Western Geco

Cairo, Egypt

Western Geco

Cairo, Egypt
Time filter
Source Type

Johnson G.M.,Western Geco | Miller P.J.,Schlumberger
74th European Association of Geoscientists and Engineers Conference and Exhibition 2012 Incorporating SPE EUROPEC 2012: Responsibly Securing Natural Resources | Year: 2012

With a typical 3350m lateral well with more than 30 completion stages costing $8 million and upwards (upstreamonline.com 2011), the infill plan dramatically impacts long-term economics of the program. For very little relative additional cost, 3D seismic technology can be effectively utilized to reduce the risk of drilling costs overrun and maximise ultimate recovery from the field. The key is processing the seismic data specifically for these types of plays without taking shortcuts due to perceived time and cost constraints. We present a case study from the Bakken shale play in North Dakota, U.S., where advanced imaging and inversion techniques unlock the true predictive power of 3D seismic methodology for optimal development of unconventional resource plays.

Laake A.W.,Schlumberger | Sheneshen M.S.,Western Geco | Strobbia C.,Schlumberger | Velasco L.,Schlumberger | Cutts A.,Schlumberger
Petroleum Geoscience | Year: 2011

Reservoir mapping in the Gulf of Suez petroleum system is challenging because rift-parallel and cross-rift faults disrupted the sediments, leaving the reservoirs confined to stratigraphic, structural, and combined traps. We have developed a technique to address this challenge that integrates fault outcrop mapping using satellite image interpretation, seismic near-surface characterization techniques such as Rayleigh wave velocity mapping and ray parameter interferometry, as well as ant tracking of faults and geobody delineation on a prestack time-migrated (PSTM) cube. The technique uses a combination of geographic information system (GIS) and geological modelling software such as Petrel for surface/subsurface integration. The joint analysis of Rayleigh wave data with satellite imagery provides a near-surface structural geological model. The acquisition, processing, and interpretation of point-receiver seismic data enables the interpretation of near-surface geological structures. Detailed shallow structural geology can be imaged in the near surface, a data regime that is conventionally masked by the acquisition noise from the seismic acquisition. The shallow geological model comprises shallow lithological horizons as well as fault zones, the mapping of which may assist with the mitigation of shallow drilling risks. The integration of surface and subsurface structural mapping provides a tectonic framework for the delineation of reservoirs in the rift-faulted environment of the Gulf of Suez. © 2011 EAGE/Geological Society of London.

Fletcher R.P.,Western Geco | Robertsson J.O.A.,Schlumberger
SEG Technical Program Expanded Abstracts | Year: 2011

We propose two new boundary conditions to regulate coherent reflections from the model boundaries in numerical solutions of wave equations. Both boundary conditions have the common feature that the boundary condition is varied with respect to time. The first boundary condition expands or contracts the computational model during a modeling simulation. The effect is to cause a Doppler shift in the reflected wavefield that can be used to shift energy outside a frequency band of interest. Additionally, when the computational domain is expanding, the range of possible incidence angles on the boundary is restricted. This can be used to increase the effectiveness of many existing absorbing boundary conditions that are more effective for incidence angles close to normal. The second boundary condition is an extension of random boundaries. By carefully changing the realization of a random boundary over time, a more diffusive wavefield can be simulated. We show results with 2D numerical simulations of the scalar wave equation for both these boundary conditions. While the first boundary condition has application to modeling, both of these boundary conditions have potential applications within algorithms that rely upon modeling kernels, such as reverse-time migration and full-waveform inversion. © 2011 Society of Exploration Geophysicists.

Hermanrud C.,Statoil | Simmenes T.H.,Statoil | Ersland R.A.,Western Geco | Georgescu L.,University of Bergen
4th International Conference on Fault and Top Seals 2015: Art or Science? | Year: 2015

Analyses of hydrocarbon-related bright amplitudes in overburden rocks have demonstrated that such amplitude anomalies can often be associated with gas leakage from faults or fault intersections that offset underlying reservoirs. The position of the gas water contact frequently coincides with the depth of the top reservoir surface where it is intersected by the faults. The acoustic expression of the leaked gas differs significantly among areas, and is largely controlled by the caprock lithology.

Fowler P.J.,Western Geco | Lapilli C.,Western Geco
74th European Association of Geoscientists and Engineers Conference and Exhibition 2012 Incorporating SPE EUROPEC 2012: Responsibly Securing Natural Resources | Year: 2012

We derive separable approximations to orthorhombic dispersion relations that allow accurate and efficient modeling of P-waves. These allow extension to orthorhombic media of generalized pseudospectral methods previously used for modeling and reverse-time migration of P-waves in transversely isotropic media.

Abdeen M.M.,Cairo University | Abdelghaffar A.A.,Western Geco
Precambrian Research | Year: 2011

The Allaqi-Heiani suture (AHS) is the western part of the main Allaqi-Heiani-Gerf-Onib-Sol Hamed-Yanbu suture and represents one of the Neoproterozoic, arc-arc sutures in the Arabian-Nubian Shield (ANS). It separates the ca. 750. Ma South Eastern Desert terrane in the north from the ca. 830-720. Ma Gabgaba terrane in the south. The AHS is a deformed belt of ophiolitic rocks, syn-tectonic granitoids and metasediments. The central AHS zone is divided into three structural domains. The western domain (I) is characterized by NNE dipping thrusts and SSW-vergent folds. The central domain (II) includes upright tight to isoclinal NNW-SSE oriented folds and transpressional faults. The eastern domain (III) shows NNW-SSE oriented open folds. Structural analysis indicates that the area has a poly-phase deformation history involving at least two events. Event D1 was an N-S to NNE-SSW regional shortening generating the SSW-verging folds and the NNE dipping thrusts. Event D2 was an ENE-WSW shortening producing NNW-SSE oriented folds in the central and eastern parts of the study area and reactivating older thrusts with oblique-slip reverse fault movement. The tectonic evolution of the area involves two episodes of collision: an early collision between the South Eastern Desert terrane and the Gabgaba terrane along the AHS after the consumption of a basin floored by oceanic crust above a north-dipping subduction zone; and a later collision between East- and West-Gondwanas at ca. 750-650. Ma, leading to the closure of the Mozambique Ocean. This collision deformed the AHS along N-S trending shortening zones and produced NW-SE and NE-SW oriented sinistral and dextral transpressional faults, respectively. The early collision episode is related to the terrane accretion during the early Pan-African orogen, while the later phase is related to a late Pan-African or Najd orogen. © 2011 Elsevier B.V.

Fowler P.J.,Western Geco | King R.,Western Geco
SEG Technical Program Expanded Abstracts | Year: 2011

We derive coupled partial differential equations that accurately describe the propagation of pseudo-acoustic P-waves in orthorhombic media but do not require explicit knowledge of shear velocities. These allow extension to orthorhombic media of efficient methods commonly used for modeling and for reverse time migration of P-waves in transversely isotropic media. © 2011 Society of Exploration Geophysicists.

Johnson C.L.,University of Utah | Semple I.L.,Western Geco | Creem-Regehr S.H.,University of Utah
Journal of Geoscience Education | Year: 2013

The scale of features shown on outcrop photographs can be critical to geoscience interpretations, yet little is known about how well individuals estimate scale in images. This study utilizes a visualization test in which participants were asked to estimate the absolute size of several boxes shown in outcrop images using high resolution, stitched photopanoramas (Gigapans). Participants viewed two different outcrops that highlight different kinds of photographic distortion, first using static images and then with "interactive" Gigapans that permitted zooming and panning. A test group was given basic scaling cues in the form of distance to and height of the outcrops, whereas a control group completed the test without any scaling cues. Other population comparisons were investigated (e.g., gender, age, experience level, and major) but no other statistically significant population difference was observed. Therefore, scaling cues seem to invoke a primary effect at least in the first part of the exercise. Results show that scaling cues increase accuracy overall, but with wider spread and a tendency to cause overestimation of size. The control group, which was not given any scaling information, was less accurate overall and tended to underestimate the size of features. Both groups gave more accurate scale estimates with smaller standard deviations for the extension-distorted photopanorama than the compression-distorted image. Participants also generally showed improved accuracy in the second part of the test, which probably reflects the impact of interactivity, although a training effect cannot be discounted. These results suggest that nonembedded scaling cues (as opposed to physical objects denoting scale in photographs) can be useful for some individuals to estimate the size of features shown in outcrop images. Results also underscore the importance of interactivity and multiple exposures in classroom applications. © 2013 National Association of Geoscience Teachers.

Campbell T.,Western Geco
World Oil | Year: 2010

Recent projects completed in sparsely explored areas offshore Greenland and Brazil demonstrate the importance of using marine magnetotellurics (MMT) and controlled-source electromagnetics (CSEM) to gain pre-drill geologic knowledge and limit risk exposure. A group led by Encana Corporation, commissioned CSEM surveys over the two blocks to resolve questions over the prospectivity of Cretaceous reservoirs at 3,000 m below the seabed. Developing integrated interpretations of the geologic, gravity, magnetic, and seismic data yielded inversion volumes from the EM data sets that coincided with seismic volumes for each prospect. A basin study was launched in the deepwater Potiguar Basin off Brazil by CSEM, to evaluate prospects where the position and the depth of the target are known or likely. The study showed that integrating resistivity volumes obtained through 3D anisotropic inversions of the five CSEM data sets enhanced understanding of the earth model.

Lira J.M.,Petrobras | Innanen K.A.,University of Houston | Weglein A.B.,University of Houston | Ramirez A.C.,Western Geco
Journal of Seismic Exploration | Year: 2010

Western-Geco, Houston, TX, U.S.A. The objective of extracting the spatial location of a reflector, and its local angle-dependent reflection coefficient, from seismic data, depends on the ability to identify and to remove the effect on primary amplitudes of propagation down to and back from the reflector. All conventional methods that seek to correct for such transmission loss require estimates of the properties of the overburden. In this paper we propose a fundamentally new approach that will in principle permit correction of primaries for such transmission loss without requiring overburden properties as input. The approach is based on the amplitude of the first term of the inverse scattering series internal multiple attenuation algorithm, which predicts the correct phase and approximate amplitude of first order internal multiples. The amplitude is estimated to within a factor determined by plane wave transmission loss down to and across the reflector producing the event's shallowest downward reflection. Hence, the amplitude difference between a given predicted and actual multiple, both of which are directly available from the data and the algorithm output, in principle contain all necessary information to correct specific primary reflections for their overburden transmission losses. We identify absorptive overburdens/media as requiring particular focus, so as a first step, previous amplitude analysis of the internal multiple attenuation algorithm is here extended to include stratified absorptive media. Using this newly derived relationship between predicted and actual internal multiples, and existing results for acoustic/elastic media, correction operators, to be applied to specific, isolated primaries in both types of media, are then computed using combinations of multiples and their respective predictions. We illustrate the approach on synthetic data for the absorptive case with three earth models with different Q profiles. Further research into the amplitudes of the plane wave internal multiple predictions in 2D and 3D media is a likely pre-requisite to field data application of this concept-level algorithm. © 2010 Geophysical Press Ltd.

Loading Western Geco collaborators
Loading Western Geco collaborators