Tectonic Pattern and Genetic Mechanism at Nanguan Area, West Hill of Beijing
-
摘要: 北京西山地区广泛发育SE-NW向近乎同时期的逆冲推覆构造和伸展构造，为理解华北克拉通东部构造演化至关重要，而其构造组合特征、变形时代、形成机制和构造动力学背景却没有明确的认识.精细的野外构造研究表明北京西山的南观地区，发育逆冲推覆构造+变质核杂岩的构造组合，形成一种新的构造组合型式：“楔沉式”.“楔沉式”构造组合型式的特征：（1）产状相近的一套逆冲断层和正断层，共同构成上窄下宽的楔状褶皱-断层构造；（2）楔状体斜向向下楔入；（3）中间为比较新的地层（倒转向斜），两侧为老的地层.通过对卷入逆冲推覆构造呈“布丁状”透镜体产出的花岗岩脉和闪长玢岩脉进行锆石U-Pb年代学研究，其形成年龄分别为141±2 Ma和139±2 Ma.结合前人对侵入逆冲推覆构造的（南窖）石英二长岩岩枝的形成时代（128~136 Ma），认为南观逆冲推覆构造的形成时代为140~130 Ma，稍早于、或与房山变质核杂岩的形成时代近乎同时.逆冲推覆方向为320°~335°，与变质核杂岩代表的伸展构造的最大拉伸方向（SE-NW向）近乎一致.因此，北京西山地区（乃至华北克拉通东部）晚中生代逆冲构造-岩浆活动-伸展构造，这种独特的构造组合型式是构造体制从挤压向伸展转换的体现，也是华北克拉通破坏的构造体现，其形成机制可能与太平洋板块的俯冲紧密相关.Abstract: A series of tectonic association of the thrust nappe structure and the extensional tectonics are widely developed in the West Hill of Beijing, which are very important for understanding the tectonic evolution of the eastern part of North China craton (NCC). However, their deformed age, tectonic dynamic background and genetic mechanism are poorly understood. The Nanguan area in the West Hill of Beijing is an ideal place to decipher such a tectonic pattern. The detailed field structure observations show a tectonic association of the thrust nappe structure and the metamorphic core complex structure in the Nanguan area, generating a new type of tectonic pattern: the downward diapiric tectonics. It has the following characteristics: (1) wedge-shaped fold-fault structure with a normal fault along one side of the fold and a thrust fault along another side; (2) the fold (overturned syncline) is centered and both sides are older strata or basements, and (3) downward diapiric structure of the wedge-shaped body. Pudding-shaped lens of granitic and dioritic dykes were found in the thrust nappe. The granitic and dioritic lens give two weighted zircon U-Pb age of 141±2 Ma and 139±2 Ma, respectively. The previous studies suggest that a quartz monozite, which intruded into the thrust nappe, has zircon U-Pb age of 128-136 Ma. Thus, the deformation time of the thrust nappe is between ca. 140 and 130 Ma, which is a little earlier than or nearly coeval with the extensional tectonics represented by the metamorphic core complex structure. The orientation of the thrust nappe structure was generally W320°-335°N. The principal stress orientation of the extensional tectonics was also SE-NW trending. Thus, the tectonic pattern of compression-magmatism-extension in the West Hill of Beijing (and even in the eastern part of NCC) might be closely related to SE-NW-trending subduction of the Pacific plate. The tectonic pattern also might be an expression to the destroy or lithospheric thinning of the NCC.
-
图 1 华北克拉通地质简图(a)和北京西山南部区域地质构造略图(b)
a.据Wang et al.(2011)修改; b. 据舒坦等(2019)修改. 1. 第四系; 2. 白垩系; 3. 侏罗系; 4. 三叠系‒石炭系; 5. 寒武系‒奥陶系; 6. 新元古界青白口系; 7. 中元古界蓟县系; 8. 早元古界长城系; 9. 太古宇官地杂岩; 10. 房山花岗闪长岩体; 11. 背斜轴迹; 12. 向斜轴迹; 13. 拆离断层; 14. 逆断层及产状(°); 15. 正断层及产状(°); 16. 地质界线; 17. 平行不整合及角度不整合; 18. 面理产状(°); 19. 城镇及居民点; 20. 剖面线
Fig. 1. Geologic sketch map of the North China craton (a) and regional structural and geological sketch map of the southern part of the West Hill of Beijing (b)
图 2 东岭子‒南观区域地质构造略图
据《周口店地质图》(1∶5万)修改. 1. 第四系; 2. 下‒中二叠统山西组; 3. 中石炭‒下二叠统太原组; 4. 中石炭统本溪组; 5. 下‒中奥陶统冶里‒马家沟组; 6. 上寒武统炒米店组; 7. 中元古界下马岭组; 8. 早元古界长城系; 9. 太古宇官地杂岩; 10. 房山花岗闪长岩; 11. 房山石英闪长岩; 12. 拆离断层; 13. 逆断层; 14. 地质界线; 15. 糜棱面理或韧性剪切带产状(°); 16. 地层产状(°); 17. 倒转地层产状(°); 18. 剖面线
Fig. 2. Regional structural and geological sketch map of the Donglingzi-Nanguan area
图 3 南观实测剖面(A-A’)(a)和野外照片(b~g)
b.花岗质糜棱岩(官地杂岩), 糜棱面理的产状为46°∠66°; c.下马岭组(Pt2x)粉砂质板岩, 层理产状为44°∠72°; d.炒米店组(∈4ch), 地层产状为57°∠62°; e.冶里组‒马家沟组(O1y-2m)灰岩, 地层产状为46°∠73°; f.炒米店组(∈4ch), 地层倒转，产状为53°∠50°; g.长城系(Pt1ch)砂质板岩(面理产状为62°∠53°)呈“布丁状”透镜体的花岗岩脉; h.长城系(Pt1ch)砂质板岩呈“布丁状”透镜体的闪长玢岩脉. 图例同图 2
Fig. 3. Measured section (A-A') at the Nanguan area (a) and the relevant field pictures (b-g)
图 4 官地杂岩中的花岗质糜棱岩和韧性剪切带
a.韧性剪切带野外照片，角闪岩被剪切呈透镜体状; b.东岭子村东万路北侧太古代花岗质糜棱岩(Arg)野外素描图
Fig. 4. Granitic mylonite and ductile shear zone in Archean rocks
图 5 向斜倒转翼炒米店组(∈4ch)中发育的不对称小褶皱
a.野外照片; b.素描图，显示“左行”剪切变形
Fig. 5. Asymmetrical small fold at the synclinal inverted wing (Chaomidian Formation, ∈4ch)
图 6 向斜倒转翼炒米店组(∈4ch)中发育的次级褶皱
a.野外照片; b.素描图，显示“左行”剪切变形
Fig. 6. Sunsidiary fold at the synclinal inverted wing (Chaomidian Formation, ∈4ch)
图 7 向斜转折端炒米店组(∈4ch)中发育的次级褶皱
a.野外照片; b.三维素描图，显示转折端加厚
Fig. 7. Sunsidiary fold at the synclinal turning end (Chaomidian Formation, ∈4ch)
图 8 (a) “布丁状”花岗岩脉; (b) 左上角的插图是局部放大, 标注测年样品采集点
Fig. 8. Granitic lenses in pudding shape (a); illustration at the top left corner is a local zoom showing location of dating sample (b)
图 9 “布丁状”闪长玢岩脉, 标注测年样品采集点(a)和局部放大图(b)
Fig. 9. Puddings of diorite porphyrite showing location of dating sample (a) and the local zoom (b)
图 10 部分锆石CL图像和相应的206Pb/238U年龄
a.花岗岩脉(17NG01); b. 闪长玢岩脉(17NG02). 黄色圈为锆石U-Pb原位测年点(束斑大小: 32 μm)
Fig. 10. CL images of representative zircon grains with 206Pb/238U age of the dykes at the Nanguan area
图 12 闪长玢岩脉锆石U-Pb年龄
a.所有测年数据包括继承核、捕虏晶和岩浆结晶颗粒; b.早白垩世岩浆结晶年龄数据
Fig. 12. Zircon U-Pb concordia diagrams for the dyke of diorite porphyrite
图 13 “布丁状”岩脉透镜体形成示意图
a.~140 Ma, 花岗岩脉和闪长玢岩脉侵入长城系(Pt1ch); b.140~130 Ma(?), 南观逆冲推覆构造发育过程中，岩脉发生简单剪切变形(如图所示)
Fig. 13. Schematic diagrams of the dyke lenses in pudding shape
-
[1] Boyer, S.E., Elliott, D., 1982. Thrust System. The American Association of Petroleum Geologist Bulletin, 68(9): 1196-1230. https://doi.org/10.1016/s0040-1951(00)00252-3 [2] Cai, J.H., Yan, G.H., Mu, B.L., et al., 2005. Zircon U-Pb Age, Sr-Nd-Pb Isotopic Compositions and Trace Element of Fangshan Complex in Beijing and Their Petrogenesis Significance. Acta Petrologica Sinica, 21(3): 776-788 (in Chinese with English abstract). [3] Chapman, J.B., Carrapa, B., Ballato, P., et al., 2017. Intracontinental Subduction beneath the Pamir Mountains: Constraints from Thermokinematic Modeling of Shortening in the Tajik Fold-and-Thrust Belt. Geological Society of America Bulletin, 129 (11-12): 1450-1471. https://doi.org/10.1130/B31730.1 [4] Chen, K., Xiong, Y.X., 1935. Reverse Faults in the Western Hills of Beijing. Journal of the Chinese Geological Society, 14(4): 535-567 (in Chinese). [5] Chen, L., Ai, Y. S., 2009. Discontinuity Structure of the Mantle Transition Zone beneath the North China Craton from Receiver Function Migration. Journal of Geophysical Research: Solid Earth, 114(B6): 52. https://doi.org/10.1029/2008JB006221 [6] Chen, N.S., Wang, F.Z., 2006. Single-Grain Evaporation Zircon Pb-Pb Ages of Guandi Complex, Zhoukoudian Area, Western Hills of Beijing: Archaean Genesis and Cratonization Events of the North China Craton. Geological Science and Technology Information, 25(3): 41-44 (in Chinese with English abstract). [7] Chen, Y., Zhu, G., Jiang, D. Z., et al., 2013. Timing Determination of Phase B of the Yanshanian Movement in the Eastern North China Craton: Evidence from Dating of a Ductile Shear Zone in Sihetang, Northeastern Beijing. Acta Geologica Sinica, 87(3): 295-310 (in Chinese with English abstract). [8] Chen, Y., Zhu, G., Jiang, D. Z., et al., 2014. Deformation Characteristics and Formation Mechanism of the Yunmengshan Metamorphic Core Complex. Chinese Science Bulletin, 59(16): 1525-1541 (in Chinese). doi: 10.1360/csb2014-59-16-1525 [9] Cogné, J. P., Kravchinsky, V. A., Halim, N., et al., 2005. Late Jurassic-Early Cretaceous Closure of the Mongol-Okhotsk Ocean Demonstrated by New Mesozoic Palaeomagnetic Results from the Trans-Baïkal Area (SE Siberia). Geophysical Journal International, 163(2): 813-832. https://doi.org/10.1111/j.1365-246X.2005.02782.x [10] Coney, P. J., 1987. The Regional Tectonic Setting and Possible Causes of Cenozoic Extension in the North American Cordillera. Geological Society, London, Special Publications, 28(1): 177-186. https://doi.org/10.1144/gsl.sp.1987.028.01.13 [11] Cope, T. D., Shultz, M. R., Graham, S. A., 2007. Detrital Record of Mesozoic Shortening in the Yanshan Belt, NE China: Testing Structural Interpretations with Basin Analysis. Basin Research, 19(2): 253-272. https://doi.org/10.1111/j.1365-2117.2007.00321.x [12] Davis, G.A., Zheng, Y.D., Wang, C., et al., 1998. Geometry and Geochronology of Yanshan Belt Tectonics. In: Department of Geology, Peking University, ed., Papers Collection of International Geological Conference at Peking University. Seismological Press, Beijing, 275-292. [13] Davis, G.A., Zheng, Y.D., Wang, C., et al., 2001. Mesozoic Tectonic Evolution of the Yanshan Fold and Thrust Belt, with Emphasis on Hebei and Liaoning Provinces, Northern China. In: Hedrix, M.S., Davis, G.A., eds., Paleozoic and Mesozoic Tectonic Evolution of Central Asia. Form Continental Assembly to Intracontinental Deformation, Geological Society of America Memoir, Boulder, Colorado, 194: 171-197. [14] Deng, J.F., Zhao, G. C., Zhao, H.L., et al., 2000. Yanshanian Igneous Petrotectonic Assemblsge and Orogenic-Deep Processes in East China. Geological Review, 46(1): 41- 48 (in Chinese with English abstract). [15] Deng, J.F., Zhao, H.L., Mo, X.X., et al., 1996. Continental Roots-Plume Tectonics of China: Key to the Continental Dynamics. Geological Publishing House, Beijing, 1-110 (in Chinese). [16] Diwu, C. R., Sun, Y., Guo, A. L., et al., 2011. Crustal Growth in the North China Craton at ~2.5 Ga: Evidence from In Situ Zircon U-Pb Ages, Hf Isotopes and Whole-Rock Geochemistry of the Dengfeng Complex. Gondwana Research, 20(1): 149-170. https://doi.org/10.1016/j.gr.2011.01.011 [17] Dong, S.W., Wu, X.H., Wu, Z.H., et al., 2000. On Tectonic Seesawing of the East Asia Continent—Global Implication of the Yanshanian Movement. Geological Review, 46(1): 7-13 (in Chinese with English abstract). [18] Dumitru, T. A., Zhou, D., Chang, E. Z., et al., 2001. Uplift, Exhumation, and Deformation in the Chinese Tian Shan. In: Hendrix, M. S., Davis, G. A., eds., Paleozoic and Mesozoic Tectonic Evolution of Central Asia: From Continental Assembly to Intracontinental Deformation. Geol. Soc. Am. Mem., 194: 71-99. [19] Ge, M.C., Ren, J.Y., 1990. Nappe Structures in the Western Hills of Beijing. In: Zhang, J.S., Shan, W.L., eds, Geological Study of the Western Hills of Beijing. China University of Geosciences Press, Wuhan, 30-41 (in Chinese). [20] Griffin, W. L., Andi, Z., O'Reilly, S. Y., et al., 1998. Phanerozoic Evolution of the Lithosphere beneath the Sino-Korean Craton. Mantle Dynamics and Plate Interactions in East Asia. American Geophysical Union, New York, 107-126. https://doi.org/10.1029/gd027p0107 [21] Guillot, S., Replumaz, A., 2013. Importance of Continental Subductions for the Growth of the Tibetan Plateau. Bulletin de La Société Géologique de France, 184(3): 199-223. https://doi.org/10.2113/gssgfbull.184.3.199 [22] He, B., Xu, Y.G., Wang, Y.M., et al., 2005. Magmatic Diapir of Fangshan Pluton in the Western Hills, Beijing and Its Geological Significance. Earth Science, 30(3): 298-308 (in Chinese with English abstract). [23] Hu, Z. C., Zhang, W., Liu, Y. S., et al., 2015. "Wave" Signal-Smoothing and Mercury-Removing Device for Laser Ablation Quadrupole and Multiple Collector ICP-MS Analysis: Application to Lead Isotope Analysis. Analytical Chemistry, 87(2): 1152-1157. https://doi.org/10.1021/ac503749k [24] Huang, J. L., Zhao, D. P., 2006. High-Resolution Mantle Tomography of China and Surrounding Regions. Journal of Geophysical Research Atmospheres, 111(B9): B09305. https://doi.org/10.1029/2005jb004066 [25] Li, D.X., 2015. Synthetical Analyses of the Formation and Deformation of the Beiling Syncline in Fangshan, Beijing. Geoscience, 29(3): 481-493 (in Chinese with English abstract). [26] Li, J.X., Li, Z.W., Liu, S.G., et al., 2015. Analysis of Microtectonics in Deformed Rocks of Main Faults of Daba Acuate Orogenic Belts, China. Geotectonica et Metallogenia, 39(4): 587-600 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DGYK201504003.htm [27] Li, J.Y., 1998. Some New Ideas on Tectonics of NE China and Its Neighboring Areas. Geological Review, 44(4): 339-347 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZLP199804001.htm [28] Li, J.Y., Qu, J.F., Zhang, J., et al., 2013. New Developments on the Reconstruction of Phanerozoic Geological History and Research of Metallogenic Geological Settings of the Northern China Orogenic Region. Geological Bulletin of China, 32(2): 207-219 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-ZQYD2013Z1000.htm [29] Li, W.P., Lu, F.X., Li, X.H., et al., 2001. Geochemical Features and Origin of Volcanic Rocks of Tiaojishan Formation in Western Hills of Beijing. Acta Petrologica et Mineralogica, 20(2): 123-133 (in Chinese with English abstract). [30] Lin, W., Wang, Q. C., Wang, J., et al., 2011. Late Mesozoic Extensional Tectonics of the Liaodong Peninsula Massif: Response of Crust to Continental Lithosphere Destruction of the North China Craton. Science in China (Series D: Earth Sciences), 41(5): 638-653 (in Chinese). [31] Liu, Y., Gao, S., Hu, Z., et al., 2010. Continental and Oceanic Crust Recycling-Induced Melt-Peridotite Interactions in the Trans-North China Orogen: U-Pb Dating, Hf Isotopes and Trace Elements in Zircons from Mantle Xenoliths. Journal of Petrology, 51(1-2): 537-571. https://doi.org/10.1093/petrology/egp082 [32] Ludwig, K.R., 2003. Isoplot 3.00: A Geochronological Toolkit for Microsoft Excel. Berkeley Geochronology Center Special Publication, Berkeley, 70. [33] Ma, C.Q., 1988. The Magma-Dynamic Mechanism of Emplacement and Compositional Zonation of the Zhoukoudian Stock, Beijing. Acta Geologica Sinica, 62 (4): 329-341 (in Chinese with English abstract). [34] Niu, B.G., He, Z.J., Song, B., 2003. SHRIMP Geochronology of Volcanics of the Zhangjiakou Formation and Its Great Significance. Geological Bulletin of China, 22(2): 140-141 (in Chinese). [35] Niu, B.G., He, Z.J., Song, B., et al., 2004. SHRIMP Geochronology of Volcanics of the Zhangjiakou and Yixian Formations, Northern Hebei Province, with a Discussion on the Age of the Xing'anling Group of the Great Hinggan Mountains and Volcanic Strata of the Southeastern Coastal Area of China. Acta Geologica Sinica, 78(6): 1214-1228. https://doi.org/10.1111/j.1755-6724.2004.tb00778.x [36] Qi, J.F., Yang, Q., Lu, K.Z., et al., 2004. Geologic Map of Sub-Outcrop and Its Implied Information of Tectogenesis in Bohai Bay Basin Province. Earth Science Frontiers, 11(3): 299-307 (in Chinese with English abstract). [37] Ren, J.S., 1990. Tectonic Evolution and Mineralization of Continental Lithosphere in Eastern China and Adjacent Areas. Science Press, Beijing (in Chinese). [38] Scisciani, V., Tavarnelli, E., Calamita, F., 2002. The Interaction of Extensional and Contractional Deformations in the Outer Zones of the Central Apennines, Italy. Journal of Structural Geology, 24(10): 1647-1658. https://doi.org/10.1016/s0191-8141(01)00164-x [39] Sengor, A. M. C., 1996. Paleotectonics of Asia: Fragments of a Synthesis. In: Yin, A., Harrison, T. M., eds., The Tectonic Evolution of Asia. Cambridge University Press, Cambridge, 486-640. [40] Shan, W. L., Wang, F. Z., Fu, Z. R., et al., 1989. On the Tectonic Evolution of Cover Rocks in the Southern Part of West-Hill, Beijing. Earth Science, 14(1): 37-44 (in Chinese with English abstract). [41] Shu, T., Xu, H.J., Zhang, J.F., et al., 2019. Deformation Characteristics and Time of Taipingshan Folds in Fangshan Area, Beijing: Implications for Early Cretaceous Compressional Tectonics of North China Craton. Earth Science, 44(5): 1734-1748 (in Chinese with English abstract). [42] Song, H.L., 1996. Characteristics of Fangshan Metamorphic Core Complex, Beijing and a Discussion about Its Origin. Geoscience, 10(2): 149-158 (in Chinese with English abstract). [43] Sun, J. F., Yang, J. H., Wu, F. Y., et al., 2010. Magma Mixing Controlling the Origin of the Early Cretaceous Fangshan Granitic Pluton, North China Craton: In Situ U-Pb Age and Sr-, Nd-, Hf- and O-Isotope Evidence. Lithos, 120(3-4): 421-438. https://doi.org/10.1016/j.lithos.2010.09.002 [44] Swisher, C. C., Wang, X. L., Zhou, Z. H., et al., 2002. Further Support for a Cretaceous Age for the Feathered-Dinosaur Beds of Liaoning, China: New 40Ar-39Ar Dating of the Yixian and Tuchengzi Formations. Chinese Science Bulletin, 47(2): 136-139. https://doi.org/10.1360/02tb9031 [45] Tang, Y. J., Zhang, H. F., Nakamura, E., et al., 2011. Multistage Melt/Fluid-Peridotite Interactions in the Refertilized Lithospheric Mantle beneath the North China Craton: Constraints from the Li-Sr-Nd Isotopic Disequilibrium between Minerals of Peridotite Xenoliths. Contributions to Mineralogy and Petrology, 161(6): 845-861. https://doi.org/10.1007/s00410-010-0568-1 [46] Tang, Y. J., Zhang, H. F., Ying, J. F., et al., 2013. Widespread Refertilization of Cratonic and Circum-Cratonic Lithospheric Mantle. Earth-Science Reviews, 118: 45-68. https://doi.org/10.1016/j.earscirev.2013.01.004 [47] Thompson, A. B., Schulmann, K., Jezek, J., et al., 2001. Thermally Softened Continental Extensional Zones (Arcs and Rifts) as Precursors to Thickened Orogenic Belts. Tectonophysics, 332(1-2): 115-141. https://doi.org/10.1016/s0040-1951(00)00252-3 [48] Tong, J.N., Xu, R., Yuan, Y.M., 2013. Lithostratigraphy and Reconstruction of Sedimentary Sequence and Environment in Zhoukoudian Area of Beijing. Journal of Earth Sciences and Environment, 35(1): 15-23 (in Chinese with English abstract). [49] Wan, T.F., 1981. A Discussion on the Structural Features and Formation Mechanism of the Nandazhai-Babaoshan Fault Zone in the Western Hills of Beijing. Collected Essays on Structural Geology, 1: 152-164 (in Chinese). [50] Wang, Y., Li, J.Y., 2007. Thermochronological Constraints on the Formation of ESE110°-120° Stretching Lineations at Nanjiao Area, West Hills of Beijing. Acta Petrologica Sinica, 23(3): 617-624 (in Chinese with English abstract). [51] Wang, Y., Zhou, L., Li, J., 2011. Intracontinental Superimposed Tectonics: A Case Study in the Western Hills of Beijing, Eastern China. Geological Society of America Bulletin, 123(5-6): 1033-1055. https://doi.org/10.1130/b30257.1 [52] Xiao, W. J., Windley, B. F., Hao, J., et al., 2003. Accretion Leading to Collision and the Permian Solonker Suture, Inner Mongolia, China: Termination of the Central Asian Orogenic Belt. Tectonics, 22(6): 1069-1089. https://doi.org/10.1029/2002tc001484 [53] Xu, H. J., Song, Y. R., Ye, K., et al., 2012. Petrogenesis of Mafic Dykes and High-Mg Adakitic Enclaves in the Late Mesozoic Fangshan Low-Mg Adakitic Pluton, North China Craton. Journal of Asian Earth Sciences, 54/55: 143-161. https://doi.org/10.1016/j.jseaes.2012.04.008 [54] Xu, H.J., Song, Y.R., Zhang, J.F., et al., 2012. Geological Field Practice Teaching of Magma Mixing in the Fangshan Pluton in Zhoukoudian District of Beijing. Chinese Geological Education, 4: 135-139 (in Chinese with English abstract). [55] Xu, Y. G., Blusztajn, J., Ma, J. L., et al., 2008. Late Archean to Early Proterozoic Lithospheric Mantle beneath the Western North China Craton: Sr-Nd-Os Isotopes of Peridotite Xenoliths from Yangyuan and Fansi. Lithos, 102(1-2): 25-42. https://doi.org/10.1016/j.lithos.2007.04.005 [56] Xu, Z.Q., Wang, Q., Li, Z.H., et al., 2016. Indo-Asian Collision: Tectonic Transition from Compression to Strike Slip. Acta Geologica Sinica, 90(1): 1-23 (in Chinese with English abstract). doi: 10.1111/1755-6724.12639 [57] Yakubchuk, A.S., Edwards, A.C., 1999. Auriferous Paleozoic Accretionary Terranes within the Mongol-Okhotsk Suture Zone, Russian Far East. In: Weber, G., ed., Proceedings Pacrim'99. Australasian Institute of Mining and Metallurgy, Publications Series 4/99: 347-358. [58] Yan, D.P., Zhou, M. F., Song, H.L., et al., 2005. A Geochronological Constraint to the Guandi Complex, Western Hills of Beijing, and Its Implications for the Tectonic Evolution. Earth Science Frontiers, 12(2): 332-337 (in Chinese with English abstract). [59] Yan, D. P., Zhou, M. F., Song, H. L., et al., 2006. Mesozoic Extensional Structures of the Fangshan Tectonic Dome and Their Subsequent Reworking during Collisional Accretion of the North China Block. Journal of the Geological Society, 163(1): 127-142. https://doi.org/10.1144/0016-764904-154 [60] Yan, D. P., Zhou, M. F., Zhao, D. G., et al., 2011. Origin, Ascent and Oblique Emplacement of Magmas in a Thickened Crust: An Example from the Cretaceous Fangshan Adakitic Pluton, Beijing. Lithos, 123(1-4): 102-120. https://doi.org/10.1016/j.lithos.2010.11.015 [61] Yao, L.J., Yan, D.P., Hu, L., 2007. Structure Style and Temperature-Pressure Estimation of the Detachment Fault Zone around Fangshan Dome, Western Hills of Beijing. Earth Science, 32(3): 357-365 (in Chinese with English abstract). [62] Yi, M.C., 1993. Neotectonic Movement and Wei-Yan Rift Structure. Seismological Press, Beijing, 153-170 (in Chinese). [63] Zhai, M. G., Bian, A. G., Zhao, T. P., 2000. The Amalgamation of the Supercontinent of North China Craton at the End of Neo-Archaean and Its Breakup during Late Palaeoproterozoic and Meso-Proterozoic. Science in China (Series D: Earth Sciences), 43(Suppl. ): 219-232. https://doi.org/10.1007/BF02911947 [64] Zhang, C.H., 1999. A Primary Discussion on the Intraplate Orogenic Belt. Earth Science Frontiers, 6(4): 295-308 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DXQY199904018.htm [65] Zhang, C.H., Deng, H.L., Li, C.M., et al., 2012. An Out-of-Syncline Thrust Model for the "Chengde Thrust Sheet" in Central Intraplate Yanshan Orogenic Belt, Northern North China Craton. Earth Science Frontiers, 19(5): 27-40 (in Chinese with English abstract). http://www.cqvip.com/QK/98600X/201205/44087859.html [66] Zhang, C. H., Li, C. M., Deng, H. L., et al., 2011. Mesozoic Contraction Deformation in the Yanshan and Northern Taihang Mountains and Its Implications to the Destruction of the North China Craton. Science in China (Series D: Earth Sciences), 41(5): 593-617 (in Chinese). http://www.cnki.com.cn/Article/CJFDTotal-JDXG201106003.htm [67] Zhang, C.H., Zhang, Y., Li, H.L., et al., 2006. Late Mesozoic Thrust Tectonics Framework in the Western Part of the Yanshan Orogenic Belt and the Western Hills of Beijing: Characteristics and Significance. Earth Science Frontiers, 13(2): 165-183 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DXQY200602019.htm [68] Zhang, H., Wang, M. X., Liu, X. M., 2008. LA-ICP-MS Dating of Zhangjiakou Formation Volcanic Rocks in the Zhangjiakou Region and Its Geological Significance. Progress in Natural Science, 18(8): 975-981. https://doi.org/10.1016/j.pnsc.2008.01.028 [69] Zhang, H., Wei, Z. L., Liu, X. M., et al., 2009. Constraints on the Age of the Tuchengzi Formation by LA-ICP-MS Dating in Northern Hebei-Western Liaoning, China. Science China Earth Sciences, 52(4): 461-470. https://doi.org/10.1007/s11430-009-0052-9 [70] Zhang, H. F., Goldstein, S. L., Zhou, X. H., et al., 2009. Comprehensive Refertilization of Lithospheric Mantle beneath the North China Craton: Further Os-Sr-Nd Isotopic Constraints. Journal of the Geological Society, 166(2): 249-259. https://doi.org/10.1144/0016-76492007-152 [71] Zhang, L., Liu, B., Chen, N.S., et al., 2008. Age of the Granitoid Pluton from Nanjiao, Zhoukoudian, Beijing and Its Geological Implication. Geological Science and Technology Information, 27(6): 43-46 (in Chinese with English abstract). [72] Zhang, Q., Qian, Q., Wang, E.Q., et al., 2001. An East China Plateau in Mid-Late Yanshanian Period: Implication from Adakites. Scientia Geologica Sinica, 36(2): 248-255 (in Chinese with English abstract). [73] Zhang, Z.Y., Wu, X.G., Li, H.Y., 1983. Basic Characteristics of the Nappe Structure in the Changping-Xiazhuang Area in Beijing. Journal of Shijiazhuang University of Economics, 6(3): 3-9 (in Chinese). [74] 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. https://doi.org/10.1016/j.precamres.2004.10.002 [75] Zhao, G. C., Wilde, S. A., Cawood, P. A., et al., 2002. SHRIMP U-Pb Zircon Ages of the Fuping Complex: Implications for Late Archean to Paleoproterozoic Accretion and Assembly of the North China Craton. American Journal of Science, 302(3): 191-226. https://doi.org/10.2475/ajs.302.3.191 [76] Zhao, L., Zheng, T. Y., 2005. Using Shear Wave Splitting Measurements to Investigate the Upper Mantle Anisotropy beneath the North China Craton: Distinct Variation from East to West. Geophysical Research Letters, 32(10): L10309. https://doi.org/10.1029/2005gl022585 [77] Zhao, Y., Xu, G., Zhang, S.H., et al., 2004a. Yanshanian Movement and Conversion of Tectonic Regimes in East Asia. Earth Science Frontiers, 11(3): 319-328 (in Chinese with English abstract). [78] Zhao, Y., Zhang, S.H., Xu, G., et al., 2004b. The Jurassic Major Tectonic Events of the Yanshanian Intraplate Deformation Belt. Regional Geology of China, 23(9): 854-863 (in Chinese with English abstract). [79] Zhao, Z.Y., Shan, W.L., 1994. A Preliminary Study of the Nandazhai Thrust-Nappe, Western Hill, Beijing. Journal of Hebei GEO University, 17(5): 464-470 (in Chinese with English abstract). [80] Zhu, G., Chen, Y., Jiang, D. Z., et al., 2015. Rapid Change from Compression to Extension in the North China Craton during the Early Cretaceous: Evidence from the Yunmengshan Metamorphic Core Complex. Tectonophysics, 656: 91-110. https://doi.org/10.1016/j.tecto.2015.06.009 [81] Zhu, G., Wang, W., Gu, C.C., et al., 2016. Late Mesozoic Evolution History of the Tan-Lu Fault Zone and Its Indication to Destruction Processes of the North China Craton. Acta Petrologica Sinica, 32(4): 3-17 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB201604001.htm [82] Zhu, R. X., Chen, L., Wu, F. Y., et al., 2011. Timing, Scale and Mechanism of the Destruction of the North China Craton. Science in China (Series D: Earth Sciences), 41(5): 583-592 (in Chinese). http://gji.oxfordjournals.org/external-ref?access_num=10.1007/s11430-011-4203-4&link_type=DOI [83] Zhu, R.X., Xu, Y.G., Zhu, G., et al., 2012. Destruction of the North China Craton. Science in China (Series D: Earth Sciences), 42(8): 1135-1159 (in Chinese). [84] Zong, K. Q., Klemd, R., Yuan, Y., et al., 2017. The Assembly of Rodinia: The Correlation of Early Neoproterozoic (ca. 900 Ma) High-Grade Metamorphism and Continental Arc Formation in the Southern Beishan Orogen, Southern Central Asian Orogenic Belt (CAOB). Precambrian Research, 290: 32-48. https://doi.org/10.1016/j.precamres.2016.12.010 [85] 蔡剑辉, 阎国翰, 牟保磊, 等, 2005. 北京房山岩体锆石U-Pb年龄和Sr、Nd、Pb同位素与微量元素特征及成因探讨. 岩石学报, 21(3): 776-788. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200503018.htm [86] 陈凯, 熊永先, 1935. 北京西山之逆掩断层. 中国地质学会会志, 14(4): 535-567. [87] 陈能松, 王方正, 2006. 北京西山周口店关坻杂岩蒸发法锆石Pb-Pb年龄: 太古宙成因和克拉通化事件证据. 地质科技情报, 25(3): 41-44. doi: 10.3969/j.issn.1000-7849.2006.03.007 [88] 陈印, 朱光, 姜大志, 等, 2013. 四合堂剪切带活动时代及其对燕山运动B幕时间的限定. 地质学报, 87(3): 295-310. https://www.cnki.com.cn/Article/CJFDTOTAL-DZXE201303002.htm [89] 陈印, 朱光, 姜大志, 等, 2014. 云蒙山变质核杂岩的变形规律与发育机制. 科学通报, 59(16): 1525-1541. https://www.cnki.com.cn/Article/CJFDTOTAL-KXTB201416007.htm [90] 邓晋福, 赵国春, 赵海玲, 等, 2000. 中国东部燕山期火成岩构造组合与造山-深部过程. 地质论评, 46(1): 41-48. doi: 10.3321/j.issn:0371-5736.2000.01.006 [91] 邓晋福, 赵海玲, 莫宣学, 等, 1996. 中国大陆根-柱构造: 大陆动力学的钥匙. 北京: 地质出版社, 1- 110. [92] 董树文, 吴锡浩, 吴珍汉, 等, 2000. 论东亚大陆的构造翘变: 燕山运动的全球意义. 地质论评, 46(1): 8-13. doi: 10.3321/j.issn:0371-5736.2000.01.002 [93] 葛孟春, 任建业, 1990. 北京西山推覆构造. 见: 张吉顺, 单文琅编. 北京西山地质研究. 武汉: 中国地质大学出版社, 30-41. [94] 何斌, 徐义刚, 王雅玫, 等, 2005. 北京西山房山岩体岩浆底辟构造及其地质意义. 地球科学, 30(3): 298-308. http://www.earth-science.net/article/id/1412 [95] 李东旭, 2015. 北京房山北岭向斜形成与形变综合解析. 现代地质, 29(3): 481-493. doi: 10.3969/j.issn.1000-8527.2015.03.001 [96] 李金玺, 李智武, 刘树根, 等, 2015. 大巴山弧形构造带主要断裂带变形岩石显微组构分析及意义. 大地构造与成矿学, 39(4): 587-600. https://www.cnki.com.cn/Article/CJFDTOTAL-DGYK201504003.htm [97] 李锦轶, 1998. 中国东北及邻区若干地质构造问题的新认识. 地质论评, 44(4): 339-347. doi: 10.3321/j.issn:0371-5736.1998.04.002 [98] 李锦轶, 曲军峰, 张进, 等, 2013. 中国北方造山区显生宙地质历史重建与成矿地质背景研究进展. 地质通报, 32(2): 207-219. doi: 10.3969/j.issn.1671-2552.2013.02.001 [99] 李伍平, 路凤香, 李献华, 等, 2001. 北京西山髫髻山组火山岩地球化学特征与岩浆起源. 岩石矿物学杂志, 20(2): 123-133. doi: 10.3969/j.issn.1000-6524.2001.02.003 [100] 林伟, 王清晨, 王军, 等, 2011. 辽东半岛晚中生代伸展构造: 华北克拉通破坏的地壳响应. 中国科学(D辑: 地球科学), 41(5): 638-653. https://www.cnki.com.cn/Article/CJFDTOTAL-JDXK201105004.htm [101] 马昌前, 1988. 北京周口店岩株侵位和成分分带的岩浆动力学机理. 地质学报, 62 (4): 329-341. https://www.cnki.com.cn/Article/CJFDTOTAL-DZXE198804004.htm [102] 牛宝贵, 和政军, 宋彪, 等, 2003. 张家口组火山岩SHRIMP定年及其重大意义. 地质通报, 22(2): 140-141. doi: 10.3969/j.issn.1671-2552.2003.02.010 [103] 漆家福, 杨桥, 陆克政, 等, 2004. 渤海湾盆地基岩地质图及其所包含的构造运动信息. 地学前缘, 11(3): 299-307. doi: 10.3321/j.issn:1005-2321.2004.03.028 [104] 任纪舜, 1990. 中国东部及邻区大陆岩石圈的构造演化与成矿. 北京: 科学出版社. [105] 单文琅, 王方正, 傅昭仁, 等, 1989. 论北京西山南部的盖层构造演化. 地球科学, 14(1): 37-44. doi: 10.3321/j.issn:1000-2383.1989.01.005 [106] 舒坦, 续海金, 章军锋, 等, 2019. 北京房山地区太平山褶皱的变形特征和形成时代: 华北克拉通早白垩世挤压构造的意义. 地球科学, 44(5): 1734-1748. doi: 10.3799/dqkx.2018.119 [107] 宋鸿林, 1996. 北京房山变质核杂岩的基本特征及其成因探讨. 现代地质, 10(2): 149-158. https://www.cnki.com.cn/Article/CJFDTOTAL-XDDZ602.001.htm [108] 童金南, 徐冉, 袁晏明, 2013. 北京周口店地区岩石地层及沉积序列和沉积环境恢复. 地球科学与环境学报, 35(1): 15-23. doi: 10.3969/j.issn.1672-6561.2013.01.002 [109] 万天丰, 1981. 北京西山南大寨-八宝山断裂带的构造特征及形成机理的探讨. 构造地质论丛, 1: 152-164. [110] 王瑜, 李锦轶, 2007. 北京西山南窖地区南东东110°~120°拉伸线理形成时间的年代学制约. 岩石学报, 23(3): 617-624. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200703011.htm [111] 续海金, 宋衍茹, 章军锋, 等, 2012. 北京周口店地区房山岩体中岩浆混合作用的野外实践教学. 中国地质教育, 21(4): 135-139. doi: 10.3969/j.issn.1006-9372.2012.04.040 [112] 许志琴, 王勤, 李忠海, 等, 2016. 印度－亚洲碰撞: 从挤压到走滑的构造转换. 地质学报, 90(1): 1-23. https://www.cnki.com.cn/Article/CJFDTOTAL-DZXE201601001.htm [113] 颜丹平, 周美夫, 宋鸿林, 等, 2005. 北京西山官地杂岩的形成时代及构造意义. 地学前缘, 12(2): 332-337. doi: 10.3321/j.issn:1005-2321.2005.02.035 [114] 姚丽景, 颜丹平, 胡玲, 2007. 房山变质核杂岩基底拆离断层韧性剪切变形构造及环境分析. 地球科学, 32(3): 357-365. doi: 10.3321/j.issn:1000-2383.2007.03.008 [115] 易明初, 1993. 新构造运动及渭延裂谷构造. 北京: 地震出版社, 153-170. [116] 张长厚, 1999. 初论板内造山带. 地学前缘, 6(4): 295-308. doi: 10.3321/j.issn:1005-2321.1999.04.012 [117] 张长厚, 邓洪菱, 李程明, 等, 2012. 燕山板内造山带中部"承德逆冲构造"的褶皱相关断裂构造模型. 地学前缘, 19(5): 27-40. https://www.cnki.com.cn/Article/CJFDTOTAL-DXQY201205006.htm [118] 张长厚, 李程明, 邓洪菱, 等, 2011. 燕山-太行山北段中生代收缩变形与华北克拉通破坏. 中国科学(D辑: 地球科学), 41 (5): 593- 617. https://www.cnki.com.cn/Article/CJFDTOTAL-JDXK201105002.htm [119] 张长厚, 张勇, 李海龙, 等, 2006. 燕山西段及北京西山晚中生代逆冲构造格局及其地质意义. 地学前缘, 13(2): 165-183. doi: 10.3321/j.issn:1005-2321.2006.02.015 [120] 张璐, 刘兵, 陈能松, 等, 2008. 北京周口店南窖石英二长岩岩枝的锆石U-Pb年龄和地质意义. 地质科技情报, 27(6): 43-46. doi: 10.3969/j.issn.1000-7849.2008.06.008 [121] 张旗, 钱青, 王二七, 等, 2001. 燕山中晚期的中国东部高原: 埃达克岩的启示. 地质科学, 36(2): 248-255. doi: 10.3321/j.issn:0563-5020.2001.02.014 [122] 张之一, 吴新国, 李红阳, 1983. 北京昌平县十三陵-下庄一带推复构造的基本特征. 石家庄经济学院学报, 6(3): 3-9. https://www.cnki.com.cn/Article/CJFDTOTAL-HBDX198303001.htm [123] 赵越, 徐刚, 张拴宏, 等, 2004a. 燕山运动与东亚构造体制的转变. 地学前缘, 11(3): 319-328. https://www.cnki.com.cn/Article/CJFDTOTAL-DXQY200403042.htm [124] 赵越, 张拴宏, 徐刚, 等, 2004b. 燕山板内变形带侏罗纪主要构造事件. 地质通报, 23(9): 854-863. https://www.cnki.com.cn/Article/CJFDTOTAL-ZQYD2004Z2005.htm [125] 赵占元, 单文琅, 1994. 北京西山南大寨逆冲推覆构造的初步研究. 河北地质学院学报, 17(5): 464-470. https://www.cnki.com.cn/Article/CJFDTOTAL-HBDX199405006.htm [126] 朱光, 王薇, 顾承串, 等, 2016. 郯庐断裂带晚中生代演化历史及其对华北克拉通破坏过程的指示. 岩石学报, 32(4): 3-17. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201604001.htm [127] 朱日祥, 陈凌, 吴福元, 等, 2011. 华北克拉通破坏的时间、范围与机制. 中国科学(D辑: 地球科学), 41(5): 583-592. https://www.cnki.com.cn/Article/CJFDTOTAL-JDXK201105001.htm [128] 朱日祥, 徐义刚, 朱光, 等, 2012. 华北克拉通破坏. 中国科学(D辑: 地球科学), 42(8): 1135-1159. https://www.cnki.com.cn/Article/CJFDTOTAL-JDXK201208002.htm -
dqkxzx-46-5-1657-附表1.pdf
-
下载:
点击查看大图
图(14)
计量
- 文章访问数: 821
- HTML全文浏览量: 272
- PDF下载量: 59
- 被引次数: 0
