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Paper Type | : | Research Paper |
Title | : | Delineation of Ground Water Potential zones through Electrical Resitivity Parameters in hard rock terrain , Osmania University Campus, Hyderabad, Telangana State, India. |
Country | : | India |
Authors | : | Dubba Vijay Kumar || G.Ramadass || S.V.Jagadish |
Abstract: This study motivated to determine electrical resistivity parameters of Osmania University campus area which is underlain by granitiec terrain. A total 103 Vertical Electrical Soundings were conducted with maximum electrode spacing of 150m, the results reveals four subsurface geo-electrical layers, the top soil layer of variable resisitivity value between 11.2 Ωm to 599 Ωm whose maximum thickness is 0.75 m to 8.46 m. The highly weathered second layer resistivity value varing from 1.72 Ωm to 1800 Ωm, thickness is 0.12 m to 36.6m. The third fractured layer indicated by resistivity value of 16.3 to 460 Ωm 74Ωm and thickness is 4.9 m to 87.4 m.
[1] Udayalaxmi G and Ramadass G, 2009. VES approach for delineating contaminated groundwater zones in Osmania University and Surrounding areas of Greater Hyderabad, A.P., India. Gondwana Geological Magazine, Nagpur. Vol.24 (1), pp.11-18.
[2] Patangay N.S., Ramaprasada Rao I.B., Venkata Chary M., Ram Raj Mathur and Shiva Keshavulu A., Srinivas S.R.P., 2002.Application of Geophysical techniques to trace groundwater pollution due to industrial effluents in the hard rock terrain.Jour. of Geophysics, Vol. XXIII, No.1, pp.9-12.
[3] Ebrahim.Am, Hamburger,M.V,Bayless,E.R and Krothe,N.C.1990. A study of acid mine drainage using earth resistivity measurements,Groundwater,Vol.28.No.3.pp 361-368.
[4] De Lima. O.A.L., Sato, H.K., and Porsani, M.J., 1995. Imaging industrial contaminant plumes with resistivity techniques-jour. App. Geophy. Vol 34, No.2.pp 93-108
[5] Hansen,B.P.&Lane,J.W 1996. Orientation and characteristics of Fractures in crystalline Bed rock determined by surface and borehole geophysical surveys,Millville and Uxbridge, Masssachusetts SAGEEP1996. Conference Environ, Eng.Geophysic. Soc. Proceedings,927-940
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Paper Type | : | Research Paper |
Title | : | An Integrated Study of Gravity and Magnetic Data to Determine Subsurface Structure and Depth to Basement in Alamein Area, Western Desert, Egypt. |
Country | : | Egypt |
Authors | : | Ismail S. Ismail || Saada A. Saada || Youssef M.Y. Ali || Youssef M.Y. Ibrahem |
Abstract: Abstract:The present study wascarried out to delineate the location, extension, trend and depth of subsurface structures of Alamein area. To achieve this aim, the gravity and aeromagnetic data have been subjected to different analytical techniques. The Fast Fourier Transform technique was used to separatethe residual components from the regional ones. The resulted maps showed that the area was affected mainly bytheENE, E-W, WNWand NWtectonic trends. In addition, spectral analysis technique was applied on magnetic anomalies to estimate the depth to basement surface, which varies from 3.03 in southern part to 7.24 Km in northern part.3D-Eulerdeconvloution and tilt angle derivative techniques were carried out to detect the edges of magnetic sources and to determine their depths.Correlation between them shows acoincidence between Euler solution and zero lines of tilt angle map.
[1] G. Hantar. North Western Desert. In R. Said, ed., The Geology of Egypt. (Rotterdam, Netherlands, A. A. Balkema Publishers, 1990), 293-319.
[2] W.M. Meshref. Well evaluation conference of Egypt. Schlumberger Technical Editing Services, EGPC, Egypt, 1995, 87 p.
[3] A.W. Wescot,A. Mahmoud, C.B. David, M.C. Roger, T.G. Steven, A.M. David, W.H. Walter, D.W. Amanda, C.D. John and S. Adel. Jurassic Rift Architecture in the Northeastern Western Desert, Egypt. Adapted from poster presentation at AAPG International Conference and Exhibition, Milan, Italy, October 23-26, 2011.
[4] C. Fichler, E. Rundhovde, O. Olesen, B.M. Sæther, H. Rueslatten, E. Lundin and A.G. Dore.Regional tectonic interpretation of image enhanced gravity and magnetic data covering the mid-Norwegian shelf and adjacent mainland. Tectonophysics 306, 1990, 183–197.
[5] S.D. Khan, M.S. Fathy andA. Maha. Remote sensing and geophysical investigations of Moghra Lake in the Qattara Depression, Western Desert, Egypt. Journal. Geomorphology, 207, 2011, 10–22.
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Paper Type | : | Research Paper |
Title | : | 2D-Euler Deconvolution technique and Electrical Self-Potential analysis for subsurface structures delineation in Matuu, Machakos County, Kenya |
Country | : | Kenya |
Authors | : | Odero E.O. || K'Orowe M. O. || Githiri J. G. |
Abstract: In order to evaluate groundwater potential of Matuu-Kilango area faults and fractures which are groundwater conduits had to be delineated. Earlier use of geological reconnaissance report only in siting boreholes has led to recorded cases of borehole failure in Matuu. Integrated geophysical survey involving magnetics and electrical self-potential techniques was applied over a 25 square kilometre area. Qualitative interpretation involving generation of contour maps for magnetic anomaly as well as self-potentials was attempted. Euler Deconvolution solutions were obtained using a structural index of 0.5 that gave well clustered solutions and discontinuities over the anomalous zone.
[1] E. Mathu, The Mutito faults in the Pan-African Mozambique Belt, Eastern Kenya, In Mason R. (Ed.), Basement Tectonics, (Netherlands, Kluwer Academics Publishers, 1992) 61-69.
[2] C. Nyamai, E. Mathu, N. Opiyo-Akech and E. Wallbrecher, A reappraisal of the geology, geochemistry, structures and tectonics of the Mozambique Belt in Kenya: East of the Rift system. African Journal of Science and Technology, Science and Engineering series, 4(2), 2003, 51-71.
[3] P. Mosley, Geological Evolution of the Late Proterozoic Mozambique Belt of Kenya, Tectonophys, 221, 1993, 223-250.
[4] J. Reynolds, An Introduction to Applied and Environmental Geophysics (New York, John Wiley& Sons, 1998).
[5] P. Keary, M. Brooks and I. Hill, An Introduction to Geophysical Exploration. (London, Blackwell Scientific Publications, 2002).
[6] V. Grauch, R. Hudson, A. Minor and J. Caine, Sources of along-strike variation in magnetic anomalies related to intrasedimentary faults: A case study from the Rio Grande Rift, USA. Exploration Geophysics, 37, 2006, 372-378.
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Paper Type | : | Research Paper |
Title | : | The study of sequence stratigraphy and sedimentary system in Muglad Basin |
Country | : | China |
Authors | : | Jingyao Wang |
Abstract: Application of sequence stratigraphy theory, by levels of base level cycle sequence feature analysis, combined with core and log data, establish the sequence stratigraphic framework. The Cretaceous sedimentary strata are divided into six two sequences and 14 third-order sequences. In sequence stratigraphy based, combine well logging, seismic and core observation, and comprehensive analysis of each well rock type, color, bedding and other construction phase marks. Identify the Cretaceous strata have delta, meandering fluvial facies and braided river with three main facies. Detailed study of Cretaceous sedimentary characteristics, identify each sedimentary microfacies, sedimentary facies sequence established in the region.
Keywords: Sequence Stratigraphy Stratigraphic framework Deposition System, Sedimentary microfacies
[1] Denny J K, Wang J, Cross T A, et al. PISEMA powder patterns and PISA wheels[J]. Journal of Magnetic Resonance. 2001, 152(2): 217-226.
[2] Yi M, Cross T A, Zhou H. A secondary gate as a mechanism for inhibition of the M2 proton channel by amantadine[J]. The Journal of Physical Chemistry B. 2008, 112(27): 7977-7979.
[3] Ketchem R R, Hu W, Cross T A. High-resolution conformation of gramicidin A in a lipid bilayer by solid-state NMR[J]. Science. 1993, 261(5127): 1457-1460.
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[5] Kovacs F A, Cross T A. Transmembrane four-helix bundle of influenza A M2 protein channel: structural implications from helix tilt and orientation.[J]. Biophysical journal. 1997, 73(5): 2511.
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Paper Type | : | Research Paper |
Title | : | Classification of fault systems and characteristics in Xujiaweizi depression |
Country | : | China |
Authors | : | Liulu || Yanchen Li || Meina Li |
Abstract: Xujiawezi depression experienced three evolution stages, which includes Huoshiling Formation, Shahezi Formation, Yingcheng Formation, during the fault depression period ,mainly developed five strike direction fault systems. Based on the fault systems directions characteristics, we can determine that the NNW trending Xuzhong-Xudong fault are the main strike-slip fault, the NNW, approximately SN, NW, NE and EW trending faults are the strike-slip associated secondary faults. The main strike slip fault styles, the relationships among associated structures are conformed to dextral shear deformation pattern. Keywords: Xujiaweizi depression, fault systems, fault characteristics, strike-slip
[1]. HU Ming, FU Guang. The Fault Activity Period and Its Relationship to Deep Gas Accumulation in the Xujiaweizi Depression, Songliao Basin[J], GEOLOGICAL REVIEW, 2010, 56(5): 710-718.
[2]. SYLVESTER, A. G. 1988. Strike-slip faults. Geological Society of America Bulletin, 100, 1666–1703.
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Paper Type | : | Research Paper |
Title | : | Geophysical Investigations of a Pavement Failure Along Akure-Ijare Road, Southwestern Nigeria |
Country | : | Nigeria |
Authors | : | O.O. Falowo || O.J. Akintorinwa |
Abstract: Geophysical investigations were carried out along two failed segments of Akure-Ijare road, named locality 1 and locality 2, with the aim of establishing the cause(s) of the incessant pavement failure along the road. The geophysical investigations involved the Very Low Frequency Electromagnetic (VLF-EM) and Electrical Resistivity Methods. The VLF-EM measurements were taken at intervals of 10 m along traverses parallel to road pavements. Two techniques were adopted for the electrical resistivity method namely: the vertical electrical sounding (VES) and a combination of horizontal profiling and sounding using dipole-dipole configuration with inter stations separation (a) of 5 m and an expansion factor (n) that varies from 1 to 5. The Schlumberger configuration was used for the VES with AB/2 varying from 1 to 65 m. Nine (9) and twelve (12) VES were carried out at localities 1 and 2 respectively.
[1]. Abam, T.K.S., Ofoegbu, C.O., Osadebe, C.C., and Gobo, A.E. 2000, Impact of hydrology on the Port-Harcourt-Patani-Warri road. Environmental Geology 4(2): 153-162.
[2]. Akintorinwa, O.J. and Adeusi, F.A. 2009, Integration of Geophysical and Geotechnical investigation for a proposed lecture room Complex at the Federal University of Technology, Akure, Southwestern, Nigeria. Ozean journal of Applied sciences 2(3), 2009 ISSN 1943-2429.
[3]. Alpin, L.M. 1966, The Theory of dipole sounding in Dipole methods for measuring earth conductivity: Conduit Bureau NT pg 1-60.
[4]. Anyanwu, A. 1990, Road construction and maintenance policy guidelines. Requirements for improving Nigeria Roads. Conf. pap. Transport Policy, Akure, pp. 13.
[5]. Dipro for window 2001. DiproTM version 4.0.1, Processing and Interpretation software for Electrical Resistivity data. KIGAM, Daejon, South Korea.
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Paper Type | : | Research Paper |
Title | : | Application of Remote Sensing Techniques for Change Detection in Land Use/ Land Cover of Ratnagiri District, Maharashtra |
Country | : | India |
Authors | : | Balu L. Rathod || Jagdish B. Sapkale |
Abstract:Remote sensing data and imageries have been used for the assessment and monitoring of land use
and land cover changes, so that available resources of any region may be used properly. In the coastal areas of
Maharashtra, catastrophic and human interventions are highly influencing on coastal resources. Now there is
an urgent need to use the sustainable resources by reducing the rate of degradation. The present study is an
attempt to analysis the change detection in the major aspects of land use and land cover in the Ratnagiri district
of Maharashtra. Satellite images of the years 1989, 1999 and 2009 have been obtained from Global Land Cover
Facility (GLCF) & NRSC and used for the analysis of periodic changes in LULC of Ratnagiri.
Keywords: LISS-III, LULC, GLCF, Change detection, Degradation,
[1] Anderson, James Richard. A land use and land cover classification system for use with remote sensor data. Vol. 964. US
Government Printing Office, 1976.
[2] Chen, X., Vierling, L., & Deering, D., A simple and effective radiometric correction method to improve landscape change detection
across sensors and across time. Remote Sensing of Environment, 98(1), 63-79, 2005.
[3] Jensen, J. R. (2005). Introductory digital image processing: A remote sensing perspective (3rd Edn). Upper Saddle River, NJ: Prentice-Hall , 2005.
[4] Lillesand, M. T., KIefer, W. R. and Chipman, N, J. (2008). : Remote sensing and image interpretation (6th ed). John Wiley and Sons, Inc, New York..
[5] Rathod, B.L, (2015) , " Coastal Resource Management Using Remote Sensing and GIS Techniques: A Case Study of Ratnagiri
District, Maharashtra, (2015), Unpublished Ph.D. Dissertation.
[6] Rathod, B. L., Sapkale, J.B., Status of Agriculture in Coastal Villages of Ratnagiri, Maharashtra.,. ,International Journal of Scientific and Engineering
Research, (IJSER), 6(9), 1556-1559 2015.
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Paper Type | : | Research Paper |
Title | : | Macro heterogeneity of high porosity and permeability reservoir- in Bozhong 25-1 oil field under section as an example |
Country | : | India |
Authors | : | Shizhong Ma || Heng Zhou |
Abstract: in order to improve the development effect of oilfield, in the Bohai Bay Basin Bozhong depression on the basis of sedimentary setting and tectonic background, sedimentary environment of, make use of the existing data of core, logging, seismic exploration and development and laboratory analysis, the storage layer, interlayer and plane heterogeneity, determine the reservoir types and characters, thus to study sedimentary reservoir characteristics have a more comprehensive and in-depth understanding, Bozhong depression depression Bozhong 25-1S oilfield geological fine anatomy, potential of oilfield provides solid geological basis.
Keywords: shallow water delta; sedimentary microfacies; interlayer; interlayer; reservoir heterogeneity
[1]. Quantitative description of characteristics of high-capacity channels in unconsolidated sandstone reservoirs using in situ production data[J]. Petroleum Science,2010,01:106-111.
[2] Wu Guanghui,Yang Haijun,Li Haowu,Sun Lixia. Controlling effects of the Ordovician carbonate pore structure on hydrocarbon reservoirs in the Tarim Basin, China[J]. Petroleum Science,2013,03:282-291.
[3] Deng Shaogui,Wang Yang,Hu Yunyun,Ge Xinmin,He Xuquan. Integrated petrophysical log characterization for tight carbonate reservoir effectiveness: A case study from the Longgang area, Sichuan Basin, China[J]. Petroleum Science,2013,03:336-346.
[4] Sun Liang,Zou Caineng,Liu Xiaoli,Zhu Rukai,Wang Xiaoqi. A static resistance model and the discontinuous pattern of hydrocarbon accumulation in tight oil reservoirs[J]. Petroleum Science,2014,04:469-480.
[5] Jan Einar Ringas. Reservoir Stochastic Modeling Constrained by Quantitative Geological Conceptual Patterns[J]. Petroleum Science,2006,01:27-33.
[6]. Geological Model of Member 3 of Shahejie Formation Reservoir in Liuzan Oilfield, Eastern Hebei Province[J]. Petroleum Science,2006,02:28-33.
[7] Sam Zandong Sun. Fractured reservoir modeling by discrete fracture network and seismic modeling in the Tarim Basin,China[J]. Petroleum Science,2011,04:433-445.