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Numerical simulation of the detachment dynamics in North China Basin
作者姓名:张东宁  曾融生
作者单位:Institute of Geophysics,State Seismological Bureau,Beijing 100081
摘    要:NumericalsimulationofthedetachmentdynamicsinNorthChinaBasinDong-Ning;ZHANG(张东宁)andRong-ShengZENG(曾融生)(InstituteofGeophysics,S...

收稿时间:8 August 1994
修稿时间:30 September 1994

Numerical simulation of the detachment dynamics in North China Basin
Dong-Ning, ZHANG and Rong-Sheng ZENG.Numerical simulation of the detachment dynamics in North China Basin[J].Acta Seismologica Sinica(English Edition),1995,8(4):511-517.
Authors:Dong-Ning  ZHANG and Rong-Sheng ZENG
Institution:(1) Institute of Geophysics, State Seismological Bureau, 100081 Beijing
Abstract:Refering to geological evidences and recent Lincheng-Julu deep seismic reflection profile in the west-central part of North China Basin, it is concluded preliminarily that a low angle detachment structure may exist in the central part of North China depression. Numerical method is used to simulate the influence of hot mantle intrusive bodies to Cenozoic basin tectonic movements. Numerical simulations show that, (1) The intrusion of hot mantle material has led to an extensional stress state in the upper crust in central North China depression. As time increasing, the extensional stress state changed slightly in the upper crust and was in keeping with the normal faulting tectonics in the upper crust in depression area. (2) In Cenozoic era, under the effects of magmatic intrusion and the resistance of Taihang Mountain, the weak zone produced by the Mesozoic thrust faulting would become a detachment structure. (3) With the elapse of time, the horizontal compressive stress gradually concentrated in the median crust, and the concentration of stress may generate strike-slip earthquakes in the median crust above the intrusive body. Contribution No. 95A0113, Institute of Geophysics, SSB, China.
Keywords:North China Basin  depression  detachment structure  crustal structure  finite element modelling
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