Identification of Igneous Intrusions in South Zallah Trough, Sirt Basin, Libya
Authors: Mohamed A. Saleem
Using mostly seismic data, this study intends to show some examples of igneous intrusions found in some areas of the Sirt Basin and explore the period of their emplacement as well as the interrelationships between these sills. The study area is located in the south of the Zallah Trough, south-west Sirt basin, Libya. It is precisely between the longitudes 18.35ᵒ E and 19.35ᵒ E, and the latitudes 27.8ᵒ N and 28.0ᵒ N. Based on a variety of criteria that are usually used as marks on the igneous intrusions, 12 igneous intrusions (Sills), have been detected and analysed using 3D seismic data. One or more of the following were used as identification criteria: the high amplitude reflectors paired with abrupt reflector terminations, vertical offsets, or what is described as a dike-like connection, the violation, the saucer form, and the roughness. Because of their laying between the hosting layers, the majority of these intrusions are classified as sills. Another distinguishing feature is the intersection geometry link between some of these sills. Every single sill has given a name just to distinguish the sills from each other such as S-1, S-2, and … S-12. To avoid the repetition of description, the common characteristics and some statistics of these sills are shown in summary tables, while the specific characters that are not common and have been noticed for each sill are shown individually. The sills, S-1, S-2, and S-3, are approximately parallel to one other, with the shape of these sills being governed by the syncline structure of their host layers. The faults that dominated the strata (pre-upper Cretaceous strata) have a significant impact on the sills; they caused their discontinuity, while the upper layers have a shape of anticlines. S-1 and S-10 are the group's deepest and highest sills, respectively, with S-1 seated near the basement's top and S-10 extending into the sequence of the upper cretaceous. The dramatic escalation of sill S-4 can be seen in North-South profiles. The majority of the interpreted sills are influenced and impacted by a large number of normal faults that strike in various directions and propagate vertically from the surface to the basement's top. This indicates that the sediment sequences were existed before the sill’s intrusion, deposited, and that the younger faults occurred more recently. The pre-upper cretaceous unit is the current geological depth for the Sills S-1, S-2 … S-9, while Sills S-10, S-11, and S-12 are hosted by the Cretaceous unit. Over the sills S-1, S-2, and S-3, which are the deepest sills, the pre-upper cretaceous surface has a slightly forced folding, these forced folding is also noticed above the right and left tips of sill S-8 and S-6, respectively, while the absence of these marks on the above sequences of layers supports the idea that the aforementioned sills were emplaced during the early upper cretaceous period.Procedia APA BibTeX Chicago EndNote Harvard JSON MLA RIS XML ISO 690 PDF Downloads 291
 McKenzie, D., and Peate Bickle M.J. (1988) The volume and composition of melt generated by extension of the lithosphere, J. Petrol., vol. 29 (3), p. 625-679.
 McKenzie, D.P. (1985) The extraction of magma from the crust and mantle: Earth Planetary Science Letters, v. 74, p. 81-91.
 Pitcher, W. S. (1993) The Nature and Origin of Granite. Second edition, Chapman and Hall, London.
 Wilson, M., and Guiraud R. (1998) Late Permian to Recent magmatic activity on the African-Arabian margin of Tethys, in D. S. Macgregor, R. T. J. Moody, and D. D. Clark-Lowes, (eds.)
 Sandford, K.S. (1935) Geological observations on the north-west frontiers of the Anglo-Egyptian Sudan and the adjoining part of the southern Libyan desert. Quart. Journ. Geol. Soc. London, vol. 91, p. 323-381.
 Schurmann, H.M.E. (1974) The Pre-Cambrian in North Africa. Netherlands. Brill, Leyden.
 Cahen, L., Snelling, N.J., Delhal, J. and Vail, J.R. (1984) North-East Africa and Arabia. In: The geochronology and evolution of Africa. Clarendon Press, Oxford, chap. 14, p. 254-269.
 Morgan, M.A., Grocott, J. and Moody, R.T.J. (1998) The structural Baudet, D. (1988) Precambrian palynomorphs from northeast Libya. In: Subsurface palynostratigraphy of northeast Libya, (eds.) A. El-Arnauti, B. Owens and B. Thusu). Research Centre, Garyounis University, Benghazi, p. 17-26.
 Oun, K.M., Liegeois, J.P. and Daly, S. (2000). Evolution of the Pan-African Jabal al Hasawnah granites (abstract only). Second Symposium on the Sedimentary Basins of Libya, Geology of Northwest Libya. Book of abstracts, p. 71.
 Baudet, D. (1988) Precambrian palynomorphs from northeast Libya. In: Subsurface palynostratigraphy of northeast Libya, (eds.) A. El-Arnauti, B. Owens and B. Thusu). Research Centre, Garyounis University, Benghazi, p. 17-26.
 Banerjee, S. (1980) Stratigraphic Lexicon of Libya. Bulletin No. 13. Industrial Research Centre, Tripoli, p300.
 Van Houten, F.B. (1983) Sirt Basin, north central Libya; Cretaceous rifting above a fixed mantle hotspot, Geology, vol. 11, p. 115-118.
 Hallett, D. (2002) Petroleum Geology of Libya, Amsterdam: Elsevier.
 Gumati, Y.D., (1985) Crustal extension, subsidence, and thermal history of the Sirte Basin, Libya. ESRI Occasional publication No.3. Columbia, S. Carolina, 207p
 Polteau, S., Mazzini, A., Galland, O., and Planke S. (2007a), Saucer-shaped intrusions: Occurrences, emplacement and implications, Physics of Geological Processes, University of Oslo, Oslo, Norway.
 Dercourt, J., Zonenhain, L.P., Ricou, L.E. et al. (1986) Geological evolution of the Tethys belt from the Atlantic to the Pamirs since the Lias. Tectonophysics, vol. 123: p. 241-315.