郯庐断裂带中段周边挤压应力场演变过程
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摘要
目前,对华北克拉通破坏的机制、过程与动力作用方式等方面的认识非常有限,华北克拉通破坏机制是一个当前讨论最激烈的问题。为了获得华北克拉通破坏的机制,本文通过对华北克拉通东部郯庐断裂带中段及周边的胶莱盆地、鲁西南地区以及合肥盆地等地区进行详细的野外观察,同时对上述地区进行古应力场数据采集,获得了216组逆冲断层和走滑断层的数据,室内工作通过利用法国巴黎南方大学研制的计算机程序反演了研究区内自早白垩世到新近纪的古应力场的演化过程,得出华北克拉通东部自早白垩世以来存在脉动式挤压活动。根据古应力场测量结果,本文认为在该地区早白垩世为NWW向挤压,晚白垩世为EW向挤压和NE向挤压,古近纪为NNW向挤压、SN向挤压、NNE向挤压,新近纪为NW向挤压。通过把应力场分期数据与太平洋板块的运动方向的变化相结合,综合分析得出结论,认为华北克拉通东部的破坏机制及动力来源是太平洋板块向欧亚板块下俯冲所产生的。
Now, few about the mechanism, process as well as dynamical mode during destruction of the North China Craton (NCC) are obtained and the destruction mechanism of the NCC is one of controversial problems and is still not solved. In order to obtain the destruction mechanism of the NCC, we present detailed structural analysis of the middle segment of Tan-Lu Fault and its adjacent Jiaolai Basin, western Shandong Province and Hefei Basin and collect compressional stress data from all these areas. In this work, we obtain 216 groups data of thrust fault and strike-slip fault in these areas. We utilize the computer program that programmed by the Southern Paris University to inverse the evolution of the compressional stress from the Early Cretaceous to the Neocene. Therefore, a conclusion can be drawn that there are pulsant compressional action happening since the Early Cretaceous. The direction of the compressional stress is NWW in the Early Cretaceous, EW in the late Cretaceous, NNE, S-N and NNW in the Paleocene and NW in the Neocene. Combining with the moving direction of the Pacific plate, we suggest that destruction of the NCC is mostly caused by the subduction of the Pacific plate beneath the Euro-Asia plate.
Now, few about the mechanism, process as well as dynamical mode during destruction of the North China Craton (NCC) are obtained and the destruction mechanism of the NCC is one of controversial problems and is still not solved. In order to obtain the destruction mechanism of the NCC, we present detailed structural analysis of the middle segment of Tan-Lu Fault and its adjacent Jiaolai Basin, western Shandong Province and Hefei Basin and collect compressional stress data from all these areas. In this work, we obtain 216 groups data of thrust fault and strike-slip fault in these areas. We utilize the computer program that programmed by the Southern Paris University to inverse the evolution of the compressional stress from the Early Cretaceous to the Neocene. Therefore, a conclusion can be drawn that there are pulsant compressional action happening since the Early Cretaceous. The direction of the compressional stress is NWW in the Early Cretaceous, EW in the late Cretaceous, NNE, S-N and NNW in the Paleocene and NW in the Neocene. Combining with the moving direction of the Pacific plate, we suggest that destruction of the NCC is mostly caused by the subduction of the Pacific plate beneath the Euro-Asia plate.
引文
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[4] Djomani,Y.H.,OReilly.S.Y..The density structure of subcontinental lithosphere through time.EPSL, 2001, 184: 605-621.
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[8] Gao S, Rudnick RL, Yuan HL, Liu XM, Liu YS, Xu WL, Ling WL, Ayers J, Wang XC, Wang QH. Recycling lower continental crust in the North China craton. Nature, 2004, 432: 892-897.
[9] Gao S, Rudnick RL, Xu WL, Yuan HL, Hu ZC, Liu XM. Lithospheric evolution of the North China Craton: Evidence from high-Mg adakitic rocks and their entrained xenoliths (Abstract for Goldschmidt Conference). Geochim. Cosmochim. Acta, 2006, 70: 13-19.
[10] Kaneoka I, Notsu K, Takigami Y, et al. Constraints on the evolution of the Japan Sea based on 40Ar/39Ar ages and Sr isotopic ratios for volcanic rocks of the Yamato Seamount chain in the Japan Sea. Earth Planet. Sci. Lett., 1990, 97: 211-225
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[12] Maruyama S, Isozaki Y, Kimura G, et al. Paleogeographic maps ofthe Japanese Islands:plate tectonic systhesis from 750 Ma to the present. The Island Arc, 1997, 6: 121-142.
[13] Menzies, M., Xu, Y.G., Zhang, H. F., Fang, W. M.. Integration of geology, geophysics and geochemistry: A key to understanding the North China Craton. Lithos. 2007, 1-21
[14] Mercier, J. L., Hou Mingjin, Vergely, P., Wang Yongmin. Structural and stratigraphical constraints on the kinematics history of the Southern Tan-Lu Fault Zone during the Mesozoic, Anhui Province, China. Tectonophysics, 2007, 439:33-66.
[15] Meissner, M. and Mooney, W. Weakness of the lower continental crust: a condition for delamination, uplift, and escapes. Tectonophysics, 1998, 296: 47-60.
[16] Menzies MA, Xu YG. Geodynamics of the North China Craton. In Mantle Dynamics and Plate Interactions in East Asia (eds. Flower MFJ, Chung SL, Lo CH, Lee TY), Am. Geophy. Union, Washington, D. C., Geodyn. Ser., 1998, 27: 155-165.
[17] Menzies MA, Fan WM, Zhang M. Palaeozoic and Cenozoic lithoprobe and the loss of >120km of Archean lithosphere, Sino-Korean craton, China. In Magmatic Processes and Plate Tectonic (eds. Prichard HM, Alabaster T, Harris NBW, Neary CR). Geol. Soc. Special Publ., 1993, 76: 71-81.
[18] Miguel Doblas.Slickenside kinematic indicators.Tectonophysics, 1998, 295: 187-197.
[19] Otofuji Y, Hayashida A, Tom M. When was the Japan Sea opened? Paleomagnetic evidence from southwest Japan. in: Nasu N, Uyeda S, Kushiro I, Kobayashi K and Kagami H. eds. Formation of Active Ocean Margins. Tokyo Terra. 1985, 551-566.
[20] Park J O, Tokyuama H, Shinohara M, et al. Seismic record of tectonic evolution and backarc rifting in the southern Ryukyu island arc system. Tectonophysics. 1998, 294: 21-42.
[21] The golden transformation of the Cretaceous plate subduction in the west Pacific. Earth Planet. Sci. Lett., 2007, 262: 533-542.
[22] Sun WD, Ding X, Hu YH, Li XH. The golden transformation of the Cretaceous plate subduction in the west Pacific. Earth an Planetary Science Letters 262(2007)553-542
[23] Wilde SA, Zhou XH, Nemchin AA, Sun M. Mesozoic crust–mantle interaction beneath the North China craton: a consequence of the dispersal of Gondwanaland and accretion of Asia. Geology, 2003, 31: 817–820.
[24] Xu, Y. G. Diachronous lithospheric thinning of the North China Craton and formation of the Daxin'anling-Taihangshan gravity lineament. Lithos. 2007, 281-298.
[25] Xu WL, Gao S, Wang QH, Wang, DY, Liu YS. Mesozoic crustal thickening of the eastern North China craton: Evidence from eclogite xenoliths and petrologic implications. Geology, 2006, 34: 721-724.
[26] Zhang RY, Liou JG, Yang JS, Ye K. Ultrahigh-pressure metamorphism in the forbidden zone: the Xugou garnet peridotite, Sulu terrane, eastern China. J. Metamorph. Geol.,2003, 21: 539-550.
[27] Zhao DP, Maruyama S, Omori S. Mantle dynamics of Western Pacific and East Asia: Insight from seismic tomography and mineral physics. Gondwana Res., 2007, 11: 120-131.
[28] Zhang YQ, Dong SW, Shi W. Cretaceous deformation history of the middle Tan-Lu fault zone in Shandong Province, eastern China.Tectonophysics, 2003, 363: 243-258.
[29] Zheng JP, O’Reilly SY, Griffin WL, Lu FX, Zhang M. Nature and evolution of Cenozoic lithospheric mantle beneath Shandong Peninsula, Sino-Korean Craton, Eastern China. Inter. Geol. Rev. 1998, 40: 471-499.
[30] Zheng JP, Griffin WL, O’Reilly SY, Yu CM, Zhang HF, Pearson N, Zhang M. Mechanism and timing of lithospheric modification and replacement beneath the eastern North China Craton: peridotitic xenoliths from the 100 Ma Fuxin basalts and a regional synthesis. Geochim. Cosmochim. Acta, 2007, 71: 5203-5225.
[31]陈刚,赵重远,李丕龙,任战利等.合肥盆地构造热演化的裂变径迹证据.地球物理学报, 2005, 48(6):
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[33]陈义贤.辽河裂谷盆地断裂演化序次和油气藏形成模式.石油学报, 1985,6(2): 1-11.
[34]邓晋福,莫宣学,赵海玲,罗照华,杜杨松.中国东部岩石圈根/去根作用与大陆“活化”.现代地质, 1994, 8: 349-356.
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