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Geochemical classifiion, petrogenetic association of
Jul 04, 2015 · Geochemical Classifiion, Petrogenetic Association of Magmatic Rocks in the Gboko Area and the TectonoMagmatic Influence on the Evolution of the (Gboko Area) Lower Benue Trough of Nigeria
Earth Sciences Research Journal Universidad Nacional De
Adeleye (1975a,b) viewed the Bida basin as a gently downwarped trough, whose genesis may be closely connected with southeastern Nigeria and the Benue valley's Santonian orogenic movements, while Whiteman (1982) has suggested that the basin was formed from simple cratonic sag.
Characterization and Classifiion of the Saline
Lower Benue Trough Awe, Azara, Ribi, Akiri and in the Kanje area in the Middle Benue Trough [19], [20]. II. Geology of the Study Area The Benue Trough of Nigeria is a linear NESW trending rift system whose development is closely associated with the separation of Africa from South America and the opening of the South Atlantic Ocean
Pattern of Geochemical and Sedimentological Variability of
This study presents the pattern of geochemical and sedimentological variability of the Albian to Cenomanian Upper Bima sandstone in Upper Benue Trough, NE Nigeria. The intent is to apply sedimentological investigations and major element concentrations of the upper Bima sediments (fine grained sandstones) in order
Lead Wikipedia
In Africa, lead mining and smelting were known in the Benue Trough and the lower Congo Basin, where lead was used for trade with Europeans, and as a currency by the 17th century, well before the scramble for Africa. Lead mining in the upper Mississippi River region in the United States in 1865.
Hydrocarbon prospectivity of Nigeria's inland basins: From
On a basinal evaluation level, incorporating source rock data from the other formations in the respective sectors, plots on the modified Van Krevelen diagram alongside biomarker and maceral data indie good to fair source rock qualities (oil and gas) in the Anambra basin and middle Benue trough and fair to poor source rock qualities (gaseous
Published in: AAPG Bulletin · 2004Authors: N G Obaje · H Wehner · G Scheeder · M B Abubakar · A JauroAffiliation: Nasarawa State University · Institute For Geosciences and Natural Resources · AbubaAbout: Cenomanian · Sterane · Maceral · Cretaceous · Sedimentary rock · Pyrolysis
Provenance and Paleoenvironmental Study of Bima Sandstone
Provenance and paleoenvironmental study of Bima sandstone of Upper Benue Trough was attempted using representative samples from two widely separated areas, and taking azimuth directions of cross beds, ripple marks and elongation of pebbles in the areas.
Evaluation and characterization of groundwater of the
Hydrochemical assessment of groundwater in the Lafia formation, Central Benue trough, Nigeria was carried out with the aim of determining its quality for domestic and irrigation purposes. Thirty groundwater samples from boreholes and handdug wells were analyzed using
Facies Associations and Successions in Amaseri Sandstones
the rose diagram constructed from the azimuths of the trough cross beds indie two directional modes, the The Benue Trough is a part of the extensive West and Central African Rift Systems
PALEOENVIRONMENTAL ANALYSIS OUTCROP IN
The Benue Trough of Nigeria is a deep linear sediments filled basin and it extends from the Niger Delta towards the NorthEast. It is subdivided into Upper, Middle and Lower Benue Trough. The Afikpo Basin lies in the SouthEastern part of the Lower Benue Trough. Hence, the Benue Trough
Journal of Sciences Geochemistry of the OgwashiAsaba
QFL provenance diagram plotted mainly in the recycled orogen field, these recycled sands may be sourced from associated platform at the southwestern edge of the Benue Trough in Nigeria (Figure 1). The proto Anambra Basin was a platform during Journal of Sciences Geochemistry of the OgwashiAsaba Formation, Anambra Basin, Nigeria
Original Research Article Petrographic Analysis and Total
Key word: Benue Trough, igneous rock, Intracratonic, graben basin, Early Cretaceous. Introduction The Benue Trough like most similar geological structures in different part of the world (e.g the Gulf of Suez) is known to be petroliferous. Thus by analogy, one would expect the Benue Trough to be prospective (Nwachukwu, 1985).
Pb In THE BENUE TROUGH AND CAMEROON LINE A
THE BENUE TROUGH AND CAMEROON LINEA MIGRATING RIFT SYSTEM IN WEST AFRICA PbIn dopes 80rytes de:x>s Brine springs J.G. FITTON Grant Institute of Geology, University of Edinburgh, Edinburgh (U.K.) Received May 22,1980 The remarkable similarity in shape between the Benue trough and the volcanic Cameroon line suggest that they Fernanda
Author: J. G. Fitton
Stratigraphic Report of the Middle Benue Trough, Nigeria
transgression into the Benue Trough and is probably the age equivalent of the marine slumps and turbidities that make up the Ekebeligwe Formation in the Lower Benue Trough. This transgression entered the Benue Trough from the newly opened Equatorial Atlantic Ocean and reached its peak towards the end of Middle Albian.
Provenance and Paleoenvironmental Study of Bima Sandstone
igneous and metamorphic origin. Rose diagrams of paleocurrent directions show predominance of 210o 240o trend in the eastern margin of Gongola Arm, and a predominance of the 300o 330o direction in the southern margin of Yola Arm of the Upper Benue Trough. Interpretation of the results revealed the crystalline basement of Adamawa, Cameroon
Alkaline Magmatism in the Lower Benue Trough, Southeastern
The Benue Trough is a continental rift related to the opening of the equatorial domain of South Atlantic, and was initiated in the late Jurassic and early Cretaceous times. The megastructure is filled with continental and marine sediments of up to 6,500 m in thickness.
A Study of the Middle Benue Trough (Nigeria) Based on
With an upbeat in petroleum exploration efforts in the Middle and Upper Benue Trough, emphasis is increasingly laid on the structural setting of the basin. This work reports the results of the analysis of aeromagnetic data over the Middle Benue Trough, Nigeria. It is well known that the expression
Earth Sciences Research Journal Universidad Nacional De
Since the southern part of the area lies on the sedimentbasement boundary (part of the Cretaceous Benue Trough's northern margin), the causative sources were considered to be deeperseated intrabasement basic intrusive rock bodies. The anomaly occurred in the NESW and EW trend following the Benue Trough's general trends.
WA5 UNITED STATES DEPARTMENT OF THE INTERIOR
Benue Trough. Although these particular deltas do not extend up the Benue depression, deltas of similar age may have been built in the lower reaches of the Bida Basin and Yola Trough and could contain coal deposits. During the Maestrichtian transgression, marine sedimentation reached the
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INTERNATIONAL JOURNAL OF SCIENTIFIC & TECHNOLOGY
of the Benue Trough. Results from the interpretations indie anomaly trends in the NESW, NWSE, EW, and NNESSW directions. The rose diagrams obtained from the magnetic residual map and the satellite imagery suggest predominantly NESW, NWSE directions, the consistency in the
Provenance and Paleoenvironmental Study of Bima Sandstone
igneous and metamorphic origin. Rose diagrams of paleocurrent directions show predominance of 210o 240o trend in the eastern margin of Gongola Arm, and a predominance of the 300o 330o direction in the southern margin of Yola Arm of the Upper Benue Trough. Interpretation of the results revealed the crystalline basement of Adamawa, Cameroon
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