Property identification of anomalous seismic bodies by GMES techniques, a case historyApplied Geophysics - Tập 2 - Trang 135-139 - 2005
Yunxiang Liu, Weibin Sun, Dechun Li, Xiaofang Xu
What are the anomalous seismic reflection bodies at depths of over 6000 m? Are
they reefs or igneous rock? This is a difficult problem for seismic techniques,
but the GMES technique can handle it. The GMES technique is a joint exploration
technique combining gravity, magnetic, electrical, and seismic techniques. The
specific procedure is to conduct a 2D interface-constrained CEMP inversion using
2... hiện toàn bộ
Irregular surface seismic forward modeling by a body-fitted rotated–staggered-grid finite-difference methodApplied Geophysics - Tập 15 Số 3 - Trang 420-431 - 2018
Cheng, Jing-Wang, Fan, Na, Zhang, You-Yuan, Lü, Xiao-Chun
Finite-difference (FD) methods are widely used in seismic forward modeling owing
to their computational efficiency but are not readily applicable to irregular
topographies. Thus, several FD methods based on the transformation to
curvilinear coordinates using body-fitted grids have been proposed, e.g., stand
staggered grid (SSG) with interpolation, nonstaggered grid, rotated staggered
grid (RSG), a... hiện toàn bộ
A three-dimensional transient electromagnetic data inversion method based on a time—frequency transformationApplied Geophysics - Tập 17 - Trang 361-376 - 2021
Yun-Jian Yang, Xu-Ben Wang, Xue-Jun Liu, Xiao-Li Mi, Lifeng Mao
Herein, a three-dimensional (3D) inversion method in the frequency domain based
on a time–frequency transformation was developed to improve the efficiency of
the 3D inversion of transient electromagnetic (TEM) data. The Fourier transform
related to the electromagnetic response in the frequency and time domains
becomes a sine or cosine transform under the excitation of downward-step
current. We est... hiện toàn bộ
An analysis of seismic scattering attenuation in a random elastic mediumApplied Geophysics - Tập 8 - Trang 344-354 - 2011
Jiong Liu, Xiu-Cheng Wei, Yu-Xin Ji, Tian-Sheng Chen, Chun-Yuan Liu, Chun-Tao Zhang, Ming-Gang Dai
Seismic attenuation has been an interesting topic of research, for it reflects
the inherent media characteristics in which seismic waves propagate. There are
many factors that cause seismic wave attenuation, such as geometry attenuation
caused by energy dissipating during propagation, friction attenuation by
relative sliding among rock grains, and scattering attenuation by rock
heterogeneity. In t... hiện toàn bộ
Reduction of distortion and improvement of efficiency for gridding of scattered gravity and magnetic dataApplied Geophysics - Tập 9 - Trang 378-390 - 2012
Chen Zhang, Chang-Li Yao, Yong-Mao Xie, Yuan-Man Zheng, Hu-Liang Guan, Dong-Ming Hong
This paper presents a reasonable gridding-parameters extraction method for
setting the optimal interpolation nodes in the gridding of scattered observed
data. The method can extract optimized gridding parameters based on the
distribution of features in raw data. Modeling analysis proves that distortion
caused by gridding can be greatly reduced when using such parameters. We also
present some impro... hiện toàn bộ
Velocity dispersion and fluid substitution in sandstone under partially saturated conditionsApplied Geophysics - Tập 15 - Trang 188-196 - 2018
Xiao-Yi Ma, Shang-Xu Wang, Jian-Guo Zhao, Han-Jun Yin, Li-Ming Zhao
The elastic moduli of four sandstone samples are measured at seismic (2−2000 Hz)
and ultrasonic (1 MHz) frequencies and water- and glycerin-saturated conditions.
We observe that the high-permeability samples under partially water-saturated
conditions and the low-permeability samples under partially glycerin-saturated
conditions show little dispersion at low frequencies (2−2000 Hz). However, the
hi... hiện toàn bộ
Amplitude-preserving plane-wave prestack time migration for AVO analysisApplied Geophysics - Tập 5 - Trang 212-218 - 2008
Di Wang, Xiaodong Zheng, Jiubing Cheng, Huazhong Wang, Zaitian Ma
To support amplitude variation with offset (AVO) analysis in complex structure
areas, we introduce an amplitude-preserving plane-wave prestack time migration
approach based on the double-square-root wave equation in media with little
lateral velocity variation. In its implementation, a data mapping algorithm is
used to obtain offset-plane-wave data sets from the common-midpoint gathers
followed by... hiện toàn bộ
Seismic data reconstruction based on CS and Fourier theoryApplied Geophysics - Tập 10 - Trang 170-180 - 2013
Hua Zhang, Xiao-Hong Chen, Xin-Min Wu
Traditional seismic data sampling follows the Nyquist sampling theorem. In this
paper, we introduce the theory of compressive sensing (CS), breaking through the
limitations of the traditional Nyquist sampling theorem, rendering the coherent
aliases of regular undersampling into harmless incoherent random noise using
random undersampling, and effectively turning the reconstruction problem into a
mu... hiện toàn bộ
Full tensor gravity gradiometry data inversion: Performance analysis of parallel computing algorithmsApplied Geophysics - Tập 12 - Trang 292-302 - 2015
Zhen-Long Hou, Xiao-Hui Wei, Da-Nian Huang, Xu Sun
We apply reweighted inversion focusing to full tensor gravity gradiometry data
using message-passing interface (MPI) and compute unified device architecture
(CUDA) parallel computing algorithms, and then combine MPI with CUDA to
formulate a hybrid algorithm. Parallel computing performance metrics are
introduced to analyze and compare the performance of the algorithms. We
summarize the rules for th... hiện toàn bộ