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国家自然科学基金(40721003): 作品数：15 被引量：266H指数：7; 相关作者：张素芳王二七刘一峰张中杰苏哲更多>>; 相关机构：中国科学院中国科学院研究生院中国海洋石油有限公司更多>>; 发文基金：国家自然科学基金中国科学院知识创新工程重要方向项目国家重点基础研究发展计划更多>>; 相关领域：天文地球石油与天然气工程交通运输工程更多>>

频谱分析法在反演造山带地形高差演化中的应用——以中国大别山、米仓山和美国内华达山脉为例: 近年来迅速发展的低温热年代学已极大改善了人们对地壳内(1～6 km)隆升和剥蚀过程的认识。然而在实际工作中,样品的采集除了受到气候、地理环境等恶劣条件的制约以外,在对低温热年代学数据进行解释或以此计算造山带的隆升剥露速率...; 苏哲刘静张鲁新王二七; 关键词：古地形构造地貌学; 文献传递

Comparative study of the free-surface boundary condition in two-dimensional finite-difference elastic wave field simulation: The finite-difference(FD) method is a powerful tool in seismic wave field modelling for understanding seismic ...; Haiqiang Lan and Zhongjie Zhang State Key Laboratory of Lithospheric Evolution,Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,People’s Republic of China; 关键词：ACCURACY; 文献传递

青藏高原中部Quasi-Love波的识别及其转换点揭示的东西向方位各向异性变化: 2009年; 目前人们利用4种基本的地震波现象研究地震各向异性,如横波双折射、面波散射、与传播方向有关的走时异常和PS转换波震相.本文利用面波散射产生的Quasi-Love(QL)波研究青藏高原上地幔顶部的各向异性结构特征.首先利用中国地震台网昌都(CAD)台记录的地震波形资料识别出产生QL波的路径,并利用合成地震记录和垂直偏振极性分析证实所观测到的为QL波,而不是高阶振型的Rayleigh波或其他体波震相;然后由Rayleigh波、Love波和QL波的群速度估算了各向异性结构横向变化的转换点;不同周期时,转换点的位置不同.这种频率依赖性还需要进一步的模拟研究.Love波向Rayleigh波耦合(产生QL波)的转换点位置揭示了青藏高原面波方位各向异性变化特征,并以南北向构造带的东西分段性、上地幔流引起的地球内力诱导岩石形变解释了青藏高原各向异性的东西向差异性.; 张素芳; 关键词：青藏高原中部各向异性

Amorphization in natural omphacite and its implications: High-resolution transmission electron microscopic data have revealed the existence of nanoscale intra-granular...; Geoffrey D.BromileySimon A.T.Redfern; 关键词：MICRO-FRACTURE OMPHACITE SUBDUCTION; 文献传递

Slip partitioning in the northeast Pamir-Tian Shan convergence zone: Based on a detailed analysis of satellite imagery combined with field geologic and geomorphic observations, we...; Yoshiki Ninomiya; 文献传递

Three-Dimensional Wave-Field Simulation in Heterogeneous Transversely Isotropic Medium with Irregular Free Surface: Modeling of seismic-wave propagation in anisotropic medium with irregular topography is beneficial to interpre...; Haiqiang Lan and Zhongjie Zhang State Key Laboratory of Lithosphere Evolution Institute of Geology and Geophysics Chinese Academy of Sciences Beijing,100029,PR China; 文献传递

接收函数方法估计Moho倾斜地区的地壳速度比: ＜正＞地壳速度比（Vp/Vs）是研究地壳属性的重要参数,接收函数方法在估计这一参数方面具有独特的优势。构造活动区的复杂力系作用往往使Moho界面发生变形,局部表现为倾斜。通过模型分析显示,当Moho界面倾角＞4°时,估计...; 张洪双田小波滕吉文; 文献传递

Short Note Segmentally Iterative Ray Tracing in Complex 2D and 3D Heterogeneous Block Models: We describe a complex geologic model as an aggregate of arbitrarily shaped blocks separated by cubic splines i...; Ergen Gao; 文献传递

Young,active conjugate strike-slip deformation in West Sichuan:evidence for the stress-strain pattern of the southeastern Tibetan Plateau: <正>The active kinematics of the eastern Tibetan Plateau are characterized by the southeastward movement of a m...; Zhe SuErchie WangKevin P.FurlongXuhua ShiGang WangChun Fan; 文献传递

SUB-TRIANGLE SHOOTING RAY-TRACING IN COMPLEX 3D VTI MEDIA: We model a complex 3D anisotropic structure as an aggregate of arbitrarily shaped blocks or volumes separated ...; TAO XU~1.ZHONGJIE ZHANG~1,AIHUA ZHAO~2,ANJIA ZHANG~1,XI ZHANG~1 and HONGSHUANG ZHANG~1 1 State Key Laboratory of Lithosphere Evolution,Institute of Geology and Geophysics.Chinese Academy of Sciences,China. 2 Institute of Geology and Geophysics,China Earthquake Administration,China.; 文献传递

国家自然科学基金(40721003)