Version-2 (Jan-Feb-2017)
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Abstract: A hydrogeological study of any area is essential to know about the ground water condition, ground water resource , ground water quality and it is also essential to find out the suitable area for ground water recharge, discharge and ground water development. Durg blocks comes under the Durg district which is located almost in the central part of the Chhattisgarh state. Durg block falls between Latitude 21° 02' 00" N and 21°22' 00" N and Longitude "81°08' 00" E and 81° 28' 00" E and most of the area covered in toposheet no. 64G/8. Its Covering an area of 675.17 sq.km. Geologically.........
Keywords: Water level fluctuation, water level trend, depth to water level, water resources, pre-monsoon, post –monsoon.
[1]. Central ground water board (C.G.W.B), Report, Durg Brochure, 2013.
[2]. District Resource Map (2003), District Durg, Chhattisgarh
[3]. District statistical booklet 2013-14), District Durg, Chhattisgarh
[4]. Ground water resources and development potential of durg district, Chhattisgarh report 2011, Central ground water board.
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Abstract: The lithosphere-asthenosphere system has been represented by multi-layered model consisting of two parallel layers, the first one is elastic and the second one is viscoelastic, overlying a viscoelastic half-space and they are assumed to be in welded contact. A vertical buried strike-slip fault is taken to be situated in the viscoelastic layer. The fault undergoes a sudden slip under the action of tectonic forces such as mantle convection. Analytical expressions for displacements, stresses and strains are calculated for both layers and half-space by using modified Green's function technique and correspondence principle. Numerical computations have been carried out to find the effect of fault movement in change of surface shear stress. The contour map for the stress pattern in both of the first layer and second layer have been prepared.
Keywords: Lithosphere-asthenosphere system, aseismic state, strike-slip fault, mantle-convection, sudden movement, Green's function, correspondence principle, Maxwell type.
[1]. K. Rybicki. "The elastic residual field of a very long strike-slip fault in the presence of a discontinuity". Bull. Seis. Soc. Am., 61, 79-92, 1971.
[2]. K. Rybicki. "Static deformation of a multilayered half-space by a very long strike-slip fault", Pure and Applied Geophysics, 110, p-1955-1966, 1973.
[3]. A. Mukhopadhyay et.al. "On two interacting creeping vertical surface breaking strike-slip fault in the lithosphere,". Bull. Soc. Earthq. Tech., vol. 21, pp. 163-19, 1984, . (with P. Mukherjee).
[4]. A. Mukhopadhyay et al. "On two Aseismically creeping and interacting buried vertical strike-slip faults in the lithosphere". Bull. Soc. Earthquake Tech., vol.23, pp. 91, 1986.
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Abstract: The Shoushan Basin is an important hydrocarbon province in the northern Western Desert, Egypt. The present study deals with petrophysical evaluation, the identification of the potential and generating capability of hydrocarbon generation of Jurassic and Cretaceous formations in Shoushan Basin were investigated by studying the composite logs for five wells. Jurassic units include; Ras Qattara, Khatatba and Masajid formations. Jurassic formations are not recorded in the investigated wells except at TUT-21 well. Cretaceous units are represented by Alam El Bueib, Kharita and Abu Roash formations. The Alam El-Bueib Formation can be considered as an important reservoir rock in the Shoushan Basin..........
Keywords: Petrophysical Evaluation, hydrocarbon Generation, Source rock, Shoushan Basin, Western Desert
[1]. El Ayouty, M.K., 1990. Petroleum geology. In: Said, R. (Ed.), The Geology of Egypt. A.A. Balkema, Rotterdam, pp. 567–599.
[2]. Alsharhan, A.S., Abd El-Gawad, E.A., 2008. Geochemical characterization of potential Jurassic/Cretaceous source rocks in the Shushan Basin, north Western Desert, Egypt. J. Pet. Geol. 31:191–212.
[3]. Dahi, M., and Shahin, A.N., 1992. Paleozoic rocks distribution and hydrocarbon potential in the Western Desert, Egypt. Paper presented at the 11th Petroleum Exploration and Development Conference, Cairo.
[4]. Khaled, K.A., 1999. Cretaceous source rocks at Abu Gharadig oil and gas field, north Western Desert, Egypt. J. Pet. Geol. 22:377–395
[5]. Sharaf, L.M., 2003. Source rock evaluation and geochemistry of condensates and natural gases, offshore Nile Delta, Egypt. J. Pet. Geol 26:189–209
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Abstract: Mahabunagar District falls in rain shadow zone with a low annual normal rainfall of 604 mm. The recurrence of drought is increasing considerably and unless collective measures are initiated on a permanent basis the situation will become grim in future. Gokaphasalwada watershed in Mahabubnagar District is selected to demonstrate the capability of high resolution satellite data in ground water mapping at village level. This watershed is located in Survey of India toposheet Nos. 56H/9 NW. This watershed with an area of about 57 sq.km is underlined by granite gneiss and migmatite traversed by dolerite dykes..........
[1]. Bhagavan, S.V.B.K and Raghu, V. (2000). "Integrated Remote Sensing based Study of National Watershed Development Project for Rained Area in A.P". Abstract Volume of National Symposium on Remote Sensing for Natural Resources with Special Emphasis on Watershed Management, Bhubaneswar, and pp.15.
[2]. Central Research Institute for Dry land Agriculture, (1990). Field Manual on Watershed management, CRIDA, Hyderabad.
[3]. Department of Space/ ISRO (1988). Manual for Hydrogeomorphological mapping for drinking water mission.
[4]. NRSA (National Remote Sensing Agency) 2008. Ground Water Prospects Mapping Using Remote Sensing and Geographic Information System, Rajiv Gandhi National Drinking Water Mission Project, Manual,256p.
[5]. 18. Sankar, K. (2002), Evaluation of Ground water potential zones using Remote Sensing Data in Upper Vaigai River basin, Tamilnadu, India. J. Indian Soc. Remote Sensing, 30(3), pp 119-128.
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Abstract: Aeromagnetic data over Wase and its adjoining areas were obtained and analyzed for delineation and analysis of magnetic (subsurface) and surface lineaments which often act as hosts or structural control on mineralization in basement areas. The magnetic lineaments were inferred from the colour shaded map of the first vertical gradient of the residual magnetic field. Lineament contour maps of the magnetic and surface lineaments showed correlation between the areas of highest lineaments density with the exposed basement areas and low lineament density with the sedimentary parts of the area...........
Keywords: First vertical derivative, lineament density, lineament length density, rose diagram, first Fourier transform.
[1]. Carter, J. D., Barber, W. and Tait, E. A. (1963). The geology of parts of Adamawa, Bauchi and Borno Provinces in Northern
Nigeria. Bulletin of Geological Survey of Nigeria. 30.
[2]. Jacobson, R. R. E., Macleod, M. W. and Black, R. (1958). Ring complexes of younger granite province of northern Nigeria.
Geological Survey of London Memoir, 172.
[3]. Oyawoye, M. O. (1964). The geology of the Nigerian basement complex. Journal of Mining and Geology and MetallurgicalSociety.
1(2); 87-103.
[4]. Ajakaiye, D. E. (1974). Gravity survey over the Nigerian younger granite province. In C. A. Kogbe(Ed); Geology of Nigeria:(287-
294. Elizabethan Publishing Company Lagos.
[5]. Hunt, G. R., Salisbury, J. W. and Len Hoff, C. J. (1974). Visible and near infrared spectra of minerals and rocks. Modern Geology,
5: 15-22.
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Paper Type | : | Research Paper |
Title | : | Analysis of Soil Transfer Function in Izmir Metropolitan Area, Turkey |
Country | : | Turkey |
Authors | : | Caglar Ozer |
: | 10.9790/0990-0501026370 |
Abstract: The soil transfer function of Izmir, one of the most seismically active regions in Turkey has been determined by using IzmirNET strong motion stations. We conducted Standard Spectral Ratio (SSR) method using five well-spread earthquakes S- wave recording. These events have been selected with respect to azimuthal distribution for each and after that their spectrums were calculated considering some data processing condition. These stations spectrums have been divided by the reference station amplification which was selected as YMN and afterwards, standard spectral ratio of chosen earthquakes was shown as chart for each station.........
Keywords: Engineering Seismology, IzmirNET, Site effect, Standard spectral ratio
[1]. E. Gök and O. Polat, Strong-Ground Motion Earthquake Station Network of Izmir : IzmirNET, Süleyman Demirel Üniversitesi, Fen Bilimleri Enstitüsü Dergisi.;15(3), 2011, 233–243.
[2]. O. Polat, U. Ceken, T. Uran, E. Gok, N. Yilmaz, M. Beyhan, N. Koc, B. Arslan, D. Yilmaz and M. Utku, IzmirNet: A strong-motion Network in Metropolitan Izmir, Western Anatolia, Turkey. Seismological Research Letters, 80(5), 2009, 831-838.
[3]. B. Uzel, H. Sözbilir and C. Ozkaymak, Neotectonic Evolution of an Actively Growing Superimposed Basin in Western Anatolia: The Inner Bay of İzmir,Turkey. Turkish Journal of Earth Sciences, 21, 2012, 439-471.
[4]. H. Sozbilir, B. Sari, B. Uzel, O. Sümer and S. Akkiraz, Tectonic implications of transtensional supradetachment basin development in an extension-parallel transfer zone: The Kocaçay Basin, western Anatolia, Turkey, Basin Research.;23(4), 2011, 423–48.
[5]. E. Gok, M. Kececioglu, U. Ceken and O, Polat, Estimation of Soil Transfer Functions of Izmirnet, DEU Mühendislik Fakultesi Muhendislik Bilimleri Dergisi, 14(41), 2012, 1–11.
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Abstract: The geoelectric survey have been done to identify the potential of rock as a groundwater aquifer at Tanjung Kuba district Air Putih Batu Bara regency. The geoeletric measurements have been done at three points of vertical electrical sounding (VES) by using Sclumberger configuration with 150 to 200 meter of current electrode spacing (AB/2) and 0,5 to 10 meter of potential electrode spacing (MN/2). Interpretation of the resistivity value resulted that cover layer has resistivity value of 140 to 232 ohm-meter (Ω/m)...........
Keywords: Geoelectric resistivity, aquifer
[1]. Azhar dan Gunawan Handayani, 2004. Penerapan Metode Geolistrik Konfigurasi Schlumberger untuk Penentuan Tahanan Jenis Batubara. Bandung
[2]. David Keith Todd, 1980, Groundwater Hydrology, Toppan Company, Dobrin M.B,1967,Introduction to Geophysical Prospecting, Mc Graw Hill, New York
[3]. Fetter,1990. Applied Hydrogeology, University of Wisconsin, United States of America Fitch A. A,1981 Development in Geophysical Exploration Methods, Applied Science Publisher
[4]. Heru Hendrayana, 1994, Pemodelan Airtanah, Gadjah Mada Univiversity Press, Yogyakarta Loke, M.H.2014., Tutorial 2-D & 3-D Electrical Imaging Surveys, http//www.geolectrical.com Nostrand. 1966. Interpretation of Resistivity Data. Washington: Geological Survey.
[5]. Siddalingamurthy,S., Nagaraju,D dan Balasuraramanian, A.,2014., Studies of Groundwater exploration In Chamaranjagar Taluk, Using Electrical Resistivity Tehniquies, International journal of Geology,Earth & Environmental Sciences, pp 123-137
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Abstract: Gender imbalance in different sectors is one of the current critical issues that requires immediate intervention and empowerment of females in decision making and implementation of affirmative action to correct it. The main objective of this study is to examine development and gender socialization mainstreaming issues at higher education. This study is a case study research designs undertaken using quantitative and qualitative methods, in which the university community (staff and students of both sexes) participated. The results of this study indicated that university related issues such as rules and regulations...........
Keywords: Development, gender, higher education, mainstream, practices, socialization.
[1]. Alebachew Adem. (2001). Gender, Development and Migration Linkages in Ethiopia: Ethiopian Development
[2]. Forum vol. 2, No. 3, Institute of Development Research, A.A.U
[3]. Anderson,M & Margaret, L.( 2003) "The social construction of gender." In Thinking about Women: Sociological Perspectives on Sex and Gender.Edited by Margaret L. Anderson. New York: Allyn & Bacon, pp. 21–54.
[4]. Aizer, A., (2010). The Gender Wage Gap and Domestic Violence. American Economic Review100(4),1847-59
[5]. Burke,J& Peter J.(2002) "Marital socialization, gender, and identity change." Paper presented at The Pacific Sociological Association, Vancouver, BC, Canada.