Some characteristics and applications of a general purpose optimum multichannel stacking filter

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2-d Zo Crs Stack By Considering An Acquisition Line With Smooth Topography

The land seismic data suffers from effects due to the near surface irregularities and the existence of topography, For obtaining a high resolution seismic image, these effects should be corrected by using seismic processing techniques, e.g. field and residual static corrections. The Common-Reflection- Surface (CRS) stack method is a new processing technique to simulate zero-offset (ZO) seismic sections from multi-coverage seismic data. It is based on a second-order hyperbolic paraxial traveltime approximation referred to a central normal ray. By considering a planar measurement surface, the CRS stacking operator is defined by means of three parameters, namely the emergence angle of the normal ray, the curvature of the normal incidence point (NIP) wave, and the curvature of the normal (N) wave. In this paper the 2-D ZO CRS stack method is modified in order to consider effects due to the smooth topography. By means of this new CRS formalism, we obtain a high resolution ZO seismic section, without applying static corrections. As by-products the 2-D ZO CRS stack method we estimate at each point of the ZO seismic section the three relevant parameters associated to the CRS stack process. © 2005 Sociedade Brasileira de Geofísica.2311525BARD, B., (1974) Nonlinear parameter estimation, , Academic PressBIRGIN, E., BILOTI, R., TYGEL, M., SANTOS, L.T., Restricted optimization: A clue to a fast and accurate implementation of the common reflection surface stack (1999) Journal of Applied Geophysics, 42, pp. 143-155ČERVENÝ, V., PSENSIK, I., (1988) Ray tracing program, , Charles University, CzechoslovakiaCHIRA, P., (2003) Empilhamento pelo método Superfície, , de Reflexão Comum 2-D com topografia e introdução ao caso 3-D, Ph.D. thesis, Federal University of Para, BrazilCHIRA-OLIVA, P., HUBRAL, P., Traveltime formulas of near-zero-offset primary reflections for a curved 2-D measurement surface (2003) Geophysics, 68 (1), pp. 255-261CHIRA-OLIVA, P., TYGEL, M., ZHANG, Y., HUBRAL, P., Analytic CRS stack formula for a 2D curved measurement surface and finite-offset reflections (2001) Journal of Seismic Exploration, 10, pp. 245-262GARABITO, G., CRUZ, J.C., HUBRAL, P., COSTA, J., Common Reflection Surface Stack: A new parameter search strategy by global optimization, 71th, SEG Mtg (2001) Expanded Abstracts, , San Antonio, Texas,USAGILL, P.E., MURRAY, W., WRIGHT, M.H., (1981) Practical optimization, , Academic PressGUO, N., FAGIN, S., Becoming effective velocity-model builders and depth imagers, part 2 - the basics of velocity-model building, examples and discussions Multifocusing (2002) The Leading Edge, pp. 1210-1216HUBRAL, P., Computing true amplitude reflections in a laterally inhomogeneous earth (1983) Geophysics, 48, pp. 1051-1062MANN, J., JÄGER, R., MÜLLER, T., HÖCHT, G., HUBRAL, P., Common-reflection-surface stack - A real data example (1999) Journal of Applied Geophysics, 42, pp. 301-318MÜLLER, T., (1999) The common reflection surface stack method - seismic imaging without explicit knowledge of the velocity model, , Ph.D. Thesis, University of Karlsruhe, GermanySEN, M., STOFFA, P., (1995) Global optimization methods in geophysical inversion, , Elsevier, Science Publ. CoZHANG, Y., HÖCHT, G., HUBRAL, P., 2D and 3D ZO CRS stack for a complex top-surface topography, Expanded (2002) 64th EAGE Conference and Technical Exhibition, , Abstract of th

PULSE DISTORTION IN-DEPTH MIGRATION

When migrating seismic primary reflections obtained from arbitrary source-receiver configurations (e.g., common shot or constant offset) into depth, a pulse distortion occurs along the reflector. This distortion exists even if the migration was performed using the correct velocity model. Regardless of the migration algorithm, this distortion is a consequence of varying reflection angle, reflector dip, and/or velocity variation. The relationship between the original time pulse and the depth pulse after migration can be explained and quantified in terms of a prestack, Kirchhoff-type, diffraction-stack migration theory.59101561156

A Miocene tectonic inversion in the Ionian Sea (Central Mediterranean): evidence from multi-channel seismic data

It is widely accepted that the Central and Eastern Mediterranean are remnants of the Neo-Tethys. However, the orientation and timing of spreading of this domain remain controversial. Here, we present time migrated and pre-stack depth migrated NW-SE oriented Archimede (1997) lines together with the PrisMed01 (1993) profile to constrain the evolution of the Ionian basin. Our interpretation allows us to identify a large-scale set of SW-NE striking reverse faults beneath the Ionian Abyssal Plain. These primarily NW vergent faults are characterized by a spacing comprised between 10 to 20 km and a dip ranging from 60 to 65{degree sign}. Following very recent paleogeographic reconstructions, we propose that the set of N{degree sign}55 features initially formed as normal faults during the NW-SE trending seafloor spreading of the Ionian basin after its late Triassic-early Jurassic rifting. Based on geometric comparisons with the intraplate deformation observed beneath the Central Indian Ocean, we show that the inherited oceanic normal faults were reactivated under compression as reverse faults. Well-developed Tortonian syntectonic basins developed NW of the major faults and the base of the Messinian evaporites (Mobile Unit) is slightly folded by the activity of the faults. We show that 3-4 km of total shortening occurs over a 80 km wide area beneath the Ionian Abyssal Plain, resulting in a bulk shortening of 3.5-5 %. We propose a link between the Tortonian-early Messinian inversion of the fault pattern and a plate tectonic reorganization prior to the main phase of back-arc opening of the Tyrrhenian domain

The common reflecting element (CRE) method revisited

The common reflecting element (CRE) method is an interesting alternative to the familiar methods of common midpoint (CMP) stack or migration to zero offset (MZO). Like these two methods, the CRE method aims at constructing a stacked zero-offset section from a set of constant-offset sections. However, it requires no more knowledge about the generally laterally inhomogeneous subsurface model than the near-surface values of the velocity field. In addition to being a tool to construct a stacked zero-offset section, the CRE method simultaneously obtains information about the laterally inhomogeneous macrovelocity model. An important feature of the CRE method is that it does not suffer from pulse stretch. Moreover, it gives an alternative solution for conflicting dip problems. In the 1-D case, CRE is closely related to the optical stack. For the price of having to search for two data-derived parameters instead of one, the CRE method provides important advantages over the conventional CMP stack. Its results are similar to those of the MZO process, which is commonly implemented as an NMO correction followed by a dip moveout (DMO) correction applied to the original constant-offset section. The CRE method is based on 2-D kinematic considerations only and is not an amplitude-preserving process.65397999

50 Years Geophysical Institute Karlsruhe, 1964 to 2014 - Expectations and Surprises

Die Festschrift anlässlich des 50. Geburtstags des Geophysikalischen Instituts in 2014 wurde hauptsächlich von Herrn Dr. Claus Prodehl zusammengestellt. Die einzelnen Beiträge stammen von ehemaligen und aktuellen GPI-Mitarbeitern und Mitarbeiterinnen

Mechanisms of extension at nonvolcanic margins: Evidence from the Galicia interior basin, west of Iberia

We have studied a nonvolcanic margin, the West Iberia margin, to understand how the mechanisms of thinning evolve with increasing extension. We present a coincident prestack depth‐migrated seismic section and a wide‐angle profile across a Mesozoic abandoned rift, the Galicia Interior Basin (GIB). The data show that the basin is asymmetric, with major faults dipping to the east. The velocity structure at both basin flanks is different, suggesting that the basin formed along a Paleozoic terrain boundary. The ratios of upper to lower crustal thickness and tectonic structure are used to infer the mechanisms of extension. At the rift flanks (stretching factor, β ≤ 2) the ratio is fairly constant, indicating that stretching of upper and lower crust was uniform. Toward the center of the basin (β ∼ 3.5–5.5), fault‐block size decreases as the crust thins and faults reach progressively deeper crustal levels, indicating a switch from ductile to brittle behavior of the lower crust. At β ≥ 3.5, faults exhume lower crustal rocks to shallow levels, creating an excess of lower crust within their footwalls. We infer that initially, extension occurred by large‐scale uniform pure shear but as extension increased, it switched to simple shear along deep penetrating faults as most of the crust was brittle. The predominant brittle deformation might have driven small‐scale flow (≤40 km) of the deepest crust to accommodate fault offsets, resulting in a smooth Moho topography. The GIB might provide a type example of nonvolcanic rifting of cold and thin crust