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Abstract: The acquired high-resolution airborne total magnetic intensity data over the West-of-Edfu region, within the southern Egyptian western desert, were consistently and extensively inverted in terms of two- and three-dimensional (2D/3D) magnetic susceptibility layered-earth models to accurately delineate the deep-seated basement structures and configuration. The starting models for all inversion trails were initially built-up using a-priori information gained from the progressive standard qualitative and semiqualitative interpretation results.........
Keywords:Two- and three-dimensional magnetic susceptibility layered-earth models, deep-sated basement structures, West-of-Edfu region, Upper Egypt.
[5]. Bhattacharyya, B.KK., 1965.Twwo-dimennsionall harmonic analysis as a tool for magneticm interppretation. Geophysics,30, 829–857.
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Abstract: Geoelectrical sounding to determine the groundwater prospect in Awgu and its environs has been carried out. The study area lies within longitudes 007025'E and 0070 35'E and latitudes 06002'N and 06017'N with an area extent of 513sqkm. The area is underlain by two lithostratigraphic units, Awgu Shale and Owelli Sandstone. A total of ninety five (95) Vertical Electrical Soundings (VES) was acquired employing the Schlumberger electrode array configuration, with a maximum electrode separation ranging from 700m to 800m. Data analysis was done using a computer program RESOUND to generate the layer apparent resistivity, thickness and depth. A maximum of eight (8) layer resistivity were generated in each sounding point with a depth range of 50m to 356m...........
Keywords: Geoelectric sounding, transverse resistance, Longitudinal Conductance, Groundwater Potential zones, Groundwater flow directions.
[1]. A. R. ZohdyApplication of surface geophysical (electrical methods to groundwater Investigations) techniques of water resources investigations of the United States Geological Survey. , (1976). 5-55.
[2]. A.C. Okonkwo , C. C. Ezeh , A.I, Opara., R.A.N. Nwatarali, M.S. Dimanyi, and E. Enang,
[3]. Using the Dar- Zarrouk Concept to Infer the Subsurface Lithological Extent of Agbani Sandstone, Enugu State,Nigeria. International Research Journal of Geology and Mining (IRJGM) (2276-6618) Vol. 4(1) (2014) pp. 29-36,
[4]. C. Aneke, Water Resources of the Awgu Shale group, Enugu state, southeastern Nigeria. Unpub1. Ph.D Thesis, University of Nigeria, Nsukka. (2007).
[5]. C. Ezeh, Hydrogeophysical studies for the Delineation of potential Groundwater zones In Enugu State, Nigeria. Int. Res. J. Geol. Min. (2012). 2(5):103- 112.
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Abstract: A great number of studies on the relationship between solar activity and various terrestrial phenomena, both in the climatic and geophysical fields, have been carried out over several decades. In the present work we analyse the shorter oscillations of the solar activity such as the ones recognized in the climatic and oceanographic oscillations, for which, as it is known, longer series of observations are unavailable. Specially we analyse both the sunspot series (Wolf relative number series) considered an index of solar activity and observed since 1700 and the series of the mean sea level variation of the longest ones available in the word and relative to three oceanographic stations in Poland (Swinoujscie)...........
Keywords: Solar activity, sunspot series, spectral analyses.
[1]. F. Mosetti. – On temporary fluctuations of some natural phenomena, Boll. Geof. Teor. Appl., VIII (29), 1966, 62-76.
[2]. F. Mosetti – Natural and geophysical fluctuations. The meaning and their detection, O.G.S. Silver Ann., Oss. Geof. Sper. Ed.,
Trieste, 1984, 11-15.
[3]. S. Fais, F. Mosetti – On periodicities in the sunspot series, Boll. Geof. Teor. Appl., XXXI (123-124), 1989, 315-320.
[4]. J.W. Cooley, J.W. Tukey– An algorithm for the machine calculation of complex Fourier series, Math. Computation, 19, 1965, 297-
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[5]. S.L. Marple – Digital spectral analysis with applications (Prentice-Hall, 1987).
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Abstract: The Municipal Center for Art and Culture Exmà is an excellent result of the transformation of a mono-functional structure (the old abattoir of Cagliari) into a polyfunctional pole dedicated to art that has hosted major events since nineties. In order to monitor the conservation state of the building materials of this monument, mostly carbonate rocks, non-destructive ultrasonic analyses have been carried out since 2007. Ultrasonic data have been related to the physical and mineralogical-petrographic features of the investigated building materials, in order to correlate the elastic properties with their intrinsic ones...........
Keywords: Degradation monitoring, monumental structures; refraction techniques, restoration effectiveness, ultrasonic velocity.
[1]. M. Montoto, L. Calleja, B. Perez Garcia, L.M. Suarez Del Rio, V.G. Ruiz De Argandoña, R.M. Esbert, C.M. Grossi, Non-destructive ultrasonic procedure to evaluate in situ the relative deterioration of monumental stones: preliminary results, Proc. of Science, Technology and European Cultural Heritage, Bologna, Italy, 1991, 545-548.
[2]. S. Abbaneo, M. Berra, L. Binda and A. Fatticcioni, Non-destructive evaluation of bricks-masonry structures: Calibration of sonic wave propagation procedures, in: Schickert G. & Wiggenhauser H. (Eds). Proc.of the International Symposium Non-Destructive Testing in Civil Engineering (NDT-CE), Berlin, Deutsche Gesellschaft fur Zerstorungsfreie Prufung (DGZfP), Berlin, 1, 1995, 253–260.
[3]. B. Christaras, Estimation of damage at the surface of stones using non-destructive techniques. Proc. of the 5th International Congress of Structural Studies, Repairs and Maintenance of Historical Buildings, San Sebastian. Advances in Architectural Series of Computational Mechanics Publications, 3, Southampton, 1997, 121–128.
[4]. B. Christaras, F. Cuccuru, S. Fais, H. Papanikolaou, Application of non destructive ultrasonic techniques for the analysis of the conservation status of building materials in monumental structures, in G. Lollino et al. (Eds.), Engineering geology for society and territory - Volume 8 preservation of cultural heritage, Springer International Publishing Switzerland, 2015, 139–143.
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Abstract: Bengkulu Province is a region located on the a subduction zone in the West coast of Sumatra. It's a highly prone and risk of earthquakes. One of the important effects of earthquakes is Peak Ground Acceleration (PGA). This value is needed to determine the strength of the foundation of the building to be constructed. This article presents comparisons among the three PGA models in Bengkulu province, Indonesia. Research on the three models of PGA in the first generation, namely; Esteva, Pathwardan and Crouse have been tested and compared on the Bengkulu area based on historical data of earthquakes with magnitude, M ≥ 4 SR and hypocenter, H ≤ 100 km that occurred in 1974 - 2014............
Keywords: Crouse Model, Esteva Model, Hypocentre, Pathwardan Model, Peak Ground Acceleration.
[1] Prawirodikromo, W, Seismologi Teknik dan Rekayasa Kegempaan (Pustaka Pelajar, Yogjakarta, 2012).
[2] Wald, David, Quitoriano, J V, and Heaton, TH, Relationships Between Peak Ground Acceleration, Peak Ground Velocity, and
Modified Meercalli Intensity in California, Earthquake Spectra, 15(3), 1999, 557 – 564.
[3] Sung, Kun-Sung, Attenuation Relationships of Peak Ground Acceleration and Velocity for Crustal Earthquakes in Taiwan, Bulletin
of the Seismological Society of America, 95(3), 2005, 1045-1058.
[4] Tselentis, G-Akis and Danciu, L, Empirical Relationships Between Modified Mercalli Intensity and Engineering Ground –Motion
Parameters in Greece, Bulletin of the Seismological Society of America, 98(4) 2008, 1863-1875.
[5] Pailoplee, S, Relationship between Modified Mercalli Intensity and peak ground acceleration in Myanmar, Natural Science, 4 ,
2012, 624-630.
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Paper Type | : | Research Paper |
Title | : | Review of the Basement Geology and Mineral Belts of Nigeria |
Country | : | Nigeria |
Authors | : | I.V. Haruna |
: | 10.9790/0990-0501013745 |
Abstract: The mineral belts of Nigeria include both Pan African structures (N-S, NNE-SSW, ENE-WSW), well preserved in the Western Province of the Nigeria basement complex and the Mesozoic to Early Cenozoic structures (NE-SW and ENE-WSW), less well defined in the Eastern Province of the Nigeria basement. Analyses of these belts revealed that the stress pattern of the Nigerian landmass has changed appreciably from N-S and NNE-SSW trend to NE-SW and ENE-WSW trend over a period of time from Pan African to Early Cenozoic. These changes have led to the growth of intraplate tensional stresses...........
Keywords: Basement complex, Mineral belts, Nigeria, Uranium
[1]. A.C. Ajibade, W.R Fitches, and J.B. Wright, The Zungeru Mylonites, Nigeria: recognition of a major tectonic unit. Rev. De Geol. Phys. 21, 1979, 359-363.
[2]. A.C. Ajibade, and J.B. Wright, The Togo-Benin-Nigeria Shield: evidence of crustal aggregation in the Pan-African belt. Tectonophysics. 165, 1989,125-129.
[3]. E. Ball, An example of very consistent brittle deformation over a wide intercontinental area: The late Pan-African fracture system of the Taureg and Nigeria shield. Tectonophys. 61, 1980, 363-379.
[4]. M.E. Barley, B. Eisenlohr, D.I. Groves, C.S. Perring, and I.R. Vearncombe, Late Archean convergent margin tectonics and gold mineralisation. A new look at the Norsema-Wiluma belt, western Australia: Geology 17, 1989, 826-829.
[5]. C. Coulon, P. Vidal, C. Dupuy, P. Baudin, M. Popoff, H. Maluski, and D. Hermitte, The Mesozoic to Early Cenozoic magmatism of the Benue Trough (Nigeria); Geochemical evidence for the involvement of the St. Helena Plume. Journal of Petrology. 37, 1996, 1341-1358.
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Abstract: The proposed Siyan Gad small hydroelectric project is a run of the river scheme, on Siyan Gad River near Harsil in Uttarakashi district of Uttarakhand. The water will be diverted by a 6m high weir through a 2.72 km long power tunnel to a surface power house near Jhala village to produce 5 MW of electric power. The whole project is located within the rocks of Harsil Metamorphics of Vaikrita Group. This study includes detailed discussion and control measures for engineering geological problems likely to be encountered during construction or post construction period. The rocks at the project site are classified according to Rock Mass Rating (RMR) system and also by Q-system in order to predict rock load and support requirements.
Keywords: Siyan Gad small hydroelectric project, RMR, Q-system, in-situ stresses, remedial measures.
[1]. Barton, N., Lien, R., and Lunde, J.; (1974), Engineering Classification of Rock Masses for the Design of Tunnel Support; Rock
Mechanics, Springer-Verlag, vol.6; pp 189-236
[2]. Bieniaswksi, Z. T., (1989); Engineering Rock Mass Classification; John Willey & Sons. LTD., London; pp 30-90
[3]. Bagri, D. S., Lakshmanan, K., Anbalagan, R. and Bipin, P.(2016); Stability Evaluation Of Slopes Around Rim Of Reservoir of
Diversion Dam Of Vishnugad–Pipalkoti Hydroelectric Project, Garhwal Himalaya, India; International Journal of Current Research
Vol. 8, Issue, 11, pp.42565-42575, November, 2016
[4]. Singh, B., Goel, R. K.,(1999); Rock Mass Classification- A Practical Approach in Civil Engineering; Elsvier Science Ltd., Oxford;
pp 34-89
[5]. Jain, A.K., Singh, S., and Manickavasagam, R.M.(2002); Himalayan Collision Technocic; Gondwana research group, Memoir no.
7; pp 57-101
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Abstract: Where would be our knowledge about early history of earth without zircon? Zircon, tiny but timely are able to provide a picture of evolution of crust and mantle. Zircon due to its robust characteristic has been long recognized as a suitable candidate playing a key role in crustal evolution studies as a best geochronometers. Recent development in analytical techniques such as high precision mass spectrometry and verity of microscopic imaging methods permits investigation of complex grain at high spatial resolution. Coupled measurement of the isotopes of oxygen and hafnium provide insight into the crust differentiation and the processes involved in crustal evolution. Such information from zircon is an invaluable help to geochemist and other earthscientist to unravel even more complex geological system.
[1]. Amelin, Y., Lee, D.-C., Halliday, A.N., 2000. Early-middle Archaean crustal evolution deduced from Lu–Hf and U–Pb isotopic studies of single zircon grains. Geochim. Cosmochim. Acta 64, 4205–4225.
[2]. Geisler T, Schaltegger U, Tomaschek F (2007) Re-equilibration of zircon in aqueous fluids and melts. Elements 3: 43-50
[3]. Hawkesworth, C. J. & Kemp, A. I. S. (2006). Using hafnium and oxygen isotopes in zircons to unravel the record of crustal evolution. Chemical Geology 226, 144-162.
[4]. Hanchar JM, van Westrenen W (2007) Rare earth element behaviour in zircon–melt systems. Elements 3: 37-42.
[5]. Harley SL, Kelly NM, Möller A (2007) Zircon behaviour and the thermal histories of mountain chains. Elements 3: 25-30
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Abstract: Twelve representative marble samples were collected from Jakura and environs and tested for specific gravity, density, compressive strength, porosity, flexural strength, hardness water absorption, soundness or durability and Los Angeles Abrasion to ensure its suitability for use in the production of tiles. The flexural strength, hardness and compressive strength shows its high resistance to crushing and bending effects while the specific gravity and density values proves its ability to bear the impact of the objects that will be placed on it. The soundness and water absorption values makes them suitable for flooring and outdoor cladding due to its resistance to weathering and thawing because of its low rate of water absorption.
Keywords: Tiles, Compressive strength, Porosity, Flexural strength, Water absorption.
[1]. Oluyide, P.O. and Okunlola, O.A, (1995): Litho-structural Controls of the Precambrian Carbonate Mineralization in Burum-Takalafia Area, F.C.T. Abuja, Nigeria. Mining and Geosciences Society, 31st, annual conference, abstracts Vol.1 pp. 6 – 7.
[2]. Ako, T.A, Onoduku, U.S. and Abdulfatai, I.A. (2012): Economic evaluation of Burum Takalafia marble deposit, Federal Capital Territory Abuja. Research Journal of Science and IT Management Vol. 1(12) pp. 23-32.
[3]. Alabi, A.B, Olatunji, S. Babalola, O.A, Nwankwo, L.I, Johnson, L.M, Odutayo, J.O and Alabi, A (2013): Structural and qualitative analysis of solid minerals (marble) in selected location in Nigeria. Nigeria Journal of Physics Vol. 24. pp 68-76.
[4]. Elueze, A. (1993): Indications from Nigeria on the Industrialization and Employment.
[5]. Ofulume, A.B (1993): An Assessment of the Suitability of Jakura marble for use as flux in steel making. Journal of Mining and GeologyVol. 19(1) pp 1-9.
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Abstract: There has been varying conclusions on the rank of coal a Maiganga over the years. This paper examined the Maiganga coal with the aim of establishing its actual rank. Proximate analysis was undertaken on some samples from Maiganga coal mine. The analysis determined the percentage moisture content, volatile matter, fixed carbon, ash content, and calorific value. Although not directly relevant for the determination of the rank of coal, the total sulfur of the coals were evaluated also. The Maiganga A1 and Maiganga A2 samples were from the first seam. Maiganga B1 and Maiganga B2 were collected from seam two of the coal deposit............
Keywords: Proximate analysis, Maiganga, Coal, Lignite, Fixed Carbon
[1]. C.J. Varnell, J.V. Brahna, and K. Steele, The Influence of Coal Quality Variation on Utilization of Water from Abandoned Coal Mines as a Municipal Water Source, Mine Water and Environment, 23, 2004, 204-208.
[2]. T.K. Ghosh and M.A. Prelas, Coal, in T.K. Ghosh and M.A. Prelas, Energy Resources and Systems: Fundamentals and Non-Renewable Resources, 1(New York, Springer Science+Business Media B.V. 2009) 159-279.
[3]. B. Li, X. Zhuang, S. Zhao, Geological Controls on Coal Quality of the Yili Basin, Xinjiang, Northwest China, International Journal of Coal Geology, 131, 2014, 186-199.
[4]. F.B. Waanders, A. Govender, Mineral Associations in Coal and their Transformation during Gasification, Springer Science+Business Media B. V., 166, 2006, 67-691.
[5]. L.A. Amakin, Redox Conditions and the Transformation of Organic Matter in Coal, Coke and Chemistry, 51(4), 2008, 199-124.
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Abstract: Geological mapping of Kaltungo inlier was carried out, and a geological map of the area was produced. The area is dominantly underlain by porphyritic granites, coarse biotite granites and medium grained granites. Bima sandstone and some volcanic rocks mainly basalts intruding the sandstone have also been mapped. However, this work is essentially centralised on the granitic rocks. The samples of the granitic rocks were analysed in the field using hand lens and in the laboratory using a polarizing microscope...........
Keywords: Geologic mapping, Petrographic study, Granitic rocks, Kaltungo Inlier, Polarizing microscope.
[1]. Baba, S. (2009). Planning for Geological Fieldwork in a Semi-arid Zone. Proceedings of Field Mapping Standardization Workshop. Ibadan University Press. pp 65-77
[2]. Benkhelil, J., and Robineau, B. (1983). Fault Rocks of Kaltungo Lineament of North-eastern Nigeria and their Relationship with the Benue Trough Tectonics. Journal of the Geological Society. 143, 567-569
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[5]. Islam, M. R., and Baba S. (1988). A Report of Northern Part of Mandara Hills, Nigerian Journal of Borno. Vol. 1 No. 7. pp 99-105
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Abstract: July oilfield is a major normal fault–bounded structural block. It is a multi-reservoir oilfield located in the central part of the Gulf of Suez. July Member sandstone (Lower Rudeis) is the main reservoir and it was deposited during the Early Miocene (Burdigalian). July Member sandstone has been studied for the interpretation of its depositional environment on the basis of the four defining parameters of: facies; lithology, sedimentary structures, fossil contents and geometry. Petrographic studies of the cored intervals and ditch cuttings description of the four wells that were used in this study have revealed that July Member sandstone has the signatures of a shallow marine environment............
Keywords: Sedimentological Technique, Geophysical Technique, Depositional History, July Member, July Oilfield, Gulf of Suez and Egypt
[1]. Selly, R.C., Ancient sedimentary environments: Cornell University press, (3rd Ed.) 1984, pp. 7-26, 252-253 & 260-271.
[2]. Pivnic, D., M. Ramzy, B.L. Steer, J. Thorseth, Z. El Sisi, I. Gaafar, J.D. Garing, and Tucker, R.S., Episodic growth of normal faults as recorded by syntectonic sediments, July oil field, Suez rift, Egypt, AAPG Bulletin, v. 87, 2003, pp. 1015-1030.
[3]. ABD EL-GAWAD, M., The Gulf of Suez: a brief review of stratigraphy and structure: Phil. Trans. Roy. Soc. London A267: 1970, pp.41–48.
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[5]. Khalil, B.A., Geological and sedimentological studies of Oligo-Miocene section in Abu Zenima area and October Field. M.Sc. Thesis, Geology Department, Ain Shams University, Cairo. 1984, p.284.
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Abstract: Because the reservoir simulation models arising from real field may consist of hundreds of thousands or millions of grid blocks, traditional reservoir simulators can be quite time-consuming. This also led to computational cost of production optimization and history matching process of closed-loop reservoir management be greatly increased. Improving reservoir simulation speed is the urgent problem to be solved. In this paper, the proper orthogonal decomposition (POD) model order reduction method is applied in reservoir numerical simulation. First of all, in the training process, full order reservoir simulator is run to get snapshots and the POD base matrix is constructed..............
Keywords: Reservoir numerical simulation; fully implicit; model order reduction; proper orthogonal decomposition (POD); control system
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[5]. P. Sarma. Efficient Closed-Loop Optimal Control of Petroleum Reservoirs under Uncertainty. PhD thesis, Stanford University, 2006.