颜丹平,周美夫,王焰,等. 都龙Song Chay变质穹窿体变形与构造年代:南海盆地北缘早期扩张作用始于华南地块张裂的证据[J]. 地球科学:中国地质大学学报,2005,30(4):402-411. Yan Danping, Zhou Meifu, Wang Yan, et al. Structural Styles and Chronological Evidences from Dulong-Song Chay Tectonic Dome:Earlier Spreading of South China Sea Basin Due to Late Mesozoic to Early Cenozoic Extension of South China Block[J].Earth Science:Journal of China University of Geosciences, 2005,30(4):402-411.
[20] Yan D P, Zhou M F, Wan Y C, et al. Structural and Geochronological Constraints on the Dulong-Song Chay Tectonic Dome in SE Yunnan(SW China) and Northern Vietnam[J]. Journal of Asian Earth Sciences, 2006, 28(4):332-353.
[21] 吕伟,冯明刚,胡长寿. 滇东南南温河地区猛洞岩群变质作用特征[J]. 云南地质,2001,20(1):25-33. Lü Wei, Feng Minggang, Hu Changshou. Metamorphism of Mengdong Lithological Group in Nanwenhe Area of Southeast Yunnan[J]. Yunnan Geological, 2001, 20(1):25-33.
[22] 陈学明,林棕,谢福昌. 云南白牛厂超大型银多金属矿床叠加成矿的地质地化特征[J]. 地质科学,1998,33(1):115-124. Chen Xueming, Lin Zong, Xie Fuchang. Geological and Geochemical Characteristic of the Bainiuchang Superlarge Silver Polymetallic Deposit of Superimposed[J]. Scientia Geologica Sinica, 1998, 33(1):115-124.
[23] 徐伟. 滇东南南温河花岗岩年代学和地球化学初步研究[D]. 贵阳:中国科学院地球化学研究所,2007:1-72. Xu Wei.Primary Research on Geochronology and Geochemistry of Nanwenhe Granite, Southeast Yunnan[D].Guiyang:Institute of Geochemistry, Chinese Academy of Sciences, 2007:1-72.
[24] Guo L G, Liu Y P, Li C Y, et al. SHRIMP Zircon U-Pb Geochronology and Lithogeochemistry of Caledonian Granites from the Laojunshan Area, Southeastern Yunnan Province, China:Implications for the Collision Between the Yangtze and Cathaysia Blocks[J]. Geochemical Journal, 2009, 43:101-122.
[25] 谭洪旗,刘玉平,徐伟,等. 中-浅正变质岩锆石SHRIMP法与TIMS法测年结果不一致处理:以滇东南南温河花岗岩为例[J]. 矿物学报,2011,31(1):62-69. Tan Hongqi, Liu Yuping, Xu Wei, et al. A Study on SHRIMP and TIMS Zircon Dating on Low to Medium Grade Ortho-Metamorphic Rocks:Example on the Nanwenhe Granites, Southeastern Yunnan Province, China[J]. Acta Mineralogica Sinica, 2011, 31(1):62-69.
[26] 张斌辉,丁俊,任光明,等. 云南马关老君山花岗岩的年代学、地球化学特征及地质意义[J].地质学报,2012,86(4):587-601. Zhang Binhui, Ding Jun, Ren Guangming, et al. Geochronology and Geochemical Characteristics of the Laojunshan Granites in Maguan County, Yunnan Province, and Its Geological Implications[J].Acta Geologica Sinica, 2012, 86(4):587-601.
[27] 王丹丹,李宝龙,朱德全,等. 滇东南老君山地区变质岩锆石U-Pb年代学及其构造意义[J]. 地质学报,2015,89(10):1718-1734. Wang Dandan, Li Baolong, Zhu Dequan, et al. Zircon U-Pb Geochronology of Metamorphic Complex in the Laojunshan District, Southeastern Yunnan Province and Its Tectonic Implication[J]. Acta Geologica Sinica, 2015, 89(10):1718-1734.
[28] Peng T P, Fan W M, Zhao G C, et al. Petrogenesis of the Early Paleozoic Strongly Peraluminous Granites in the Western South China Block and Its Tectonic Implications[J]. Journal of Asian Earth Sciences, 2015, 98:399-420.
[29] Xu B, Jiang S Y, Hofmann A W, et al. Geoch-ronology and Geochemical Constraints on Petrogenesis of Early Paleozoic Granites from the Laojunshan District in Yunnan Province of South China[J]. Gondwana Research, 2016, 29:248-263.
[30] Roger F, Leloup P H, Jolivet M, et al. Long and Co-mplex Thermal History of the Song Chay Metamorphic Dome (Northern Vietnam) by Multi-System Geochronology[J]. Tectonophysics, 2000, 321:449-466.
[31] Carter A, Roques D, Bristow C, et al. Understan-ding Mesozoic Accretion in Southeast Asia:Significance of Triassic Thermotectonism (Indosinian Orogeny) in Vietnam[J]. Geology, 2001, 29:211-214.
[32] 刘玉平,李正祥,李惠民,等. 都龙锡锌矿床锡石和锆石U-Pb年代学:滇东南白垩纪大规模花岗岩成岩-成矿事件[J]. 岩石学报,2007,23(5):967-976. Liu Yuping, Li Zhengxiang, Li Huimin, et al. U-Pb Geochronology of Cassiterite and Zircon from Dulong Sn-Zn Deposit:Evidence for Cretaceous Large-Scale Granitic Magmatism and Mineralization Events in Southeastern Yunnan Province, China[J]. Acta Petrologica Sinica, 2007, 23(5):967-976.
[33] 程彦博,毛景文,谢桂青,等. 云南个旧老厂-卡房花岗岩体成因:锆石U-Pb年代学和岩石地球化学约束[J]. 地质学报,2008,82(11):1478-1493. Cheng Yanbo, Mao Jingwen, Xie Guiqing, et al. Petrogenesis of the Laochang-Kafang Granite in the Gejiu Area, Yunnan Province:Constraints from Geochemistry and Zircon U-Pb Dating[J]. Acta Geologica Sinica, 2008, 82(11):1478-1493.
[34] 程彦博,毛景文,陈小林,等. 滇东南薄竹山花岗岩的LA-ICP-MS锆石U-Pb定年及地质意义[J]. 吉林大学学报(地球科学版),2010,40(4):869-878. Cheng Yanbo, Mao Jingwen, Chen Xiaolin, et al. LA-ICP-MS Zircon U-Pb Dating of the Bozhushan Granite in Southeastern Yunnan Province and Its Significance[J].Journal of Jilin University (Earth Science Edition), 2010, 40(4):869-878.
[35] 冯佳睿,毛景文,裴荣富,等. 云南瓦渣钨矿区老君山花岗岩体的SHRIMP锆石U-Pb定年、地球化学特征及成因探讨[J]. 岩石学报,2010,26(3):845-857. Feng Jiarui, Mao Jingwen, Pei Rongfu, et al. SHRIMP Zircon U-Pb Dating and Geochemical Characteristics of Laojunshan Granite Intrusion from the Wazha Tungsten Deposit, Yunnan Province and Their Implications for Petrogenesis[J]. Acta Petrologica Sinica, 2010, 26(3):845-857.
[36] 刘艳宾,莫宣学,张达,等. 滇东南老君山地区晚白垩世花岗岩的成因[J]. 岩石学报,2014,30(11):3271-3286. Liu Yanbin, Mo Xuanxue, Zhang Da, et al. Petrogenesis of the Late Cretaceous Granite Discovered in the Laojunshan Region, Southeastern Yunnan Province[J]. Acta Petrologica Sinica, 2014, 30(11):3271-3286.
[37] 谭洪旗,刘玉平. 滇东南猛洞岩群构造环境:变质碎屑岩地球化学约束[J]. 地质学报,2017,91(7):1416-1432. Tan Hongqi, Liu Yuping. Tectonic Setting of the Mengdong Group-Complex, Southeast Yunnan Province:Constraints from Geochemical of Metasedimentary Rocks[J]. Acta Geologica Sinica, 2017, 91(7):1416-1432.
[38] 谭洪旗,刘玉平. 滇东南猛洞岩群变质-变形研究及构造意义[J]. 地质学报,2017,91(1):15-42. Tan Hongqi, Liu Yuping. Metamorphic-Deformation of Mengdong Group-Complex and Their Tectonic Implication, Southeastern Yunnan Province[J]. Acta Geologica Sinica, 2017, 91(1):15-42.
[39] 刘玉平,叶霖,李朝阳,等. 滇东南发现新元古代岩浆岩:SHRIMP锆石U-Pb年代学和岩石地球化学证据[J]. 岩石学报,2006,22(4):916-926. Liu Yuping, Ye Lin, Li Chaoyang, et al. Discovery of the Neoproterozoic Magmatics in Southeastern Yunnan:Evidence from SHRIMP Zircon U-Pb Dating and Lithogeochemistry[J]. Acta Petrologica Sinica, 2006, 22(4):916-926.
[40] 蔡永丰,王岳军,刘汇川,等. 哀牢山新元古代斜长角闪岩的形成时代、地球化学特征及其大地构造意义[J]. 大地构造与成矿学,2014,38(1):168-180. Cai Yongfeng, Wang Yuejun, Liu Huichuan, et al. Geochronological and Geochemical Characteristics of the Neoproterozoic Amphibolite from Ailaoshan Zone, Western Yunnan and Its Tectonic Implications[J]. Geotectonica et Metallogenia, 2014, 38(1):168-180.
[41] 王冬兵,唐渊,廖世勇,等. 滇西哀牢山变质岩系锆石U-Pb定年及其地质意义[J]. 岩石学报,2013,29(4):1261-1278. Wang Dongbing, Tang Yuan, Liao Shiyong, et al. Zircon U-Pb Dating and Its Geological Implications of the Metamorphic Rock Series in Ailao Shan Ranges, Western Yunnan[J]. Acta Petrologica Sinica, 2013, 29(4):1261-1278.
[42] Qi L,Gregoire D C. Determination of Trace Elements in Twenty Six Chinese Geochemistry Reference Materials by Inductively Coupled Plasma-Mass Spectrometry[J]. Geostandards Newslett, 2000, 24:51-63.
[43] 路远发. GeoKit:一个用VBA构建的地球化学工具软件包[J]. 地球化学,2004,33(5):459-464. Lu Yuanfa. Geokit:A Geochemical Toolkit for Microsoft Excel[J]. Geochimica, 2004, 33(5):459-464.
[44] GB/T 15617-2002硅酸盐矿物的电子探针定量分析方法[S]. 北京:中华人民共和国国家质量监督检验检疫总局,2003. GB/T 15617-2002 A quantitative Analysis Method for the Electron Probe of Silicate Minerals[S]. Beijing:General Administration of Quality Supervision, Inspection and Quarantine of the People's Republic of China, 2003.
[45] Wilson M. Igneous Petrogenesis[M]. London:Unwin Hyman, 1989:1-466.
[46] Shaw D M. The Origin of the Apsley Gneiss, Ontario[J]. Can J Earth Sci, 1972, 9(1):18-35.
[47] 周世泰. 对17种恢复变质岩原岩的岩石化学方法的检验结果[J]. 地质论评,1984,30(1):81-84. Zhou Shitai. Examination of 17 Petrochemical Methods of Restoring Protoliths of Metamorphic Rocks[J]. Geological Review, 1984, 30(1):81-84.
[48] 王仁民,贺高品,陈珍珍,等. 变质岩原岩图解判别法[M]. 北京:地质出版社,1987:1-199. Wang Renmin, He Gaopin, Chen Zhenzhen, et al. Using Diagrams Disciminate Metamorphic Rock of the Original Rock[M]. Beijing:Geological Publishing House, 1987:1-199.
[49] 王中刚,于学元,赵振华. 稀土元素地球化学[M]. 北京:科学出版社,1989:1-535. Wang Zhonggang, Yu Xueyuan, Zhao Zhenhua. Rare Earth Element Geochemistry[M]. Beijing:Science Press, 1989:1-535.
[50] 赵振华. 微量元素地球化学原理[M]. 北京:科学出版社,1997:1-238. Zhao Zhenhua. The Principle of Trace Element Geochemical[M]. Beijing:Science Press,1997:1-238.
[51] Sun S S, McDonough W F. Chemical and Isotopic Systematics of Ocean Basalts:Implications for Mantle Composition and Process[C]//Saunders A D, Norry M J. Magmatism in Ocean Basins. London:Geological Society, Special Publications, 1989:313-345.
[52] Pearce J A. Trace Elements Characteristics of Lavas from Destructive Plate Boundaries[C]//Thorpe R S. Andesites. New Yolk:John Willey and Suns, 1982:525-548.
[53] Leake B E, Woolley A R, Arps C E S, et al. Nomen-clature of Amphiboles:Report of the Subcommittee on Amphiboles of the International Mineralogical Association, Commission on New Minerals and Mineral Names[J]. Can Mineral, 1997, 35:219-246.
[54] Leake B E, Woolley A R, Birch W D, et al. Nomen-clature of Amphiboles:Additions and Revisions to the International Mineralogical Association's Amphibole Nomenclature[J]. Can Mineral, 2003, 41:1355-1370.
[55] Holland T, Blundy J. Non-Ideal Interactions in Calcic Amphiboles and Their Bearing on Amphibole-Plagioclase Thermometry[J]. Contrib Mineral Petrol, 1994, 116:433-447.
[56] Blundy J D, Holland T J. Calcic Amphibole Equilibria and a New Amphibole-Plagioclase Geothermometer[J]. Contrib Mineral Petrol, 1990, 104:208-224.
[57] Schmidt M W. Amphibole Composition in Tonalite as a Function of Pressure:An Experimental Calibration of the Al in Hornblende Barometer[J]. Contributions to Mineralogy and Petrology, 1992, 110:304-310.
[58] Anderson J L, Smith D R.The Effect of Temperature and Oxygen Fugacity on Al-in-Hornblende Barometry[J].American Mineralogist, 1995, 80:549-559.
[59] Bhadra S, Bhattacharya A. The Barometer Tremolite + Tschermakite +2 Albite=2 Pargasite +8 Quartz:Constraints from Experimental Data at Unit Silica Activity, with Application to Garnet-Free Natural Assemblages[J]. American Mineralogist, 2007, 92:491-502.
[60] Hammarstrom, Zenk. Aluminum in Hornblende:An Empirical Igneous Geobarometer[J]. American Mineralogist, 1986, 71:1297-1313.
[61] Holdaway M J, Mukhopadhyay B.A Reevaluation of the Stability Relations of Andalusite:Thermochemical Data and Phase Diagram for the Aluminum Silicates[J].American Mineralogist, 1993, 78:298-315.
[62] 薛治君,白学让,陈武. 成因矿物学[M]. 武汉:武汉地质学院出版社,1986:1-179. Xue Zhijun, Bai Xuerang, Chen Wu. Genetic Mineralogy[M]. Wuhan:Wuhan College of Geosciences Press, 1986:1-179.
[63] 章邦桐,凌洪飞,陈培荣,等. 正、副角闪岩判别标志的新认识:赣中前寒武纪正、副角闪岩的矿物-岩石地球化学特征对比研究[J]. 地质找矿论丛,2005,20(4):223-232. Zhang Bangtong, Ling Hongfei, Chen Peirong, et al. New Recognition Criteria for Ortho and Para Amphibolites:The Comparative Study on Mineral Petrochemical from Xiangshan, Central Jiangxi Province[J]. Contributions to Geology and Mineral Resources Research, 2005, 20(4):223-232.
[64] Winchester J A, Floyd P A.Geochemical Discrimi-nation of Different Magma Series and Their Differentiation Products Using Immobile Elements[J].Chemical Geology, 1977, 20:325-343.
[65] Condie K C. Geochemical Changes in Basalts and Andesites Across the Archaean-Proterozoic Boundary:Identification and Significance[J]. Lithos, 1989, 23:l-18.
[66] 董云鹏,朱炳泉,常向阳,等. 滇东师宗弥勒带北段基性火山岩地球化学及其对华南大陆构造格局的制约[J]. 岩石学报,2002,18(1):37-46. Dong Yunpeng, Zhu Bingquan, Chang Xiangyang, et al. Geochemistry of Basalts from North of the Shizong-Mile Belt, Eastern Yunnan Province:Constraints on the Tectonic Framework of the South China Continent[J]. Acta Petrologica Sinica, 2002,18(1):37-46.
[67] Mullen E D. MnO/TiO2/P2O5:A Minor Element Discriminant for Basaltic Rocks of Oceanic Environments and Its Implication for Petro Genesis[J]. Earth Planet Sci Lett,1983,62:53-63.
[68] Campbell I H, Griffiths R W. Implication of Mantle Plume Structure for the Evolution of Flood Basalts[J]. Earth and Planetary Science Letters, 1990, 99:79-93.
[69] 孙书勤,汪云亮,张成江. 玄武岩类岩石大地构造环境的Th、Nb、Zr判别[J]. 地质论评,2003,49(1):40-47. Sun Shuqin, Wang Yunliang, Zhang Chengjiang. Discrimination of the Tectonic Setting of Basalts by Th, Nb and Zr[J]. Geological Review, 2003, 49(1):40-47.
[70] 汪云亮,张成江,修淑芝. 玄武岩形成的大地构造背景的Th/Hf-Ta/Hf图解判别[J]. 岩石学报,2001,17(3):413-421. Wang Yunliang, Zhang Chengjiang, Xiu Shuzhi. Th/Hf -Ta/Hf Identification of Tectonic Setting of Basalts[J]. Acta Petrologica Sinica, 2001, 17(3):413-421.
[71] 舒良树. 华南前泥盆纪构造演化:从华夏地块到加里东期造山带[J]. 高校地质学报,2006,12(4):418-431. Shu Liangshu. PredevonianTectonic Evolution of South China:From Cathaysian Block to Caledonian Period Folded Orogenic Belt[J]. Geological Journal of China Universities, 2006, 12(4):418-431.
[72] 谭洪旗. 滇东南猛洞岩群变质-变形与地球化学研究[D]. 贵阳:中国科学院地球化学研究所,2010:1-86. Tan Hongqi. Metamorphism-Deformation and Geochemistry of the Mengdong Group-Complex, Southeastern Yunnan, China[D].Guiyang:Institute of Geochemistry, Chinese Academy of Sciences, 2010:1-86.
[73] Maluskia H, Lepvrierb C, Jolivetb L, et al. Ar-Ar and Fission-Rack Ages in the Song Chay Massif:Early Triassic and Cenozoic Tectonics in Northern Vietnam[J]. Journal of Asian Earth Sciences, 2001, 19:233-248.
[74] 符巩固,陈广浩,吴春明. 变质作用高峰期后的离子再交换与纯转换反应及对温度压力计算的影响[J]. 矿物岩石地球化学通报,2004,23(4):362-367. Fu Gonggu, Chen Guanghao, Wu Chunming. The Effects of Post-Peak Retrograde Ion-Exchange and Net Transfer Reactions on the Calculated Temperatures and Pressures[J]. Bulletin of Mineralogy, Petrology and Geochemistry, 2004, 23(4):362-367.
[75] 刘玉平,徐伟,廖震,等. 老君山变质核杂岩隆升的热历史解析与动力学机制探讨[J]. 矿物岩石地球化学通报,2007,26(增刊1):87-88. Liu Yuping, Xu Wei, Liao Zhen, et al. Thermal History Analytical and Dynamics Mechanism Discussed of the Laojunshan Metamorphic Core Complex Uplift[J]. Bulletin of Mineralogy, Petrology and Geochemistry, 2007, 26(Sup. 1):87-88.
[76] 徐先兵,张岳桥,贾东,等. 华南早中生代大地构造过程[J]. 中国地质,2009,36(3):573-593. Xu Xianbing, Zhang Yueqiao, Jia Dong, et al. Early Mesozoic Geotectonic Processes in South China[J]. Geology in China, 2009, 36(3):573-593.
[77] 张岳桥,徐先兵,贾东,等. 华南早中生代从印支期碰撞构造体系向燕山期俯冲构造体系转换的形变记录[J]. 地学前缘,2009,16(1):234-246. Zhang Yueqiao, Xu Xianbing, Jia Dong, et al. Deformation Record of the Change from Indosinian Collision-Related Tectonic System to Yanshanian Subduction-Related Tectonic System in South China During the Early Mesozoic[J]. Earth Science Frontiers, 2009, 16(1):234-246.
[1] 张强, 丁清峰, 宋凯, 程龙. 东昆仑洪水河铁矿区狼牙山组千枚岩碎屑锆石U-Pb年龄、Hf同位素及其地质意义[J]. 吉林大学学报(地球科学版), 2018, 48(4): 1085-1104.
[2] 郭春涛, 李如一, 陈树民. 塔里木盆地古城地区鹰山组白云岩稀土元素地球化学特征及成因[J]. 吉林大学学报(地球科学版), 2018, 48(4): 1121-1134.
[3] 崔亚川, 于介江, 杨万志, 张元厚, 崔策, 于介禄. 东天山觉罗塔格带黄山地区角闪辉长岩岩体的年代学、地球化学特征及岩石成因[J]. 吉林大学学报(地球科学版), 2018, 48(4): 1105-1120.
[4] 赵希林, 姜杨, 邢光福, 于胜尧, 彭银彪, 黄文成, 王存智, 靳国栋. 陈蔡早古生代俯冲增生杂岩对华夏与扬子地块拼合过程的指示意义[J]. 吉林大学学报(地球科学版), 2018, 48(4): 1135-1153.
[5] 王朝阳, 孟恩, 李壮, 李艳广, 靳梦琪. 吉东南新太古代晚期片麻岩类的时代、成因及其对早期地壳形成演化的制约[J]. 吉林大学学报(地球科学版), 2018, 48(3): 587-625.
[6] 尹业长, 郝立波, 赵玉岩, 石厚礼, 田午, 张豫华, 陆继龙. 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.
[7] 齐天骄, 薛春纪, 许碧霞. 新疆昭苏布合塔铜(金)矿化区花岗质岩石锆石U-Pb年龄、地球化学特征及其成因[J]. 吉林大学学报(地球科学版), 2018, 48(1): 132-144.
[8] 孙凡婷, 刘晨, 邱殿明, 鲁倩, 贺云鹏, 张铭杰. 大兴安岭东坡小奎勒河中基性侵入岩成因及地球动力学意义:锆石U-Pb年代学、元素和Hf同位素地球化学证据[J]. 吉林大学学报(地球科学版), 2018, 48(1): 145-164.
[9] 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.
[10] 施珂, 张达玉, 丁宁, 王德恩, 陈雪锋. 皖南逍遥岩体的年代学、地球化学特征及其成因分析[J]. 吉林大学学报(地球科学版), 2017, 47(6): 1746-1762.
[11] 陈治军, 任来义, 贺永红, 刘护创, 宋健. 银额盆地哈日凹陷银根组优质烃源岩地球化学特征及其形成环境[J]. 吉林大学学报(地球科学版), 2017, 47(5): 1352-1364.
[12] 王师捷, 徐仲元, 董晓杰, 杜洋, 崔维龙, 王阳. 华北板块北缘中段二叠纪的构造属性:来自火山岩锆石U-Pb年代学与地球化学的制约[J]. 吉林大学学报(地球科学版), 2017, 47(5): 1442-1457.
[13] 许中杰, 蓝艺植, 程日辉, 李双林. 句容地区下奥陶统仑山组海平面变化的碳酸盐岩地球化学记录[J]. 吉林大学学报(地球科学版), 2017, 47(5): 1458-1470.
[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] 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.
Viewed
Full text


Abstract

Cited
  Shared   
  Discussed   
No Suggested Reading articles found!
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