Abstract

Remote sensing analysis is an efficient tool for updating geological maps. The regional scale map obtained in this project from compilation of the pre-existing maps and of a number of space images is somewhat more complete. It takes into account the usual field and laboratory parameters of the rock units, through the previous geologic maps, together with remote sensing parameters such as spectral signatures, textures, roughness, morphology that are observed from optical, microwave and DEM imagery. With more rock characteristics, the old maps are obligatory improved. The Cenozoic faulting in the Al Hamra al Hamadah plateau is largely influenced by the tectonics affecting the Paleozoic oil bearing structures that are hidden by the late Cretaceous-Paleocene layers. The tectonic style is that of reactivation of the Paleozoic faults under effects of the NNE-trending regional tension. Then the faults on the surface of the plateau would indicate location of the hidden Paleozoic faults in depth. A flat plateau, in the arid environment, appears to be a very favorable environment for mapping of gentle folds, faults and tectonic sinkholes. Remote sensing is a fruitful approach in this case study. The gentle anticlines for instance are undetectable in the field, but computer assisted shadowing with a low elevation angle of illumination is the key processing for evidencing these features. Problems of drillings in the area are well known for example to Waha, AGOCO and PB Companies during their exploration activities in the concessions in Ghadames Basin. According to them several incidents of losing drilling Pits have occurred and drilling came into a hole. Because this paper is aimed to know the exact location of sinkholes in the Ghadames basin, I would recommend all the oil companies to review this work and try to trace the sinkholes indicated to minimize the risk of drilling problems.

Highlights

  • The study area comprises different zones (Figure 1)

  • Remote sensing analysis is an efficient tool for updating geological maps

  • The regional scale map obtained in this project from compilation of the pre-existing maps and of a number of space images is somewhat more complete

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Summary

Introduction

The study area comprises different zones (Figure 1). The Al Hamada al Hamra plateau is essentially a flat area of large dimensions. The satellite data and maps are included into Geographic Information Systems (GIS) where they are geo-coded or at least georeferenced From the beginning these techniques have been increasingly applied to the exploration process of oil and gas. Maybe the methodology has not yet been sufficiently adapted to oil and gas exploration, and the satellite remote sensing imagery alone is insufficient if not correlated with other data and completed with the most recent knowledge and understandings of the various other related earth science disciplines, including fieldwork. A detailed analysis of the Earth Observation Data (EOD) was undertaken in order to better understand the outcrops of the Paleozoic in the region, with a view to using them as direct analogues in order to assist in the interpretation of the equivalent horizons in the subsurface

Geological Setting of Al Hamadah Al Hamra Plateau
Image Characteristics of the Units
Evidencing Anticlines
Fold Closures of Layer Traces
Maestrichtian Outcrops
Folded Topographic Surfaces
Topographic Cross-Section
Hydrologic Network Anomalies
Types of Drainage Anomalies
Approach
Mapping
Venues
Pull-Apart
Description
Local Sites
Types of Sinkholes
Age Determination
Reactivation of Palaeozoic Faults
10. Conclusions
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