Deformation characteristics, deformation age and dynamic background of Dagujia ductile shear zone in Qingyuan, northern Liaoning Province
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摘要:
辽北清原地区位于华北克拉通北缘东段，发育大规模强变形花岗质岩石，是进一步研究中生代燕山运动和东北地区多构造体系叠加、转换过程的重要窗口。通过详细的宏微观构造解析、有限应变测量、石英EBSD组构分析和锆石U−Pb测年，厘定了区域内大孤家韧性剪切带的变形特征、变形时代和动力学背景。结果显示，大孤家韧性剪切带发育走向NW―SE的构造面理和倾伏向SE的矿物拉伸线理，整体具有NW向左行走滑剪切特点。岩石变形温度较高，介于550~650°C之间。剪切带内花岗质岩石主要形成于中生代多期次岩浆活动，结合区域构造年代学资料，限定剪切带变形时代为晚侏罗世末—早白垩世初，为燕山运动B幕在辽北地区的局部响应。古太平洋板片俯冲导致的区域断裂带重新活化是大孤家韧性剪切带形成的主要原因。
Abstract:The Qingyuan area in northern Liaoning Province is located in the eastern segment of the northern margin of the North China Craton, with large−scale strongly deformed granitic rocks. It is an important window to further study the Mesozoic Yanshanian movement and the superposition and transformation of multiple tectonic regimes of NE China. In this paper, the deformation characteristics, age and dynamical background of the regional Dagujia ductile shear zone are determined by detailed macro− and micro−structure analysis, finite strain measurements, quartz EBSD fabric and zircon U−Pb dating. The results show that the Dagujia ductile shear zone develops NW−SE−trending foliations and SE−plunging mineral stretching lineations, with a NW−trending sinistral strike−slip shear characteristics. The deformation temperatures of the rocks are relatively high, ranging between 550°C and 650°C. The granitic rocks in the shear zone primarily formed in Mesozoic multi−stage magmatism. Combined with the regional tectonic chronology data, the deformation age of the shear zone is the latest Late Jurassic to earliest Early Cretaceous, reflecting the local response of the Yanshanian Movement B−episode in the northern Liaoning Province. The Reactivation of regional fault zones caused by the subduction of the Paleo−Pacific Plate is the main reason for the formation of the Dagujia ductile shear zone.
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图 1 华北克拉通和中亚造山带大地构造分区图（a, 据Wu et al., 2011修改）及研究区地质简图（b, 据Gu et al., 2018；段东等, 2024修改；黄色方框中数字代表区域内岩浆岩的形成年龄）
Ⅰ—额尔古纳地块；Ⅱ—兴安地体；Ⅲ—松嫩-张广才岭地块；Ⅳ—佳木斯-兴凯地块；Ⅴ—那丹哈达地体；Ⅵ—陆源活动带；A—索伦-西拉木伦-长春-延吉缝合带；B—新林-喜桂图缝合带；C—黑河-贺根山缝合带；D—嘉荫-牡丹江缝合带；E—跃进山缝合带；F1—赤峰-开原断裂；F2—依兰-伊通断裂；F3—敦化-密山断裂；F4—郯庐断裂
Figure 1. Tectonic division of the North China Craton and the Central Asian Orogenic Belt (a), and geological map of the study area (b)
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图 2 辽北清原大孤家镇地区地质简图（底图据1∶50000大孤家幅、猴石幅地质图修改）
Figure 2. Geological map of the Dagujia Town, Qingyuan, northern Liaoning Province
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图 3 辽北清原大孤家镇典型变形岩石石英C轴组构图（m.u.d.代表极点密度）
Figure 3. Quartz C-axis pole figures of typical deformed rocks in Dagujia Town, Qingyuan, northern Liaoning Province
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图 5 辽北清原大孤家镇强变形岩石中部分锆石的阴极发光图像
Figure 5. Cathodoluminescence images of some zircons from strongly deformed rocks in Dagujia Town, Qingyuan, northern Liaoning Province
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图 4 Flinn有限应变判别图解（底图据郑亚东等, 1985）
Figure 4. Flinn finite strain discrimination diagram
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图 6 辽北清原大孤家镇强变形岩石锆石U−Pb年龄谐和图
Figure 6. Zircon U−Pb concordia diagrams of strongly deformed rocks from Dagujia Town, Qingyuan, northern Liaoning Province
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图 7 早白垩世粗粒碱性花岗岩宏微观结构特征及锆石U−Pb谐和图
Figure 7. Field and microstructural characteristics of Early Cretaceous coarse−grained alkaline granite and zircon U−Pb concordia diagram
表 1 辽北清原大孤家韧性剪切带典型露头产状
Table 1 Typical outcrop occurrences in the Dagujia ductile shear zone in Qingyuan, northern Liaoning Province
样品点 采样位置 主要岩石类型 面理（S）和线理（L） 21QY1 42°19′40.6″N、
124°54′37.9″E花岗质糜棱岩 22°∠66°(S); 45°∠84°(S); 45°∠74°(S); 35°∠70°(S); 115°∠18°(L) 21QY2 42°23′08.4″N、
124°50′00.4″E花岗质糜棱岩 40°∠24°(S); 50°∠19°(S); 60°∠14°(S); 115°∠9°(L);
50°∠12°(S); 123°∠4°(L); 70°∠31°(S); 65°∠32°(S)21QY4 42°22′27.9″N、
124°54′59.4″E钾长花岗质糜棱岩 37°∠59°(S); 120°∠26°(L); 43°∠62°(S); 120°∠24°(L) 23QY1 42°19′07.0″N、
124°56′18.8″E黑云母钾长质花岗糜棱岩 54°∠72°(S); 66°∠80°(S) 23QY3 42°19′23.3″N、
124°54′35.0″E黑云母花岗质糜棱岩 45°∠71°(S); 38°∠75°(S); 32°∠63°(S) 23QY5 42°22′17.7″N、
124°52′55.2″E花岗质糜棱岩 22°∠48°(S) 23QY7 42°22′08.6″N、
124°45′01.3″E花岗质糜棱岩 34°∠56°(S); 32°∠58°(S) 23QY11 42°26′22.4″N、
124°55′23.8″E花岗质糜棱岩 42°∠34°(S); 50°∠21°(S); 58°∠19°(S); 20°∠33°(S); 12°∠35°(S); 42°∠44°(S);
20°∠29°(S); 107°∠12°(L); 18°∠36°(S); 89°∠15°(L)
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表 2 辽北清原大孤家镇变形岩石的有限应变测量结果
Table 2 Finite strain results of typical deformed rock in Dagujia Town, Qingyuan, northern Liaoning Province
样品号 长短轴法 Fry法 X/Z Y/Z X/Y Flinn参数（K） X/Z Y/Z X/Y Flinn参数（K） 20QY5-1 1.44 1.29 1.12 0.43 1.49 1.34 1.11 0.36 21QY1-1 1.81 1.61 1.12 0.25 1.83 1.63 1.12 0.24 21QY1-2 1.67 1.52 1.10 0.22 1.62 1.46 1.11 0.27 21QY1-4 1.74 1.57 1.11 0.23 1.81 1.64 1.10 0.20 21QY2-1 1.98 1.56 1.27 0.54 1.91 1.51 1.26 0.57 21QY2-2 1.88 1.58 1.19 0.38 1.85 1.55 1.19 0.40 21QY2-a 1.79 1.44 1.24 0.60 1.75 1.41 1.24 0.63 21QY2-2a 1.96 1.61 1.22 0.41 1.95 1.59 1.23 0.44 21QY3-1 2.12 1.78 1.19 0.30 2.08 1.74 1.20 0.32 21QY3-2 2.07 1.69 1.22 0.39 2.11 1.72 1.23 0.38 21QY4-4 1.35 1.22 1.11 0.51 1.43 1.28 1.12 0.45 21QY4-a 1.47 1.29 1.14 0.51 1.52 1.31 1.16 0.55 23QY1-1 1.77 1.49 1.19 0.43 1.72 1.45 1.19 0.46 23QY3-1 2.13 1.63 1.31 0.55 2.04 1.58 1.29 0.56 23QY11-1 1.89 1.66 1.14 0.26 1.82 1.61 1.13 0.26
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