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

江西景德镇地区中生代推覆构造变形特征与年代学约束

霍海龙 张达 陈正乐 毕珉烽 陈国华 贺晓龙 李宁 李兴俭 薛伟 欧阳永棚

霍海龙, 张达, 陈正乐, 等, 2018. 江西景德镇地区中生代推覆构造变形特征与年代学约束. 地质力学学报, 24 (1): 9-24. DOI: 10.12090/j.issn.1006-6616.2018.24.01.002
引用本文: 霍海龙, 张达, 陈正乐, 等, 2018. 江西景德镇地区中生代推覆构造变形特征与年代学约束. 地质力学学报, 24 (1): 9-24. DOI: 10.12090/j.issn.1006-6616.2018.24.01.002
HUO Hailong, ZHANG Da, CHEN Zhengle, et al., 2018. DEFORMATION CHARACTERISTICS AND GEOCHRONOLOGICAL CONSTRAINTS OF MESOZOIC NAPPE STRUCTURE IN JINGDEZHEN AREA, NORTHEASTERN JIANGXI. Journal of Geomechanics, 24 (1): 9-24. DOI: 10.12090/j.issn.1006-6616.2018.24.01.002
Citation: HUO Hailong, ZHANG Da, CHEN Zhengle, et al., 2018. DEFORMATION CHARACTERISTICS AND GEOCHRONOLOGICAL CONSTRAINTS OF MESOZOIC NAPPE STRUCTURE IN JINGDEZHEN AREA, NORTHEASTERN JIANGXI. Journal of Geomechanics, 24 (1): 9-24. DOI: 10.12090/j.issn.1006-6616.2018.24.01.002

江西景德镇地区中生代推覆构造变形特征与年代学约束

doi: 10.12090/j.issn.1006-6616.2018.24.01.002
基金项目: 

公益性行业科研专项 201411035-3

国家科技支撑计划项目 2015BAB05B04-01

国家科技支撑计划项目 2015BAB05B04-02

中国地质调查局项目 DD20160053

详细信息
    作者简介:

    霍海龙(1988-), 男, 博士研究生, 构造地质学专业、主要从事区域构造研究。E-mail:huohailong2012@163.com

    通讯作者:

    张达(1967-), 男, 博士, 教授, 主要从事区域构造、矿田构造、构造演化与成矿规律研究。E-mail:zhangda@cugb.edu.cn

  • 中图分类号: P548;P597.3

DEFORMATION CHARACTERISTICS AND GEOCHRONOLOGICAL CONSTRAINTS OF MESOZOIC NAPPE STRUCTURE IN JINGDEZHEN AREA, NORTHEASTERN JIANGXI

  • 摘要: 景德镇地区位于江西省东北部,扬子板块东部,区内经历了长期的构造演化。通过对区域构造剖面的研究,认为研究区中生代推覆构造的主要形式为由北西向南东的推覆,新元古代双桥山群地层上覆于石炭-三叠纪地层之上,总体构成叠瓦扇或双重构造。最大主压应力(σ1)主要为北西-南东向。在推覆构造系统中,发育于推覆构造断层内的未变形花岗岩锆石U-Pb年龄显示此次构造活动的时间为157~172 Ma,为燕山早期。受中生代推覆构造作用控制,研究区内与推覆构造同期或者稍晚的岩浆作用沿推覆构造界面侵位并在适当的位置成矿,推覆构造制约着与成矿有关的岩浆运移通道与就位空间。

     

  • 图  1  赣东北地区地质简图(b)[19]和景德镇地区地质图(c)[28]

    F1—寿安断裂; F2—塔前断裂; F3—大游山断裂; F4—涌山断裂

    Figure  1.  Simplified geologic map of the northeastern Jiangxi and Jingdezhen area

    图  2  双桥山群内变形特征

    a—不协调褶皱; b—膝折; c—不协调褶皱; d—尖棱褶皱; e—组内次级断裂; f—粉砂质板岩中共轭节理; g—砂质千枚岩中线理发育; h—板理发育; i—紧闭褶皱

    Figure  2.  Deformation characteristics of the Shuangqiaoshan Group

    图  3  原地岩系变形特征

    a—石炭系灰岩尖棱褶皱; b—二叠系炭质页岩发生褶皱; c—石炭系灰岩中倒转背斜; d—鹅湖岩体发育共轭节理; e—灰岩中发育角砾岩; f—栖霞组地层与小江边组地层呈整合接触, 且呈单斜地层; g—灰岩中不协调褶皱; h—灰岩中共轭节理; i—灰岩中发育擦痕

    Figure  3.  Deformation characteristics of autochthonous system

    图  4  塔前—临港构造剖面图

    Figure  4.  Tectonic section of Taqian-Lingang

    图  5  双桥山群逆冲于安源群地层之上

    Figure  5.  The Shuangqiaoshan Group thrusting upon the Anyuan Group

    图  6  双桥山群地层逆冲于石炭系黄龙组灰岩之上

    Figure  6.  The Shuangqiaoshan Group thrusting upon the Huanglomg Formation

    图  7  双桥山群上覆于老虎洞组灰岩之上

    Figure  7.  The Shuangqiaoshan Group overlying upon the Laohudong Formation

    图  8  双桥山群推覆于三叠系安源群之上

    Figure  8.  The Shuangqiaoshan Group pushed upon the Anyuan Group

    图  9  双桥山群(Ptsh)地层逆冲于老虎洞组(C2l)地层之上

    Figure  9.  The Shuangqiaoshan Group thrusting upon the Laohudong Formation

    图  10  寿安—鹄山构造剖面图

    Figure  10.  Tectonic section of Shouan-Hushan

    图  11  双桥山群变质岩上覆于安源群含炭砂岩之上

    Figure  11.  The Shuangqiaoshan Group overlying upon the Anyuan Group

    图  12  北安地区双桥山群上覆于安源群地层之上

    Figure  12.  The Shuangqiaoshan Group overlying upon the Anyuan Group

    图  13  景德镇地区褶皱枢纽及节理赤平投影(下半球)及主压应力图

    Figure  13.  Stereo-projection of fold hinges and joints and principal compressive stress in Jingdezhen area

    图  14  花岗岩脉野外露头(a)和镜下照片(b)

    Figure  14.  Outcrops and microscope photos of the granites (a, b)

    图  15  Bzx15-06阴极发光CL图像(a)和锆石U-Pb一致曲线(b)

    Figure  15.  Cathodoluminescence (CL) images and Concordia diagram of zircon U-Pb ages of Bzx15-06

    图  16  景德镇地区推覆构造模式图

    Figure  16.  The thrust-nappe structure model in Jingdezhen area

    表  1  花岗岩体锆石U-Pb同位素数据

    Table  1.   Zircon U-Pb isotopic dating results of samples from the granites

    Spot 含量/×10-6 Th/U 同位素比值 年龄/Ma
    Pb Th U 207Pb/206Pb 1δ 207Pb/235U 1δ 206Pb/238U 1δ 207Pb/206Pb 1δ 207Pb/235U 206Pb/238U 1δ
    Bzx15-06
    B06-01 683.54 401.24 1135.24 0.35 0.0556 0.0021 0.2498 0.0093 0.0326 0.0004 436 83 226 8 207 3
    B06-02 355.32 310.81 547.00 0.57 0.1235 0.0038 5.5043 0.1616 0.3232 0.0039 2007 53 1901 25 1805 19
    B06-03 207.15 259.53 285.87 0.91 0.0685 0.0025 1.2997 0.0458 0.1376 0.0018 884 74 846 20 831 10
    B06-04 217.57 118.41 365.27 0.32 0.0481 0.0032 0.1708 0.0110 0.0257 0.0004 105 148 160 10 164 3
    B06-05 100.51 118.36 141.90 0.83 0.1741 0.0056 11.3295 0.3486 0.4719 0.0061 2597 52 2551 29 2492 27
    B06-06 350.92 169.94 598.02 0.28 0.0498 0.0027 0.1729 0.0091 0.0252 0.0004 186 121 162 8 160 2
    B06-07 385.99 217.39 644.94 0.34 0.0500 0.0026 0.1802 0.0090 0.0261 0.0004 195 114 168 8 166 2
    B06-08 195.35 217.73 280.98 0.77 0.0666 0.0026 1.2515 0.0465 0.1363 0.0018 824 78 824 21 824 10
    B06-09 312.00 274.84 479.50 0.57 0.0673 0.0024 1.2950 0.0445 0.1395 0.0018 848 72 844 20 842 10
    B06-10 395.24 258.15 645.40 0.40 0.0502 0.0026 0.1785 0.0089 0.0258 0.0004 202 114 167 8 164 2
    B06-11 86.75 124.06 113.23 1.10 0.0669 0.0033 1.2605 0.0598 0.1367 0.0021 834 99 828 27 826 12
    B06-12 624.97 413.43 1018.32 0.41 0.0495 0.0022 0.1844 0.0080 0.0270 0.0004 172 101 172 7 172 2
    B06-13 185.10 166.47 283.03 0.59 0.0831 0.0036 0.7866 0.0331 0.0686 0.0010 1272 83 589 19 428 6
    B06-14 413.73 204.97 703.12 0.29 0.0507 0.0026 0.1765 0.0088 0.0252 0.0004 229 114 165 8 161 2
    B06-15 542.96 367.76 881.07 0.42 0.0493 0.0024 0.1736 0.0081 0.0255 0.0004 164 108 163 7 162 2
    B06-16 373.59 178.91 637.50 0.28 0.0507 0.0027 0.1776 0.0091 0.0254 0.0004 227 118 166 8 162 2
    B06-17 767.34 574.41 1222.13 0.47 0.0491 0.0022 0.1669 0.0073 0.0247 0.0003 151 102 157 6 157 2
    B06-18 339.71 182.96 571.14 0.32 0.0506 0.0029 0.1673 0.0093 0.0240 0.0004 224 127 157 8 153 2
    B06-19 428.74 239.39 717.25 0.33 0.0805 0.0031 0.8933 0.0331 0.0805 0.0011 1209 74 648 18 499 6
    B06-20 469.45 740.47 583.59 1.27 0.0513 0.0028 0.1792 0.0095 0.0254 0.0004 252 121 167 8 161 2
    B06-21 242.58 181.55 386.37 0.47 0.0618 0.0031 0.3532 0.0174 0.0414 0.0006 668 105 307 13 262 4
    B06-22 174.83 263.79 222.39 1.19 0.0704 0.0030 1.3785 0.0566 0.1420 0.0020 940 85 880 24 856 11
    B06-23 185.09 138.31 294.90 0.47 0.0683 0.0031 0.7677 0.0338 0.0815 0.0012 877 92 578 19 505 7
    B06-24 149.34 192.29 203.90 0.94 0.0762 0.0032 1.9809 0.0794 0.1884 0.0027 1101 81 1109 27 1113 14
    B06-25 604.06 297.90 1027.15 0.29 0.0647 0.0025 0.7763 0.0291 0.0870 0.0012 764 80 583 17 538 7
    B06-26 111.53 105.45 168.36 0.63 0.0946 0.0038 3.5367 0.1374 0.2712 0.0038 1520 74 1536 31 1547 19
    B06-27 771.46 518.76 1253.46 0.41 0.0675 0.0027 0.5225 0.0203 0.0561 0.0008 854 81 427 14 352 5
    B06-28 494.42 308.79 813.32 0.38 0.0953 0.0044 0.3507 0.0154 0.0267 0.0004 1534 83 305 12 170 3
    下载: 导出CSV
  • [1] Guo L Z, Shi Y S, Lu H F, et al. The pre-Devonian tectonic patterns and evolution of South China[J]. Journal of Southeast Asian Earth Sciences, 1989, 3(1/4):87~93. https://www.sciencedirect.com/science/article/pii/0743954789900123
    [2] Zhao G C, Guo J H. Precambrian geology of China:Preface[J]. Precambrian Research, 2012, 222~223:1~12. doi: 10.1016/j.precamres.2012.09.018
    [3] Charvet J, Lapierre H, Yu Y W. Geodynamic significance of the Mesozoic volcanism of southeastern China[J]. Journal of Southeast Asian Earth Sciences, 1994, 9(4):387~396. doi: 10.1016/0743-9547(94)90050-7
    [4] Shu L S, Charvet J. Kinematics and geochronology of the Proterozoic Dongxiang-Shexian ductile shear zone:with HP metamorphism and ophiolitic mélange (Jiangnan Region, South China)[J]. Tectonophysics, 1996, 267(1/4):291~302. https://www.researchgate.net/publication/222997748_Kinematics_and_geochronology_of_the_Proterozoic_Dongxiang-Shexian_ductile_shear_zone_with_HP_metamorphism_and_ophiolitic_melange_Jiangnan_Region_South_China
    [5] Li X H, Li Z X, Ge W C, et al. Neoproterozoic granitoids in South China:Crustal melting above a mantle plume at ca. 825 Ma?[J]. Precambrian Research, 2003, 122(1/4):45~83. https://www.sciencedirect.com/science/article/pii/S0301926802002073
    [6] Li L M, Sun M, Wang Y J, et al. U-Pb and Hf isotopic study of detrital zircons from the meta-sedimentary rocks in central Jiangxi Province, South China:Implications for the Neoproterozoic tectonic evolution of South China Block[J]. Journal of Asian Earth Sciences, 2011, 41(1):44~55. doi: 10.1016/j.jseaes.2010.12.004
    [7] Sun W H, Zhou M F, Gao J F, et al. Detrital zircon U-Pb geochronological and Lu-Hf isotopic constraints on the Precambrian magmatic and crustal evolution of the western Yangtze Block, SW China[J]. Precambrian Research, 2009, 172(1/2):99~126. https://www.researchgate.net/publication/257128083_Detrital_zircon_U-Pb_geochronological_and_Lu-Hf_isotopic_constraints_on_the_Precambrian_magmatic_and_crustal_evolution_of_the_western_Yangtze_Block_SW_China
    [8] Wang X L, Zhou J C, Qiu J S, et al. Geochemistry of the Meso-to Neoproterozoic basic-acid rocks from Hunan Province, South China:Implications for the evolution of the western Jiangnan orogen[J]. Precambrian Research, 2004, 135(1/2):79~103. https://www.researchgate.net/publication/258419310_Geochemistry_of_the_Meso-_Neoproterozoic_volcanic-intrusive_rocks_from_Hunan_Province_and_its_petrogenic_significances
    [9] 郭令智, 卢华复, 施央申, 等.江南中、新元古代岛弧的运动学和动力学[J].高校地质学报, 1996, 2(1):1~13. http://www.cqvip.com/qk/90539X/199601/2410749.html

    GUO Lingzhi, LU Huafu, SHI Yangshen, et al. On the Meso-neoproterozoic Jiangnan island arc:Its kinematics and dynamics[J]. Geological Journal of Universities, 1996, 2(1):1~13. (in Chinese with English abstract) http://www.cqvip.com/qk/90539X/199601/2410749.html
    [10] 张国伟, 郭安林, 王岳军, 等.中国华南大陆构造与问题[J].中国科学:地球科学, 2013, 43(10):1553~1582. http://www.irgrid.ac.cn/handle/1471x/873131?mode=full

    ZHANG Guowei, GUO Anlin, WANG Yuejun, et al. Tectonics of South China continent and its implications[J]. Science China Earth Sciences, 2013, 56(11):1804~1828. http://www.irgrid.ac.cn/handle/1471x/873131?mode=full
    [11] Dong S W, Zhang Y Q, Zhang F Q, et al. Late Jurassic-Early Cretaceous continental convergence and intracontinental orogenesis in East Asia:A synthesis of the Yanshan Revolution[J]. Journal of Asian Earth Sciences, 2015, 114:750~770. doi: 10.1016/j.jseaes.2015.08.011
    [12] 郑永飞, 张少兵.华南前寒武纪大陆地壳的形成和演化[J].科学通报, 2007, 52(1):1~10. http://www.doc88.com/p-9022057016956.html

    ZHENG Yongfei, ZHANG Shaobing. Formation and evolution of Precambrian continental crust in South China[J]. Chinese Science Bulletin, 2007, 52(1):1~12. http://www.doc88.com/p-9022057016956.html
    [13] 王长明, 吴淦国, 张达, 等.赣东北地区的区域成矿特征和成矿谱系[J].世界地质, 2010, 29(4):588~600. http://d.old.wanfangdata.com.cn/Periodical/sjdz201004009

    WANG Changming, WU Ganguo, ZHANG Da, et al. Regional metallogenic characteristics and mineralizing pedigree in northeastern Jiangxi[J]. Global Geology, 2010, 29(4):588~600. (in Chinese with English abstract) http://d.old.wanfangdata.com.cn/Periodical/sjdz201004009
    [14] 董树文, 薛怀民, 项新葵, 等.赣北庐山地区新元古代细碧-角斑岩系枕状熔岩的发现及其地质意义[J]中国地质, 2010, 37(4):1021~1033. http://d.old.wanfangdata.com.cn/Periodical/zgdizhi201004017

    DONG Shuwen, XUE Huaimin, XIANG Xinkui, et al. The discovery of Neoproterozoic pillow lava in spilite-ceratophyre of Lushan area, northern Jiangxi Province, and its geological significance[J]. Geology in China, 2010, 37(4):1021~1033. (in Chinese with English abstract) http://d.old.wanfangdata.com.cn/Periodical/zgdizhi201004017
    [15] 赵崇贺, 何科昭, 周正国, 等.关于华南大地构造问题的再认识[J].现代地质, 1996, 10(4):512~517. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=xddz604.010&dbname=CJFD&dbcode=CJFQ

    ZHAO Chonghe, HE Kezhao, ZHOU Zhengguo, et al. New understanding on Geotectonic problem in South China block[J]. Geoscience, 1996, 10(4):512~517. (in Chinese with English abstract) http://kns.cnki.net/KCMS/detail/detail.aspx?filename=xddz604.010&dbname=CJFD&dbcode=CJFQ
    [16] 李献华, 李武显, 何斌.华南陆块的形成与Rodinia超大陆聚合-裂解——观察、解释与检验[J].矿物岩石地球化学通报, 2012, 31(6):543~559. doi: 10.3969/j.issn.1007-2802.2012.06.002

    LI Xianhua, LI Wuxian, HE Bin. Building of the South China Block and its relevance to assembly and breakup of Rodinia supercontinent:Observations, interpretations and tests[J]. Bulletin of Mineralogy, Petrology and Geochemistry, 2012, 31(6):543~559. (in Chinese with English abstract) doi: 10.3969/j.issn.1007-2802.2012.06.002
    [17] Li S Z, Santosh M, Zhao G C, et al. Intracontinental deformation in a frontier of super-convergence:A perspective on the tectonic milieu of the South China Block[J]. Journal of Asian Earth Sciences, 2012, 49:313~329. doi: 10.1016/j.jseaes.2011.07.026
    [18] 舒良树.华南构造演化的基本特征[J].地质通报, 2012, 31(7):1035~1053. https://wap.cnki.net/qikan-ZQYD201207004.html

    SHU Liangshu. An analysis of principal features of tectonic evolution in South China Block[J]. Geological Bulletin of China, 2012, 31(7):1035~1053. (in Chinese with English abstract) https://wap.cnki.net/qikan-ZQYD201207004.html
    [19] Wang W, Zhou M F, Yan D P, et al. Detrital zircon record of Neoproterozoic active-margin sedimentation in the eastern Jiangnan Orogen, South China[J]. Precambrian Research, 2013, 235:1~19. doi: 10.1016/j.precamres.2013.05.013
    [20] 高林志, 杨明桂, 丁孝忠, 等.华南双桥山群和河上镇群凝灰岩中的锆石SHRIMP U-Pb年龄——对江南新元古代造山带演化的制约[J].地质通报, 2008, 27(10):1744~1751. doi: 10.3969/j.issn.1671-2552.2008.10.017

    GAO Linzhi, YANG Minggui, DING Xiaozhong, et al. SHRIMP U-Pb zircon dating of tuff in the Shuangqiaoshan and Heshangzhen groups in South China-constraints on the evolution of the Jiangnan Neoproterozoic orogenic belt[J]. Geological Bulletin of China, 2008, 27(10):1744~1751. (in Chinese with English abstract) doi: 10.3969/j.issn.1671-2552.2008.10.017
    [21] 刘树文, 杨朋涛, 王宗起, 等.赣东北婺源-德兴地区新元古代浅变质火山岩的地球化学和锆石U-Pb年龄[J].岩石学报, 2013, 29(2):581~593. https://www.researchgate.net/profile/Shuwen_Liu2/publication/294738562_gandongbeiwuyuandexingdequxinyuangudaiqianbianzhihuoshanyande_deqiuhuaxuehegaoshiU-Pbnianling/links/56c3c63d08ae60234250b729/gandongbeiwuyuandexingdequxinyuangudaiqianbianzhihuoshanyande-deqiuhuaxuehegaoshiU-Pbnianling.pdf

    LIU Shuwen, YANG Pengtao, WANG Zongqi, et al. LA-ICPMS zircon U-Pb ages and geochemistry of Neoproterozoic low-grade metavolcanic rocks in Wuyuan-Dexing area of northeastern Jianxi Province[J]. Acta Petrologica Sinica, 2013, 29(2):581~593. (in Chinese with English abstract) https://www.researchgate.net/profile/Shuwen_Liu2/publication/294738562_gandongbeiwuyuandexingdequxinyuangudaiqianbianzhihuoshanyande_deqiuhuaxuehegaoshiU-Pbnianling/links/56c3c63d08ae60234250b729/gandongbeiwuyuandexingdequxinyuangudaiqianbianzhihuoshanyande-deqiuhuaxuehegaoshiU-Pbnianling.pdf
    [22] 毛景文, 谢桂青, 程彦博, 等.华南地区中生代主要金属矿床模型[J].地质论评, 2009, 55(3):347~354. http://d.old.wanfangdata.com.cn/Periodical/dzlp200903005

    MAO Jingwen, XIE Guiqing, CHENG Yanbo, et al. Mineral deposit models of Mesozoic ore deposits in South China[J]. Geological Review, 2009, 55(3):347~354. (in Chinese with English abstract) http://d.old.wanfangdata.com.cn/Periodical/dzlp200903005
    [23] 毛景文, 陈懋弘, 袁顺达, 等.华南地区钦杭成矿带地质特征和矿床时空分布规律[J].地质学报, 2011, 85(5):636~658. https://www.wenkuxiazai.com/doc/7067107d0722192e4536f6ce-2.html

    MAO Jingwen, CHEN Maohong, YUAN Shunda, et al. Geological characteristics of the Qinhang (or Shihang) Metallogenic belt in South China and spatial-temporal distribution regularity of mineral deposits[J]. Acta Geologica Sinica, 2011, 85(5):636~658. (in Chinese with English abstract) https://www.wenkuxiazai.com/doc/7067107d0722192e4536f6ce-2.html
    [24] 陈国华, 万浩章, 舒良树, 等.江西景德镇朱溪铜钨多金属矿床地质特征与控矿条件分析[J].岩石学报, 2012, 28(12):3901~3914. http://www.ysxb.ac.cn/ysxb/ch/reader/view_abstract.aspx?file_no=20121209&journal_id=ysxb

    CHEN Guohua, WAN Haozhang, SHU Liangshu, et al. An analysis on ore-controlling conditions and geological features of the Cu-W polymetallic ore deposit in the Zhuxi area of Jingdezhen, Jiangxi Province[J]. Acta Petrologica Sinica, 2012, 28(12):3901~3914. (in Chinese with English abstract) http://www.ysxb.ac.cn/ysxb/ch/reader/view_abstract.aspx?file_no=20121209&journal_id=ysxb
    [25] 陈国华, 舒良树, 舒立旻, 等.江南东段朱溪钨(铜)多金属矿床的地质特征与成矿背景[J].中国科学:地球科学, 2015, 45(12):1799~1818. doi: 10.1007/s11430-015-5200-9-52?slug=full%20text

    CHEN Guohua, SHU Liangshu, SHU Limin, et al. Geological characteristics and mineralization setting of the Zhuxi tungsten (copper) polymetallic deposit in the Eastern Jiangnan Orogen[J]. Science China Earth Sciences, 2016, 59(4):803~823. doi: 10.1007/s11430-015-5200-9-52?slug=full%20text
    [26] 华仁民, 李光来, 张文兰, 等.华南钨和锡大规模成矿作用的差异及其原因初探[J].矿床地质, 2010, 29(1):9~23. https://www.cnki.com.cn/qikan-KCDZ201001004.html

    HUA Renmin, LI Guanglai, ZHANG Wenlan, et al. A tentative discussion on differences between large-scale tungsten and tin mineralizations in South China[J]. Mineral Deposits, 2010, 29(1):9~23. (in Chinese with English abstract) https://www.cnki.com.cn/qikan-KCDZ201001004.html
    [27] 杨明桂, 王发宁, 曾勇, 等.江西北部金属成矿地质[M].北京:中国大地出版社, 2004, 1~60.

    YANG Minggui, WANG Faning, ZENG Yong, et al. Metal mineralization in northern Jiangxi geological[M]. Beijing:China Land Press, 2004, 1~60. (in Chinese)
    [28] 江西省地矿局. 乐平幅地质图(1: 200000)[M]. 1971.

    Bureau of Geology and Mineral Resources of Jiangxi Province. Regional geology of Leping region (1: 200000)[M]. 1971. (in Chinese)
    [29] 朱志澄, 叶俊林, 杨坤光.幕阜山-九岭隆起侧缘逆冲推覆和滑动拆离以及山体的不对称性[J].地球科学-武汉地质学院学报, 1987, 12(5):503~510. https://www.wenkuxiazai.com/doc/c601b3ebe009581b6bd9eb4d.html

    ZHU Zhicheng, YE Junlin, YANG Kunguang. On thrust-nappe and gliding-detachment on both sides of Mufushan-Jiuling uplift and asymmetrical tectonic architecture of mountain[J]. Earth Science-Journal of Wuhan College Geology, 1987, 12(5):503~510. (in Chinese with English abstract) https://www.wenkuxiazai.com/doc/c601b3ebe009581b6bd9eb4d.html
    [30] 朱志澄.逆冲推覆构造[M].武汉:中国地质大学出版社, 1992, 82~83.

    ZHU Zhicheng. Thrust nappe structure[M]. Wuhan:China University of Geosciences Publishing House, 1992, 82~83. (in Chinese)
    [31] Hsu K J, Shu S, Li J L, et al. Mesozoic overthrust tectonics in South China[J]. Geology, 1988, 16(5):418~421. doi: 10.1130/0091-7613(1988)016<0418:MOTISC>2.3.CO;2
    [32] 钟南昌, 黄金喜, 诸宝森, 等.江西宜丰-乐平推覆构造特征及找矿研究[J].江西地质, 1991, 5(S1):1~116. https://www.hanspub.org/journal/PaperInformation.aspx?paperID=22401

    ZHONG Nanchang, HUANG Jinxi, ZHU Baosen, et al. Tectonic characteristics and ore prospecting of Yifeng-Leping nappe in Jiangxi Province[J]. Jiangxi Geology, 1991, 5(S1):1~116. (in Chinese) https://www.hanspub.org/journal/PaperInformation.aspx?paperID=22401
    [33] 宋鸿林, 朱忠, 颜丹平.赣北萍乐拗陷是对冲构造还是巨型构造窗?[J].地质通报, 2003, 22(2):124~129. http://d.old.wanfangdata.com.cn/Periodical/zgqydz200302007

    SONG Honglin, ZHU Zhong, YAN Danping. Is the Pingle depression a ramp faults zone or a huge tectonic window?[J]. Geological Bulletin of China, 2003, 22(2):124~129. (in Chinese with English abstract) http://d.old.wanfangdata.com.cn/Periodical/zgqydz200302007
    [34] 舒良树, 施央申, 郭令智, 等.江南中段板块-地体构造与碰撞造山运动学[M].南京:南京大学出版社, 1995, 17~28.

    SHU Liangshu, SHI Yangshen, GUO Lingzhi, et al. Middle section of Jiangnan plateau-tectonic structure and collision orogeny kinematics[M]. Nanjing:Nanjing University Press, 1995, 17~28. (in Chinese)
    [35] 万天丰.中国大地构造学纲要[M].北京:地质出版社, 2004, 135~150.

    WAN Tianfeng. Outline of tectonics in China[M]. Beijing:Geological Publishing House, 2004, 135~150. (in Chinese)
    [36] 董树文, 张岳桥, 陈宣华, 等.晚侏罗世东亚多向汇聚构造体系的形成与变形特征[J].地球学报, 2008, 29(3):306~317. http://www.cqvip.com/QK/98325A/200803/27855295.html

    DONG Shuwen, ZHANG Yueqiao, CHEN Xuanhua, et al. The formation and deformational characteristics of East Asia multi-direction convergent tectonic system in Late Jurassic[J]. Acta Geoscientica Sinica, 2008, 29(3):306~317. (in Chinese with English abstract) http://www.cqvip.com/QK/98325A/200803/27855295.html
    [37] 张岳桥, 董树文, 李建华, 等.华南中生代大地构造研究新进展[J].地球学报, 2012, 33(3):257~279. http://d.old.wanfangdata.com.cn/Periodical/dqxb201203001

    ZHANG Yueqiao, DONG Shuwen, LI Jianhua, et al. The new progress in the study of Mesozoic tectonics of South China[J]. Acta Geoscientica Sinica, 2012, 33(3):257~279. (in Chinese with English abstract) http://d.old.wanfangdata.com.cn/Periodical/dqxb201203001
    [38] Liu Y S, Hu Z C, Gao S, 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(1/2):34~43. https://www.sciencedirect.com/science/article/pii/S0024493713004301
    [39] 吴元保, 郑永飞.锆石成因矿物学研究及其对U-Pb年龄解释的制约[J].科学通报, 2004, 49(16):1589~1604. http://www.docin.com/p-768282725.html

    WU Yuanbao, ZHENG Yongfei. Genesis of zircon and its constraints on interpretation of U-Pb age[J]. Chinese Science Bulletin, 2004, 49(15):1554~1569. http://www.docin.com/p-768282725.html
    [40] 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):234~247. http://www.wenkuxiazai.com/doc/038c95707fd5360cba1adb2b.html

    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):234~247. (in Chinese with English abstract) http://www.wenkuxiazai.com/doc/038c95707fd5360cba1adb2b.html
    [41] 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. https://www.researchgate.net/profile/Xianbing_Xu2/publication/282543455_Early_Mesozoic_geotectonic_processes_in_South_China/links/56392ef808ae2da875c7a289.pdf

    XU Xianbing, ZHANG Yueqiao, JIA Dong, et al. Early Mesozoic geotectonic processes in South China[J]. Geology in China, 2009, 36(3):573~593. (in Chinese with English abstract) https://www.researchgate.net/profile/Xianbing_Xu2/publication/282543455_Early_Mesozoic_geotectonic_processes_in_South_China/links/56392ef808ae2da875c7a289.pdf
    [42] Li J H, Zhang Y Q, Dong S W, et al. Cretaceous tectonic evolution of South China:A preliminary synthesis[J]. Earth-Science Reviews, 2014, 134:98~136. doi: 10.1016/j.earscirev.2014.03.008
    [43] 毛建仁, 厉子龙, 叶海敏.华南中生代构造-岩浆活动研究:现状与前景[J].中国科学:地球科学, 2014, 44(12):2593~2617. http://www.docin.com/p-1299792380.html

    MAO Jianren, LI Zilong, YE Haimin. Mesozoic tectono-magmatic activities in South China:Retrospect and prospect[J]. Science China Earth Sciences, 2014, 57(12):2853~2877. http://www.docin.com/p-1299792380.html
    [44] 狄永军, 徐贻赣, 吴淦国, 等.江西冷水坑银铅锌矿田推覆构造的形成时代:来自年代学的约束[J].地学前缘, 2013, 20(4):340~349. http://www.doc88.com/p-4189036763571.html

    DI Yongjun, XU Yigan, WU Ganguo, et al. The formation era of nappe structure in Lengshuikeng Ag-Pb-Zn Ore Field, Jiangxi:Constraints from geochronology[J]. Earth Science Frontiers, 2013, 20(4):340~349. (in Chinese with English abstract) http://www.doc88.com/p-4189036763571.html
    [45] 阙朝阳, 张达, 狄永军, 等.滇东南麻栗坡南温河-洒西一带钨矿控矿要素及深部找矿突破[J].地学前缘, 2014, 21(2):286~300. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=dxqy201402025&dbname=CJFD&dbcode=CJFQ

    QUE Chaoyang, ZHANG Da, DI Yongjun, et al. Ore-controlling characteristics of tungsten deposits in the Nanwenhe-Saxi area and deep prospecting breakthrough[J]. Earth Science Frontiers, 2014, 21(2):286~300. (in Chinese with English abstract) http://kns.cnki.net/KCMS/detail/detail.aspx?filename=dxqy201402025&dbname=CJFD&dbcode=CJFQ
    [46] 毕珉烽, 张达, 吴淦国, 等.滇东南麻栗坡一带中生代构造变形及其对钨多金属矿床的控制作用[J].地学前缘, 2015, 22(4):223~238. http://d.old.wanfangdata.com.cn/Periodical/dxqy201504023

    BI Minfeng, ZHANG Da, WU Fanguo, et al. Mesozoic tectonic deformation and ore-controlling of tungsten polymetallic deposits in Malipo area, southeastern Yunnan[J]. Earth Science Frontiers, 2015, 22(4):223~238. (in Chinese with English abstract) http://d.old.wanfangdata.com.cn/Periodical/dxqy201504023
    [47] 霍海龙, 张达, 狄永军, 等.江西景德镇朱溪铜钨矿床控矿构造特征及矿床成因探讨[J].矿物学报, 2015, 35(S1):24~25. http://d.old.wanfangdata.com.cn/Conference/9133007

    HUO Hailong, ZHANG Da, DI Yongjun, et al. Ore controlling structural characteristics of Zhuxi copper-tungsten deposit in Jingdezhen, Jiangxi Province[J]. Acta Mineralogica Sinica, 2015, 35(S1):24~25. (in Chinese) http://d.old.wanfangdata.com.cn/Conference/9133007
  • 加载中
图(16) / 表(1)
计量
  • 文章访问数:  422
  • HTML全文浏览量:  156
  • PDF下载量:  28
  • 被引次数: 0
出版历程
  • 收稿日期:  2017-06-22
  • 修回日期:  2017-12-13
  • 刊出日期:  2018-02-01

目录

    /

    返回文章
    返回