检索结果-南通市图书馆

An eikonal equation-based earthquake location method by inversion of multiple phase arrivals

Science China Earth Sciences 2024年第6期67卷 1802-1817页

作者： Gaoyue LAO dinghui yang Shaolin LIU Guiju DONG Wenshuai WANG Kui LIU National Institute of Natural Hazards Ministry of Emergency Management of ChinaBeijing 100085China School of Earth Sciences Yunnan UniversityKunming 650091China Department of Mathematical Sciences Tsinghua UniversityBeijing 100084China School of Mathematics and Statistics Ningxia UniversityYinchuan 750021China

The precise determination of earthquake location is the fundamental basis in seismological community,and is crucial for analyzing seismic activity and performing seismic *** arrivals are generally used to practically determine earthquake ***,first-arrival traveltimes are not sensitive to focal ***,they cannot accurately constrain focal *** improve the accuracy,researchers have analyzed the depth phases of earthquake *** traveltimes of depth phases are sensitive to focal depths,and the joint inversion of depth phases and direct phases can be implemented to potentially obtain accurate earthquake ***,researchers can determine earthquake locations in layered *** layered models can only represent the first-order feature of subsurface structures,the advantages of joint inversion are not fully explored if layered models are *** resolve the issue of current joint inversions,we use the traveltimes of three seismic phases to determine earthquake locations in heterogeneous *** three seismic phases used in this study are the first P-,sPg-and *** calculate the traveltimes of the three seismic phases by solving an eikonal equation with an upwind difference scheme and use the traveltimes to determine earthquake *** verify the accuracy of the earthquake location method by the inversion of three seismic phases,we take the 2021 M_(S)6.4 yangbi,Yunnan earthquake as an example and locate this earthquake using synthetic and real seismic *** tests demonstrate that the eikonal equation-based earthquake location method,which involves the inversion of multiple phase arrivals,can effectively improve earthquake location accuracy.

关键词： Earthquake location Eikonal equation Fast marching method Heterogeneous model

来源：

维普期刊数据库

同方期刊数据库评论

在线全文

学校读者我要写书评

暂无评论

A holistic perspective on Earth system science

引用

Science China Earth Sciences 2024年第10期67卷 3013-3040页

作者： Yongfei ZHENG Zhengtang GUO Nianzhi JIAO Mu MU Shilong PIAO Suiyan FU dinghui yang Maoyan ZHU State Key Laboratory of Lithospheric and Environmental Coevolution School of Earth and Space SciencesUniversity of Science and Technology of ChinaHefei 230026China State Key Laboratory of Lithospheric and Environmental Coevolution Institute of Geology and GeophysicsChinese Academy of SciencesBeijing 100029China School of Ocean and Earth Sciences Xiamen UniversityXiamen 361102China Department of Atmospheric and Oceanic Sciences Fudan UniversityShanghai 200438China School of Environment Peking UniversityBeijing 100871China School of Earth and Space Sciences Peking UniversityBeijing 100871China Department of Mathematical Sciences Tsinghua UniversityBeijing 100084China Nanjing Institute of Geology and Palaeontology Chinese Academy of SciencesNanjing 210008China

Earth system can be categorized into three parts, solid Earth system, surface Earth system, and Sun-Earth space system. These three subsystems not only have mutual transmission and coupling relationships in both energy and matter but also involve multiple scales from microscopic to macroscopic. Earth system science is characterized by its globality and unity with a holistic view and a systematic view at multiple scales in both space and time. It focuses not only on the physical, chemical and biological interactions between various geospheres but also on the properties, behaviors, processes, and mechanisms of the entire Earth and its spheres. Although significant progress has been made in the study of internal disciplines of these three subsystems,there is still insufficient understanding of their overall behavior and interactions between individuals, thus facing challenges of different types and levels. The solid Earth system is composed of the crust, mantle, and core. Existing observational techniques struggle to penetrate deep into the mantle, making direct observation and data acquisition difficult;the extreme environments within Earth, such as high temperature, high pressure, and strong magnetic fields, also pose great challenges to observational equipment and scientific experiments. The surface Earth system is an open complex mega-system, in which there are complex interactions and feedback mechanisms among its geospheres(such as atmosphere, hydrosphere, biosphere, pedosphere and lithosphere), leading to difficulties in understanding of its overall behavior and long-term evolution. Biological activities have become increasingly significant in affecting the surface Earth system. The coupling between the internal and external Earth systems becomes more complex. Distinguishing and quantifying the impacts of Earth spherical interactions and biological activities on the surface Earth system is a major challenge. The Sun-Earth space system involves multiple physical

关键词： Earth's interior Earth's exterior Geospheres Energy exchange Material transfer

来源：

维普期刊数据库

同方期刊数据库评论

在线全文

学校读者我要写书评

暂无评论

Remnant Paleoproterozoic Subduction or Lithospheric Drip Initiation at the Yilgarn Craton Margin: Constraints from P-wave Tomography

引用

Acta Geologica Sinica(English Edition) 2024年第S1期 72-74页

作者： XU Xiaobing WANG Kun yang dinghui ZHAO Liang YUAN Huaiyu Department of Mathematical Sciences Tsinghua University Institute of Geophysics China Earthquake Administration State Key Laboratory of Lithospheric Evolution Institute of Geology and Geophysics Chinese Academy of Sciences University of Chinese Academy of Sciences ARC Centre of Excellence for Core to Crust Fluid Systems Department of Earth and Environmental SciencesMacquarie University Centre for Exploration Targeting University of Western Australia

The Paleoproterozoic was a critical time in whether modern-style plate tectonics had become globally dominant(e.g., Wan et al., 2020). The Capricorn Orogen witnessed the assembly of the Pilbara and Yilgarn Cratons and an exotic microcontinent, the Glenburgh Terrane, to form the West Australia Craton(WAC) through two collisional orogenic events, the 2215–2145 Ma Ophthalmian and 2005–1950 Ma Glenburgh Orogenies(Johnson et al., 2013; Fig. 1). Compared to other Proterozoic orogenic belts in Australia, the Capricorn Orogen preserves ‘complete' opposing continental margin successions, together with intervening arc fragments associated with oceanic closure and foreland basins associated with collisional loading(Cawood et al., 2009).

关键词：

来源：

同方期刊数据库评论

在线全文

同方期刊数据库

学校读者我要写书评

暂无评论

青藏高原东北缘基于W2度量的全波形成像

引用

地球物理学报 2024年第3期67卷 843-854页

作者：董兴朋杨顶辉蒙伟娟中国地震局地质研究所北京100029 清华大学数学科学系北京100084

本研究收集青藏高原东北缘区域114个宽频带地震台站记录到的50个区域地震事件波形数据,采用基于二次Wasserstein(W2)度量的全波形成像方法,获得了10~100 s频带下该区域的高分辨率壳幔结构图像.结果显示,秦岭造山带中下地壳呈高速特征,... 详细信息

本研究收集青藏高原东北缘区域114个宽频带地震台站记录到的50个区域地震事件波形数据,采用基于二次Wasserstein(W2)度量的全波形成像方法,获得了10~100 s频带下该区域的高分辨率壳幔结构图像.结果显示,秦岭造山带中下地壳呈高速特征,表明高原内部弱物质未流入此处;而从松潘—甘孜地块跨过昆仑断裂至秦祁地块内的中下地壳呈现低S波速、正径向各向异性(V_(SH)>V_(SV))和高泊松比异常,暗示深部地壳物质存在水平流动.在秦祁地块中部,深部地壳高速特性及负径向各向异性(V_(SH)

关键词：青藏高原东北缘 Wasserstein度量波形反演地壳流径向各向异性泊松比

来源：

维普期刊数据库博看期刊

同方期刊数据库评论

在线全文

学校读者我要写书评

暂无评论

全球非均匀模型中的远震走时层析成像

引用

地球物理学报 2024年第4期67卷 1426-1438页

作者：潘阳刘少林杨顶辉徐锡伟李小凡汪文帅李孟洋应急管理部国家自然灾害防治研究院北京100085 中国科学院地质与地球物理研究所岩石圈演化国家重点实验室北京100029 清华大学数学科学系北京100084 中国地质大学地球物理与空间信息学院武汉430074 宁夏大学数学统计学院银川750021 中国科学院大学地球与行星科学学院北京100049

远震走时层析成像是研究地球内部结构的重要工具.通常,远震走时层析成像使用一维地球参考模型计算研究区域外地震射线.由于地球存在广泛非均匀结构,传统远震走时层析成像在计算射线时忽略了研究区域外非均匀结构对射线的影响,最终导致... 详细信息

远震走时层析成像是研究地球内部结构的重要工具.通常,远震走时层析成像使用一维地球参考模型计算研究区域外地震射线.由于地球存在广泛非均匀结构,传统远震走时层析成像在计算射线时忽略了研究区域外非均匀结构对射线的影响,最终导致对研究区域内的成像结果产生影响.为了减小模型外地球非均匀结构对远震走时层析成像的影响,本文利用迎风差分格式数值求解程函方程,得到全球非均匀模型中的远震射线,以此为基础发展了基于全球非均匀模型的远震走时成像方法.为了检验本文成像方法提升成像精度的有效性,选取青藏高原东北缘为研究对象.合成测试和实际数据成像结果显示,在考虑地球非均匀结构以后,成像结果更精确,结果展现更多成像细节.

关键词：走时层析成像地震射线非均匀模型青藏高原东北缘

来源：

维普期刊数据库

同方期刊数据库评论

在线全文

学校读者我要写书评

暂无评论

基于逐元和轴对称谱元的混合方法及远震波场模拟

引用

地球物理学报 2024年第5期67卷 1819-1831页

作者：李昊臻刘少林董兴朋蒙伟娟杨顶辉清华大学数学科学系北京100084 应急管理部国家自然灾害防治研究院北京100085 中国地震局地质研究所北京100029

远震波形成像是研究地球内部结构和动力学过程的重要手段.然而,由于巨大的计算需求,当前在全球尺度(包含震源-台站)数值模拟高频(频率到2 Hz)地震波传播并不现实.谱元法是一种高有效性的数值模拟算法,具有高精度和网格剖分灵活的优点,... 详细信息

远震波形成像是研究地球内部结构和动力学过程的重要手段.然而,由于巨大的计算需求,当前在全球尺度(包含震源-台站)数值模拟高频(频率到2 Hz)地震波传播并不现实.谱元法是一种高有效性的数值模拟算法,具有高精度和网格剖分灵活的优点,并且已经成功应用于弹性波方程求解中.但缺点是求解远震问题时计算量和存储量较大.为了克服上述难题,本文发展了一种基于逐元并行谱元法与轴对称谱元法相结合的混合方法:即在全球尺度层状模型下使用具有快速计算效率的轴对称谱元法模拟远震背景波场,而在研究区域内使用逐元并行谱元法精确计算非均匀介质中远震波场传播.该方法减少了非均匀介质中远震波场模拟的计算量与存储量,并保持了逐元并行谱元法高精度、低存储量、易并行的优点.数值实验验证了该混合方法的可行性和精确性,并有望进一步应用于实际地震数据远震波形成像研究中.

关键词：弹性波方程混合方法逐元谱元法轴对称谱元法远震波场模拟

来源：

维普期刊数据库

同方期刊数据库博看期刊评论

在线全文

学校读者我要写书评

暂无评论

A modified nearly analytic discrete method and wavefield simulations in transversely isotropic media

引用

Science China Earth Sciences 2005年第8期48卷 1321-1328页

作者： LU Ming yang dinghui Department of Mathematical Sciences Tsinghua University Beijing 100084 China Department of Mathematical Sciences Tsinghua University Beijing 100084 China

Nearly analytic discrete method (NADM) is a higher accurate method for elastic wave equation that can suppress effectively numerical dispersion caused by discretizing the wave equation. In this paper we investigate the efficient implementation of NADM and present a refinement of the original NADM. Our theoretical analyses show that the modified NADM can improve significantly over the original one in numerous perspectives including numerical errors, storage spaces, and computational costs. Three-component synthetic VSP seismograms in 3-layered transversely isotropic (TI) media generated by the modified NADM are also reported. Theoretical analyses and numerical results show that the modified NADM can reduce storage space about 53 percent and computational costs about 30 percent compared with the original NADM. Moreover the accuracy of the modified NADM in time increases from 2-order of the original NADM to 4-order. Numerical results suggest that the modified NADM is more suitable to large-scale modeling because the modified method has little numerical dispersions even when too-coarse grids are used.

关键词： nearly analytic discrete method (NADM), elastic wave, three-component VSP seismogram, transversely isotropic(TI), seismic wave.

来源：

维普期刊数据库

同方期刊数据库评论

在线全文

学校读者我要写书评

暂无评论

The ONAD method for solving the SH-wave equation and simulation of the SH-wave propagation in the Earth's mantle

引用

Science China Earth Sciences 2013年第6期56卷 913-921页

作者： LI XiaoXiao yang dinghui TONG Ping Department of Mathematical Sciences Tsinghua University

The optimal nearly-analytic discrete(ONAD) method is a new numerical method developed in recent years for solving the wave *** with other methods,such as popularly-used finite-difference methods,the ONAD method can effectively suppress the numerical dispersion when coarse grids are *** this paper,the ONAD method is extended to solve the 2-dimensional SH-wave equation in the spherical *** investigate the accuracy and the efficiency of the ONAD method,we compare the numerical results calculated by the ONAD method and other methods for both the homogeneous model and the inhomogeneous IASP91 *** comparisons indicate that the ONAD method for solving the SH-wave equation in the spherical coordinates has the advantages of less numerical dispersion,small memory requirement for computer codes,and fast *** an application,we use the ONAD method to simulate the SH-wave propagating between the Earth's surface and the core-mantle boundary(CMB).Meanwhile,we investigate the SH-wave propagating in the mantle through analyzing the wave-field snapshots in different times and synthetic seismograms.

关键词： numerical dispersion spherical coordinates SH wave ONAD method mantle

来源：

维普期刊数据库

同方期刊数据库评论

在线全文

学校读者我要写书评

暂无评论

Wave dispersion and attenuation in viscoelastic isotropic media containing multiphase flow and its application

引用

Science China(Physics,Mechanics & Astronomy) 2014年第6期57卷 1068-1077页

作者： yang Lei yang dinghui NIE JianXin Department of Mathematical Sciences Tsinghua University Computational Geophysics Laboratory Tsinghua University State Key Laboratory of Explosion Science and Technology Beijing Institute of Technology

In this paper, we introduce the complex modulus to express the viscoelasticity of a medium. According to the correspondence principle, the Biot-Squirt （BISQ） equations in the steady-state case are presented for the space-frequency domain described by solid displacements and fluid pressure in a homogeneous viscoelastic medium. The effective bulk modulus of a multiphase flow is computed by the Voigt formula, and the characteristic squirt-flow length is revised for the gas-included case. We then build a viscoelastic BISQ model containing a multiphase flow. Through using this model, wave dispersion and attenuation are studied in a medium with low porosity and low permeability. Furthermore, this model is applied to observed interwell seismic data. Analysis of these data reveals that the viscoelastic parameter tan6 is not a constant. Thus, we present a linear frequen- cy-dependent function in the interwell seismic frequency range to express tanG. This improves the fit between the observed data and theoretical results.

关键词： multiphase flow viscoelastic BISQ model wave dispersion attenuation

来源：

维普期刊数据库

同方期刊数据库评论

在线全文

学校读者我要写书评

暂无评论

A wave propagation model with the Biot and the fractional viscoelastic mechanisms

引用

Science China Earth Sciences 2021年第3期64卷 364-376页

作者： Jiaming yang dinghui yang Hongwei HAN Lingyun QIU Yuanfeng CHENG Department of Mathematical Sciences Tsinghua UniversityBeijing 100084China Shengli Geophysical Research Institute of SINOPEC Dongying 257000China Yau Mathematical Sciences Center Tsinghua UniversityBeijing 100084China

Energy loss in porous media containing fluids is typically caused by a variety of dynamic *** the Biot theory,energy loss only includes the frictional dissipation between the solid phase and the fluid phase,resulting in underestimation of the dispersion and attenuation of the waves in the low frequency *** develop a dynamic model that can predict the high dispersion and strong attenuation of waves at the seismic band,we introduce viscoelasticity into the Biot model and use fractional derivatives to describe the viscoelastic mechanism,and finally propose a new wave propagation *** the Biot model,the proposed model includes the intrinsic dissipation of the solid *** investigate the effects of the fractional order parameters on the dispersion and attenuation of the P-and S-waves using several numerical ***,we use several groups of experimental data from different fluid-saturated rocks to testify the validity of the new *** results demonstrate that the new model provides more accurate predictions of high dispersion and strong attenuation of different waves in the low frequency range.

关键词： Poroviscoelasticity Wave propagation Dispersion and attenuation Fractional derivative

来源：

维普期刊数据库

同方期刊数据库评论

在线全文

学校读者我要写书评

暂无评论

欢迎您,

建议与咨询留下您的常用邮箱和电话号码，以便我们向您反馈解决方案和替代方法

时间限定

文献类型

馆藏选择

核心期刊

语言

文献类型

帮助

文字说明：

检索规则说明：

检索范例：

分类表

所选分类

限定检索结果

文献类型

馆藏范围

日期分布

学科分类号

主题

机构

作者

语言

在线全文

在线全文

在线全文

在线全文

在线全文

在线全文

在线全文

在线全文

在线全文

在线全文

请选择保存的检索档案：

请选择收藏分类：

通借通还

欢迎您,

建议与咨询 留下您的常用邮箱和电话号码，以便我们向您反馈解决方案和替代方法

时间限定

文献类型

馆藏选择

核心期刊

语言

文献类型

帮助

文字说明：

检索规则说明：

检索范例：

分类表

所选分类

限定检索结果

文献类型

馆藏范围

日期分布

学科分类号

主题

机构

作者

语言

在线全文

在线全文

在线全文

在线全文

在线全文

在线全文

在线全文

在线全文

在线全文

在线全文

请选择保存的检索档案： 新增检索档案 确定 取消

请选择收藏分类： 新增自定义分类 确定 取消

通借通还

建议与咨询留下您的常用邮箱和电话号码，以便我们向您反馈解决方案和替代方法

请选择保存的检索档案：

请选择收藏分类：