• 中国出版政府奖提名奖

    中国百强科技报刊

    湖北出版政府奖

    中国高校百佳科技期刊

    中国最美期刊

    留言板

    尊敬的读者、作者、审稿人, 关于本刊的投稿、审稿、编辑和出版的任何问题, 您可以本页添加留言。我们将尽快给您答复。谢谢您的支持!

    姓名
    邮箱
    手机号码
    标题
    留言内容
    验证码

    滇西澜沧江构造带中-南段澜沧群变质变形期次及Ar-Ar年代学约束

    毕丽莎 梁晓 王根厚 张海迪 王泉 吴春娇

    毕丽莎, 梁晓, 王根厚, 张海迪, 王泉, 吴春娇, 2018. 滇西澜沧江构造带中-南段澜沧群变质变形期次及Ar-Ar年代学约束. 地球科学, 43(9): 3252-3266. doi: 10.3799/dqkx.2018.999
    引用本文: 毕丽莎, 梁晓, 王根厚, 张海迪, 王泉, 吴春娇, 2018. 滇西澜沧江构造带中-南段澜沧群变质变形期次及Ar-Ar年代学约束. 地球科学, 43(9): 3252-3266. doi: 10.3799/dqkx.2018.999
    Bi Lisha, Liang Xiao, Wang Genhou, Zhang Haidi, Wang Quan, Wu Chunjiao, 2018. Metamorphism-Deformation Phases and Ar-Ar Chronological Constraints of the Lancang Group in the Middle and Southern Sections of the Lancangjiang Tectonic Belt, Western Yunnan. Earth Science, 43(9): 3252-3266. doi: 10.3799/dqkx.2018.999
    Citation: Bi Lisha, Liang Xiao, Wang Genhou, Zhang Haidi, Wang Quan, Wu Chunjiao, 2018. Metamorphism-Deformation Phases and Ar-Ar Chronological Constraints of the Lancang Group in the Middle and Southern Sections of the Lancangjiang Tectonic Belt, Western Yunnan. Earth Science, 43(9): 3252-3266. doi: 10.3799/dqkx.2018.999

    滇西澜沧江构造带中-南段澜沧群变质变形期次及Ar-Ar年代学约束

    doi: 10.3799/dqkx.2018.999
    基金项目: 

    中央高校基本科研业务费专项资金 2652014004

    中国地质调查局项目 12120115026901

    国家自然科学基金青年基金项目 41402177

    详细信息
      作者简介:

      毕丽莎(1988-), 女, 工程师, 主要从事固体矿产勘查方面的研究工作

      通讯作者:

      梁晓

    • 中图分类号: P54

    Metamorphism-Deformation Phases and Ar-Ar Chronological Constraints of the Lancang Group in the Middle and Southern Sections of the Lancangjiang Tectonic Belt, Western Yunnan

    • 摘要: 澜沧群变质变形过程的厘定有助于揭示澜沧江构造带的演化历史.通过对双江-惠民地区出露的中-低绿片岩相变质岩系与高压变质岩系的"构造-变质"双重解析,发现澜沧群变质岩系:(1)以挤压体制下的褶劈理S2为区域性面理,浅变质岩系中石英脉条带代表的面理S1与层理S0产状一致,并在第2期强烈压扁后与S2近平行;(2)构造样式与变质变形期次在研究区域内基本一致,表现为二叠纪-三叠纪两期次中深构造层次透入性变形为侏罗纪-新生代浅-表层次变形所叠加;(3)高压变质岩记录了两个期次的深层次构造变形,电气石与石榴石变斑晶具有明显的两阶段生长模式,核部(M1aD1a)可能代表了峰期榴辉岩相变质作用,边部代表折返过程中的蓝片岩相(M1bD1b)阶段.高压变质岩与浅变质岩第2期(M2D2)构造层次及变形样式一致,代表折返后的挤压拼贴过程,两者的剪切型褶劈理S2均指示上盘S向的剪切滑动.结合新生代三江地区发生的近90°块体旋转,恢复第2期为上盘指向E的逆冲剪切作用.通过对幸福变质石英砂岩白云母、小黑江多硅白云母和蓝闪石的40Ar-39Ar定年,以及对前人小黑江蓝闪石40Ar-39Ar年龄的重新解释,共厘定出澜沧群4个构造阶段:(1)高压变质岩第1期晚期(D1b)蓝片岩相变质作用(~250 Ma);(2)第2期(M2D2)中层次挤压(215~214 Ma);(3)浅变质岩系第3期早期(D3a)N-S向纵弯褶皱(111.9~103.7 Ma)与晚期(D3b)逆冲(~82.28 Ma);(4)第4期近E-W向纵弯褶皱(新生代,很可能晚于59.18 Ma).

       

    • 图  1  滇西三江构造带大地构造单元划分及澜沧江构造带地质简图

      修改自Heppe(2006)

      Fig.  1.  The general division of tectonic units in the Sanjiang orogenic belt and the geological sketch of the Lancangjiang tectonic belt in western Yunnan

      图  2  临沧幸福镇-澜沧县区域地质简图(a)及澜沧群各期次构造的极射赤平投影(下半球)(b)

      图a显示澜沧江构造带东西向构造分区,修改自王丹丹等(2014);图b显示幸福浅变质岩系、上允北小黑江高压变质岩系、澜沧-惠民浅变质岩系的各期次构造要素

      Fig.  2.  Geological sketch along Xingfu of Lincang-Lancang (a) and the lower hemisphere stereonets of the structures of each deformation stage (b)

      图  3  澜沧-惠民浅变质岩系变形特征

      图a显示面理S2上盘指向S的右行剪切滑动(双重逆冲构造);图b为细长的σ形不对称石香肠,指示上盘S向滑动;图c显示面理S2、S1与S0的置换关系;图d显示收缩型褶劈理(CCC);图e显示近N-S走向的低缓逆冲断层(D3b)截切第3期(D3a)N-S向纵弯褶皱;图f显示第3期(D3)NE向纵弯褶皱

      Fig.  3.  Deformation characteristics of the low-grade metamorphosed rock complex in Lancang-Huimin

      图  4  小黑江高压变质岩系的变形特征

      图a和图b显示面理S2为剪切型褶劈理,内部夹持的石英脉香肠指示上盘向南的左行滑动;图c显示第4期(D4)近E-W向纵弯褶皱与轴面劈理S4;图d显示低角度脆性正断层(D5)

      Fig.  4.  Deformation characteristics of the high-pressure metamorphic rocks in Xiaoheijiang

      图  5  幸福浅变质岩系的变形样式

      图a显示粉砂质或泥质千枚岩中面理S2已经完全置换透入性石英条带代表的第1期面理S1,同斜褶皱指示露头中两者呈平行状;图b~d显示石英砂岩中第3期(D3a)纵弯褶皱及其压溶轴面劈理对面理S2的置换,其中图d显示面理S3已经十分透入(对应Ar-Ar定年样品7-20-6-DKW1);图e显示D3b期脆韧性逆冲断层对D3a期直立褶皱的叠加;图f表明轴面劈理S4对透入性面理S2的置换

      Fig.  5.  Deformation style of shallow metamorphosed clastic rocks in Xingfu

      图  6  澜沧群变质岩系的显微变形特征和构造期次划分

      图a为澜沧-上允浅变质岩系面理S2的显微特征,绢云母/白云母显微形态显示两期变形面理(与图 3c露头相邻);图b为幸福石英砂岩中面理S3对S2的置换,变质相明显高于澜沧-惠民地区(对应Ar-Ar定年样品7-20-6-DKW1);图c显示小黑江多硅白云母片岩中透入性面理S2及后期压溶面理S3,蓝闪石和榍石已明显定向,表明蓝片岩与云母片岩的混合不晚于面理S2时代;图d为多硅白云母片岩中面理S2夹持的电气石构造前变斑晶,核部富集针状蓝闪石(D1a),并被干净的边部(D1b)包围;图e显示多硅白云母片岩中面理S2夹持的石榴石构造前变斑晶,具有两个期次的自形结构,核部白云母等包裹体呈S形(D1a),边部环带干净(D1b);图f显示蓝片岩中透入性面理S2和塑性拉长后的定向蓝闪石、钠长石、绿帘石

      Fig.  6.  Microscopic characteristics of metamorphism/deformation and the classification of structural sequence for Lancang Group

      图  7  澜沧群高压变质矿物40Ar-39Ar年龄谱及白云母Arrhenius图解

      图a为幸福白云母Ar-Ar年龄谱,以及逐步加热过程中10个加热阶段的Ca/K比值变化趋势;图b为重新定义的赵靖等(1994b)粟义蓝闪石Ar-Ar年龄谱;图c~e为白云母York、Arrhenius图解,图d中T为开尔文温度

      Fig.  7.  40Ar-39Ar age spectrum of the high-pressure metamorphic minerals and the Arrhenius diagram of muscovite form Lancang Group

      表  1  澜沧群浅变质岩系二叠纪以后的变质变形期次划分

      Table  1.   The division of the multi-stage metamorphism/deformation since Permian for epimetamorphic rocks of Lancang Group

      期次 变质相 变形样式及层次 时代
      M1D1 澜沧-惠民:低绿片岩相,Chl+Ser+Qtz±Bi
      幸福:部分达中-高绿片岩相,Mus+Ab+Qtz
      递进剪切流变,伴随强烈的压溶分异,绢云母或白云母定向排列构成透入性面理S1,微劈石域见石英脉条带. P2-T2
      M2D2 澜沧-惠民:<低绿片岩相,±Ser±Chl
      幸福:低绿片岩相
      压扁+简单剪切,S1褶皱形成褶劈理S2,沿劈理面指向E的剪切滑动.石英脉变形:紧闭-同斜褶皱、无根褶皱、不对称石香肠. T3
      D3a 澜沧-惠民:未变质
      幸福:透入性压溶作用
      以S2为标志面形成N-S向中常褶皱,次生调节褶皱不均匀应变的小型陡倾逆冲断裂.
      幸福:以S2为标志面形成N-S向中常褶皱,发育较透入轴面劈理S3.
      103.7 Ma
      D3b 未变质 澜沧-惠民:近N-S向近水平逆冲断层,切割D3a褶皱
      幸福:向东陡倾的逆冲断层切过D3a褶皱
      82.28 Ma
      D4 未变质 澜沧-惠民:以S2为标志面形成E-W向中常-开阔褶皱及小型逆冲断层.
      幸福:近E-W向纵弯褶皱及轴面劈理.
      新生代
      (晚于59.18 Ma)
      下载: 导出CSV

      表  2  小黑江高压变质岩二叠纪以后的变质变形期次划分

      Table  2.   The classification of metamorphism/deformation since Permian for the high-pressure metamorphic rocks in Xiaoheijiang area

      期次 变质相 变形样式 时代
      M1aD1a 早期变质(可能为榴辉岩相-EC?)Grt+白云母 Grt1同构造或构造后变斑晶及内部S形白云母包迹面理S1a >255 Ma
      M1bD1b 蓝片岩相(Ep-BS)多硅白云母片岩:Grt+Phen+Gl+Tur+Ttn;蓝片岩,Gl+Ep+Ab 多硅白云母片岩:Grt2后构造变斑晶,矩形石英条带;Tur后构造变斑晶及内部Gl包体面理S1b. 248.5~255.0 Ma
      M2D2 绿片岩相(GS)Bi+Ab Phen(M1D1)旋转后定向排列构成褶劈理S2,劈理域内浸染状分布Bi;Ab同构造变斑晶压力影构造,内含S1bPhen的S形包迹;石英亚晶粒及波状消光. 215~214 Ma
      D3 ≤低绿片岩相(GS) 近N-S向宽缓褶皱及膝褶(赵靖等, 1994a, 1994b). 111.9±0.4 Ma
      D4 <低绿片岩相(GS) 褶劈理S2发生近E-W向宽缓褶皱,形成轴面劈理S4. 晚白垩世?
      D5 未变质 倾向W或SW的低角度韧-脆性正断层. 新生代?
      下载: 导出CSV

      表  3  幸福变质石英砂岩白云母40Ar-39Ar测年同位素比值结果

      Table  3.   40Ar-39Ar isotopic dating results of muscovite fractions from metamorphic quartz sandstone in Xingfu

      加热阶段 T
      (℃)
      (40Ar/
      39Ar)m
      (36Ar/
      39Ar)m
      (37Ar/
      39Ar)m
      (38Ar/
      39Ar)m
      40Ar
      (%)
      F 39Ar
      (10-14 mol)
      39Ar(累计)
      (%)
      年龄
      (Ma)
      ±1σ
      (Ma)
      Ca/
      K
      1 700 22.046 0 0.030 4 0.368 0 0.019 2 59.30 13.077 0 0.64 4.64 59.18 0.70 0.634 4
      2 740 18.946 9 0.003 8 0.351 9 0.014 1 94.11 17.835 2 1.57 16.01 80.23 0.81 0.606 6
      3 780 18.502 2 0.001 9 0.047 0 0.013 1 97.01 17.949 0 1.98 30.41 80.73 0.81 0.081 1
      4 820 18.833 7 0.001 8 0.064 8 0.012 9 97.16 18.299 5 2.46 48.27 82.28 0.81 0.111 8
      5 860 20.006 8 0.002 0 0.093 9 0.013 5 97.00 19.407 9 3.10 70.73 87.14 0.85 0.162 0
      6 900 20.941 3 0.003 4 0.134 2 0.013 6 95.22 19.942 9 1.01 78.08 89.48 0.91 0.231 3
      7 950 22.833 4 0.004 9 0.120 1 0.013 8 93.64 21.383 9 1.42 88.39 95.78 0.94 0.207 1
      8 1 000 24.860 4 0.005 7 0.184 4 0.013 9 93.31 23.200 0 1.16 96.80 103.70 1.00 0.317 9
      9 1 050 68.725 4 0.170 3 1.200 7 0.043 9 26.91 18.510 7 0.36 99.41 83.20 1.20 2.069 9
      10 1 120 88.314 7 0.215 0 2.233 2 0.055 7 28.24 24.981 6 0.08 100.00 111.40 4.10 3.850 1
      注:表中下标m代表样品中测定的同位素比值;Total age=85.8 Ma;F=40Ar*/39Ar,代表放射性40Ar和39Ar的比值.样品编号为7-20-6-DKW1,单矿物为白云母,W=27.73 mg,J=0.002 550.
      下载: 导出CSV
    • Chen, B.W., Wang, K.Y., Liu, W.X., et al., 1987.The Tectonic of Nujiang-Lancang-Jinsha River Region.Geological Publishing House, Beijing (in Chinese).
      Fan, C.J., Zhang, Y.F., 1993.On The Structural Pattern of Western Yunnan.Yunnan Geology, 12(2):101-110 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-YNZD199302000.htm
      Feng, Q.L., Shen, S.Y., Liu, B.P., et al., 2002.Permian Radiolarians, Chert and Basalt from the Daxinshan Formation in Lancangjiang Belt of Southwestern Yunnan, China.Sience in China (Series D), 32(3):220-226 (in Chinese). http://kns.cnki.net/KCMS/detail/detail.aspx?filename=JDXG200201006&dbname=CJFD&dbcode=CJFQ
      Forster, M.A., Lister, G.S., 2004.The Interpretation of 40Ar/39Ar Apparent Age Spectra Produced by Mixing:Application of the Method of Asymptotes and Limits.Journal of Structural Geology, 26(2):287-305. https://doi.org/10.1016/j.jsg.2003.10.004
      Harrison, T.M., Célérier, J., Aikman, A.B., et al., 2009.Diffusion of 40Ar in Muscovite.Geochimica et Cosmochimica Acta, 73(4):1039-1051. https://doi.org/10.1016/j.gca.2008.09.038
      Heppe, K., 2006.Plate Tectonic Evolution and Mineral Resource Potential of the Lancang River Zone, Southwestern Yunnan, People's Republic of China.Schweizerbart Science Publishers, Stuttgart, 159.
      Ji, F.B., Qi, X.X., Chang, Y.L., et al., 2015.Cenozoic Polyphase Structural Deformation Characterization in the Middle Segment of the Lancang Tectonic Zone, Western Yunnan, and Its Geochronological Constraints.Acta Petrologica Sinica, 31(12):3713-3724 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-YSXB201512015.htm
      Liu, B.P., Feng, Q.L., Chonglakmani, C., et al., 2002.Framework of Paleotethyan Archipelago Ocean of Western Yunnan and Its Elongation towards North and South.Earth Science Frontiers, 9(3):161-171 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dxqy200203020
      Liu, D.Z., Wang, G.Z., Tao, X.F., et al., 2000.Study of the Lancang River Tectonic Mélange Zone in Western Yunnan.Regional Geology of China, 19(3):312-317 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zgqydz200003016
      Ludwig, K.R., 2001.Using Isoplot/EX, Version 2.49: A Geolocronolgical Toolkit for Microsoft Excel.Berkeley Geochronological Center, Berkeley.
      McDougalll, I., Harrison, T.M., 1999.Geohronology and Thermochronology by the 40Ar/39Ar Method.Oxford Univerity Press, Oxford.
      Mo, X.X., Shen, S.Y., et al., 1998.Volcanic-Ophiolite and Mineralization in Middle-South of Sanjiang Region.Geological Publishing House, Beijing (in Chinese).
      Peng, T.P., Wang, Y.J., Zhao, G.C., et al., 2008.Arc-Like Volcanic Rocks from the Southern Lancangjiang Zone, SW China:Geochronological and Geochemical Constraints on Their Petrogenesis and Tectonic Implications.Lithos, 102(1-2):358-373. https://doi.org/10.1016/j.lithos.2007.08.012
      Peng, X.J., Luo, W.L., 1982.Discovery and Tectonic Significance of Glaucophane, Southern Section of Lancangjiang, West Yunnan.Regional Geology of China, 1(2):69-75 (in Chinese).
      Shan, W.L., Song, H.L., Fu, Z.R., et al., 1991.The Theory, Methods and Practice of Tectonic Deformation Analysis.China University of Geosciences Press, Wuhan (in Chinese).
      Shen, S.Y., Feng, Q.L., Liu, B.P., et al., 2002.Tectonomagmatic Types of Volcanic Rocks in South Lancang River Belt, Jinshajiang River-Lancangjiang River-Nujiang River Area in China.Journal of Mineralogy and Petrology, 22(3):66-71 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-KWYS200203014.htm
      Villa, I.M., Hermann, J., Müntener, O., et al., 2000.39Ar-40Ar Dating of Multiply Zoned Amphibole Generations (Malenco, Italian Alps).Contributions to Mineralogy and Petrology, 140(3):363-381. https://doi.org/10.1007/s004100000197
      Wang, D.D., Li, B.L., Ji, J.Q., et al., 2014.Zircon SHRIMP U-Pb Geochronology and Its Tectonic Implication of the Metamorphic Rocks in Southern Lancang River Tectonic Zone West Yunnan Province.Acta Petrologica Sinica, 30(9):2725-2738 (in Chinese with English abstract).
      Wang, F., Shi, W.B., Zhu, R.X., et al., 2014.Problems of Modern 40Ar/39Ar Geochronology:Reviews.Acta Petrologica Sinica, 30(2):326-339 (in Chinese with English abstract).
      Wang, G.H., Han, F.L., Yang, Y.J., et al., 2009.Discovery and Geologic Significance of Late Paleozoic Accretionary Complexes in Central Qiangtang, Northern Tibet, China.Geological Bulletin of China, 28(9):1181-1187 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-ZQYD200909004.htm
      Wang, G.H., Zhou, X., Ciren, P., et al., 1996.Tectonic Deformation and Evolution of Taniantaweng Mountains in Tibet.Geological Publishing House, Beijing (in Chinese).
      Wang, Y.J., Zhang, A.M., Fan, W.M., et al., 2010.Petrogenesis of Late Triassic Post-Collisional Basaltic Rocks of the Lancangjiang Tectonic Zone, Southwest China, and Tectonic Implications for the Evolution of the Eastern Paleotethys:Geochronological and Geochemical Constraints.Lithos, 120(3-4):529-546. https://doi.org/10.1016/j.lithos.2010.09.012
      Xue, X.H., Xiong, J.Y., Hu, Y., et al., 1989.Yunnan Metamorphic Complex 1:2 000 000 Metamorphic Geological Map Instructions of Yunnan Province.Yunnan Science and Technology Press, Kunming (in Chinese).
      Yang, K.H., Mo, X.X., 1993.Late Paleozoic Rifting-Related Volcanic Rocks and Tectonic Evolution in Southwestern Yunnan.Acta Petrologica et Mineralogica, 12(4):297-311 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSKW199304002.htm
      Yang, W.Q., Feng, Q.L., Duan, X.D., et al., 2007.Late Devonian Pillow Basalts and Bedded Cherts in Changning-Menglian Tectonic Belt of Southwestern Yunnan, China.Geological Bulletin of China, 26(6):739-747 (in Chinese with English abstract). http://en.cnki.com.cn/article_en/cjfdtotal-zqyd200706016.htm
      Zhai, M.G., Cong, B.L., Qiao, G.S., et al., 1990.Sm-Nd and Rb-Sr Geochronolgy of Metmorphic Rocks form SW Yunnan Orogenic Zones, China.Acta Petrologica Sinica, 6(4):1-11 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB199004000.htm
      Zhang, B., Zhang, J.J., Zhong, D.L., et al., 2008.Strain and Kinematic Vorticity Analysis:An Indicator for Sinistral Transpressional Strain-Partitioning along the Lancangjiang Shear Zone, Western Yunnan, China.Science in China (Series D), 38(10):1268-1283 (in Chinese). doi: 10.1007-s11430-009-0065-4/
      Zhang, F., Feng, Q.L., Duan, X.D., et al., 2006.Research on the Western Belt of Changning-Menglian Tectonic Belt:Exampled by the Nongba Section in Gengma, Southwest of Yunnan, China.Geological Science and Technology Information, 25(3):13-20 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZKQ200603002.htm
      Zhang, Q., Li, D.Z., Zhang, K.W., et al., 1985.Preliminary Study on Tongchangjie Ophiolite Melange from Yun County, Yunnan Province.Acta Petrologica Sinica, 1(3):1-14 (in Chinese with English abstract).
      Zhang, R.Y., Cong, B.L., Maruyama, S., et al., 1993.Metamorphism and Tectonic Evolution of the Lancang Paired Metamorphic Belts, South-Western China.Journal of Metamorphic Geology, 11(4):605-619. https://doi.org/10.1111/j.1525-1314.1993.tb00175.x
      Zhao, J., Zhong, D.L., Wang, Y., et al., 1992.The Disintegration of "Lancang Group" and Its Tectonic Significance, Western Yunnan.Earthquake Press, Beijing, 12-24 (in Chinese).
      Zhao, J., Zhong, D.L., Wang, Y., et al., 1994a.A Preliminary Study on Deformation Sequence and Metamorphism in Lancang Metamorphic Belt of West Yunnan.Chinese Journal of Geology, 29(4):366-371 (in Chinese with English abstract). http://www.dzkx.org/EN/abstract/abstract10066.shtml
      Zhao, J., Zhong, D.L., Wang, Y., et al., 1994b.Metamorphism of Lancang Metamorphic Belt, the Western Yunnan and Its Relation to Deformation.Acta Petrologica Sinica, 10(1):27-29 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-YSXB199401002.htm
      Zhong, D.L., 1998.Paleotethys Orogen in Western Section of Yunnan and Sichuan Province.Science Press, Beijing (in Chinese).
      Zhou, W.Q., Lin, W.X., 1982.The Features of the Glaucophane Schist in the Southern Part of the Lancang Jiang Metamorphic Belt.Regional Geology of China, (2):76-85 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK000004038883
      陈炳蔚, 王铠元, 刘万熹, 等, 1987.怒江-澜沧江-金沙江地区大地构造.北京:地质出版社.
      范承钧, 张翼飞, 1993.云南西部地质构造格局.云南地质, 12(2):101-110. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK000004870204
      冯庆来, 沈上越, 刘本培, 等, 2002.滇西南澜沧江构造带大新山组放射虫、硅质岩和玄武岩研究.中国科学(D辑), 32(3):220-226. http://d.old.wanfangdata.com.cn/Periodical/zgkx-cd200203006
      吉风宝, 戚学祥, 常裕林, 等, 2015.滇西澜沧江构造带中段新生代多期构造变形特征及时代约束.岩石学报, 31(12):3713-3724. http://d.old.wanfangdata.com.cn/Periodical/ysxb98201512015
      刘本培, 冯庆来, Chonglakman, C., 等, 2002.滇西古特提斯多岛洋的结构及其南北延伸.地学前缘, 9(3):161-171. doi: 10.3321/j.issn:1005-2321.2002.03.020
      刘登忠, 王国芝, 陶晓风, 等, 2000.澜沧江构造混杂带的初步研究.中国区域地质, 19(3):312-317. doi: 10.3969/j.issn.1671-2552.2000.03.016
      莫宣学, 沈上越, 1998.三江中南段火山岩-蛇绿岩与成矿.北京:地质出版社.
      彭兴阶, 罗万林, 1982.滇西澜沧江南段蓝闪片岩带的发现及其大地构造意义.中国区域地质, 1(2):69-75. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK000004038882
      单文琅, 宋鸿林, 傅昭仁, 等, 1991.构造变形分析的理论、方法和实践.武汉:中国地质大学出版社.
      沈上越, 冯庆来, 刘本培, 等, 2002.三江地区南澜沧江带火山岩构造岩浆类型.矿物岩石, 22(3):66-71. doi: 10.3969/j.issn.1001-6872.2002.03.015
      王丹丹, 李宝龙, 季建清, 等, 2014.澜沧江构造带南段变质岩系锆石U-Pb年代学及构造涵义.岩石学报, 30(9):2725-2738. http://d.old.wanfangdata.com.cn/Periodical/ysxb98201409021
      王非, 师文贝, 朱日祥, 等, 2014.40Ar/39Ar年代学中几个重要问题的讨论.岩石学报, 30(2):326-339. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98201402002
      王根厚, 韩芳林, 杨运军, 等, 2009.藏北羌塘中部晚古生代增生杂岩的发现及其地质意义.地质通报, 28(9):1181-1187. doi: 10.3969/j.issn.1671-2552.2009.09.003
      王根厚, 周详, 普布次仁, 等, 1996.西藏他念他翁山链构造变形及其演化.北京:地质出版社.
      薛玺会, 熊家镛, 胡英, 等, 1989.云南变质杂岩1:200万云南省变质地质图说明书.昆明:云南科技出版社.
      杨开辉, 莫宣学, 1993.滇西南晚古生代火山岩与裂谷作用及区域构造演化.岩石矿物学杂志, 12(4):297-311. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK000003625455
      杨文强, 冯庆来, 段向东, 等, 2007.滇西南昌宁-孟连构造带晚泥盆世枕状玄武岩和层状硅质岩的特征.地质通报, 26(6):739-747. doi: 10.3969/j.issn.1671-2552.2007.06.016
      翟明国, 从柏林, 乔广生, 等, 1990.中国滇西南造山带变质岩的Sm-Nd和Rb-Sr同位素年代学.岩石学报, 6(4):1-11. doi: 10.3321/j.issn:1000-0569.1990.04.001
      张波, 张进江, 钟大赉, 等, 2008.滇西澜沧江左旋走滑挤压带应变分解的应变和运动学涡度证据.中国科学(D辑), 38(10):1268-1283. doi: 10.3321/j.issn:1006-9267.2008.10.010
      张凡, 冯庆来, 段向东, 等, 2006.滇西南昌宁-孟连构造带西带研究初探——以耿马弄巴剖面为例.地质科技情报, 25(3):13-20. doi: 10.3969/j.issn.1000-7849.2006.03.003
      张旗, 李达周, 张魁武, 等, 1985.云南省云县铜厂街蛇绿混杂岩的初步研究.岩石学报, 1(3):1-14. doi: 10.3321/j.issn:1000-0569.1985.03.001
      赵靖, 钟大赉, 王毅, 等, 1992.滇西"澜沧群"的解体及其大地构造意义.北京:地震出版社, 12-24.
      赵靖, 钟大赉, 王毅, 等, 1994a.滇西澜沧变质带的变形序列与变质作用初步研究.地质科学, 29(4):366-371. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK199400056105
      赵靖, 钟大赉, 王毅, 等, 1994b.滇西澜沧变质带变质作用和变形作用的关系.岩石学报, 10(1):27-29. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK199400757095
      钟大赉, 1998.滇川西部古特提斯造山带.北京:科学出版社.
      周维全, 林文信, 1982.澜沧江变质带南段蓝闪石片岩特征.中国区域地质, (2):76-85. doi: 10.1053-j.tvir.2010.03.009/
    • 加载中
    图(7) / 表(3)
    计量
    • 文章访问数:  3939
    • HTML全文浏览量:  1696
    • PDF下载量:  36
    • 被引次数: 0
    出版历程
    • 收稿日期:  2017-12-10
    • 刊出日期:  2018-09-15

    目录

      /

      返回文章
      返回