Version-2 (Sep-Oct-2017)
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Abstract: The Manair River is an important tributary of river Godavari and forms part of Karimnagar district of Telangana State. The geomorphological studies have been carried out with a view to understand the impact of these parameters over the ground water occurrence in the area. The area is covered with hard rock's i.e., granites and granitic gneisses traversed by dykes and numerous veins of quartz, epidote and pegmatite. The morphometric analysis has been carried out in addition to the study of land forms. The structural features has strong bearing over the development of drainage pattern and it is mostly dendritic to sub-dendritic nature and the Manair river is designated as sixth order stream. The lower................
Keywords: Drainage Characteristics, Morphometric Analysis, Manair Basin, Karimnagar District
[1] Agarwal,C.S.(1998) Study of drainage pattern through aerial data in Nahagarh area of Varanasi District .U.P. Jour .Indian Soc. Remote Sensing V.26(4),pp.169-175.
[2] Das,A.K. and Mukharajee,S.(2005) Drainage morphometry using satellite data GIS in Raigad district. Maharastra.Jour.Geol. Soc. India , v.65.pp,.577-586
[3] Melton,M.A (1958a) A derivation of Strahlers "s Channel-ordering system, Jour., Geol,. V. 67,pp 345-346
[4] NAG,.S.K (1998) Morhometric Analysis using remote sensing techniques imn the Chuka, Sub-basin, Perulia district, West Bengal Jour,. Indian Remote Sensimg, v,.26(*1&2).pp., 69 -76
[5] Chow,V.T., 1964.Handbook of Applied hydrology.McGraw Hill Inc., U.S.A.
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Abstract: Radial derivatives is horizontal derivatives of gravity anomaly along radial directions from a point wich selected as a centre of gravity anomaly. The second radial derivatives is derivatives of radial deriatives or the twice treatment of radial derivatives. The Time Lapse micro-gravity also known as 4D microgravity has long been developed and applied for various purposes related to the dynamics change beneath the earth's surface. The principle of this method is a repeated and periodic measurement to determine the change in gravity value at that time interval as a result of the dynamics changes in the density distribution of the subsurface. Time lapse microgravity or 4D microgravity can be used for monitoring and identify gas injections in oil reservoirs. Mass density changes due to gas injection provide changes in the response of gravity values over time. This respons change over time allows us to identify the dynamics..............
Keywords: Radial derivatives, reservoir, gas injection
[1]. Telford, W.M., Geldart, L.P., Sherif, R.E., and Keys, D.A., 1990,Applied Geophysics, CambridgeUniversity Press, Cambridge.
[2]. Nabighian, M.N., Ander,M.E., Grauch, V.J.S.,Hansen, R.O., LaFehr, T.R., Li, Y., Pearson, W.C., Pierce, J.W., Phillips, J.D., and Ruder, M.E., 2005, 75th Anniversary: Historical development of the gravity method in exploration, Geophysics, Vol. 70 (6),. P 63ND-89ND.
[3]. Grand, F.S. and West, G.F., 1965,"Interpretation Theory injeksi Applied Geophysics", McGraw Hill Inc.
[4]. Reynolds, J.M., 1997, "An introduction to applied and environmental geophysics", John Wiley & Sons, Chichester
[5]. Eiken, O., Zumberge, M., and Stenvold, T., (2004)"Gravimetric monitoring of gas production from the Troll field"SEG Int'l Exposition and 74th Annual Meeting, Denver, Colorado..
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Abstract: The study encompasses two tectonically active areas of northeast India viz. the Arunachal Himalaya and Mishmi Massif and the Indo-Burman Ranges (IBR). The former is governed by collisional tectonics of the Himalayas and the latter by the subduction tectonics. This work aims at looking into the characteristics of Lg wave attenuation for earthquakes sourced in these two tectonic domains. The regional average of QLg was computed for both the study areas by using the method given by Ottemöler et al. (2002). It is found that both the study areas are tectonically active and attenuation of Lg is governed by frequency which is indicative of scattering attenuation. But then, IBR is relatively less attenuative than the Arunachal Himalayas and the Mishmi Massif, given the low value of Qo for the latter.
Keywords: Attenuation, Collision, Lg, Scattering, Subduction
[1] T. Furumura, T.K. Hong, and B.L.N. Kennett, Lg wave propagation in the area around Japan: observations and simulations. Progress in Earth and Planetary Science, 1(10), 2014
[2] S. Sargeant and L. Ottemöller, Lg wave attenuation in Britain. Geophys. J. Int. 179, 2009, 1593-1606.
[3] L.N. Kennett, Lg waves and structural boundaries. Bull. Seism. Soc. Am. 76, 1986, 1133-1141.
[4] B.J. Mitchell and H.J. Hwang, Effect of low Q sediments and crustal Q on Lg attenuation in the United States. Bull. Seism. Soc. Am., 77, 1987, 1197-1210.
[5] J.R. Bowman and B.L.N. Kennett, Propagation of Lg waves in the North Australian craton: influence of crustal velocity gradients. Bull. Seism. Soc. Am. 81, 1991, 592-610..
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Abstract: In this paper, we started by providing a fundamental information regarding tuta absoluta– a devastating pest of tomato or a harmful leaf mining moth with a strong preference for tomato plant – in the Mediterranean Basin countries and South America. We further review history of its invasion in Europe and Africa with the potential future spread of the pest in West Africa. The natural enemies in tomato crops in the aforementioned continents were documented with control method within IPM scheme.
Keywords: Tomato, Tuta Absoluta, Pest
[1] Abbes. K., Harbi, A. Chermiti, B. (2012).The tomato leafminer Tuta absoluta (Meyrick) in Tunisia: current status and management strategies. EPPO Bull. 42:226-233.
[2] Agarwal,S. and Rao , A.V (2000)Tomato lycopene and its role in human health and chronic diseases. CMAJ 2000;163 (6):739-44.
[3] Amizadeh, M., Hejazi M. J., Niknam, N., Arzanlou, M. (2015). Compatibility and interaction between Bacillus thuringiensis and certain insecticides: perspective in management of Tuta absoluta (Lepidoptera: Gelechiidae). Biocon. Sci. Technol. 25:671-684.
[4] Animashaun, M. (2016) On combating "Tomato Ebola‟ without unleashing cancer on Nigerians by the Vanguard Newspaper June 19,2016.
[5] Arno, J., Gabara, R. (2010). Controlling Tuta absoluta, a new invasive pest in Europe,Training in integrated Pest management – No 5IRTA cabrils, spain.
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Abstract: The study area south of Chumukedima in the Dimapur district of Nagaland provides unique opportunity to study the Surma – Tipam Transitional Sequences (STTS) hitherto undocumented in Naga Hills. Study of Vertical Profile Sections documents five distinct Lithofacies, namely Sand-Sale facies (SSH), Silty Shale facies (SLS), Sandstone facies (SST), Deformed Sand-Shale facies (DSS) and Hummocky Crossstratified sandstone facies (HCS). Spectacularly preserved sedimentary structures include lunate ripples, ripple
cross-laminae, parallel laminations, flaser and lenticular beddings, interfering ripples, trough cross beddi gs,
herringbone cross-stratifications, hummocky cross-stratifications. An attempt has been made to develope facies scheme and interpret the depositional milieu for the development of STTS. The conceptual model depicts mudflat – mixedflat – sandflat environments in an intertidal – subtidal setting intermittently influenced by strom and fluvial processes.
Keywords: Lithofacies, depositional environment, sedimentary structures, Surma-Tipam TransitionalSequence
[1] Adnan, A., Shukla, U.K. (2014) A case of normal regression with sea level transgression: Example from the Ganurgarh Shale,
Vindhyan Basin, Maihar area, M.P., India. GEOL. SOC. INDIA, v.84, pp 406-416.
[2] Dott., R.H. and Bourgeois, J. (1982) Hummocky stratification: significance of variable bedding sequences, Geol. Soc. Am. Bull.
v.93, pp663-680.
[3] Duke, W.I. (1987) Hummocky cross-stratification, tropical storms, and intense winter storms, Reply. Sedimentology. v.34, pp344-
352.
[4] Evans, P. (1932) Tertiary succession in Assam. Trans. Min. Geol. Inst. India. v.27, pp155-260.
[5] Evans, P. (1959) Stratigraphy and tectonics of the Assam Oilfield Region. E. C. A. F. E. Symposium, 1958, New Delhi, 170p
(United Nations, Bangkok). cabrils, spain.
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Abstract: The One-Dimensional Magnetotelluric forward modelling response has been carried out at the Tiris Geothermal area to obtain apparent resistivity and impedance phase responses as function of frequency due to the effect of resistivity and different layer depth. The resistivity and layer depth model are obtained from tentative model that result from previous research, using forward modelling with recursive technique. Base on apparent resistivity and impedance phase curve, the value of apparent resistivity varies by frequency and resistivity of each layer. In general, the apparent resistivity value approaches resistivity of the bottom layer determined by skin depth. The impedance phase varies around 45 degrees, affected by the frequency and resistivity of each layer. Finally, the magneto-telluric method can be used for more detailed exploration at Tiris geothermal area..
Keywords: 1D Magnetotelluric, recursive method, geothermal area, Tiris
[1] W.J. Book, Modelling design and control of flexible manipulator arms: A tutorial review, Proc. 29th IEEE Conf. on Decision and Control, San Francisco, CA, 1990, 500-506 (8)
[2] S.L. Kunsrat., "Report of investigation of geology and geochemistry at Mount Lamongan", East Java, Center for Volcanology and Geological Hazard Mitigation (PVMBG), 2010.
[3] A. Suprianto, Wahyudi, W.Utama, Suharno, and W. Suryanto, 2012, Analysis of the Reservoir type and Temperature of The Tiris Geothermal Prospect, 2nd Jogja International Conference, September 2012.
[4] M.S. Jaya, P. Jousset, F. Deon, A. Gassner, D. Putriatni, Supoyo., A. Suprianto, T.M. Kusuma, and K. Erbas, 2013, "Passive seismic monitoring studies at Tiris Geothermal field in East Java, Indonesia", Geophysical Research Abstract, Vol.15, EGU2013-13637-3, EGU General Assembly, 2013.
[5] A. Suprianto, Wahyudi, W. Suryanto, M.S. Jaya, F. Deon, A. Gassner, K. Erbas, W. Utama, T.M. Putrakusuma, D. Putriatni, and Supoyo, 2013, "Installing Surface Microseismic Monitoring in Mt. Lamongan Geothermal Area (LGA), East java, Indonesia", The 3rd Basic UB Proceedings, 2013..
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Abstract: The study deals with identification of potential groundwater areas in parts of Karwi block area, Chitrakoot district, Uttar Pradesh. Based on the incorporated studies, it has been observed that the lithology, geomorphology, lineaments, slope and land use/land cover was generated from IRS P6 LISS III data and Survey of India, toposheet on 1:50,000 scale and incorporated data with raster based Geographical Information System (GIS) to identify the groundwater potential zones. The assessment of satellite images, topographic maps supported by ground truth survey revealed that the area has a network of interlinked subsurface features. For surface water resources and ground water resources, the appropriate assessment of water potential helps in additional exploration at voluntary level................
Keywords: DEM, GIS, Geomorphology, Remote Sensing
[1] Adhikari, S.K. and Kumar, S., 2006. ―Groundwater Prospecting and Management‖, Springer Hydrogeology, pp 1-219, DOI 10.1007/978-981-10-1148-1_2
[2] Dykes, AP., 2008. ―Geomorphological maps of Irish peat landslides created using hand-held GPS‖, Journal of Maps, pp 258-276.
[3] Janaki, A. and Subramani, T., 2016. ―Identification Of Aquifer And Its Management Of Ground Water Resource Using GIS In Karur‖, International Journal of Emerging Trends & Technology in Computer Science (IJETTCS), 5(3), pp 81-92.
[4] Jose, S. K., Jayasree, R., Kumar, S. and Rajendran, S., 2012. ―Identification of Ground Water Potential Zones in Palakkad District, Kerala Through Multicriteria Analysis Techniques using Geo-information Technology‖, Bonfring International Journal of Industrial Engineering and Management Science, 2(Special Issue 1), pp 62-68.
[5] Khan, S. U., 2013. ―Harvest The Rainwater Wherever it Pours: Every Drop Counts‖, Excellence International Journal of Education and Research, 1(3), pp 122-130.
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Abstract: We report here the composition and mineralogy of a meteorite, fell in Mahuramukh area near Kamargaon Town (93o46' E, 26o39'N;) of Golaghat District, Assam on November 13, 2015 at 12:00 hrs IST, weighing about 12.095 Kg, registered as KomarGaon Meteorite and reported in the Meteoritical Bulletin No. 104, 2016; classed as ordinary L6 meteorite. The meteoriteiscovered with encrustations of varied colourfusion crusts, thickness and occasional regmaglypts in its outer facewith radiating shock veins. The inner face is light greyish white studded with brown native metal. Thin............
Keywords: Kamargaon Meteorite, ordinary chondrites, shock structures, mineral chemistry
[1]. Engellhard, T.W. and Graup, G. 1984. Suevite of the Ries crater, Germany: Source rocks and implications for cratering mechanics. Geol. Rundsch. 73, pp. 447-481.
[2]. Goswami, T.K., Ray, D., Sarmah, R.K., Goswami, U., Bhattacharyya, P., Majumdar, D., Bezbaruah, D., Borgohain, P., 2016. Komargaon, Assam (India), witnessed a new meteorite fall, PLANEX, 6, 1, 10-11, ISSN: 2320 7108
a. Hutchison, R. 2004. Meteorites: a Petrologic, Chemical, and Isotopic Synthesis. Cambridge Univ. Press, Cambridge, 506 p.
b. Kerr, R.A. 2013.Meteorite mystery edges closer to an answer-or the end of a field. Science, 341, pp.126–127.
c. Kieffler, S. W. and Simonds, C. H., 1980. The role of volatiles and lithology in the impact cratering process. Rev. Geophys. Space Phys., 18, pp.143-181..
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Abstract: study aims to obtain a picture of the problems experienced by teacher of a remote area in following the training and learningisolated students in the province of Central Sulawesi. The type of descriptive research is qualitative case study design. Informants of District and Sub-district Education Office and Isolated elementary school teacher of Oguang, Palasa District, ParigiMoutong Regency and Elementary School 4TomadoSangali, Lindu District, Central Sulawesi District. Data obtained through interviews and observation. The results showed that both regions had various problems following the training and carrying out the task of teaching students, namely: 1) georafis, 2)...............
Keywords: Analisys, Teacher Problems, Isolated Region
[1]. Arifin, D. (2010). Manajemen Pembelajaran Efektif. Bandung: Pustaka Al-Kasyaf.
[2]. Baedhowi. (2009). Prosedur Operasional Standar Penyelenggaraan KKG dan MGMP. Jakarta: Direktorat Peningkatan Mutu Pendidik dan Tenaga Kependidikann.
[3]. Djamarah, S. B., & Zain, A. (2002). Strategi Belajar Mengajar (Edisi Baru). Jakarta: Rineka Cipta.
[4]. Efendy, M. (2017). Pidato Menteri Pendidikan dan Kebudayaan pada Upacara Hari Pendidikan Nasional, 2 Mei 2017. Jakarta: Kementerian Pendidikan Nasional.
[5]. Joyce, T. M. (2014). Quality basic education for all: Challenges in multi-grade teaching in rural schools. Mediterranean Journal of Social Sciences, 5(1), 531. Diambil dari http://www.mcser.org/journal/index.php/mjss/article/download/1931/1930.
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Abstract: Reservoir characterization has long been identified as the main process employed in detailed description of any reservoir in order to properly study and analyze the reserve as well as to optimally place the wells for optima production of the reservoir. Seismic attributes of Field K is used in quantitative characterization of the reservoir, onshore Niger Delta Area of Nigeria. Three reservoir wellswere correlated for lithology delineation.Two reservoir sands were identified based on the similarities in geometry and petrophysical properties of the wells, while fault and Horizon were interpreted to generate the structural map of the field and reservoir in general. The seismic and well data were used to delineate the system tracts of the reservoir. The two hydrocarbon bearing reservoir...............
Keywords: Seismic Attributes, Characterization, Porosity, Water Saturation, Shale Volume, Structural, Stratigraphy, Delineation, faults
[1]. Akinwumi, F. V., Arochukwu, E. C., and Abdul-Kareem, A. S. (2004). "Managing Uncertainties in Hydrocarbon-in-place Volumes in a Northern Depobelt Field, Niger Delta, Nigeria" paper SPE 88880, presented at the 28th Annual SPE International Technical Conference and Exhibition in Abuja, Nigeria.
[2]. Doust, H. and Omatsola, E. (1989). Niger delta: AAPG Memoir 48 p. 201-238.
[3]. Ekweozor, C.M. and Dankoru, E.M., (1994): North Delta depobelt portion of the Akata – Agbada (1) Petroleum System , Niger Delta, Nigeria, in Magon, L.B., and Dow, W.G., eds. The petroleum system from source to trap, American Association of Petroleum Geologist, memoir 60; Tulsa, pp. 599 -614.
[4]. Etu-Effeotor. J.O., (1997): Fundamentals of Petroleum Geology. Department of Geological Sciences, University of Port Harcourt, Rivers State, Nigeria. pp. 23-65.
[5]. Evamy B. D., Haremboure J., Kamerling P., Knaap W. A., Molloy F. A. and Rowlands P. H., (1978): Hydrocarbon habitat of Tertiary Niger Delta. American Association Petroleum Geologist, Bulletin.Vol. 62. pp. 1 - 39.