Results 11 to 20 of about 809,381 (295)
Basis Pursuit Receiver Function [PDF]
Abstract Receiver functions (RFs) are derived by deconvolution of the horizontal (radial or transverse) component of ground motion from the vertical component, which segregates the PS phases. Many methods have been proposed to employ deconvolution in frequency as well as in time domain. These methods vary in their approaches to impose regularization
Sen, Mrinal K. +3 more
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Gravity inversion constrained by OBS receiver function reveals crustal structure in Ryukyu Trench
The Ryukyu Trench is located in the northern Philippine Sea. The subduction of the Philippine Sea Plate to the Eurasia Plate along the Ryukyu Trench in the NNW direction leads to extremely complex tectonic processes such as subduction, collision ...
Tingwei Yang +16 more
doaj +1 more source
Sharpness of the transition zone seismic discontinuities and seismic velocity jump across the discontinuities provide important constraint on water content and mineral composition near the transition zone.
Jing XUE, Xinxin YU, Jun LI
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To systematically investigate seismic azimuthal anisotropy in the Sumatra subduction zone and probe mantle dynamics associated with the subduction of the Australian Plate beneath the Sunda Plate, a total of 169 pairs of teleseismic XKS (including PKS ...
Fansheng Kong +4 more
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A new approach for inversion of receiver function for crustal structure in the depth domain
A method for reconstructing crustal velocity structure using the optimization of stacking receiver function amplitude in the depth domain, named common conversion amplitude (CCA) inversion, is presented.
TianYu Zheng, YuMei He, Yue Zhu
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Matlab files of stacked receiver functions after common conversion point stacking based on the IASP91 velocity model.
Yingkai Wu, Xuewei Bao
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Multiple tectonic events since the Neoproterozoic era have framed the present-day lithosphere in the Fujian province affiliated with the eastern part of the South China Block. Comprehensive information of the crustal structure and bulk properties can aid
Ayush Goyal, Shu-Huei Hung
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Receiver Function Seismology [PDF]
The application results of the receiver function technique are briefly outlined. The topography of the main seismic boundaries in the mantle transition zone is evaluated with resolution of about 3 km in depth and about 200 km laterally. The maximal amplitudes of depth variations of the main boundaries reach tens of kilometers.
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Lung Function in Patients Receiving Busulphan [PDF]
An attempt was made to achieve earlier detection of busulphan lung (fibrosing alveolitis) and to determine its incidence by means of serial studies during life, including measurement of the gas transfer factor. Twenty-three patients were investigated over an average period of nearly two years of busulphan treatment.
W A, Littler, C, Ogilvie
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Seismic anisotropy beneath eastern North America, as expressed in shear wave splitting observations, has been attributed to plate motion‐parallel shear in the asthenosphere, resulting in fast axes aligned with the plate motion.
Yantao Luo +4 more
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