地震地质 ›› 2015, Vol. 37 ›› Issue (2): 598-612.DOI: 10.3969/j.issn.0253-4967.2015.02.021

• 研究论文 • 上一篇    下一篇

共轭断层系统的非线性有限元模拟与震群模型讨论

郭婷婷1,2,3, 徐锡伟3, 邢会林4, 于贵华3   

  1. 1. 山东省工程地震研究中心, 济南 250021;
    2. 山东省地震局, 济南 250014;
    3. 中国地震局地质研究所, 活动构造与火山重点实验室, 北京 100029 ;
    4. Earth Systems Science Computational Centre(ESSCC), University of Queensland, St Lucia QLD 4072, Australia
  • 收稿日期:2014-11-14 修回日期:2015-04-27 出版日期:2015-06-20 发布日期:2015-08-19
  • 通讯作者: 徐锡伟,研究员,主要从事活动构造学及其在减轻地震灾害中的应用研究,E-mail:xiweixu@vip.sina.com
  • 作者简介:郭婷婷,女,1979年生,2013年于中国地震局地质研究所获构造地质学博士学位,副研究员,主要从事岩土工程与构造应力分析研究,电话:0531-88556102,E-mail:gtt.yy@163.com。
  • 基金资助:

    山东省自然科学基金(ZR2014DQ022)、国家自然科学基金(91214201)和山东省地震局科研基金(JJ1303)共同资助。

NONLINEAR FINITE-ELEMENT SIMULATION OF CONJUGATE FAULTS SYSTEM AND ASSOCIATED EARTHQUAKE SWARM

GUO Ting-ting1,2,3, XU Xi-wei3, XING Hui-lin4, Yu Gui-hua3   

  1. 1. Shandong Institute of Earthquake Engineering, Jinan 250021, China;
    2. Earthquake Administration of Shandong Province, Jinan 250014, China;
    3. Key Laboratory of Active Tectonics and Volcano, Institute of Geology, China Earthquake Administration, Beijing 100029, China;
    4. Earth Systems Science Computational Centre ESSCC, the University of Queensland, St. Lucia, QLD 4072, Australia
  • Received:2014-11-14 Revised:2015-04-27 Online:2015-06-20 Published:2015-08-19

摘要:

采用断层摩擦接触的非线性有限元模拟方法, 对单断层与交叉断层2种断层模型分别进行数值模拟计算对比, 结合中国大陆双震或震群型地震孕育发生的构造条件对共轭断层系统的孕震与发震机理进行了讨论与分析。 断面滑动摩擦机制较好地解释了共轭断层由闭锁状态进入发生地震的滑动状态的过程, 共轭断层系统会交替地发生失稳事件, 验证了2组共轭断层系统构成的地震模型的滑动习性。其数值模拟与讨论分析结果可为共轭断层发育区的地震监测预报提供科学依据。

关键词: 共轭断层系统, 地震构造模型, 摩擦接触, 非线性有限元模拟

Abstract:

In this paper, adopting nonlinear finite-element method for faults with frictional contact, single fault and conjugate faults are calculated and compared respectively. And conjugate faults system is analyzed about its structural significance, combined with preparation and occurrence of strong earthquakes in the capital circle region. Study shows that seismogenic process of typical conjugated fault system from lock to unlock is well explained by Coulomb friction criteria, and unstable events can take place alternately along conjugate faults. The slip behavior of seismogenic tectonic model of great earthquake composed of two conjugate faults is verified. The numerical simulation as well as the analysis and discussion on the results provide scientific basis for earthquake forecasting and monitoring in areas where conjugate faults have developed.

Key words: conjugate faults system, seismotectonic model, frictional contact, nonlinear finite-element simulation

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