نتایج جستجو برای: seismic cross

تعداد نتایج: 525892  

2004
Igor Morozov

We summarize the recent development of our broad-range seismic and geophysical data processing system. The system implements a novel data handling and analysis framework, currently includes ~200 tools and allows inclusion of unlimited number and types of algorithms. It provides standardized input/output, common parameterization of all tools, common graphical look and feel, automated maintenance...

2015
Cornelis Weemstra Roel Snieder Lapo Boschi

S U M M A R Y Cross-correlation of ambient seismic noise recorded by two seismic stations may result in an estimate of the Green’s function between those two receivers. Several authors have recently attempted to measure attenuation based on these interferometric, receiver–receiver surface waves. By now, however, it is well established that the loss of coherence of the crosscorrelation as a func...

2004
N. M. Shapiro M. Campillo

[1] We demonstrate that the coherent information about the Earth structure can be extracted from the ambient seismic noise. We compute cross-correlations of vertical component records of several days of seismic noise at different pairs of stations separated by distances from about one hundred to more than two thousand kilometers. Coherent broadband dispersive wavetrains clearly emerge with grou...

2008
Stephen A. Ketcham Jason R. McKenna Roy J. Greenfield Thomas S. Anderson

Dynamic mechanical activity in a tunnel can be measured as ground vibrations at offset distances. These signals can be processed in sensing algorithms for detection, location, and discrimination of the activity. The objective of this work is to demonstrate that seismic simulations can reveal the effect of the environment on seismic energy as it propagates from tunnels. Using massively parallel ...

1996
Yair Shimshoni Nathan Intrator

| This paper proposes a classiication scheme based on integration of multiple Ensembles of ANNs. It is demonstrated on a classiication problem, in which seismic signals of Natural Earthquakes must be distinguished from seismic signals of Artiicial Explosions. A Redundant Classiication Environment consists of several Ensembles of Neural Networks is created and trained on Bootstrap Sample Sets, u...

2017
Chunquan Yu Yingcai Zheng Xuefeng Shang

We introduce an open-source MATLAB software package, named Crazyseismic, for passive seismic data preprocessing. Built-in core functions such as seismic phase travel-time calculation and multichannel cross correlation significantly improve the efficiency of data processing. Compared with conventional command-line-style toolboxes, all functions in Crazyseismic are embedded in one single graphic ...

2017
Loı̈c Viens Marine Denolle Hiroe Miyake Shin’ichi Sakai Shigeki Nakagawa

S U M M A R Y Seismic interferometry is now widely used to retrieve the impulse response function of the Earth between two distant seismometers. The phase information has been the focus of most passive imaging studies, as conventional seismic tomography uses traveltime measurements. The amplitude information, however, is harder to interpret because it strongly depends on the distribution of amb...

Journal: :فیزیک زمین و فضا 0
علی هاشمی گازار عبدالرحیم جواهریان

seismic coherency is a measure of lateral changes in acoustic impedance that are caused by variations in structure, stratigraphy, lithology, porosity, and fluid content. seismic coherency is a geometrical attribute that establishes temporal and lateral relationships with other attributes. seismic coherency can be defined by coherency attributes. when coherency attributes are applied to seismic ...

2017

Mathematical morphology has its applications in both optical and acoustic image analysis and is useful in image cleaning, image enhancement, feature selection and extraction, quantitative analysis, etc. Morphology has the capabilities of performing quantitative analysis of images using morphological operation. Partial differential equation(PDE) is employed for Anisotropic Diffusion filtering te...

2012
Michael A. Lewis Peter Gerstoft

S U M M A R Y We use cross-correlation of seismic noise recorded at stations in the San Andreas Fault Observatory at Depth (SAFOD) pilot hole to extract P and S waves and measure S-wave anisotropy on the horizontal components. The data are recorded at seven three-component stations at depths from 1857 to 2097 m in the pilot hole. In late September and early 2004 October drilling noise underneat...

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