THE DUCTILE SHEAR DEFORMATION AGE OF THE JIAMUSI-YITONG FAULT AND ITS GEOLOGICAL SIGNIFICANCE
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摘要: 作为郯庐断裂北段主干断裂的佳木斯-伊通断裂（简称佳-伊断裂），其最早开始活动的时代一直以来都存在争议。为了更好确定其活动时代，对佳-伊断裂昌图段南城水库附近的韧性剪切带展开了详细研究。野外构造解析和显微构造特征显示，剪切带糜棱面理走向北北东-南南西，其上发育北东方向的缓倾拉伸线理，指示该剪切带为逆冲-走滑韧性剪切特征。锆石U-Pb年龄测试结果表明，剪切带中糜棱花岗岩形成在174~173 Ma，该糜棱岩带被后期未变形辉绿岩脉侵入，辉绿岩脉的锆石U-Pb年龄为164 Ma，从而限定该期次韧性变形发生在174~164 Ma之间的中侏罗晚期。取自剪切带糜棱花岗岩内的变形黑云母40Ar/39Ar测试结果表明，糜棱花岗岩在187~166 Ma左右受到了显著的热事件的扰动。这些证据证明，佳-伊断裂在中侏罗晚期发生过显著的左行走滑韧性剪切，结合对东北地区火成岩研究成果的分析，佳-伊断裂中侏罗晚期的韧性变形可能与古太平洋板块向欧亚大陆的俯冲有关，该时期侵位的岩浆活动开始显著受到俯冲引发的挤压应力作用的影响。Abstract: As a major section in the northern part of Tan-Lu fault, the ductile shear deformation age of Jiamusi-Yitong fault (Jia-Yi fault for short) is still an unsolved scientific problem. In this study, a ductile shear zone was discovered near the Nancheng reservoir in the Changtu section of Jia-Yi fault. The field structural analysis and microstructural features show that the shear zones strike ~NNE, dip at a high angle, with a trending ~NE stretching lineation, indicating the shear zone a thrust-slip shear ductile shear. The U-Pb age of zircon from mylonite granites in the shear zone indicate that the granite was formed at 173-174 Ma, which was invaded by the later diabase, and the U-Pb age of zircon from the diabase dykes was 164Ma, so the shear ductile deformation occurred in the late Middle Jurassic between 174-164 Ma. The deformed biotite taken from within the shear zone was disturbed by significant thermal events around 187-166 Ma. The result suggest that significant left-lateral strike-slip ductile shear occurred at the northern section of Tan-Lu fault during the Middle-Late Jurassic. Combined with recent research achievements of igneous rock in Northeast China, the ductile shear deformation of Jia-Yi fault may be associated with the subduction of the Paleo-Pacific plate under the East Asia continent, and magmatic emplacement during Mid-Late Jurassic began to be significantly affected by the compressive stress induced by the subduction.
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Key words:
- Tan-Lu Fault /
- Jiamusi-Yitong Fault /
- The ductile shear zone /
- Paleo-Pacific Plate
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图 1 东北地区构造单元划分图
1—额尔古纳地块；2—兴安地块；3—松辽-锡林浩特地块；4—佳木斯地块；5—松辽盆地；6—华北地块；7—完达山地体；8—主要断裂；9—研究区位置图
Figure 1. Tectonic sub-division of Northeast China
图 2 韧性剪切带区域地质简图
a—奥陶系马家沟组灰岩；b—志留纪花岗岩；c—石炭系本溪组砂岩；d—早二叠世二长花岗岩；e—早二叠超基性岩；f—侏罗纪花岗岩；g—白垩纪花岗岩；h—白垩系砂岩、泥岩；i—第四纪沉积物；j—韧性剪切带；k—断层；N—野外观测点
Figure 2. Geological sketch map of the ductile shear zone
图 3 南城水库韧性剪切带野外剖面
a—南城水库韧性剪切带剖面；b—构造要素赤平投影图
Figure 3. Structural section of the ductile shear zone in Nancheng reservoir
图 4 韧性剪切带糜棱花岗岩野外特征
a—侵入剪切带未变形辉绿岩脉；b—暗色包体沿糜棱面理定向排列；c—包体指示左旋剪切
Figure 4. Deformation photos of mylonite granites in the field
图 5 韧性剪切带显微镜下特征
a—SL011F显微镜下的长石定向排列；b—SL011 N显微镜下的长石旋转碎斑；Kf—钾长石；Qtz—石英
Figure 5. Ductile deformation photos under microscope
图 6 韧性剪切带糜棱花岗岩及辉绿岩脉代表性锆石CL图像及锆石U-Pb年龄谐和图
a—样品SL011D典型锆石CL图像；b—样品SL011D锆石U-Pb年龄谐和图；c—样品SL011 J典型锆石CL图像；d—样品SL011 J锆石U-Pb年龄谐和图；e—样品SL011T典型锆石CL图像；f—样品SL011T锆石U-Pb年龄谐和图
Figure 6. Representative zircon CL images with analyzed spots and U-Pb concordia diagram of mylonite granites and diabase from the shear zone
图 7 糜棱花岗岩黑云母40Ar/39Ar年龄谱
Figure 7. 40Ar/39Ar age spectum for biotites from mylonitic granites
表 1 糜棱花岗岩及辉绿岩锆石U-Pb年代学结果
Table 1. The result of zircon U-Pb from mylonite granites and diabase
点号 Th U Th/U 同位素比值 年龄/Ma ×10-6 ×10-6 207Pb/206Pb 1sigma 207Pb/235U 1sigma 206Pb/238U 1sigma 207Pb/206Pb 1sigma 206Pb/238U 1sigma SL011D 1.1 180.80 293.23 0.62 0.05378 0.00506 0.20319 0.01892 0.02759 0.00061 361 181 175 4 2.1 155.67 218.18 0.71 0.05168 0.00262 0.19136 0.00934 0.02738 0.00054 333 117 174 3 3.1 169.02 395.60 0.43 0.05136 0.00598 0.19572 0.02473 0.02704 0.00083 257 248 172 5 4.1 133.63 321.15 0.42 0.05270 0.01108 0.20255 0.04103 0.02825 0.00131 317 428 180 8 5.1 112.76 185.66 0.61 0.05350 0.00588 0.20377 0.01872 0.02844 0.00065 350 255 181 4 6.1 159.18 373.62 0.43 0.05120 0.00275 0.19311 0.01042 0.02744 0.00038 250 124 175 2 7.1 251.35 373.73 0.67 0.05102 0.00606 0.18744 0.02230 0.02705 0.00113 243 252 172 7 8.1 258.35 366.03 0.71 0.04979 0.00707 0.18628 0.02957 0.02676 0.00032 183 304 170 2 9.1 327.23 579.68 0.56 0.05045 0.00288 0.18788 0.01067 0.02711 0.00044 217 131 172 3 10.1 85.95 239.54 0.36 0.05501 0.00782 0.19898 0.02430 0.02731 0.00079 413 322 174 5 11.1 192.60 260.42 0.74 0.04942 0.00660 0.18287 0.02853 0.02656 0.00144 169 285 169 9 12.1 139.81 273.83 0.51 0.05299 0.01644 0.19522 0.05309 0.02794 0.00136 328 594 178 9 13.1 341.88 779.17 0.44 0.05132 0.00261 0.19103 0.00968 0.02703 0.00046 254 84 172 3 14.1 181.49 408.88 0.44 0.05315 0.00593 0.20188 0.02449 0.02744 0.00098 345 254 175 6 15.1 125.38 268.68 0.47 0.05352 0.00615 0.19413 0.01927 0.02751 0.00128 350 256 175 8 16.1 137.36 376.73 0.36 0.05253 0.00258 0.19585 0.00915 0.02749 0.00031 309 113 175 2 17.1 112.05 126.85 0.88 0.04901 0.01131 0.19625 0.05573 0.02824 0.00209 150 467 180 13 SL011 J 1.1 198.44 548.75 0.36 0.05029 0.00263 0.19032 0.00946 0.02768 0.00037 209 120 176 2 2.1 205.54 1174.35 0.18 0.05001 0.00150 0.18478 0.00552 0.02690 0.00030 195 70 171 2 3.1 83.75 342.43 0.24 0.05050 0.00303 0.19102 0.01193 0.02752 0.00044 217 139 175 3 4.1 212.42 480.29 0.44 0.05115 0.00351 0.19049 0.01282 0.02732 0.00067 256 157 174 4 5.1 243.39 427.44 0.57 0.05476 0.00281 0.20772 0.01037 0.02760 0.00045 467 119 175 3 6.1 132.20 245.62 0.54 0.05347 0.00359 0.19959 0.01325 0.02720 0.00043 350 152 173 3 7.1 206.47 540.07 0.38 0.05366 0.00430 0.20242 0.01681 0.02745 0.00072 367 181 175 5 8.1 116.83 239.88 0.49 0.05359 0.00503 0.21620 0.02259 0.02897 0.00081 354 213 184 5 9.1 273.11 345.52 0.79 0.04932 0.00577 0.18697 0.02155 0.02736 0.00111 161 256 174 7 10.1 146.09 203.41 0.72 0.05560 0.01009 0.19454 0.03292 0.02608 0.00085 435 363 166 5 11.1 330.23 738.29 0.45 0.05255 0.00207 0.20157 0.00774 0.02791 0.00029 309 91 177 2 12.1 1341.93 1931.32 0.69 0.05130 0.00190 0.19133 0.00692 0.02698 0.00033 254 90 172 2 13.1 418.26 460.23 0.91 0.04991 0.00219 0.18688 0.00809 0.02722 0.00033 191 106 173 2 SL011T 1.1 336.63 559.89 0.60 0.05264 0.00497 0.18088 0.01641 0.02506 0.00056 322 219 160 4 2.1 209.99 366.47 0.57 0.05361 0.00946 0.17914 0.03089 0.02502 0.00087 354 356 159 5 3.1 140.99 292.80 0.48 0.05133 0.00742 0.18798 0.02703 0.02625 0.00090 257 309 167 6 4.1 172.89 369.22 0.47 0.05192 0.00584 0.18519 0.02049 0.02608 0.00072 283 60 166 5 5.1 180.47 303.25 0.60 0.05346 0.00305 0.18867 0.01017 0.02573 0.00035 350 130 164 2 6.1 328.22 400.90 0.82 0.05078 0.00240 0.17860 0.00811 0.02575 0.00031 232 114 164 2 7.1 239.00 288.88 0.83 0.05378 0.00458 0.18730 0.01640 0.02532 0.00072 361 188 161 5 8.1 139.38 210.48 0.66 0.05148 0.00542 0.18111 0.01972 0.02593 0.00068 261 44 165 4 9.1 200.92 272.51 0.74 0.05144 0.00268 0.18046 0.00928 0.02566 0.00034 261 88 163 2 10.1 207.68 261.23 0.80 0.05388 0.01021 0.18979 0.03259 0.02610 0.00138 365 381 166 9 11.1 397.41 541.50 0.73 0.04893 0.00415 0.17701 0.01637 0.02592 0.00059 143 189 165 4 12.1 262.79 547.40 0.48 0.05095 0.00460 0.17670 0.01577 0.02519 0.00062 239 209 160 4 13.1 304.08 602.09 0.51 0.05075 0.00387 0.17999 0.01457 0.02572 0.00069 228 178 164 4 14.1 194.73 235.44 0.83 0.05105 0.00749 0.18596 0.03266 0.02602 0.00122 243 307 166 8 15.1 264.73 276.40 0.96 0.05292 0.00788 0.18701 0.02714 0.02566 0.00131 324 307 163 8 16.1 617.91 574.82 1.07 0.05041 0.00377 0.18433 0.01398 0.02650 0.00046 213 179 169 3 17.1 223.00 488.49 0.46 0.05128 0.00240 0.18294 0.00857 0.02602 0.00039 254 112 166 2 
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表 2 南城水库韧性剪切带糜棱岩中黑云母40Ar/39Ar分析数据
Table 2. The data of biotite 40Ar/39Ar from Nancheng reservoir shear zone
T/℃ (40Ar/39Ar)m (36Ar/39Ar)m (37Ar0/39Ar)m (38Ar/39Ar)m 40Ar/% 40Ar/39Ar 39Ar/×10-12mol 39Ar/% Age/Ma(T±1σ) 700 287.8370 0.8525 0.0612 0.2220 12.48 35.9230 0.00 0.05 238±193 770 53.8437 0.1557 1.5780 0.0449 14.77 7.9613 0.66 11.26 55.61±0.97 810 56.9651 0.1421 3.5330 0.0418 26.69 15.2498 0.60 21.57 105.1±1.3 860 37.4604 0.0573 0.5333 0.0275 54.89 20.5722 0.64 32.58 140.3±1.4 910 32.9916 0.0249 0.0771 0.0219 77.69 25.6343 0.83 46.71 173.2±1.7 950 30.5730 0.0147 0.1192 0.0181 85.78 26.2275 0.46 54.64 177.1±2.0 1000 35.1301 0.0275 0.0945 0.0221 76.90 27.0169 0.68 66.24 182.1±1.9 1050 34.7155 0.0233 0.1101 0.0211 80.18 27.8388 0.93 82.11 187.4±1.8 1100 29.5513 0.0122 0.2629 0.0179 87.84 25.9623 0.53 91.09 175.4±1.8 1150 29.2123 0.0158 1.2449 0.0201 84.30 24.6516 0.26 95.50 166.9±2.2 1250 32.0643 0.0247 4.1140 0.0239 78.11 25.1284 0.20 98.98 170.0±2.6 1400 30.9065 0.0288 1.2120 0.0143 72.76 22.5080 0.06 100.00 153.0±5.5
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