Discussion on Initiation Time of the Latest Tectonic Movement in Break-up Region of the North China Craton
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摘要: 华北克拉通破坏区是历史破坏性地震频发区，震源机制解和地震地表破裂带等反映出历史地震的发震断层为新生走滑断层，很难用地壳的伸展构造系统来合理解释.首先对1679年三河-平谷M8.0级地震的大厂隐伏凹陷西边界夏垫断裂进行高分辨率地震勘探和上盘钻孔地层进行标定，然后在河套断陷盆地带大青山南麓晚更新世湖相地层中识别出2期角度不整合面（UC1和UC2），并进行了系统测年，综合近年来活动断层比例尺填图和城市活动断层探测成果，明确指出，在华北克拉通破坏区，代表新生代早期地壳伸展运动的铲形正断层的活动性在上新世至第四纪早期逐渐减弱，到晚更新世早期基本停止活动；晚更新世中期以来大青山构造运动为华北克拉通破坏区最新一期构造运动，主要表现为区域剪切应变条件下新生走滑断层形成和扩展，并伴随相关地震活动.最新构造运动的主要动力来源于青藏高原物质东向挤出，以及其对鄂尔多斯块体西南缘强烈东向推挤作用.这些新认识对深化华北克拉通破坏区地震发震机理研究，理解板内最新变形动力学，均具有十分重要的科学价值.Abstract: The break-up region of the North China craton is an area where historically destructive earthquakes have frequently occurred. The focal mechanism solutions and earthquake surface rupture zones indicate that these historical earthquakes were dominated by the newly-formed seismogenic strike-slip faults, which are incompatible with the crustal extensional tectonics. This research firstly examines the high-resolution seismic reflection profile and borehole stratigraphy on the hanging wall of the Xiadian fault, which resulted in the 1679 Sanhe-Pinggu M8.0 earthquake ruptures along the western boundary of the Dachang concealed sag. Then, two unconformity contacts (UC1 and UC2) are distinguished by careful checks on structural and stratigraphic features from a cross section of the Late Pleistocene lacustrine at the southern piedmont of the Daqingshan. Combined with the results of active fault mappings with 1:50 000 scale and urban active fault detection in recent years, we conclude that the listric normal faults, which represent crustal extension in the Early Cenozoic, had been weakening in the Pliocene to the Early Quaternary, and had ceased activity by the early Late Pleistocene. The Daqingshan tectonic movement has initiated since the middle of the Late Pleistocene, representing the latest tectonic movement in break-up region of the North China craton, in which new strike-slip faults have formed under a shear-strain crustal condition owing to continuous eastward extrusion of the Qinghai-Tibet Plateau and strong eastward push on the southwestern margin of the Ordos block. These new points of view have important academic value for understanding mechanism of earthquake occurrence and dynamics of the latest crustal deformation in intra-plate.
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图 1 华北克拉通破坏区活动构造分布
左下方黑色箭头代表青藏高原东北缘对鄂尔多斯块体向东作用力；半圆圈箭头代表块体转动方向
Fig. 1. Distribution of active tectonics in break-up region of the North China craton
图 2 三河-平谷M8.0级地震区新生走滑断层与隐伏铲形正断层关系
红线为地震地表断层；被红线切截的黑粗线为夏垫铲形断裂；虚线代表隐伏断层；长黑细线为深地震反射测线；短细线为浅层地震勘探线；绿线代表河流；阴影区为前新生代基岩分布区；带三角的线为盆地边界，三角指向盆地侧；细线上数字代表新生代地层厚度(m)
Fig. 2. Map demonstrating relation between newly-formed strike-slip fault and hidden listric normal fault in the epicenter of the Sanhe-Pinggu M8.0 earthquake
图 3 三河-平谷M8.0级地震区跨地震断层浅层SH波地震反射叠加时-深解释剖面
F1.夏垫铲形正断裂；F2.夏垫断裂；数字代表距离或深度(m); Qh.全新统；Qp3.上更新统：Qp2.中更新统；Qp1.下更新统；N2.上新统；O.奥陶纪灰岩；ZK1~ZK7.钻孔编号
Fig. 3. Stacked time-depth section of the shallow seismic SH wave reflection across the earthquake fault in the epicenter of the Sanhe-Pinggu M8.0 earthquake zone
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Allmendinger, R.W., Oliver, J., Hauge, T.A., et al., 1987.Tectonic Heredity and the Layered Lower Crust in the Basin and Range Province, Western United States.Geological Society, London, Special Publications, 28(1):223-246. https://doi.org/10.1144/gsl.sp.1987.028.01.16 Bai, L.X., 2017.The Age of the Latest Tectonic Movement in Daqingshan and Its Influence on Tectonic Evolution of Hetao Basin (Dissertation).Institute of Geology, China Earthquake Administration, Beijing, 75(in Chinese with English abstract). Cavalié, O., Lasserre, C., Doin, M.P., et al., 2008.Measurement of Interseismic Strain across the Haiyuan Fault (Gansu, China), by InSAR.Earth and Planetary Science Letters, 275(3-4):246-257. https://doi.org/10.1016/j.epsl.2008.07.057 Chadin, T.D., Licent, F., 1924.On the Discovery of a Palaeolithic Industry in Northern China.Bulletin of the Geological Society of China, 3(1):45-50. https://doi.org/10.1111/j.1755-6724.1924.mp3001005.x Chao, H.T., Li, J.L., Cui, Z.W., et al., 1995.Active Faults in Tanlu (Tancheng-Lujiang) Fault Zone and the Hazards Produced by the 1668 Tancheng Earthquake (M=8.5).Marine Geology & Quaternary Geology, 15(3):69-80(in Chinese with English abstract). Chen, F.H., Fan, Y.X., Madsen, D.B., et al., 2008.Preliminary Study on the Formation Mechanism of the "Jilantai-Hetao" Megalake and the Lake Evolutionary History in Hetao Region.Quaternary Sciences, 28(5):866-873(in Chinese with English abstract). Chen, G.D., 1956.Examples of "Activizing Region" in the Chinese Platform with Special Reference to the "Cathaysla" Problem.Acta Geologica Sinica, 30(3):239-271(in Chinese with English abstract). Chen, W.P., Nábelek, J., 1988.Seismogenic Strike-Slip Faulting and the Development of the North China Basin.Tectonics, 7(5):975-989. https://doi.org/10.1029/tc007i005p00975 Cheng, S.P., Deng, Q.D., Min, W., et al., 1998.Yellow River and Quaternary Tectonic Movements of the Ordos Plateau.Quaternary Sciences, (3):238-248(in Chinese with English abstract). doi: 10.1046-j.1365-3121.2002.00350.x/ Deng, Q.D., Zhang, P.Z., Ran, Y.K., et al., 2002.Basic Characteristics of Active Tectonics of China.Science in China (Series D:Earth Sciences), 32(12):1020-1030(in Chinese). DePolo, C.M., Clark, D.G., Slemmons, D.B., et al., 1991.Historical Surface Faulting in the Basin and Range Province, Western North America:Implications for Fault Segmentation.Journal of Structural Geology, 13(2):123-136. https://doi.org/10.1016/0191-8141(91)90061-m Dong, S.P., Zhang, P.Z., Zheng, W.J., et al., 2018.Paleoseismological Research on the Langshan Range-Front Fault, Hetao Area, China:Insights for Studies on Tectonics and Seismic Risk.Seismology and Geology, 40(6):1216-1239(in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/dzdz201806003 Eaton, G.P., 1982.The Basin and Range Province:Origin and Tectonic Significance.Annual Review of Earth and Planetary Sciences, 10:409-440. https://doi.org/10.1146/annurev.ea.10.050182.002205 Feng, S.Y., Gao, R., Long, C.X., et al., 2011.The Compressive Stress Field of Yinchuan Graben:Deep Seismic Reflection Profile.Chinese Journal of Geophysics, 54(3):692-697(in Chinese with English abstract). Gao, B., Zhou, S.Y., Jiang, C.S., 2016.Estimate of Dip Angles of Faults around Ordos Block Based on Earthquakes.Chinese Journal of Geophysics, 59(7):2444-2452(in Chinese with English abstract). Gao, Z.W., Wu, H., Li, G.T., et al., 2014.Late Quaternary Activity of the Central-North Segment of Taihang Mountain Piedmont Fault Zone.Technology for Earthquake Disaster Prevention, 9(2):159-170(in Chinese with English abstract). Gong, W.B., Hu, J.M., Li, Z.H., et al., 2013.The Sediment Features of Lower Piedmont Platforms along Western Hetao Basin and Implication for Subsiding Process and Controlling Factors of "Jilantai-Hetao" Megalake.Earth Science Frontiers, 20(4):190-198(in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/dxqy201304015 He, L.J., 2015.Thermal Regime of the North China Craton:Implications for Craton Destruction.Earth-Science Reviews, 140:14-26. https://doi.org/10.1016/j.earscirev.2014.10.011 Hu, L.Y., Xu, X.S., Sun, S.C., 1994.Geomorphological Characteristics of the Modern Movement of the Maoshan Fault.Jiangsu Geology, 18(1):3-9(in Chinese with English abstract). Huang, W., 1993.Morphologic Patterns of Stream Channels on the Active Yishi Fault, Southern Shandong Province, Eastern China:Implications for Repeated Great Earthquakes in the Holocene.Tectonophysics, 219(4):283-304. https://doi.org/10.1016/0040-1951(93)90179-n Li, J.B., Ran, Y.K., Guo, W.S., 2007.Division of Quaternary Beds and Environment Evolution in Hubao Basin in China.Quaternary Sciences, 27(4):632-644(in Chinese with English abstract). Li, J.J., Fang, X.M., van der Voo, R., et al., 1997.Magnetostratigraphic Dating of River Terraces:Rapid and Intermittent Incision by the Yellow River of the Northeastern Margin of the Tibetan Plateau during the Quaternary.Journal of Geophysical Research (Solid Earth), 102(B5):10121-10132. https://doi.org/10.1029/97jb00275 Li, K., Xu, X.W., Jiang, G.Y., et al., 2016.Evidence of Southward Extend of the 1668 Tancheng Earthquake Surface Rupture from Trench Profiles.Technology for Earthquake Disaster Prevention, 11(2):199-206(in Chinese with English abstract). Li, T., Wang, Z.X., 2009.Tectonic Division of the Upper Crust of the North China Block.Earth Science Frontiers, 16(4):215-224(in Chinese with English abstract). Li, X.N., Zhang, P.Z., Zheng, W.J., et al., 2018.Kinematics of Late Quaternary Slip along the Qishan-Mazhao Fault:Implications for Tectonic Deformation on the Southwestern Ordos, China.Tectonics, 37(9):2983-3000. https://doi.org/10.1029/2018tc005043 Liu, B.J., Zhang, X.K., Chen, Y., et al., 2011.Research on Crustal Structure and Active Faultin the Sanhe-Pinggu Earthquake (M8.0) Zone Based on Single-Fold Deep Seismic Reflection and Shallow Seismic Reflection Profiling.Chinese J.Geophys., 54(5):1251-1259(in Chinese with English abstract). Jia, T.F., Yin, S., Zhao, M., et al., 2001.A Study on the Lake Deposits on the Tuoketuo Section of Yellow River in the Early and Middle Stage of Pleistocene.Journal of Inner Mongolia Normal University (Natural Science Edition), 30(1):74-78(in Chinese with English abstract). Jiao, Q.S., Jiang, W.L., Zhang, J.F., et al., 2016.Identification of Paleoearthquakes Based on Geomorphological Evidence and Their Tectonic Implications for the Southern Part of the Active Anqiu-Juxian Fault, Eastern China.Journal of Asian Earth Sciences, 132:1-8. https://doi.org/10.1016/j.jseaes.2016.10.012 Jiang, W.L., Zhang, Y.L., 1997.Characteristics of NW Trending Surface Fractures of Strong Earthquakes and Activity of the Holocene Faults of the Boundary of North China Plain.Earthquake Research in China, 13(3):263-270(in Chinese with English abstract). Ma, X.Y., 1982.On Extensional Tectonics.Earth Science, 7(3):15-22(in Chinese with English abstract). doi: 10.1029-JB089iB07p05733/ Ma, X.Y., Liu, H.F., Wang, W.X., et al., 1983.Meso-Cenozoic Taphrogeny and Extensional Tectonics in Eastern China.Acta Geologica Sinica, 57(1):22-32(in Chinese with English abstract). Menzies, M., Xu, Y.G., 1998.Geodynamics of the North China Craton.In: Flower, M.F.J., Chung, S.L., Lee, T.Y., eds., Mantle Dynamics and Plate Interations in East Asian.Amer.Geophy.Union, Washington D.C., Geodyn.Ser., 27: 155-165. Middleton, T.A., Walker, R.T., Rood, D.H., et al., 2016.The Tectonics of the Western Ordos Plateau, Ningxia, China:Slip Rates on the Luoshan and East Helanshan Faults.Tectonics, 35(11):2754-2777. https://doi.org/10.1002/2016tc004230 Qi, J.F., Yang, Q., 2010.Cenozoic Structural Deformation and Dynamic Processes of the Bohai Bay Basin Province, China.Marine and Petroleum Geology, 27(4):757-771. https://doi.org/10.1016/j.marpetgeo.2009.08.012 Ren, J.Y., Tamaki, K., Li, S.T., et al., 2002.Late Mesozoic and Cenozoic Rifting and Its Dynamic Setting in Eastern China and Adjacent Areas.Tectonophysics, 344(3-4):175-205. https://doi.org/10.1016/s0040-1951(01)00271-2 Si, S.P., Li, Y.L., Lü, S.H., et al., 2014.Holocene Slip Rate and Paleoearthquake Records of the Salt Lake Segment of the Northern Zhongtiaoshan Fault, Shanxi Province.Science China Earth Sciences, 57(9):2079-2088. https://doi.org/10.1007/s11430-014-4887-3 Su, Z.Z., Dong, G.R., Jin, H.L., 1997.A Geochronological Study of the Salawusu Strata in North China.Journal of Geomechanics, 3(4):90-96(in Chinese with English abstract). Suo, Y.H., Li, S.Z., Liu, X., et al., 2013.Structural Characteristics of NWW-Trending Active Fault Zones in East China:A Case Study of the Zhangjiakou-Penglai Fault Zone.Acta Petrologica Sinica, 29(3):953-966(in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/ysxb98201303017 Suter, M., 2002.Active Tectonics of Northeastern Sonora, Mexico (Southern Basin and Range Province) and the 3 May 1887 Mw 7.4 Earthquake.Bulletin of the Seismological Society of America, 92(2):581-589. https://doi.org/10.1785/0120000220 de Chardin, P.T., Licent, E., 1924.On the Discovery of a Paleolithic Industry in Northern China.Bulletin of the Geological Society of China, 3(1):45-50. Tian, Q.J., Shen, X.H., Feng, X.J., et al., 2003.Primary Study on Quaternary Tectonic Events Based on Variation of Fault Activity in Weihe Basin.Seismology and Geology, 25(1):146-154(in Chinese with English abstract). Wan, T.F., 1994.Tectonic Event and Stress Field of Quaternary in China.Quaternary Sciences, 14(1):48-55(in Chinese with English abstract). Wan, T.F., Cao, R.P., 1992.Mesozoic-Early Pleistocene Tectonic Events and Stress Fields in China.Geoscience, 6(3):275-284(in Chinese with English abstract). Wang, C.Y., Wang, G.M., Lin, Z.Y., et al., 1993.A Study on Fine Crustal Structure in Xingtai Earthquake Area Based on Deep Seismic Reflection Profiling.Chinese Journal of Geophysics, 36(4):445-452(in Chinese with English abstract). Wernicke, B., Axen, G.J., 1988.On the Role of Isostasy in the Evolution of Normal Fault Systems.Geology, 16(9):848-851.https://doi.org/10.1130/0091-7613(1988)016<0848:otroii>2.3.co;2 doi: 10.1130/0091-7613(1988)016<0848:otroii>2.3.co;2 Wu, F., Lin, J.Q., Wilde, S.A., et al., 2005.Nature and Significance of the Early Cretaceous Giant Igneous Event in Eastern China.Earth and Planetary Science Letters, 233(1-2):103-119. https://doi.org/10.1016/j.epsl.2005.02.019 Wu, F.Y., Xu, Y.G., Gao, S., et al., 2008.Lithospheric Thinning and Destruction of the North China Craton.Acta Petrologica Sinica, 24(6):1145-1174(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB200806001.htm Wu, M.J., Lin, X.D., Xu, P., 2011.Analysis of Focal Mechnism and Tectonic Stress Field Features in Northern Part of North China.Journal of Geodesy and Geodynamics, 31(5):39-43(in Chinese with English abstract). Xiang, H.F., Wang, X.C., Guo, S.M., et al., 2000.Integrated Survey and Investigation on the Quaternary Activity of the Liaocheng-Lankao Buried Fault.Seismology and Geology, 22(4):351-359(in Chinese with English abstract). Xu, J., Gao, Z.W., Song, C.Q., et al., 2000.The Structural Characters of the Piedmont Fault Zone of Taihang Mountain.Seismology and Geology, 22(2):111-122(in Chinese with English abstract). Xu, J., Niu, L.F., Wang, C.H., et al., 1996.Tangshan-Hejian-Cixian Newly-Generated Seismotectonic Zone.Seismology and Geology, 18(3):193-198(in Chinese with English abstract). Xu, J., Song, C.Q., Chu, Q.Z., 1998.Preliminary Study on the Seismotectonic Characters of the Zhangjiakou-Penglai Fault Zone.Seismology and Geology, 20(2):146-154(in Chinese with English abstract). Xu, X.W., Cheng, G.L., Ma, X.Y., et al., 1994.Rotation Model and Dynamics of Blocks in North China and Its Adjacent Areas.Earth Science, 19(2):129-138(in Chinese with English abstract). Xu, X.W., Deng, Q.D., 1990.The Features of Late Quaternary Activity of the Piedmont Fault of Mt.Huoshan, Shanxi Province and 1303 Hongdong Earthquake (Ms=8).Seismology and Geology, 12(1):21-30(in Chinese with English abstract). Xu, X.W., Deng, Q.D., 1996.Nonlinear Characteristics of Paleoseismicity in China.Journal of Geophysical Research (Solid Earth), 101(B3):6209-6231. https://doi.org/10.1029/95jb01238 Xu, X.W., Ma, X.Y., 1992.Geodynamics of the Shanxi Rift System, China.Tectonophysics, 208(1-3):325-340. https://doi.org/10.1016/0040-1951(92)90353-8 Xu, X.W., Ma, X.Y., Deng, Q.D., 1993.Neotectonic Activity along the Shanxi Rift System, China.Tectonophysics, 219(4):305-325. https://doi.org/10.1016/0040-1951(93)90180-r Xu, X.W., Wen, X.Z., Zheng, R.Z., et al., 2003.Pattern of Latest Tectonic Motion and Its Dynamics for Active Blocks in Sichuan-Yunnan Region, China.Science in China (Series D:Earth Sciences), 33(S1):210-226. Xu, X.W., Wu, W.M., Zhang, X.K., et al., 2002.Latest Crustal Tectonic Movement and Related Earthquakes in the Capital Region, China.Seismological Press, Beijing, 376(in Chinese with English abstract). Xu, X.W., Yu, G.H., Ran, Y.K., et al., 2015.Introduction to Fault Activity in the Urban Region, China-Results from Active Fault's Survey and Detection in 20 Cities.Seismological Press, Beijing, 484(in Chinese with English abstract). Xu, X.W., Yu, G.H., Wang, F., et al., 2000.Seismogenic Model for the 1966 Xingtai Earthquakes-Nucleation of New-Born Fault or Strick-Slip of Pre-Existing Fault?.Earthquake Research in China, 16(4):364-378(in Chinese with English abstract). Xu, Z.B., Liu, B.J., Ji, J.F., et al., 2019.Imaging for Shallow Velocity Structure and Buried Faults in the Southern Margin of Taihang Mountains.Journal of Geodesy and Geodynamics, 39(1):88-92(in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/dkxbydz201901017 Xu, Z.H., Yan, M., Zhao, Z.H., 1983.Evalution of the Direction of Tectonic Stress in North China from Recorded Data of a Large Number of Small Earthquakes.Acta Seismologica Sinica, 5(3):268-279(in Chinese with English abstract). Zhang, P., Wang, L.S., Zhong, K., et al., 2007.Research on the Segmentation of Tancheng-Lujiang Fault Zone.Geological Review, 53(5):586-591(in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/OA000004804 Zhang, P.Z., Deng, Q.D., Zhang, G.M., et al., 2003.Active Tectonic Blocks and Strong Earthquakes in Continent of China.Science in China (Series D:Earth Sciences), 33(Suppl.):12-20(in Chinese). Zhang, P.Z., Wang, Q., Ma, Z.J., 2002.Present-Day Velocity Field of the Continent of China and Active Blocks.Earth Science Frontiers, 9(2):430-441(in Chinese with English abstract). Zhang, W.Y., Zhang, K., Zhao, Y.G., et al., 1983.The Mesozoic and Cenozoic Geotectonic Characteristics and Dynamical Model of the Lithosphere in North China Fault Block Region.Acta Geologica Sinica, 57(1):33-42(in Chinese with English abstract). Zhao, X.C., 1991.Fissures and Its Characteristics of Heze Earthquake M7.0 in 1937.Crustal Deformation and Earthquake, 11(1):93-96(in Chinese with English abstract). Zhu, R.X., 2018.Review of the Achievements of Major Research Plan on" Destruction of North China Craton".China Science Foundation, 3:282-290(in Chinese with English abstract). 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). 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). http://d.old.wanfangdata.com.cn/Periodical/ysxb98201604001 Zhu, R.X., Zheng, T.Y., 2009.Destruction Geodynamics of the North China Craton and Its Paleoproterozoic Plate Tectonics.Chinese Science Bulletin, 54(14):1950-1961(in Chinese). Zoback, M.L., 1989.State of Stress and Modern Deformation of the Northern Basin and Range Province.Journal of Geophysical Research (Solid Earth), 94(B6):7105-7128. https://doi.org/10.1029/jb094ib06p07105 白鸾羲, 2017.大青山最新构造运动的时代厘定及其对河套盆地构造演化影响(硕士学位论文).北京: 中国地震局地质研究所, 75. 晁洪太, 李家灵, 崔昭文, 等, 1995.郯庐活断层与1668年郯城8.5级地震灾害.海洋地质与第四纪地质, 15(3):69-80. 陈发虎, 范育新, Madsen, D.B., 等, 2008.河套地区新生代湖泊演化与"吉兰泰-河套"古大湖形成机制的初步研究.第四纪研究, 28(5):866-873. doi: 10.3321/j.issn:1001-7410.2008.05.009 陈国达, 1956.中国地台"活化区"的实例并着重讨论"华夏古陆"问题.地质学报, 30(3):239-271. http://www.cnki.com.cn/Article/CJFDTOTAL-DZXE195603000.htm 程绍平, 邓起东, 闵伟, 等, 1998.黄河晋陕峡谷河流阶地和鄂尔多斯高原第四纪构造运动.第四纪研究, (3):238-248. doi: 10.3321/j.issn:1001-7410.1998.03.007 邓起东, 张培震, 冉勇康, 等, 2002.中国活动构造基本特征.中国科学(D辑:地球科学), 32(12):1020-1030. http://d.old.wanfangdata.com.cn/Periodical/zgkx-cd200212007 董绍鹏, 张培震, 郑文俊, 等, 2018.河套地区狼山山前断裂的古地震研究——构造及地震危险性启示.地震地质, 40(6):1216-1239. http://d.old.wanfangdata.com.cn/Periodical/dzdz201806003 酆少英, 高锐, 龙长兴, 等, 2011.银川地堑地壳挤压应力场:深地震反射剖面.地球物理学报, 54(3):692-697. doi: 10.3969/j.issn.0001-5733.2011.03.008 高彬, 周仕勇, 蒋长胜, 2016.基于地震活动性资料估计鄂尔多斯块体周缘构造断层面倾角.地球物理学报, 59(7):2444-2452. http://www.cnki.com.cn/Article/CJFDTOTAL-DQWX201607011.htm 高战武, 吴昊, 李光涛, 等, 2014.太行山山前断裂带中北段晚第四纪活动性研究.震灾防御技术, 9(2):159-170. doi: 10.3969/j.issn.1673-5722.2014.02.001 公王斌, 胡健民, 李振宏, 等, 2013.河套盆地西缘山前低台地沉积特征对"吉兰泰-河套"古湖消退过程及其控制因素的指示意义.地学前缘, 20(4):190-198. 胡连英, 徐学思, 孙寿成, 1994.茅山东侧断裂现代运动的地貌学特征.江苏地质, 18(1):3-9. 李建彪, 冉勇康, 郭文生, 2007.呼包盆地第四纪地层与环境演化.第四纪研究, 27(4):632-644. doi: 10.3321/j.issn:1001-7410.2007.04.020 李康, 徐锡伟, 江国焰, 等, 2016.基于探槽剖面证据探讨1668年郯城地震地表破裂南延问题.震灾防御技术, 11(2):199-206. http://d.old.wanfangdata.com.cn/Periodical/zzfyjs201602003 李涛, 王宗秀, 2009.华北上地壳构造单元划分.地学前缘, 16(4):215-224. doi: 10.3321/j.issn:1005-2321.2009.04.021 刘保金, 张先康, 陈颙, 等, 2011.三河-平谷8.0级地震区地壳结构和活动断裂研究——利用单次覆盖深反射和浅层地震剖面.地球物理学报, 54(5):1251-1259. doi: 10.3969/j.issn.0001-5733.2011.05.014 贾铁飞, 银山, 赵明, 等, 2001.黄河托克托段早中更新世湖相地层剖面的建立及其意义.内蒙古师大学报(自然科学汉文版), 30(1):74-78. http://d.old.wanfangdata.com.cn/Periodical/nmgsdxb200101017 江娃利, 张英礼, 1997.华北平原周边北西向强震地表地震断层及全新世断裂活动特征.中国地震, 13(3):263-270. http://www.cnki.com.cn/Article/CJFDTOTAL-ZGZD703.007.htm 马杏垣, 1982.论伸展构造.地球科学, 7(3):15-22. http://d.old.wanfangdata.com.cn/Periodical/dqkx200303007 马杏垣, 刘和甫, 王维襄, 等, 1983.中国东部中、新生代裂陷作用和伸展构造.地质学报, 57(1):22-32. http://www.cnki.com.cn/Article/CJFDTOTAL-DZXE198301002.htm 苏志珠, 董光荣, 靳鹤龄, 1997.萨拉乌苏组地层年代学研究.地质力学学报, 3(4):90-96. http://www.cnki.com.cn/Article/CJFDTOTAL-DZLX704.012.htm 索艳慧, 李三忠, 刘鑫, 等, 2013.中国东部NWW向活动断裂带构造特征:以张家口-蓬莱断裂带为例.岩石学报, 29(3):953-966. http://d.old.wanfangdata.com.cn/Periodical/ysxb98201303017 田勤俭, 申旭辉, 冯希杰, 等, 2003.渭河盆地断层活动反映的第四纪构造事件初步研究.地震地质, 25(1):146-154. doi: 10.3969/j.issn.0253-4967.2003.01.014 万天丰, 1994.中国第四纪的构造事件与应力场.第四纪研究, 14(1):48-55. doi: 10.3321/j.issn:1001-7410.1994.01.005 万天丰, 曹瑞萍, 1992.中国中始新世-早更新世构造事件与应力场.现代地质, 6(3):275-284. http://mall.cnki.net/magazine/Article/XDDZ199203004.htm 王椿镛, 王贵美, 林中洋, 等, 1993.用深地震反射方法研究邢台地震区地壳细结构.地球物理学报, 36(4):445-452. doi: 10.3321/j.issn:0001-5733.1993.04.005 吴福元, 徐义刚, 高山, 等, 2008.华北岩石圈减薄与克拉通破坏研究的主要学术争论.岩石学报, 24(6):1145-1174. http://d.old.wanfangdata.com.cn/Periodical/ysxb98200806001 武敏捷, 林向东, 徐平, 2011.华北北部地区震源机制解及构造应力场特征分析.大地测量与地球动力学, 31(5):39-43. http://d.old.wanfangdata.com.cn/Periodical/dkxbydz201105009 向宏发, 王学潮, 虢顺民, 等, 2000.聊城-兰考隐伏断裂第四纪活动性的综合探测研究.地震地质, 22(4):351-359. doi: 10.3969/j.issn.0253-4967.2000.04.003 徐杰, 高战武, 宋长青, 等, 2000.太行山山前断裂带的构造特征.地震地质, 22(2):111-122. doi: 10.3969/j.issn.0253-4967.2000.02.003 徐杰, 牛娈芳, 王春华, 等, 1996.唐山-河间-磁县新生地震构造带.地震地质, 18(3):193-198. http://www.cnki.com.cn/Article/CJFDTotal-DZDZ603.000.htm 徐杰, 宋长青, 楚全芝, 1998.张家口-蓬莱断裂带地震构造特征的初步探讨.地震地质, 20(2):146-154. http://xuewen.cnki.net/CJFD-DZDZ802.009.html 徐锡伟, 程国良, 马杏垣, 等, 1994.华北及其邻区块体转动模式和动力来源.地球科学, 19(2):129-138. doi: 10.3321/j.issn:1000-2383.1994.02.005 徐锡伟, 邓起东, 1990.山西霍山山前断裂晚第四纪活动特征和1303年洪洞8级地震.地震地质, 12(1):21-30. http://cdmd.cnki.com.cn/Article/CDMD-85402-1014131207.htm 徐锡伟, 吴卫民, 张先康, 等, 2002.首都圈地区地壳最新构造变动与地震.北京:科学出版社, 376. 徐锡伟, 于贵华, 冉勇康, 等, 2015.中国城市活动断层概论——20个城市活动断层探测成果.北京:地震出版社, 484. 徐锡伟, 于贵华, 王峰, 等, 2000.1966年邢台地震群的发震构造模型——新生断层形成?先存活断层摩擦粘滑?中国地震, 16(4):364-378. doi: 10.3969/j.issn.1001-4683.2000.04.008 徐增波, 刘保金, 姬计法, 等, 2019.太行山南端浅层速度结构成像和隐伏断裂探测.大地测量与地球动力学, 39(1):88-92. http://d.old.wanfangdata.com.cn/Periodical/dkxbydz201901017 许忠淮, 阎明, 赵仲和, 1983.由多个小地震推断的华北地区构造应力场的方向.地震学报, 5(3):268-279. http://mall.cnki.net/magazine/article/DZXB198303001.htm 张鹏, 王良书, 钟锴, 等, 2007.郯庐断裂带的分段性研究.地质论评, 53(5):586-591. doi: 10.3321/j.issn:0371-5736.2007.05.002 张培震, 邓起东, 张国民, 等, 2003.中国大陆的强震活动与活动地块.中国科学(D辑:地球科学), 33(S1):12-20. http://d.old.wanfangdata.com.cn/Periodical/zgkx-cd2003z1002 张培震, 王琪, 马宗晋, 2002.中国大陆现今构造运动的GPS速度场与活动地块.地学前缘, 9(2):430-441. doi: 10.3321/j.issn:1005-2321.2002.02.022 张文佑, 张抗, 赵永贵, 等, 1983.华北断块区中、新生代地质构造特征及岩石圈动力学模型.地质学报, 57(1):33-42. http://www.cnki.com.cn/Article/CJFDTOTAL-DZXE198301003.htm 赵宪超, 1991.1937年菏泽7.0级地震的地裂缝特征.地壳形变与地震, 11(1):93-96. 朱日祥, 2018."华北克拉通破坏"重大研究计划结题综述.中国科学基金, 3:282-290. http://d.old.wanfangdata.com.cn/Periodical/dzkjqb200906003 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. http://www.cnki.com.cn/Article/CJFDTOTAL-JDXK201105001.htm 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. http://d.old.wanfangdata.com.cn/Periodical/ddgzyckx200804016 朱日祥, 郑天愉, 2009.华北克拉通破坏机制与古元古代板块构造体系.科学通报, 54(14):1950-1961. http://www.cnki.com.cn/Article/CJFDTOTAL-KXTB200914003.htm -
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