检索规则说明:AND代表“并且”;OR代表“或者”;NOT代表“不包含”;(注意必须大写,运算符两边需空一格)
检 索 范 例 :范例一: (K=图书馆学 OR K=情报学) AND A=范并思 范例二:J=计算机应用与软件 AND (U=C++ OR U=Basic) NOT M=Visual
作 者:许才军[1,2,3] 贺克锋 XU Caijun;HE Kefeng(School of Geodesy and Geomatics,Wuhan University,Wuhan 430079,China;Key Laboratory of Geospace Environment and Geodesy,Ministry of Education,Wuhan University,Wuhan 430079,China;Key Laboratory of Geophysical Geodesy,Ministry of Natural Resources,Wuhan University,Wuhan 430079,China)
机构地区:[1]武汉大学测绘学院,湖北武汉430079 [2]武汉大学地球空间环境与大地测量教育部重点实验室,湖北武汉430079 [3]武汉大学自然资源部地球物理大地测量重点实验室,湖北武汉430079
出 处:《武汉大学学报(信息科学版)》2023年第11期1736-1755,共20页Geomatics and Information Science of Wuhan University
基 金:国家自然基金创新群体项目(41721003);国家自然科学基金重点项目(42130101)。
摘 要:解析地震周期各阶段(震间、同震和震后)形变响应模型是研究地震从孕育、成核、破裂到震后调整整个过程动力学机制和探究区域壳幔流变属性的基础,在地震预测预报、防震减灾和危险性评定等方面发挥着重要作用。首先针对地震的震间形变、同震形变和震后形变的研究现状及进展进行了综述分析,指出了地震形变主流研究方法和模型的特点、不足和使用范围;然后讨论分析了地震周期形变模拟方法在现今数据快速积累情况下的机遇与挑战;最后对地震周期形变研究未来发展方向进行了展望。The deformation response models of earthquake cycle play a crucial role in studying the entire dynamic process of earthquakes,from inception,nucleation and rupture,to postseismic adjustments,as well as in exploring the rheological properties of Earth's crust and mantle.They have significant implications in earthquake prediction,forecasting,seismic hazard mitigation and risk assessment.First,this paper introduces the characteristics of deformation during the interseismic phase of the earthquake cycle.It categorizes and summarizes the corresponding models from the perspectives of dimensionality and elastic-viscoelastic models,and it elaborates on the characteristics,limitations and historical evolution of simulation methods for coseismic deformation,with a particular focus on mainstream approaches for determining the geometry of coseismic faults and selecting smoothing schemes.Then,this paper discusses the spatiotemporal evolution features of postseismic deformation,and categorizes them according to deformation mechanisms,including poroelastic rebound,viscoelastic relaxation and postseismic afterslip.It also outlines the characteristics and limitations of simulation methods for deformation phenomena and provides a classification summary of current mainstream postseismic combined models.Furthermore,this paper explores the opportunities and challenges faced by earthquake cycle deformation simulation methods in the rapidly accumulating data environment.It emphasizes the importance of three-dimensional viscoelastic models,considering the viscoelastic relaxation effects of Earth's crust and mantle.Finally,this paper offers prospects for future research directions,including single-fault earthquake cycle deformation simulation,postseismic mechanisms,dynamic modeling and interpretation of possible earthquake cycle deformation phenomena.
正在载入数据...
正在载入数据...
正在载入数据...
正在载入数据...
正在载入数据...
正在载入数据...
正在载入数据...
正在链接到云南高校图书馆文献保障联盟下载...
云南高校图书馆联盟文献共享服务平台 版权所有©
您的IP:3.128.199.33