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:王伶俐[1,3] 洪敏 牛甜[1] 李芹 杨薪俊 喻世贤 WANG Lingli;HONG Min;NIU Tian;LI Qin;YANG Xinjun;Yu Shixian(Yunnan Earthquake Agency,Kunming 650201,Yunnan,China;Yunnan Institute of Geo-environment Monitoring,Kunming 650216,Yunnan,China;Yunnan Key Laboratory of Geohazard Forecast and Geo-ecological Restoration in Plateau Mountainous Area,Kunming 650216,Yunnan,China)
机构地区:[1]云南省地震局,云南昆明650201 [2]云南省地质环境监测院,云南昆明650216 [3]自然资源部云南省高原山地地质灾害预报预警与生态保护修复重点实验室,云南昆明650216
出 处:《地震研究》2025年第1期49-60,共12页Journal of Seismological Research
基 金:云南省地震局地震科技专项基金(2022ZX02);自然资源部/云南省高原山地地质灾害预报预警与生态保护修复重点实验室开放课题(YNGGR2023-01).
摘 要:利用1999-2020年云南及邻区近300个GNSS测站的观测数据解算获取的速度场为约束,采用克里金插值方法分时段估计了1999-2007年,2009-2014年,2015-2020年三期区域应变率场;通过回溯各个观测时段之后3年内M_(S)≥5.0地震事件,分析区域地壳形变特征与地震事件发生地点之间的相关性,结果表明,绝大部分地震都发生在面应变高梯度带的张压转换区和最大剪应变率沿断层方向的高值区或其边缘。基于上述应变率场异常特征,提出格网地震危险因子算法,建立地震危险区识别模型,通过估计格网最大剪应变率和面应变率风险区划因子,定量提取异常区地震危险指标,结果显示采用数值模型识别出的异常区与地震事件具有较好地对应关系;进一步采用R值评分的方式对应变率场异常区模型识别方法进行地震预测效能量化评估与分析,结果显示3期应变率场预测结果均通过R值评分检测。In this paper,the velocity field is calculated by using the observation data from nearly 300 GNSS stations in Yunnan and its adjacent areas in the period from 1999 to 2020.Based on the velocity field,three stages(1999-2007,2009-2014,and 2015-2020)of the regional strain rate fields are estimated by Kriging interpolation method.By backtracking the earthquake events(M_(S)≥5.0)in the following 3 years of each observation stage,the correlation between the characteristics of the regional crustal deformation and the location of the earthquake events is analyzed,and some abnormal criteria of strain rate field identifying the risk locations of the strong earthquakes are summarized.That is,most of the earthquake cases occur in the tension-pressure transition zone of the high gradient zone of surface strain,and the high value zone or the edge of the maximum shear strain along the fault.Based on the abnormal characteristics of strain rate field,this paper proposes a grid algorithm of the seismic risk factor,and establishes a model of the seismic-risk area identification.By estimating the recognition factors of the risk zones of the maximum shear strain and the surface strain with the grid algorithm,the seismic risk indicators of the abnormal areas are quantitatively extracted.The abnormal areas identified by the numerical model corresponds well with the seismic events.In order to provide an objective evaluation basis for the subsequent use of this model to track earthquake conditions and to determine earthquake risk locations,this paper adopts the R-value scoring method to evaluate the efficiency of this proposed model.The results show that the prediction of the strain rate field in the three stages passes the R-value scoring.
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:216.73.216.38