Tectonic Analysis of the Al Hamadah Al Hamra Plateau of the Ghadamis Basin (NW Libya): Hydrological Network, Sinkholes, Folds and Fractures. Style of Reactivation and Setting of Cenozoic Volcanism
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.
References
[1]
Conant, L.C. and Goudarzi, G.H. (1967) Stratigraphic and Tectonic Framework of Libya. American Association of Petroleum Geologist Bulletin, 51, 719-730.
[2]
Gumati, Y.D., Kanes, W.H. and Schanel, S. (1996) An Evaluation of the Hydrocarbon Potential of the Sedimentary Basins of Libya. Journal of Petroleum Geology, 19, 95-112. https://doi.org/10.1111/j.1747-5457.1996.tb00515.x
[3]
Bellini, E. and Massa, D. (1980) A Stratigraphic Contribution to the Paleozoic of Southern Basins of Libya. In: Salem, M.J. and Busrewil, M.T., Eds., Geology of Libya, Academic Press, London, 3-56.
[4]
Goudarzi, G.H. (1980) Structure-Libya. In: Salem, M.J. and Busrewil, M.T., Eds., Second Symposium on the Geology of Libya, Vol. 3, Academic Press, London, 879-892.
[5]
Echikh, K. (1992) Geology and Hydrocarbon Potential of the Ghadamis Basin. Internal Report, National Oil Corporation of Libya (NOC), Tripoli.
[6]
Industrial Research Centre (IRC), Tripoli-Libya (1983-1985) 1:50,000, 1:250,000 and 1:1000,000 Geological Map Sheet Series from the Libya. Geological Map of Libya 1:250.000: Qarārat Al Marār NH 33-13, Sheet: Habayt Al Ghardqah.
[7]
Deffontaines, B. and Chorowicz, J. (1991) Principle of Hydrographic Network Analysis from Multisource Data. Application to Structural Analysis of the Zairian basin. Tectonophysics, 194, 237-263. https://doi.org/10.1016/0040-1951(91)90263-R
[8]
Chorowicz, J. and Deffontaines, B. (1993) Transform Faults and Pull-Apart Model in the Rhinegraben from Analysis of Multisource Data. Journal of Geophysical Research, 98, 14339-14351. https://doi.org/10.1029/93JB00190
[9]
Howard, A.D. (1967) Drainage Analysis in Geologic Interpretation: A Summation. American Association of Petroleum Geologist Bulletin, 51, 2246-2259.
[10]
Chorowicz, J. (1980) Mise à jour de notions utilisées par les géologues en télédétection. Hommes et Terres du Nord, Télédétection, 5, 203-206.
[11]
Peregi, Z., Less, G., Konrad, G., Fodor, L., Gulacsi, Z., Gyalog, L., Turki, S.M., Suwesi, S.K., Sherif, K. and Dalub, H. (2003) Geological Map of Libya 1:250,000, Sheet Al Haruj al Abyad, NG 33-8. Explanatory Booklet, 250 p. Industrial Research Centre, Tripoli.
[12]
Chorowicz, J., Bardintzeff, J.M., Rasamimanana, G., Chotin, P., Thouin, C. and Rudant, J.P. (1997) An Approach to Relate Tension Fractures to Volcanic Vents: Examples from Iceland and Madagascar. Tectonophysics, 271, 263-283. https://doi.org/10.1016/S0040-1951(96)00250-8
[13]
Korme, T., Chorowicz, J., Collet, B. and Bonavia, F.F. (1997) Volcanic Vents Rooted on Extension Fractures and Their Geodynamic Implications in the Ethiopian Rift. Journal of Volcanology and Geothermal Research, 79, 205-222. https://doi.org/10.1016/S0377-0273(97)00034-6
[14]
Adiyaman, Ö., Chorowicz, J. and Köse, O. (1998) Relationships between Volcanic Patterns and Neotectonics in Eastern Anatolia from Analysis of Satellite Images and DEM. Journal of Volcanology and Geothermal Research, 85, 17-32. https://doi.org/10.1016/S0377-0273(98)00047-X
[15]
Dhont, D., Chorowicz, J., Yürür, T., Froger, J.-L., Köse, O. and Gündogdu, N. (1998) Emplacement of Volcanic Vents and Geodynamics of Central Anatolia, Turkey. Journal of Volcanology and Geothermal Research, 85, 33-54. https://doi.org/10.1016/S0377-0273(98)00048-1
[16]
Adiyaman, Ö. Chorowicz, J., Arnaud, O.N., Gündogdu, M.N. and Gourgaud, A. (2001) Late Cenozoic Tectonics and Volcanism along the North Anatolian Fault: New Structural and Geochemical Data. Tectonophysics, 338, 135-165. https://doi.org/10.1016/S0040-1951(01)00131-7
[17]
Adiyaman, Ö. and Chorowicz, J. (2002) Late Cenozoic Tectonics and Volcanism in the Northwestern Corner of the Arabian Plate: A Consequence of the Strike-Slip Dead Sea Fault Zone and Lateral Escape of Anatolia. Journal of Volcanology and Geothermal Research, 117, 327-345. https://doi.org/10.1016/S0377-0273(02)00296-2
[18]
Navarro, A., Chorowicz, J., Miranda, J.M. and Catalão, J. (2009) Analysis of Geometry of Volcanoes and Faults in Terceira Island (Azores): Evidence for Reactivation Tectonics at EUR/AFR Plate Boundary in the Azores Triple Junction. Tectonophysics, 465, 98-113.
[19]
Chorowicz, J., Emran, A. and Alem, E.M. (2001) Tectonique et venues volcaniques en contexte de collision, exemple du massif néogène du Siroua (Atlas Marocain): Effets combinés d’une transformante et de la suture panafricaine. Canadian Journal of Earth Sciences, 38, 411-425. https://doi.org/10.1139/e00-074
[20]
Chorowicz, J. (2005) The East African Rift System. Journal of African Earth Sciences, 43, 379-410. https://doi.org/10.1016/j.jafrearsci.2005.07.019
[21]
Chorowicz, J. and Benissa, M. (2016) Remote Sensing and Field Analysis of the Palaeozoic Structural Style in NW Libya: The Qarqaf Arch a Paleo-Transfer Fault Zone between the Ghadamis and Murzuq Basins. Journal of African Earth Sciences, 123, 272-293. https://doi.org/10.1016/j.jafrearsci.2016.08.008