Abstract
Getting a geologically realistic seismic image still remains a great challenge in foothills exploration. When geological structures are complex, seismic sections show distorted images and become difficult to be interpreted. Seismic processing tools, like time and depth migrations, have been developed to deal with this. Furthermore, when lateral velocity variations are strong, depth migration is definitely required. However, for a correct application of this processing, the construction of a detailed depth model describing lateral and vertical velocity variations is essential.
This study aims at showing that, in triangle zones, the structural features can be better retrieved if the seismic wave propagation through the complex subsurface is better understood. This is obtained by application of a workflow combining direct seismic modelling and depth migration processing. The seismic modelling gives a consistent and accurate velocity model used as input in the seismic depth migration. To illustrate the benefits of this approach, we present a synthetic case study based on a schematic model and a real case study from the frontal part of the Polish Carpathians.
Access this chapter
Tax calculation will be finalised at checkout
Purchases are for personal use only
Preview
Unable to display preview. Download preview PDF.
References
Aamir M., Maas Siddiqui M. (2006), Interpretation and visualisation of thrust sheets in a triangle zone in eastern Potwar, Pakistan, The Leading Edge, 1: 24–37.
Clarke R.(1997), Modelling and inversion of 3D complex kinematic data, Ph.D thesis, Université de Pau et des pays de l’Adour.
Duquet, B., Xu S., Lambaré G. (2003), 3D multi arrival Kirchhoff versus wave equation migration, Application to the 3D SEG/EAGE salt Model, The Leading Edge, 10: 969–972.
Jones P.B. (1996), Triangle zone geometry, terminology and kinematics, Bulletin of Canadian Petroleum Geology, 2: 139–152.
Krzywiec P. (2001), Contrasting tectonic and sedimentary history of the central and eastern parts of the Polish Carpathian foredeep basin-results of seismic data interpretation, Marine and Petroleum Geology 18: 13–38.
Krzywiec P., Aleksandrowski P., Florek R., Siupik J. (2004), The structure of the Outer Carpathian orogenic front: an example of the Miocen Zglobice unit between Brzesko and Wojnicz-new data, new models, new questions, Przegload Geologiczny, 11: 1051–1059.
Lafargue E., Ellouz N., Roure F. (1994), Thrust controlled exploration plays in outer Carpathians and their foreland (Poland, Ukraine and Romania), First Break, 2: 69–79.
Rousseau V., Nicoletis L., Svay-Lucas J., Rakotoarisao H. (2000), 3D true-amplitude migration by regularization in the angle domain, 62nd EAGE Conference, Expanded Abstracts.
Author information
Authors and Affiliations
Editor information
Editors and Affiliations
Rights and permissions
Copyright information
© 2007 Springer-Verlag Berlin Heidelberg
About this paper
Cite this paper
Jardin, A., Chaker, R., Krzywiec, P. (2007). Understanding Seismic Propagation through Triangle Zones. In: Lacombe, O., Roure, F., Lavé, J., Vergés, J. (eds) Thrust Belts and Foreland Basins. Frontiers in Earth Sciences. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-540-69426-7_3
Download citation
DOI: https://doi.org/10.1007/978-3-540-69426-7_3
Publisher Name: Springer, Berlin, Heidelberg
Print ISBN: 978-3-540-69425-0
Online ISBN: 978-3-540-69426-7
eBook Packages: Earth and Environmental ScienceEarth and Environmental Science (R0)