DEFORMATION CHARACTERISTICS AND GEOCHRONOLOGICAL CONSTRAINTS OF MESOZOIC NAPPE STRUCTURE IN JINGDEZHEN AREA, NORTHEASTERN JIANGXI
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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。Abstract: Jingdezhen area is located in the northeastern Jiangxi province, which belongs to the Yangzi plate, and has undergone long-term tectonic activities. According to the study of regional tectonic section, the Mesozoic thrust-nappe structure direction of the study area is from NW to SE, the upper Shuangqiaoshan group has been pushed to the top of Carboniferous-Triassic strata, and the structural styles of the thrust belt are characterized by imbricate fans and duplexes and the maximum principal compressive stress is SE-NW trend. The study of undeformed granite zircon U-Pb isotope dating shows that the U-Pb isotope age is 157~172 Ma, and the time of tectonic movement is during early Yanshanian period. The Mesozoic thrust-nappe structure produced the magmatic mineralization process in the Jingdezhen area, and the granites of Jingdezhen area may have invaded from intracontinental subduction-related transformation tectonic setting during the early Yanshanian. The nappe structure constrains the magmatic evolution and in space associated with mineralization. Then it controls the mineralization process of the deposit.
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Key words:
- Jingdezhen area /
- Mesozoic /
- thrust-nappe structure /
- chronology
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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 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 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 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
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 1δ 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 
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