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941.
In this paper, we present a new method for seismic stratigraphic absorption compensation based on the adaptive molecular decomposition.
Using this method, we can remove most of the effects resulting from wavelets truncation and interference which usually exist
in the common time-frequency absorption compensation method. Based on the assumption that the amplitude spectrum of the source
wavelet is smooth, we first construct a set of adaptive Gabor frames based on the time-variant properties of the seismic signal
to transform the signal into the time-frequency domain and then extract the slowly varying component (the wavelet’s time-varying
amplitude spectrum) in each window in the time-frequency domain. Then we invert the absorption compensation filter parameters
with an objective function defined using the correlation coefficients in each window to get the corresponding compensation
filters. Finally, we use these filters to compensate the time-frequency spectrum in each window and then transform the time-frequency
spectrum to the time domain to obtain the absorption-compensated signal. By using adaptive molecular decomposition, this method
can adapt to isolated and overlapped seismic signals from the complex layers in the inhomogeneous viscoelastic medium. The
viability of the method is verified by synthetic and real data sets. 相似文献
942.
复杂地表条件下高斯波束叠前深度偏移(英文) 总被引:6,自引:0,他引:6
在复杂地表条件的区域,地震数据的采集和处理是一项极大的挑战。虽然可以通过静校正来消除起伏地表的影响,然而当地表高程以及近地表速度剧烈变化时,简单的垂直时移对地震波场造成的畸变会严重降低偏移成像的质量。基于射线的偏移方法可以直接在起伏地表面进行波场的延拓成像,是解决上述问题的有效手段。本文针对复杂地表条件下的高斯波束叠前深度偏移进行研究,对倾斜叠加公式进行修改,使之包含地表高程以及速度的信息,通过直接在复杂地表面进行平面波的合成,得到了一种具有更高成像精度的改进方法。首先简单介绍常规高斯波束偏移的基本原理和计算流程,并以此为基础,给出复杂地表条件下高斯波束偏移原有的实现方法以及本文的改进方法,最后通过模型和实际资料的试算验证本文方法的有效性。 相似文献
943.
In the paleogeographic reconstruction of Mexico and northern Central America, an ever-increasing amount of evidence shows
that the entire region is a collage of suspect terranes transported from abroad, whose timing and sense of motion are now
beginning to be understood. Among these, the Chortis block (nuclear Central America) and the Baja California Peninsula have
been proposed as pieces of continent separated from the Pacific coast of southwestern Mexico, that have moved either southeastward
by the Farallon plate or northwestward by the Kula plate. Previous studies mainly confined to the northern margin of the Chortis
block, confirmed a left-lateral displacement of 130 km in Neogene time. Further studies made northwestward along the Mexican
coast provided a better understanding of magmatic and metamorphic processes in the area, and suggested times of detachment
increased to 30 Ma, 40 Ma, and 66 Ma. The pre-detachment westernmost position of the block has changed, depending on the model
chosen, from Puerto Vallarta and beyond, to the current position. Here we show that the isotopic mineral ages from coastal
granites along the coast from Puerto Vallarta, Jalisco (80 Ma) to Puerto Angel, Oaxaca (11 Ma) record systematic decrease
of cooling ages from NW to SE. This pattern is interpreted to result from the progressive uplift of rocks exposed at the present-day
coast in that direction, such uplift occurred in response to the development of the Middle America Trench at the newly formed
continental margin when the Chortis block was sliding at an average rate of 1.5 cm/year in a sinistral sense to its present
position. Our results also constrain the position of the Kula-Farallon spreading axis north of Puerto Vallarta. These observations
led us to conclude that several indicators point to this time and region for the onset of strike-slip drifting of the Chortis
block toward its current position. Here, we also present several view points in terms of other possilble interpretations to
different tectonic, geologic and isotopic data sets published recently by different authors. 相似文献
944.
The 03 February 2002 Çay Earthquake (Mw ~6.7) occurred on the fault segment between Eber and Ak?ehir Lakes followed by a large aftershock (Mw ~5.6) near the western end of the fault and two sequential aftershocks. We computed the coseismic surface displacements from static GPS measurements to determine the fault geometry parameters and uniform slip components. The coseismic displacements were obtained through combining the regional pre-earthquake and post-earthquake GPS data. Fault geometry and slips were acquired through the inversion of GPS data modeling the events as elastic dislocations in a half-space and assuming all four events took place on the same fault plane. Results suggest that one-segment fault of ~33 km length and dipping ~43° northward suffices to model the dislocation, assuming uniform slip distribution with 0.51 m dip slip, 0.26 m left-lateral slip extending to a depth down to ~11.5 km which is consistent with seismological evidence. The results also verify the normal faulting in the eastern flank of Isparta Angle which has long been assumed as a thrusting structure. While the available data cannot identify the four individual events on the same day, an attempted distributed slip model differentiates dip slip and left-lateral slips near the hypocenter with maximum values of ~1 and 0.6 m, respectively. 相似文献
945.
Site classification of Turkish national strong-motion stations 总被引:1,自引:0,他引:1
M. Abdullah Sandıkkaya Mustafa Tolga Yılmaz B. Sadık Bakır Özdoğan Yılmaz 《Journal of Seismology》2010,14(3):543-563
Since 1973, the General Directorate of Disaster Affairs of Turkey has deployed several strong-motion accelerographs at selected
sites. Within the framework of the project entitled Compilation of National Strong Ground Motion Database in Accordance with International Standards, site conditions were investigated within the upper 30-m depth by surface seismic and standard penetration tests. Preliminary
characterization of the sites is made by making use of both geophysical and geotechnical criteria of NEHRP Provisions and
Eurocode-8 site classification systems. The liquefaction susceptibility of those sites which comprise saturated cohesionless
deposits is also determined. Mean shear-wave velocity, mean penetration resistance, site class, and liquefaction susceptibility
of each site are tabulated. The Turkish strong-motion database supplemented by detailed information on site conditions is
a valuable source of information particularly for those studies that put emphasis on the relationship between site conditions
and strong-motion parameters. 相似文献
946.
The M
w
6.2 Lefkada earthquake occurred on 14 August 2003 beneath the western coastline of Lefkada Island. The main shock was followed
by an intense aftershock activity, which formed a narrow band extending over the western coast of the Island and the submarine
area between Lefkada and Kefalonia Islands, whereas additional off fault aftershocks formed spatial clusters on the central
and northwestern part of the Island. The aftershock spatial distribution revealed the activation of along-strike adjacent
fault segment as well as of secondary faults close to the main rupture. The properties of the activated segments were illuminated
by the precisely located aftershocks, fault plane solutions determination and the cross sections performed parallel and normal
to their strike. The aftershock focal mechanisms exhibited mainly strike slip faulting throughout the activated area, although
deviation of the dominant stress pattern is also observed. The results help to emphasize the importance of the identification
of activated nearby fault segments possibly triggered by the main rupture. Because such segments are capable to produce moderate
events causing appreciable damage, they should be viewed with caution in seismic hazard assessment in addition to the major
regional faults. 相似文献
947.
Iunio Iervolino Carmine Galasso Edoardo Cosenza 《Bulletin of Earthquake Engineering》2010,8(2):339-362
In code-based seismic design and assessment it is often allowed the use of real records as an input for nonlinear dynamic
analysis. On the other hand, international seismic guidelines, concerning this issue, have been found hardly applicable by
practitioners. This is related to both the difficulty in rationally relating the ground motions to the hazard at the site
and the required selection criteria, which do not favor the use of real records, but rather various types of spectrum matching
signals. To overcome some of these obstacles a software tool for code-based real records selection was developed. REXEL, freely
available at the website of the Italian network of earthquake engineering university labs (), allows to search for suites of waveforms, currently from the European Strong-motion Database, compatible to reference spectra
being either user-defined or automatically generated according to Eurocode 8 and the recently released new Italian seismic
code. The selection reflects the provisions of the considered codes and others found to be important by recent research on
the topic. In the paper, record selection criteria are briefly reviewed first, and then the algorithms implemented in the
software are discussed. Finally, via some examples, it is shown how REXEL can effectively be a contribution to code-based
real records selection for seismic structural analysis. 相似文献
948.
Granitic rocks usually exhibit strongly anisotropy due to pre-existing microcracks induced by long-term geological loadings.
The understanding of the rock anisotropy in mechanical properties is critical to a variety of rock engineering applications.
In this paper, Brazilian tests are conducted statically with a material testing machine and dynamically with a split Hopkinson
pressure bar system to measure both static and dynamic tensile strength of Barre granite. To understand the anisotropy in
tensile strength, samples are cored and labelled using the three principle directions of Barre granite to form six sample
groups. For dynamic tests, a pulse shaping technique is used to achieve dynamic equilibrium in the samples during the dynamic
test. The finite element method is then implemented to formulate equations that relate the failure load to the material tensile
strength by employing an orthotropic elastic material model. For samples in the same orientation group, the tensile strength
shows clear loading rate dependence. The tensile strengths also exhibit clear anisotropy under static loading while the anisotropy
diminishes as the loading rate increases, which may be due to the interaction of pre-existing microcracks. 相似文献
949.
Irina G. Kudintseva Alexander P. Nickolaenko Masashi Hayakawa 《Surveys in Geophysics》2010,31(4):427-448
We describe the space–time distribution of the pulsed electric field in the middle atmosphere above a positive Γ-shaped lightning
stroke. The channel of such a discharge contains a vertical and a horizontal section. The current wave moves initially vertically
and then turns horizontally so that radiation appears from the vertical electric dipole followed by that from the horizontal
dipole. Combined with reflection from the perfectly conducting ground, the source provides three subsequent pulses in the
atmosphere, with the lag being determined by the finite velocity of the current wave in the Γ-shaped stroke. The pulses are
reproduced by reflections from the air-ground and the air-ionosphere interfaces and the waveform resembles the M-component,
which is often noted in the negative strokes (e.g. Yashunin et al., J Geophys Res 112:D10109, 2007). The non-stationary fine structure appears in the spatial distribution of electric field, which persists for 2 ms or even
more and exceeds the runaway electron threshold. Estimates support the idea of free electron bunching in the mesosphere by
the pulsed electric field. Focusing may occur about 10 km away from the point of electron- field interaction; it is delayed
by a few ms from the moment of interaction. The data presented might be helpful in realistic modeling of the red sprite formation. 相似文献
950.
The paper focusses on seismic damage analysis of reinforced concrete (R/C) members, accounting for shear–flexure interaction
in the inelastic range. A finite element of the beam-column type recently proposed by the writers for the seismic analysis
of R/C structures is first briefly described. The analytical model consists of two distributed flexibility sub-elements which
interact throughout the analysis to simulate inelastic flexural and shear response. The finite element accounts for shear
strength degradation with inelastic curvature demand, as well as coupling between inelastic flexural and shear deformations
after flexural yielding. Based on this model, a seismic damage index is proposed taking into account both inelastic flexural
and shear deformations, as well as their interaction. The finite element and the seismic damage index are used to analyse
the response of R/C columns tested under cyclic loading and failing either in shear or in flexure. It is shown that the analytical
model and damage index can predict and describe well the hysteretic response of R/C columns with different types of failure. 相似文献