Stratigraphie Von Benue Trough 2021 // lmcgzc.com
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The Anambra Basin in the west of the lower region is more recent than the rest of the trough, being formed during a later period of compression, but is considered part of the formation. Rifting and sedimentation. The Benue Trough was formed by rifting of the central West African basement, beginning at the start of the Cretaceous period. Basin. The Benue Trough is conventionally subdivided into a “Lower Benue Trough”, “Abakaliki Trough” of Whiteman 1982, a “Middle Benue Trough” and an “Upper Benue Trough” “Benue valley” respectively of Whiteman 1982. The Benue Trough was terminated by a Late Santonian episode of compressional folding. CRETACEOUS OF THE BENUE TROUGH, NIGERIA PETTERS, S. W.: Paralic arenaceous foraminifera from the Upper Cretaceous of the Benue Trough, Nigeria. Acta Palaeont. Polonica 24,4, 451-471, December 1979. The spectrum of depositional environments represented in the Bfnue Trough. The Benue Trough of Nigeria Figure 1a is an intracontinental basin in Central West Africa that extends NE to SW. It is over km in length and exceeds. The Benue Trough is an elongate rifted depression in which the sediments reach well over m thickness in.

Benue Trough comprises of majorly states in the Central and North-eastern parts of Nigeria such as Bauchi, Benue, Gombe, Kogi, Nasarawa, Plateau and Taraba States etc. The Benue trough is divided into three regions in Nigeria, lower, middle and upper regions; hence, the upper region is further divided into the Gongola and Yola arms. A 'read' is counted each time someone views a publication summary such as the title, abstract, and list of authors, clicks on a figure, or views or downloads the full-text.

There are many sources of underground water in the Middle Benue Trough, which have varying composition and constituents. Water samples from saline springs, boreholes, hand-dug wells and rivers / streams from the Middle Benue Trough are collected and analysed for cations, anions and heavy metals, using atomic absorption spectrometry AAS; with. This is a file from the Wikimedia Commons. Information from its description page there is shown below. Commons is a freely licensed media file repository. the Central Benue Trough[30] perhaps caused by a com- pressional event In the Central Benue Trough, [31,32]. the regressive Awe and Keana Formations were depo- sited [33] while in the Northern Benue Trough; the tran- sitional Yolde Formation marked the Cenomanian [34]. The late Cenomanian to early Turonian was a period of. The geology of the Benue Trough, though better known than the geology of many other areas of Africa, cannot be said to be well known, as not much published information on the trough exists. The absence of detailed information on some aspects of the geology of the Benue Trough has inhibited would-be researchers on different aspects of the trough.

A review on the geology and petroleum potentials of the Nigerian Benue Trough and Anambra Basin is done to identify potential petroleum systems in the basins. The tectonic, stratigraphic and organic geochemical evaluations of these basins suggest the similarity with the contiguous basins of Chad and Niger Republics and Sudan, where commercial. of the Bima Sandstones in the Upper Benue Trough, and Awe/Arufu/ Uomba Formations in the middle Benue Trough. The Asu River Group is represented in the study area by the 500 m thick seam of Abakaliki shale, which occupies the core of the Abakaliki Anticlinorium and extends to Mamfe Embayment of the South Eastern Nigeria [19,20]. The Benue Trough originated from Early Cretaceous rifling of the central West African basement uplift. It forms a regional structure which is exposed from the northern frame of the Niger Delta and runs northeastwards for about lOOOkm to underneath Lake Chad, where it terminates. Regionally, the Benue Trough is part of an Early Cretaceous rift complex known as the West and Central African Rift System. The Abakaliki lead-zinc deposit in the lower Benue Trough Nigeria represents the largest of a series of fracture controlled base metal deposits within the Lower Cretaceous Albian Asu River Group shales. Field evidence, ore microscopy and electron microprobe analysis of the lodes, suggest that the vein mineralization commenced with pre-ore.

Literature review of the lower benue trough Breakthrough Physics: An attempt is therefore made to assemble a review of the known geology of the Benue Trough in general and for the Lower and Middle Benue Trough in particular, based on the few published papers and on oral discussions with geologists and geophysicists interested in the area. It is.

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