<abstract xmlns="http://www.w3.org/1999/xhtml"><p>West Wadi El-Rayan is located in the Western Desert at about 140 km SE of Cairo. Also, it lies between Gindi basin to the east and Abu Gharadig basin to the west. In order to construct a 3D structural model and to delineate the subsurface structure styles of the area, seismic structural interpretation and structural restoration are used. The structural geometry within the area is inverted half-graben, since the area was controlled by reactivation of older faults. The magnitude of the inversion-related shortening in the study area was estimated and was suggested to be strong. The result of the strong inversion magnitude occurred toward northeast of the study area can be concluded that, the area suffered shortening and part of the Jurassic / Early Cretaceous normal faults are reactivated as reverse faults. Also the cap, the main reservoirs and the source rock sections are brought to the surface and thus breached, as well any previous mature source rock becoming non-generative where the dry wells are located. However, any less severe inversion structure in this case where producing wells are located that remain buried and will have a better chance or preserving the structure geometry and therefore top and lateral seal.</p></abstract>

West Wadi El-Rayan is located in the Western Desert at about 140 km SE of Cairo. Also, it lies between Gindi basin to the east and Abu Gharadig basin to the west. In order to construct a 3D structural model and to delineate the subsurface structure styles of the area, seismic structural interpretation and structural restoration are used. The structural geometry within the area is inverted half-graben, since the area was controlled by reactivation of older faults. The magnitude of the inversion-related shortening in the study area was estimated and was suggested to be strong. The result of the strong inversion magnitude occurred toward northeast of the study area can be concluded that, the area suffered shortening and part of the Jurassic / Early Cretaceous normal faults are reactivated as reverse faults. Also the cap, the main reservoirs and the source rock sections are brought to the surface and thus breached, as well any previous mature source rock becoming non-generative where the dry wells are located. However, any less severe inversion structure in this case where producing wells are located that remain buried and will have a better chance or preserving the structure geometry and therefore top and lateral seal.

Structural Inversion Magnitude and its Impacts on the Hydrocarbon Accumulation

Geophysics Department, Faculty of Science

Pakistan Journal of Geology

This work is licensed under the Creative Commons Attribution-NonCommercial-NoDerivatives 3.0 License.

{"article-title":"Structural Inversion Magnitude and its Impacts on the Hydrocarbon Accumulation"}

West Wadi El-Rayan is located in the Western Desert at about 140 km SE of Cairo. Also, it lies between Gindi basin to the east and Abu Gharadig basin to the...

Structural Inversion Magnitude and its Impacts on the Hydrocarbon Accumulation

Publicado en línea: 24 feb 2020

Páginas: 1 - 8

DOI: https://doi.org/10.2478/pjg-2019-0006

Palabras clave
Inversion magnitude, structural restoration, 3D seismic Interpretation, Western Desert

© 2019 Mohamed G. El-Behiry et al., published by Sciendo

This work is licensed under the Creative Commons Attribution-NonCommercial-NoDerivatives 3.0 License.

Structural Inversion Magnitude and its Impacts on the Hydrocarbon Accumulation

Publicado en línea: 24 feb 2020

Páginas: 1 - 8

DOI: https://doi.org/10.2478/pjg-2019-0006

Palabras claveInversion magnitude, structural restoration, 3D seismic Interpretation, Western Desert

© 2019 Mohamed G. El-Behiry et al., published by Sciendo

This work is licensed under the Creative Commons Attribution-NonCommercial-NoDerivatives 3.0 License.

Palabras clave
Inversion magnitude, structural restoration, 3D seismic Interpretation, Western Desert