[PDF][PDF] 短周期密集台阵被动源地震探测技术研究进展
张明辉， 武振波， 马立雪， 郑凡， 解桐桐， 郑孟杰… - 地球物理学进展, 2020 - dsjyj.com.cn
摘要近十年来, 短周期密集台阵被动源探测技术日益成长为国内外深部结构探测领域的一项重要
手段. 该技术相较于传统宽频带地震探测具有高分辨, 省时省钱, 绿色环保等优点 …
手段. 该技术相较于传统宽频带地震探测具有高分辨, 省时省钱, 绿色环保等优点 …
Shear wave velocity structure of the crust and upper mantle in Southeastern Tibet and its geodynamic implications
Southeastern Tibet, which has complex topography and strong tectonic activity, is an
important area for studying the subsurface deformation of the Tibetan Plateau. Through the …
important area for studying the subsurface deformation of the Tibetan Plateau. Through the …
The community velocity model V. 1.0 of southwest China, constructed from joint body‐and surface‐wave travel‐time tomography
Southwest China, located at the southeastern margin of the Tibetan plateau, plays an
important role for the plateau growth and its material extrusion. It has complicated tectonic …
important role for the plateau growth and its material extrusion. It has complicated tectonic …
[HTML][HTML] 利用面波频散与接收函数联合反演青藏高原东南缘地壳上地幔速度结构
郑晨， 丁志峰， 宋晓东 - 地球物理学报, 2016 - html.rhhz.net
青藏高原东南缘对于青藏高原的隆升, 增厚和物质逃逸等问题有着重要的研究价值.
本文对研究区内布设的大型流动地震台阵的观测记录进行处理, 联合反演面波频散与接收函数 …
本文对研究区内布设的大型流动地震台阵的观测记录进行处理, 联合反演面波频散与接收函数 …
A new crustal shear-velocity model in Southwest China from joint seismological inversion and its implications for regional crustal dynamics
Southwest (SW) China is located in a transition site from the active Tibetan Plateau to the
stable Yangtze craton, which has complicated tectonic deformation and severe seismic …
stable Yangtze craton, which has complicated tectonic deformation and severe seismic …
[HTML][HTML] 2021年5月21日云南漾濞MS6.4地震震区地壳结构特征与孕震背景
李大虎， 丁志峰， 吴萍萍， 刘韶， 邓菲， 张旭， 赵航 - 地球物理学报, 2021 - html.rhhz.net
本文基于" 中国地震科学台阵探测——南北地震带南段" 密集布设的流动地震台阵和川滇区域
数字测震台网等共计634 个台站所记录的观测资料, 先采用地震体波层析成像(TOMO3D) …
数字测震台网等共计634 个台站所记录的观测资料, 先采用地震体波层析成像(TOMO3D) …
The mechanism of deep material transport and seismogenic environment of the Xiaojiang fault system revealed by 3-D magnetotelluric study
The Xiaojiang fault system (XJFS), located to the southeast of the Tibetan Plateau, has a
complicated tectonic history and is an ideal location to study the Tibetan Plateau in terms of …
complicated tectonic history and is an ideal location to study the Tibetan Plateau in terms of …
利用双差层析成像方法反演青藏高原东南缘地壳速度结构
刘伟， 吴庆举， 张风雪 - 地震学报, 2019 - cqvip.com
本文利用云南及周边区域地震台网2010—2016 年记录到的近震资料, 采用双差层析成像方法
进行地震重定位并获得了青藏高原东南缘的三维地壳速度结构. 结果显示: 重定位后的震源位置 …
进行地震重定位并获得了青藏高原东南缘的三维地壳速度结构. 结果显示: 重定位后的震源位置 …
Magmatic underplating and crustal growth in the Emeishan Large Igneous Province, SW China, revealed by a passive seismic experiment
In an attempt to characterize the subsurface structure that is related to fossil mantle plume
activity, a comprehensive geophysical investigation was conducted in the Emeishan Large …
activity, a comprehensive geophysical investigation was conducted in the Emeishan Large …
Deformation of crust and upper mantle in central Tibet caused by the northward subduction and slab tearing of the Indian lithosphere: New evidence based on shear …
Shear-wave splitting provides insight into geodynamic processes such as lithospheric
deformation and upper mantle flow. This study presents shear wave splitting parameters …
deformation and upper mantle flow. This study presents shear wave splitting parameters …