Structural Properties and Kinematic Analysis of Lianshanguan Ductile Shear Zone in Northern Liao-Ji Rift Zone, Northeastern North China Craton
-
摘要: 韧性剪切带在岩石圈地壳中广泛存在，蕴含应力、应变和温压等环境参数，是构造解析、流变学和成因机制研究的重要对象.辽吉裂谷带位于辽宁东部-吉林南部，是华北克拉通重要的古元古代活动带之一.连山关岩体地处辽吉裂谷带北缘，经历复杂变质变形作用，岩体南缘发育NWW向右行走滑韧性剪切带.糜棱岩显微结构观测分析揭示，剪切带内糜棱岩以S、SL构造岩为主，总体呈压扁型应变.运动学涡度值为0.91~0.97，均大于0.75，指示简单剪切为主的变形特征.糜棱岩中云母显示塑性拉长，石英动态重结晶明显，以膨凸重结晶作用为主.EBSD分析结果表明，石英发育中低温菱面组构，对应变形温度450~550℃，暗示糜棱岩形成于低绿片岩相-低角闪岩相.结合前人研究成果，我们认为连山关韧性剪切带可能起源于早元古代晚期.连山关岩体先后经历早期隆起造成的伸展-滑脱作用和晚期与上覆辽河群共同经历的南北向挤压，从而在岩体南缘形成陡倾的右行韧性剪切带.Abstract: The ductile shear zone is widely discovered in the lithospheric crust, and it contains abundance environmental parameters such as stress, strain temperature and pressure, hence it is an important object for the study of structural analysis, rheology and genetic mechanism. The Liao-Ji rift zone is one of the ancient primitive activities of the North China craton, located in the east of Liaoning Province and North of Jilin Province. The Lianshanguan granitic body, exposed in the Northern margin of Liao-Ji rift zone, experienced complex metamorphic deformation. The mylonitic in the ductile shear zone have obvious dextral strike-slip characteristics with an NWW strike. The observation and analysis of the microstructure of mylonitic reveals that the taconite developed in shear zone is S-SL type, representing a flattening strain. Kinematics vorticity of 0.91-0.97, which are greater than 0.75, indicates that the shearing is formed in the general shear dominated simple shear. In addition, The quartz dynamic recrystallization is obvious, while the mica shows plastic elongation. The quartz c-axis EBSD analysis shows that the quartz fabric is characterized by the middle to low temperature rhomb slip system, corresponding deformation temperature of 450-550℃, consistent with a greenschist-low amphibolite facies condition. Based on the previous studies, the forming age of the ductile shear deformation is considered to be the late Early Proterozoic. In conclusion, the Lianshanguan granitic body suffered an initial uplift stage, resulting extension-stretching-decollement within the Liaohe Formation surrounding the granitic body. Subsequently, the studied area was suffered a S-N directing compression, and led to the dextral strike-slip ductile shearing.
-
Key words:
- Lianshanguan granitic body /
- ductile shear zone /
- finite strain analysis /
- fabric analysis /
- kinematic /
- Liao-Ji rift zone /
- tectonics
-
图 1 辽东连山关地区地质简图
角图根据Zhao et al.(2001, 2005)修改
Fig. 1. Regional geological map of The Lianshanguan area in East Liaoning with sample locations
图 2 连山关地区野外宏观构造特征
a.浪子山组底部石英岩中含有基底太古代花岗岩砾石(平面图)；b.岩体西端向NW方向的滑脱构造(剖面图)；c.剪切带内岩石片麻理较为发育，暗色矿物和浅色矿物分异明显(平面图)；d.岩体南缘中部产状较陡，透镜体显示强烈的右行剪切滑动构造(平面图)；e.浪子山组片岩中形成的向NE歪斜的小型褶皱(平面图)；f.连山关岩体南缘东段产状变缓(剖面图)；g.岩体东端花岗质透镜体旋转拉长，指示SE向滑脱构造(剖面图)
Fig. 2. Macroscopic structure characteristics of Lianshanguan area
图 3 连山关岩体南缘韧性剪切带内岩石变形特征
图e、c、d、g切面为XZ面，a、b、f、h切面为YZ面，图g中θ为下文的计算参数; 显微构造描述参见表 1
Fig. 3. Microphotographs ofrocks of the ductile shear zone of Southern Lianshanguan granitic body
图 4 Flinn有限应变判别图
图中红色为Fry法测量数据投点，蓝色为惯量椭圆法测量数据投点
Fig. 4. Flinn finite strain discrimination diagram
图 5 连山关地区样品石英组构图
β用于下文运动学涡度计算
Fig. 5. C-axis fabric stereograms of quartz from the sample in the Lianshanguan area
表 1 韧性剪切带变形岩石测试样品宏观、显微构造变形特征
Table 1. Structure characteristics of samples of deformed rocks for test from the ductile shear zone
样品号 岩石类型 变形强度① 产状 矿物组成 宏观变形特征 显微变形特征 14LSG11-2 花岗质
糜棱岩弱 200°∠30° 残斑20%~25%：主要成分为中细粒石英集合体；基质75%~80%：主要成分为细粒云母和长石 残斑呈透镜体产出，S-C组构发育，基质弱定向排列 石英集合体呈透镜状产出，石英颗粒波状消光，动态重结晶现象明显，长石绢云母化严重(图 3a, 3b) 14LSG11-3 白云母
石英片岩较弱 202°∠35° 石英60%，中细粒；白云母30%，细粒；长石10%，细粒 片理发育，矿物颗粒定向排列明显，S-C组构发育 石英颗粒波状消光，动态重结晶主要方式为膨凸重结晶，部分发生细粒化现象(图 3c, 3d) 14LSG7-1 变形石英岩 强 190°∠88° 石英90%，细粒；云母5%，细粒 片麻理发育，石英颗粒分带明显 石英颗粒大部分被定向拉长，带状分布明显，动态重结晶以亚颗粒重结晶为主.云母定向排列(图 3h) 14LSG18-1 变形石英岩 较弱 225°∠55° 石英95%，中细粒 片麻理发育，石英颗粒存在较弱的粒度分带，原始层理可见 石英颗粒部分被定向拉长，动态重结晶以亚颗粒重结晶为主(图 3f) 14LSG21-1 变形石英岩 较强 150°∠30° 石英85%，细粒；云母约10%，细粒 片麻理发育，原始层理可见 石英颗粒定向排列，云母颗粒定向排列，整体带状分布明显(图 3g) 15LSG69-1 含石榴石
云母片岩强 190°∠65° 云母70%，细粒；石英约15%，中细粒；石榴子石约15%，中粒 石榴石及其周围石英颗粒和云母颗粒组成S-C组构 主要成分为石英，细小的石英颗粒定向排列，石榴子石生长线理与外界剪切线理斜交，具压力影构造，阴影部分为石英颗粒(图 3e) 注：①变形强度是相对的，主要依据宏观、显微变形强弱特征以及有限应变测量结果综合判断. 
下载: 导出CSV
表 2 连山关地区样品有限应变测量数据
Table 2. Finite-strain measurement data of the sample from the Lianshanguan area
样品号 惯量椭圆法 Fry法 X/Z Y/Z X/Y ln(X/Y) ln(Y/Z) K X/Z Y/Z X/Y ln(X/Y) ln(Y/Z) K 14LSG7-1 1.49 1.28 1.16 0.15 0.25 0.62 1.56 1.30 1.20 0.18 0.26 0.69 14LSG18-1 1.43 1.25 1.15 0.14 0.22 0.60 1.82 1.45 1.26 0.23 0.37 0.61 14LSG21-1 1.53 1.46 1.05 0.05 0.38 0.12 2.00 1.70 1.18 0.16 0.53 0.31 15LSG69-1 2.31 1.96 1.18 0.16 0.67 0.24 1.75 1.60 1.09 0.09 0.47 0.19 注：K=ln(X/Y)/ln(Y/Z).
下载: 导出CSV
表 3 连山关岩体南缘韧性剪切带变形岩石运动学涡度
Table 3. Kinematic vorticity of the sample from the ductile shear zone in southern Lianshanguan rock
样品号 石英C轴组构法 斜交面理法 Rxz β Wk θ Wk 14LSG7-1 1.49 51 0.92 54 0.95 14LSG18-1 1.43 28 0.91 37 0.96 14LSG21-1 1.53 37 0.99 38 0.97 15LSG69-1 2.31 23 0.92 33 0.91 平均值 - - 0.94 - 0.95
下载: 导出CSV
-
Cai, X.L., Cao, J.M., Zhu, J.S., et al., 2008.System of Crust-Mantle Ductile Shear Zone in the Continental Lithosphere in China.Earth Science Frontiers, 15(3):36-54.doi: 10.1016/s1872-5791(08)60061-5 Chen, B., Li, Z., Wang, J.L., et al., 2016.Liaodong Peninsula -2.2 Ga Magmatic event and Its Geological Significance.Journal of Jilin University (Earth Science edition), 46(2):303-320. http://en.cnki.com.cn/Article_en/CJFDTotal-CCDZ201602001.htm Chen, R.D., 1990.The Tectonic Evolution of the Liaodong Riet.Regional Geology of China, (4):306-315, 333 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-ZQYD199004002.htm Guermani, A., Pennacchioni, G., 1998.Brittle Precursors of Plastic Deformation in a Granite:An Example from the Mont Blanc Massif (Helvetic, Western Alps).Journal of Structural Geology, 20(2-3):135-148.doi: 10.1016/s0191-8141(97)00080-1 Guo, J.H., Peng, P., Chen, Y., et al., 2012.UHT Sapphirine Granulite Metamorphism at 1.93-1.92 Ga Caused by Gabbronorite Intrusions:Implications for Tectonic Evolution of the Northern Margin of the North China Craton.Precambrian Research, 222-223:124-142.doi: 10.1016/j.precamres.2011.07.020 Guo, J.H., Sun, M., Chen, F.K., et al., 2005.Sm-Nd and SHRIMP U-Pb Zircon Geochronology of High-Pressure Granulites in the Sanggan Area, North China Craton:Timing of Paleoproterozoic Continental Collision.Journal of Asian Earth Sciences, 24(5):629-642.doi: 10.1016/j.jseaes.2004.01.017 Guo, Z.T., 1982.Geological Characteristics and Genesis Model of Lianshangun Uranium Deposit in Eastern Liaoning Province, China.Journal of Changchun University of Earth Science, (S1):84-95, 168 (in Chinese with English abstract). http://en.cnki.com.cn/article_en/cjfdtotal-ccdz1982s1006.htm Han, G.Q., Liu, Y.J., Wen, Q.B., et al., 2009.The Characteristics of Structural Deformation for the Lingxia Ductile Shear Zone of Nenjing-Balihan Fault Belt in Northeastern China.Journal of Jilin University(Earth Science Edition), 39(3):397-405(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-CCDZ200903007.htm He, G.P., Ye, H.W., 1998.Two Types of Early Proterozoic Metamorphism and Its Tectonic Significance in Eastern Liaoning and Southern Jilin Areas.Acta Petrologica Sinica, 14(2):152-162 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB802.002.htm Huang, J.J., 1994.On some Viewpoints on Studies of Mylonite and their Applications.Geology of Chemical Minerals, 16(2):117-122 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-HGKC402.007.htm Kruhl, J.H., 2003.Prism-and Basal-Plane Parallel Subgrain Boundaries in Quartz:A Microstructural Geothermobarometer.Journal of Metamorphic Geology, 14(5):581-589.doi: 10.1046/j.1525-1314.1996.00413.x Li, G., Xu, Z.Y., Liu, Z.H., et al., 2013.Early Cretaceous Extension of the Yiwulüshan Metamorphic Core Complex.Acta Petrologica Sinica, 29(3):938-952 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-YSXB201303017.htm Li, J., Liu, Y.J., Li, W.M., et al., 2016.Structural Deformation and Rheology of Granitic Gneiss from the North China Craton Basement-An Example from the Sierbao Area in Western Liaoning Province.Geotectonica et Metallogenia, 40(5):891-907 (in Chinese with English abstract). http://www.en.cnki.com.cn/Article_en/CJFDTotal-DGYK201605001.htm Li, S.Z., Han, Z.S., Liu, Y.J., et al., 2001.Regional Metamorphism Characteristics and Its Continental Dynamics Significance of Liaohe Group.Geological Review, 47(1):9-18 (in Chinese with English abstract). http://en.cnki.com.cn/article_en/cjfdtotal-dzlp200101001.htm Li, S.Z., Hao, D.F., Han, Z.Z., et al., 2003.Paleoproterozoic Deep Processes and Tectono-Thermal Evolution in Jiao-Liao Massif.Acta Geologica Sinica, 77(3):328-340(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZXE200303005.htm Li, S.Z., Hao, D.F., Zhao, G.C., et al., 2004.Geochemical Features and Origin of Dandong Granite.Acta Petrologica Sinica, 20(6):1417-1423(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-YSXB200406010.htm Li, S.Z., Liu, Y.J., 2012.Continental Dynamics and Regional Metamorphism of the Liaohe Group.Geological Review, 47(1):9-18(in Chinese with English abstract). https://www.researchgate.net/publication/291752547_Continental... Li, S.Z., Liu, Y.J., Yang, Z.S., et al., 1998.Relations between Deformation and Metamorphic Recrystallization in Metaperlite of Liaohe Group.Acta Petrologica Sinica, 14(3):351-365(in Chinese with English abstract). https://www.researchgate.net/publication/292740574_Relations... Li, S.Z., Yang, Z.S., Liu, Y.J., 1996.Uplift Bedding-Delamination Structure Analysis of Orogenic Belt in Early Proterozoic of East Liaoning Province.Journal of Changchun University of Earth Sciences, 26(3):305-309 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-CCDZ603.010.htm Li, S.Z., Yang, Z.S., Liu, Y.J., 1997a.The Stratification and Its Causes of the Liaohe Group Metamorphism.Chinese Science Bulletin, 42(24):2631-2636(in Chinese). Li, S.Z., Yang, Z.S., Liu, Y.J., et al., 1997b.Emplacement Model of Palaeoproterozoic Early-Granite in Jiao-Liao-Ji Area and Its Relation to the Uplift Bedding Delamination Structural Series.Acta Petrologica Sinica, 13(2):64-77 (in Chinese with English abstract). https://www.researchgate.net/publication/289782055_Emplacement... Li, S.Z., Zhao, G.C., Sun, M., et al, 2005.Nd Isotopic Characteristics of the South and North Liaohe Groups and Tectonic Implications.Geochimica et Cosmochimica Acta, 863-863. https://www.researchgate.net/publication/232697038_Nd_isotopic... Li, S.Z., Zhao, G.C., Santosh, M., et al., 2011.Palaeoproterozoic Tectonothermal Evolution and Deep Crustal Processes in the Jiao-Liao-Ji Belt, North China Craton:A Review.Geological Journal, 46(6):525-543.doi: 10.1002/gj.1282 Li, S.Z., Zhao, G.C., Santosh, M., et al., 2012.Paleoproterozoic Structural Evolution of the Southern Segment of the Jiao-Liao-Ji Belt, North China Craton.Precambrian Research, 200-203:59-73.doi: 10.1016/j.precamres.2012.01.007 Liang, C.Y., Liu, Y.J., Li, W., et al., 2011.Characteristics of Extensional Structure of Keluo Complex in Nenjiang Area, Heilongjiang, China.Geological Bulletin of China, 30(2):291-299(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-ZQYD2011Z1015.htm Liu, J.H., Liu, F.L., Ding, Z.J., et al, 2013.U-Pb Dating and Hf Isotope Study of Detrital Zircons from the Zhifu Group, Jiaobei Terrane, North China Craton:Provenance and Implications for Precambrian Crustal Growth and Recycling.Precambrian Research, 230-250. http://www.sciencedirect.com/science/article/pii/S030192681300209X Liu, X.D., 2012.The Relationship between the Tectonic Alteration and Uranium Deposit in Lianshan Area.Proceedings of the National Symposium on the Construction of Uranium Mines. Liu, F.L., Liu, P.H., Wang, F., et al., 2014.U-Pb Dating of Zircons from Granitic Leucosomes in Migmatites of the Jiaobei Terrane, Southwestern Jiao-Liao-Ji Belt, North China Craton:Constraints on the Timing and Nature of Partial Melting.Precambrian Research, 245:80-99.doi: 10.1016/j.precamres.2014.01.001 Liu, J.L., 1991.Deformation Structures and Deformation Mechanism in Bedding-Parallel Tectonic Schist in the Inner Zone of the Liaoji Paleaorift.Jilin Geology, 10(4):1-9 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-QHWJ2002Z1019.htm Liu, J.L., Cao, S.Y., Zou, Y.X., et al., 2008.EBSD Analysis of Rock Fabrics and Its Application.Geological Bulletin of China, 27(10):1638-1645(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-ZQYD200810006.htm Liu, Y.J., Li, S.Z., Bai, L.X., 1996.Structural Evolution of Ductile Decollement Zone Occurred between Archaean Gneiss Complexes and Proterozoic Liaohe Group in Haicheng Area, Eastern Liaoning.Journal of Changchun University of Earth Sciences, 26(2):166-171 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-LOAD4Z1.006.htm Liu, Y.J., Li, S.Z., Yang, Z.S., 1997a.Early Proterozoic Uplift-Slide Structural Model on the Eastern Margin of the Northern China Platform.Geological Review, 43(6):569-576 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-DZLP199706001.htm Liu, Y.J., Yang, Z.S., Li, S.Z., et al., 1997b.Extensional Tectonic Model of Palaeoproterozoic-An Example from Northern Shandong Peninsula, Eastern Liaoning and Southern Jilin Areas.Journal of Changchun University of Earth Sciences, 27(2):141-146 (in Chinese with English abstract). Mainprice, D., Bouchez, J.L., Blumenfeld, P., et al., 1986.Dominant c Slip in Naturally Deformed Quartz:Implications for Dramatic Plastic Softening at High Temperature.Geology, 14(10):819.doi:10.1130/0091-7613(1986)14<819:dcsind>2.0.co;2 Mancktelow, N.S., 2006.How Ductile are Ductile Shear Zones? Geology, 34(5):345.doi: 10.1130/g22260.1 Mancktelow, N.S., Pennacchioni, G., 2005.The Control of Precursor Brittle Fracture and Fluid-Rock Interaction on the Development of Single and Paired Ductile Shear Zones.Journal of Structural Geology, 27(4):645-661.doi: 10.1016/j.jsg.2004.12.001 Means, W.D., Hobbs, B.E., Lister, G.S., et al., 1980.Vorticity and Non-Coaxiality in Progressive Deformations.Journal of Structural Geology, 2(3):371-378.doi: 10.1016/0191-8141(80)90024-3 Meng, J.Y., Liu, Y.J., Liang, C.Y., et al., 2013.Characteristics of Ductile Deformation of Jiamusi-Yitong Fault.Global Geology, 32(4):800-807(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-SJDZ201304019.htm Passchier, C.W., Trouw, R.A.J., 2005.Micro Tectonics.Springer-Verlag, Berlin Heidelberg, 1-366. Passchier, C.W., 1988.The Use of Mohr Circles to Describe Non-Coaxial Progressive Deformation.Tectonophysics, 149(3-4):323-338.doi: 10.1016/0040-1951(88)90181-3 Passchier, C.W., Urai, J.L., 1988.Vorticity and Strain Analysis Using Mohr Diagrams.Journal of Structural Geology, 10(7):755-763.doi: 10.1016/0191-8141(88)90082-x Pennacchioni, G., Mancktelow, N.S., 2007.Nucleation and Initial Growth of a Shear Zone Network within Compositionally and Structurally Heterogeneous Granitoids under Amphibolite Facies Conditions.Journal of Structural Geology, 29(11):1757-1780.doi: 10.1016/j.jsg.2007.06.002 Qin, Y., Chen, D.D., Liang, Y.H., et al., 2014.Geochronology of Jian Group in Tong Hua Area, Southern Jilin Province.Earth Science, 38(11):1487-1499 (in Chinese with English abstract). Segall, P., Simpson, C., 1986.Nucleation of Ductile Shear Zones on Dilatant Fractures.Geology, 14(1):56.doi:10.1130/0091-7613(1986)14<56:nodszo>2.0.co;2 Simpson, C., De Paor, D.G., 1993.Strain and Kinematic Analysis in General Shear Zones.Journal of Structural Geology, 15(1):1-20.doi: 10.1016/0191-8141(93)90075-L Sun, M., Armstrong, R.L., Lambert, R.S., et al., 1993.Petrochemistry and Sr, Pb and Nd Isotopic Geochemistry of the Paleoproterozoic Kuandian Complex, the Eastern Liaoning Province, China.Precambrian Research, (1-2):171-190.doi: 10.1016/0191-8141(93)90075-L Wallis, S., 1995.Vorticity Analysis and Recognition of Ductile Extension in the Sanbagawa Belt, SW Japan.Journal of Structural Geology, 17(8):1077-1093.doi: 10.1016/0191-8141(95)00005-x Wallis, S.R., 1992.Vorticity Analysis in a Metachert from the Sanbagawa Belt, SW Japan.Journal of Structural Geology, 14(3):271-280.doi: 10.1016/0191-8141(92)90085-b Wan, Y.S., Song, B., Liu, D.Y., et al., 2006.SHRIMP U-Pb Zircon Geochronology of Palaeoproterozoic Metasedimentary Rocks in the North China Craton:Evidence for a Major Late Palaeoproterozoic Tectonothermal Event.Precambrian Research, 149(3-4):249-271.doi: 10.1016/j.precamres.2006.06.006 Wang, Y.B., Liang, M.H., Huo, Q.Z., et al., 2004.The Study of the Limit Deformation Measurement with Deformation Feldspar in Granite Areas.Northwestern Geology, 37(2):19-24(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-XBDI200402004.htm Weijermars, R., 1991.The Role of Stress in Ductile Deformation.Journal of Structural Geology, 13(9):1061-1078.doi: 10.1016/0191-8141(91)90057-p Weijermars, R., 1998.Taylor-Mill Analogues for Patterns of Flow and Deformation in Rocks.Journal of Structural Geology, 20(1):77-92.doi: 10.1016/s0191-8141(97)00051-5 Wu, F., Zhao, G., Wilde, S.A., et al., 2005.Nd Isotopic Constraints on Crustal Formation in the North China Craton.Journal of Asian Earth Sciences, 24(5):523-545. doi: 10.1016/j.jseaes.2003.10.011 Wu, C.L., 1991.Metamorphic Temperature-Pressure Conditions of Liaohe Group at Liaodong Peninsula.Liaoning geology, (4):342-348 (in Chinese with English abstract). Wu, D., Zhuang, T.X., Liu, X.D., et al., 2013.Petrological and Geochemical Characteristics of Remelting Chorismite in Lianshanguan Area of East Liaoning.World Nuclear Geoscience, 30(4):210-216(in Chinese with English abstract). http://d.wanfangdata.com.cn/CitedResourceRss.ashx?ID=Periodical... Xia, H.R., Liu, J.H., 2011.The Crystallographic Preferred Orientation of Quartz and Its Applications.Geological Bulletin of China, 30(1):58-70(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-ZQYD201101007.htm Xu, H.J., Jin, S.Y., Zheng, B.R., 2007.New Technique of Petrofabric:Electron Backscatter Diffraction(EBSD).Geoscience, 21(2):213-225(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-XDDZ200702006.htm Xu, Z.Q., Wang, Q., Liang, F.H., et al., 2009.Electron Backscatter Diffraction (EBSD) Technique and Its Application to Study of Continental Dynamics.Acta Petrologica Sinica, 25(7):1721-1736(in Chinese with English abstract). http://www.oalib.com/paper/1472350 Yang, Z.S., Yu, B.X., 1984.Palaeotectonics and its Evolution of the Late Precambrian in East China.Journal of Changchun University of Earth Sciences, (2):1-20 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-CCDZ198402000.htm Zhang, B., Zhang, J.J., Guo, L., 2006.Fractal Analysis of Dynamically Recrystallized Quartz Grains and Estimation of Mainly Rheological Parameters of the Rumba Ductile Shear Zone, Northern Himalayan Dome Belt.Geological Sciences, 41(1):158-169. http://en.cnki.com.cn/Article_en/CJFDTotal-DZKX200601014.htm Zhang, Q.S., 1984.Early Cambrian Geological and Mineralization in China.Jilin People's Press, Changchun, 218-450 (in Chinese). Zhang, Q.S., Yang, Z.S., Liu, L.D., 1988.The Early Crust Evolution and Minerals in the Liaodong Peninsula.Geological Publishing House, Beijing (in Chinese). Zhang, J., Zheng, Y., 1997.Polar Mohr Constructions for Strain Analysis in General Shear Zones.Journal of Structural Geology, 19(5):745-748.doi: 10.1016/s0191-8141(96)00119-8 Zhao, G.C., 2009.Metamorphic Evolution of Major Tectonic Units in the Basement of the North China Craton:Key Issues and Discussion.Acta Petrologica Sinica, 25(8):1772-1792(in Chinese with English abstract). http://d.wanfangdata.com.cn/Periodical/ysxb98200908004 Zhao, G.C., Sun, M., Wilde, S.A., et al., 2005.Late Archean to Paleoproterozoic Evolution of the North China Craton:Key Issues Revisited.Precambrian Research, 136(2):177-202.doi: 10.1016/j.precamres.2004.10.002 Zhao, G.C., Wilde, S.A., Cawood, P.A., et al., 2001.Archean Blocks and Their Boundaries in the North China Craton:Lithological, Geochemical, Structural and P-T Path Constraints and Tectonic Evolution.Precambrian Research, 107(1-2):45-73.doi: 10.1016/s0301-9268(00)00154-6 Zhao, G.C., Zhai, M.G., 2013.Lithotectonic Elements of Precambrian Basement in the North China Craton:Review and Tectonic Implications.Gondwana Research, 23(4):1207-1240.doi: 10.1016/j.gr.2012.08.016 Zheng, B.R., Jin, S.Y., 1989.Tectonic Lithography.China University of Geosciences Press, Wuhan(in Chinese). Zheng, Y.D., 2005.Kinematics and Dynamics of the Mesozoic Orogeny and Late-Orogenic Extensional Collapse in the Sino-Mongolian Border Areas.Science in China (Series D), 48(7):849.doi: 10.1360/03yd0552 Zheng, Y.D., Wang, T., 2005.Kinematics and Dynamics of the Mesozoic Orogeny and Late-Orogenic Extensional Collapse in the Sino Mongolian Border Areas.Science in China Series D:Earth Sciences, 35(4):291-303(in Chinese). http://kns.cnki.net/KCMS/detail/detail.aspx?filename=jdxg200507000&dbname=CJFD&dbcode=CJFQ Zheng, Y.D., Wang, T., Zhang, J.J., 2008.Theory and Practice of Kinematic Vorticity (Wk).Earth Science Frontiers, 15(3):209-220 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-DXQY200803019.htm Zhu, K., 2016.The Formation and Evolution of the Archaean Greenstone belt in the Anshan-Benxi Area(Dissertation).Jilin University, Changchun(in Chinese with English abstract). 陈斌, 李壮, 王家林, 等, 2016.辽东半岛~2.2Ga岩浆事件及其地质意义.吉林大学学报(地球科学版), 46(2):303-320. http://www.cnki.com.cn/Article/CJFDTotal-CCDZ201602001.htm 陈荣度, 1990.辽东裂谷的地质构造演化.中国区域地质, (4):306-315, 333. http://www.cqvip.com/QK/95894X/199004/416696.html 郭智添, 1982.辽东连山关早前寒武纪铀矿床地质特征及成矿模式.长春地质学院学报, (S1):84-95, 168. http://www.cnki.com.cn/Article/CJFDTotal-CCDZ1982S1006.htm 韩国卿, 刘永江, 温泉波, 等, 2009.嫩江-八里罕断裂带岭下韧性剪切带变形特征.吉林大学学报:地球科学版, 39(3):397-405. http://www.doc88.com/p-503837425512.html 核工业241大队, 1989. 辽宁省本溪县连山关铀矿床勘探报告. 吉林大学学报(地球科学版). 贺高品, 叶慧文, 1998b.辽东-吉南地区早元古代两种类型变质作用及其构造意义.岩石学报, 14(2):152-162. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB802.002.htm 黄建军, 1994.糜棱岩研究的若干理论与应用初评.化工矿产地质, 16(2):117-122. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=hgkc402.007&dbname=CJFD&dbcode=CJFQ 李刚, 徐仲元, 刘正宏, 等, 2013.医巫闾山变质核杂岩早白垩世伸展变形.岩石学报, 29(3):938-952. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201303017.htm 李婧, 刘永江, 李伟民, 等, 2016.华北克拉通基底花岗质片麻岩变形和流变学研究——以辽西寺儿堡地区为例.大地构造与成矿学, 40(5):891-907. http://d.wanfangdata.com.cn/Periodical/ddgzyckx201605001 李三忠, 刘永江, 2012.辽河群区域变质特征及其大陆动力学意义.地质论评, 47(1):9-18. http://www.oalib.com/paper/4885210 李三忠, 郝德峰, 韩宗珠, 等, 2003.胶辽地块古元古代构造-热演化与深部过程.地质学报, 77(3):328-340. http://www.oalib.com/paper/4876634 李三忠, 郝德峰, 赵国春, 等, 2004.丹东花岗岩的地球化学特征及其成因.岩石学报, 20(6):1417-1423. http://d.wanfangdata.com.cn/Periodical/ysxb98200406011 李三忠, 刘永江, 杨振升, 等, 1998.辽河群变质泥质岩中变质重结晶作用和形作用的关系.岩石学报, 14(3):351-365. http://edu.wanfangdata.com.cn/Periodical/Detail/gjsdz200603013 李三忠, 扬振升, 1996.辽东早元古代造山带隆滑构造解析.长春地质学院学报, 26(3):305-309. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=ccdz603.010&dbname=CJFD&dbcode=CJFQ 李三忠, 杨振升, 刘永江, 1997a.辽河群变质带垂向分层性及其起因.科学通报, 42(24):2631-2636. http://www.cqvip.com/QK/94252X/199724/2746994.html 李三忠, 杨振升, 刘永江, 等, 1997b.胶辽吉地区古元古代早期花岗岩的侵位模式及其与隆滑构造的关系.岩石学报, 13(2):64-77. http://www.oalib.com/paper/1471900 梁琛岳, 刘永江, 李伟, 等, 2011.黑龙江嫩江地区科洛杂岩伸展构造特征.地质通报, 30(2):291-299. doi: 10.3969/j.issn.1671-2552.2011.02.014 梁琛岳, 刘永江, 孟婧瑶, 等, 2015.舒兰韧性剪切带应变分析及石英动态重结晶颗粒分形特征与流变参数估算.地球科学(1):115-129. http://www.earth-science.net/WebPage/Article.aspx?id=3017 刘俊来, 1991.辽吉古裂谷内带顺层构造片岩的变形构造与变形机制.吉林地质, 10(4):1-9. http://www.cnki.com.cn/Article/CJFDTotal-JLDZ199104000.htm 刘俊来, 曹淑云, 邹运鑫, 等, 2008.岩石电子背散射衍射(EBSD)组构分析及应用.地质通报, 27(10):1638-1645. doi: 10.3969/j.issn.1671-2552.2008.10.005 刘晓东, 2012. 连山关地区构造蚀变与铀矿化的关系//全国铀矿大基地建设学术研讨会论文集(上). 刘永江, 李三忠, 白立新, 1996.辽宁海城地区辽河群底部大型韧性滑脱带的构造演化.长春地质学院学报, 26(2):166-171. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=ccdz602.007&dbname=CJFD&dbcode=CJFQ 刘永江, 李三忠, 杨振升, 1997a.华北地台东缘早元古代隆-滑构造模式.地质论评, 43(6):569-576. http://www.cqvip.com/QK/91067X/199706/2724454.html 刘永江, 杨振升, 李三忠, 等, 1997b.古元古代拉伸构造模式——以胶北、辽东和吉南地区为例.长春地质学院学报, 27(2):141-146. 孟婧瑶, 刘永江, 梁琛岳, 等, 2013.佳-伊断裂带韧性变形特征.世界地质, 32(4):800-807. http://www.cnki.com.cn/Article/CJFDTotal-SJDZ201304019.htm 王云斌, 梁明宏, 霍勤知, 等, 2004.利用变形花岗岩体中的长石矿物进行有限应变测量初探.西北地质, 37(2):19-24. http://d.wanfangdata.com.cn/Periodical/xbdz200402004 吴春林, 1991.辽东半岛辽河群变质岩温压条件.辽宁地质, (4):342-348. http://www.cnki.com.cn/Article/CJFDTOTAL-CCDZ201105007.htm 吴迪, 庄廷新, 刘晓东, 等, 2013.辽东连山关地区重熔混合岩岩石地球化学特征.世界核地质科学, 30(4):210-216. http://www.cqvip.com/QK/96867A/201304/48066752.html 夏浩然, 刘俊来, 2011.石英结晶学优选与应用.地质通报, 30(1):58-70. doi: 10.3969/j.issn.1671-2552.2011.01.006 徐海军, 金淑燕, 郑伯让, 2007.岩石组构学研究的最新技术——电子背散射衍射(EBSD).现代地质, 21(2):213-225. http://www.cnki.com.cn/Article/CJFDTotal-XDDZ200702006.htm 许志琴, 王勤, 梁凤华, 等, 2009.电子背散射衍射(EBSD)技术在大陆动力学研究中的应用.岩石学报, 25(7):1721-1736. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200907016.htm 杨振升, 俞保祥, 1984.中国东部晚前寒武纪古构造及其演化.长春地质学院学报, (2):1-20. 张秋生, 1984.中国早前寒武纪地质及成矿作用.长春:吉林人民出版社. 张秋生, 杨振升, 刘连登, 1988.辽东半岛早期地壳演化与矿产.北京:地质出版社:218-450. 赵国春, 2009.华北克拉通基底主要构造单元变质作用演化及其若干问题讨论.岩石学报, 25(8):1772-1792. http://d.wanfangdata.com.cn/Periodical/ysxb98200908004 郑伯让, 金淑燕, 1989.构造岩岩组学.武汉:中国地质大学出版社. 郑亚东, 王涛, 2005.中蒙边界区中生代推覆构造与伸展垮塌作用的运动学和动力学分析.中国科学D辑, 35(4):291-303. http://www.oalib.com/paper/4153403 郑亚东, 王涛, 张进江, 2008.运动学涡度的理论与实践.地学前缘, 15(3):209-220. http://www.wenkuxiazai.com/doc/d34683e3f121dd36a32d82bb.html 朱凯, 2016. 鞍山-本溪地区太古宙绿岩带的形成及演化(博士学位论文). 吉林: 吉林大学. -
点击查看大图
图(6) / 表(3)
计量
- 文章访问数: 4732
- HTML全文浏览量: 2109
- PDF下载量: 44
- 被引次数: 0
