Results 31 to 40 of about 809,381 (295)
Geochemistry, Geophysics, Geosystems, 2021 The Permian Emeishan large igneous province (LIP) in Southwestern China is recognized as a remnant of mantle plume activity. Its crust composition has a significant bearing on understanding the magmatic plumbing system in a LIP and the volume of magmas ...
Wei Li, Yun Chen, Yi‐Gang Xu
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The Crustal Anisotropy of West Ordos Block and Its Geodynamic Implications
Geochemistry, Geophysics, Geosystems, 2021 Based on the teleseismic records of the dense broadband seismic array, the crustal anisotropy parameters of the west Ordos block and its adjacent regions were determined with P wave receiver functions.
Jinyu Lv +7 more
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Receiver function summation without deconvolution [PDF]
Geophysical Journal International, 2010 SUMMARY The separation of the structural effects below a seismic station from other effects like structures far away or from source–time functions is the fundamental problem of the receiver function technique. Two solutions of this problem have been suggested in the early days of the receiver function analysis. One is to model the complete wavefield
Kumar, P., Kind, R., Yuan, X.
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Mid‐mantle layering from SKS receiver functions [PDF]
Geophysical Research Letters, 2010 Many seismic data on mid‐mantle discontinuities are related only to subduction zones. Here we use a method that is applicable outside subduction zones. The idea is to use SKS‐to‐P converted phases that are generated in the receiver regions and can be detected in S receiver functions.
Vinnik, L. +3 more
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Closed form metrics to accurately model the response in general arbitrarily-coupled RC trees. [PDF]
, 2003 Closed form expressions are presented for the first and second moment of the impulse response for arbitrarily-coupled RC trees with multiple drivers, and used to generate accurate second order estimations of the transfer function from any driver to the ...
Elassaad, Shauki, Pamunuwa, Dinesh B.
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Dizhen xuebao, 2022 提出了一种利用接收函数、面波频散和重力数据联合约束地壳厚度、vP/vS和平均P波速度的改进方法，并基于两种地壳模型对改进后的方法进行了验证。结果显示，改进后的方法不仅可以提高地壳厚度和波速比的估计精度，还能更准确地估计地壳平均P波速度。在此基础上，将该方法应用于华南地区两个固定台站的地壳结构分析，相关结果也证实了该方法在确定地壳结构中的可行性。
Zhiyuan Ren +3 more
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Entanglement-assisted zero-error capacity is upper-bounded by the Lovász ϑ function [PDF]
, 2010 The zero-error capacity of a classical channel is expressed in terms of the independence number of some graph and its tensor powers. This quantity is hard to compute even for small graphs such as the cycle of length seven, so upper bounds such as the ...
Beigi, Salman
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Journal of Marine Science and EngineeringIt is challenging to apply the receiver function method to teleseisms recorded by ocean-bottom seismographs (OBSs) due to a specific working environment that differs from land stations.
Wenfei Gong +5 more
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Dizhen xuebao, 2022 利用架设在我国东北地区阿尔山火山区的宽频带流动地震台站记录的远震波形数据，采用P波接收函数H-κ叠加扫描方法，得到了阿尔山火山区的地壳厚度和平均波速比。结果显示：阿尔山地区的地壳厚度范围为33.9—37.9 km，整体呈西北厚东南薄的特点，火山带附近地壳较薄；地壳平均波速比范围为1.73—1.83，主要有柴河镇—明水河镇、伊敏德仁北部和天池镇三处高波速比区。结合前人研究结果推断， 阿尔山火山区薄的地壳和高波速比值可能是由地幔物质上涌、玄武岩浆底侵下地壳所致。
Yaxi Zhang +3 more
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Receiver Algorithm based on Differential Signaling for SIMO Phase Noise Channels with Common and Separate Oscillator Configurations [PDF]
, 2015 In this paper, a receiver algorithm consisting of differential transmission and a two-stage detection for a single-input multiple-output (SIMO) phase-noise channels is studied.
Eriksson, Thomas +2 more
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