CRS SEISMIC PROCESSING OF A GEOLOGICAL COMPLEX AREA

Eduardo Jiménez¹, Carlos A. Vargas²'³ and Luis A. Montes³

¹ Geoseimic Ltda. e-mail: Eduardo.jimenez@cable.net.co

² Institute for Geophysics, University of Texas

³ Departamento de Geociencias, Universidad Nacional de Colombia, Bogotá. e-mail: lamontesv@unal.edu.co

Manuscript received: 10/06/2009 Accepted for publication: 26/10/2009

ABSTRACT

We applied the NMO and CRS (Common Reflector Surface) approaches to a complex geological area in order to compare their performances for obtaining enhanced images. Unlike NMO, CRS does not depend on a previous time velocity model and uses a hyperbolic equation to estimate 2D travel times through three parameters (Normal ray emergence angle, NIP and N wavefront curvatures). To obtain the image a solution provided by coherence analysis algorithm was used.

A low quality Colombian seismic line acquired in Middle Magdalena basin was used, where a foothill geological area is characterized by a thrusting fault. The CRS provided an enhanced image which allowed a new geological interpretation that is best constrained with other regional observations.

RESUMEN

El propósito de esta investigación es comparar las técnicas de Superficie Común de Reflexión (CRS) y Normal Move Out (NMO) en su desempeño en zonas geológicamente complejas, procurando imágenes sísmicas de mejor calidad. A diferencia del NMO, el CRS no depende de un modelo previo de velocidad y usa una ecuación hiperbólica de tiempos de viaje 2D dependiente de tres parámetros (ángulo de emergencia del rayo normal, curvatura de la onda de punto de incidencia normal y curvatura de la onda normal). Para obtener la imagen se usó una solución provista por un algoritmo de análisis de coherencia.

Se usó una línea sísmica de baja calidad adquirida en la cuenca del Valle Medio del Magdalena - Colombia, en una zona de pie de monte caracterizada por una falla de cabalgamiento. El CRS suministró una imagen mejorada que permitió una nueva interpretación geológica que se ajusta mejora con otras observaciones regionales.

Palabras clave: superficie común de reflexión CRS, Zero-offset (ZO), corrección por sobre tiempo normal (NMO), punto medio (CMP)

Introduction

The CRS method has been considered an attractive stacking method to provide improved zero offset sections (Trappe et al., 2001; Hertweck et al., 2007).

In Colombian a known example with the CRS applied to complex areas does not exist, although there is a reported paper with CRS applied to a mild topography and quiet tectoni-cally zone with relevant results (Cárdenas and Montes, 2006). In complex tectonically areas seismic tests are hampered by several factors that often lead to low quality seismic images with ravel reflectors, due to poor signal/noise ratio or weak seismic signal focusing.

In order to compare NMO and CRS performances in complex zones, a low quality seismic line of the Middle Magdalena basin was used. The area includes a thrust fault in the foothill zone. Instead of stack velocities CRS used parameters picked automatically by a coherence analysis algorithm (Birgin et al., 1999).

As result, an enhanced CRS image allowed a new geological interpretation.

The CRS stack is a theoretically well established method (Jager et al., 2001; Mann et al., 1999; Tygel et al., 1997). It considers layers separated by curved reflectors whose reflection comes from a reflecting segment. A second order approximation of transmitted and reflected travelime rays in seismic system was developed (Bortfeld, 1989). A multi-covering seismic data set is acquired over a set of homogeneous and isotropic layers, with arbitrary velocities separated by smooth interfaces.

The seismic system is defined by a zero offset ray, called Central ray, which incidences normally on the reflector.

In a second order approximation around central point (X₀) the travel time of the SRG ray is approximated by the hyperbolic function:

According Figure 1, x = (G + S)/2 is the common midpoint, h = (G- S)/2) is half offset, V0 is the near surface velocity and β and t₀ are angle of emergence and travel time of the Central ray. K_NIP is the wavefront curvature of a hypothetical wave with the source located at point NIP K_N is the wavefront curvatures of an exploding reflector segment around point NIP.

A more deep and complete theoretical development about CRS can be revised in others references (Bortfeld, 1989; Tygel etal, 1997)

Procedure

The NMO stacked section was obtained by a current seismic processing sequence in ProMAX®. Due to CRS does not require a previous known velocity model the velocity analysis and stacking steps were replaced by searching and optimizing local and global CRS parameters through coherence analysis solution until obtain an optimized stacked section. This equivalent step was done using MPT® (a Numerica's software trade mark). After stacking, the NMO and CRS images were filtered and enhanced applying the same ProMAX sequences. A flow diagram of both sequences is shown in Figure 2.

Search of CRS parameters

This non conventional procedure replaces the NMO analysis and stacking currently used in seismic processing sequences. The whole procedure is explained in the following sequence of steps with a visual description in the flow chart of Figure 3, as was defined by Muller (Muller, 1999)

The first step is to estimate V_NMO from CMP gathers at point x=x₀, this reduces equation 1 to:

This step is an NMO velocity analysis and stacking which provides an initial simulated ZO section (zero-offset).

In the second step β is searched. For that, the reflectors in anterior ZO section are considered locally flat, i.e. case of small apertures (K_N =0), that simplifies equation 1:

In the third step β is known and with the equation in zero offset configuration, K_N value is estimated from ZO section.

Geological setting

Geologically the area has been deformed by thrusting associated to compressive tectonic events. In the area a monocline dips to the East and the basement outcrops at West. The cretaceous rocks are below a gently dip Eastward Tertiary sequence, as seen in Figure 4. Different structural styles are observed: a first thrust with East vergence, a second one with West vergence and a lineation and NE-SW strike slip fault system.

A low to high dip thrust fault emerges in surface with a high inclination. This fault causes the repetition of the cretaceous sequence which was observed in the well sited at West. A second fault inferred from seismic section, allows the elevation of basement over the footwall block below the fault. A tertiary detachment fault interpreted in the seismic section was observed in the cartographic recognition of the area.

Discussion and results

An E-W acquired seismic line was selected to be processed by the two methods in order to compare their performances in producing the seismic images. At East side of the thrust fault a well allowed to identify the stratigraphic units in the seismic section.

This seismic line was previously processed using a conventional flow of processing to obtain a PSTM section, shown in Figure 5.

The seismic line was properly processed applying a conventional sequence flow with a careful selection of parameters, as result a new stacked section was obtained, providing also a more reliable NMO velocity model to be used as starting model in CRS method.

The stacked section is displayed in the figure 6, where is evident the enhancement of the image compared with that other in figure 5.

After the CRS processing a better image is showed the stacked section included in Figure 7. In figure 6 the reflectors appear weaker, strong and less coherent can be seen with a better continuity, with low noise and besides that the image owns more seismic events in the shallow part.

Compared with NMO stack section the CRS is a more enhanced and allow to constraints the monoclonal structure descripted in the geological setting section.

To compare the quality of the images a S/N content evaluation was made. First the noise was isolated from the signal in the image through band pass filters and then respective spectral analysis's were done. The results are depicted in Figure 9, at top for NMO image and at bottom CRS image. Comparing the figures 9a and 9b the random noise level is reduced from 27.8% in NMO image to 17.9 % in CRS image. It represents a significant improvement in signal to noise ratio and in consequence a rising in the seismic resolution.

A post-stack CRS migrated section was interpreted using the software Geographix (Landmark Graphics Co®). The change in the quality of the image permitted a new geological interpretation matching the seismic section with the lithological units identified in the stratigraphic column and the borehole logs (Figure 8).

The difference among the geological interpretation gotten in Figure 3 and the interpreted in Figure 10 is evident.

This new interpretation is due to the enhanced quality of the new obtained CRS image.

Conclusions

A low quality Colombian seismic line acquired in Middle Magdalena basin was processed using the NMO and the CRS techniques looking for an enhanced of the image on a thrusting fault. The CRS provided an improved image which allowed a new geological interpretation that is best constrained with other regional observations. Our observations suggest that the CRS technique improves the imaging of complex areas and constitutes an alternative in seismic processing. CRS-2D method generated seismic sections of good quality without knowledge of subsurface velocity model, essential in expensive process like pre-stack migrations.

Performance of CRS methods in thrusting zone, allowed a new interpretation and geologic model. Futures works should emphasize the CRS technology in 3-D data and use the information given by CRS, attributes in tomography inversion, AVO, migration and coherent cube analysis.

Acknowledgements

The authors express grateful to Landmark Graphics Co. Latin America to provide ProMAX and Geographix software and Numerica Ltda to permit the use of MPT (Multiparmetric Processing Tool) software implemented with CRS.

Birgin, E., Biloti, R., Tygel, M. and Santos, L. Restricted optimization: a clue to a fast and accurate implementation of the Common Reflection Surface Stack        [ Links ]

Method. Journal of Applied Geophysics. Vol, 42, Issues 3-4. P 143-155.        [ Links ]

Bortfeld, R., 1989, Geometrical ray theory: Rays and travel times in seismic systems (second-order approximations of the travel times: Geophysics, Vol 54 No. 3 P 342-349.        [ Links ]

Cardenas, A., and Montes, L. 2006, Stacking on commonreflection surface with multiparameter traveltime. Vol. 10, No. 2, Earth Sci. Res. J. P 91-103.        [ Links ]

Hubral, P., 1983, Computing true amplitude reflections in a laterally inhomogeneous earth: Geophysics, 48 No. 8, P 1051 - 1062.        [ Links ]

Hertweck, T., Schleicher, J., Mann, J. 2007. Data Stacking Beyond CMP: The Leading Edge. V 26, No.7. P818-827.        [ Links ]

Jager, R., Mann, J., Hocht, G., Hubral P. 2001. Commonre-flection Surface Stack: Image and attributes. Geophysics Vol 66 No. 1, P 97- 109.        [ Links ]

Mann, J., Jager, R., Muller, T., Hocht, G., and Hubral, P., 1999, Common-reflection- surface-stack a real data example: Journal of Applied Geophysics, 42, 301 - 318.        [ Links ]

Neidel, N., and Taner, M., 1971, Semblance and other coherency measures for multichannel data: Geophysics, 36, 482-497.        [ Links ]

Muller, T., 1999, The common Reflection Surface Stack Surface stack Method - Seismic imaging without explicit knowledge of the velocity model: Ph. D. thesis, University of Karlsruhe.        [ Links ]

Tygel, M., Muller, T., Hubral, P., and Schleicher, J., 1997, Eigenwave base multiparameter traveltime expansion: 67^th Annual Internat. Mtg. Soc. Expl, Geophys 1770 -1773.        [ Links ]

Vieth, K., 2001, Kinematic wavefield attributes in seismic imaging. Ph.D. thesis, University at Karlsruhe.        [ Links ]

Trappe, H., Gierse, G. and Pruessmann, J., 2001. Case studies show potential of Common Surface stack structural resolution in time domain beyond the conventional NMO/DMO stack. First Break, 625- 633. Special topic. Nov.        [ Links ] ]]> 42 34 34 143-155 1989 54 3 3 342-349 2006 91-103 1983 48 8 8 1051 - 1062 2007 26 7 7 P818-827 2001 66 1 1 97- 109 1999 42 301 - 318 1971 36 482-497 1999 1997 1770 -1773 2001 2001 625- 633