Version-2 (July-Aug-2017)
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| Paper Type | : | Research Paper |
| Title | : | Integrated well log and 3-D seismic data interpretation for the Kakinada area of KG – PG offshore basin |
| Country | : | India |
| Authors | : | Govindan.S |
 |
: | 10.9790/0990-0504020105  |
Abstract: In this paper Structural and stratigraphic mapping within the Krishna Godavari offshore Basin in central part of the eastern passive continental margin of India was commonly carried out using traditional field geological methods. The main objective of the study is to get the general geological setup of the area, i.e. Stratigraphy, structural setup, presence of hydrocarbon, petroleum system, and reservoir features like porosity, permeability, reservoir extent etc and a practical experience in the workstation, for this, data like various logs (GR, Resistivity, Density, Neutron and Sonic logs), seismic...........
Keywords: Krishna Godavari basin, Structuralsetup, Stratigraphy, Open- works, Seismic, Sonic
[1] Rao, G. N. 2001, Sedimentation, stratigraphy and petroleum potential of Krishna - Godavari basin, East Coast of India, AAPG Bull., 85, 1623-1643.
[2] Peter M.Barber "Regional Reservoir fairways: Deep water Krishna-Godavari basin, India". (July 2002).
[3] A. Govindan "Miocene deep water agglutinated foraminifera from offshore Krishna-Godavari Basin, India.Micropaleontology, October 1, 2004; 50(3): 213 - 252.
[4] Sheriff."Exploration Seismology"
[5] S. K. Gupta Oil and Natural Gas Corporation, Dehradun, India. "Basin architecture and petroleum system of Krishna Godavari Basin, east coast of India".
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| Paper Type | : | Research Paper |
| Title | : | Trace Including Ree+Y And Organic Geochemistry Of Kuşakdaği And Gökçepinar Formations In The Beyreli (Hadim-Konya) Area, Central Taurides, Southern Turkey: Implications For Source Rock Potential, Provenance, Paleo-Environment And Tectonic Setting |
| Country | : | Turkey |
| Authors | : | J. Kareem || Ş. Küpeli |
|
: | 10.9790/0990-0504020635 |
Abstract: The investigation area comprised of Beyreli (Hadim-Konya) village and the surrounding area in the Central Taurus Belt, Southern Turkey. A total of forty-eight bulk samples from the Late Permian and Early Triassic Kuşakdağı (K) and Gökçepınar Formations (T) were analyzed to investigate the organic carbon contents, types, maturities, hydrocarbon potentials of the Kuşakdağı Formation and tectonic settings, provenance and depositional conditions of both Formations by using geochemical data. The Formations are represented by limestone and bituminous...........
Keywords: Beyreli (Hadim-Konya, Turkey), Rare Earth Element, Rock-Eval pyrolysis, Kerogen, Kuşakdağı and Gökçepınar Formations, Tectonic Setting, Total organic carbon (TOC).
[1]. Abedini, A., and Calagari, A., 2015. Rare earth element geochemistry of the Upper Permian limestone: the Kanigorgeh mining district, NW Iran. Turkish Journal of Earth Sciences, 24 (4), 365-382.
[2]. Ala, M., Kinghorn, R., and Rahman, M., 1980. Organic geochemistry and source rock characteristics of the Zagros petroleum province, southwest Iran. Journal of Petroleum Geology, 3 (1), 61-89.
[3]. Alaug, A., Batten, D., and Ahmed, A., 2013. Organic geochemistry, palynofacies and petroleum potential of the Mukalla Formation (late Cretaceous), Block 16, eastern Yemen. Marine and Petroleum Geology, 46, 67-91.
[4]. Aliyev, S., Sarı, A., Koralay, D., and Koç, Ş., 2009. Investigation of organic carbon and trace metal enrichments of rocks at the Paleocene-Eocene boundary, NW Turkey. Petroleum Science and Technology, 27 (1), 56-71.
[5]. Alizadeh, B., Sarafdokht, H., Rajabi, M., Opera, A., and Janbaz, M., 2012. Organic geochemistry and petrography of Kazhdumi (Albian–Cenomanian) and Pabdeh (Paleogene) potential source rocks in southern part of the Dezful Embayment, Iran. Organic geochemistry, 49, 36-46..
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| Paper Type | : | Research Paper |
| Title | : | Calculating Geological Reserves of Horizontal Wells by Using Water Drive Characteristic Curve Analysis Method |
| Country | : | India |
| Authors | : | Ren Lijuan |
|
: | 10.9790/0990-0504023639 |
Abstract:Water drive characteristic curve analysis method is a method of using oil production prediction of recoverable reserves and reserves, is mainly the analysis of the relationship between cumulative oil production, cumulative water production and cumulative liquid production, in oilfield development has been widely used. This paper analyzed the method used in the calculation of the geological reserves of horizontal well water flooding characteristic curve, taking Daqing oilfield Nan1- Ping25 horizontal wells as an example, analysied the geological reserves of the horizontal well was applied to calculate the water drive characteristic curve, analyzed the results of horizontal well geological reserves, provided favorable information for evaluating the development effect of horizontal wells.
Keywords: Horizontal well, Geological reserves, Water flooding characteristic curve, Single well
[1] Chen Jun, Zhang Liehui, Feng Gang. Study on Evaluation of single well water drive [J]. Journal of Southwest Petroleum Institute, 2001, 6 (23): 129-130
[2] Yang Tongyou, Fan Yang, Chen Yuanqian, et al. Calculation methods of petroleum and natural gas reserves [M]. Beijing: Petroleum Industry Press,.1998183-207
[3] Lin Zhifang. Calculation of water drive characteristic curve. Methods of recoverable reserves in oilfield [J]. petroleum exploration and development, 1990, (6): 64-71.
[4] Chen Yuanqian. Derivation of relation formula of water drive curve [J]. Journal of Petroleum Society, 1985, (6): 69-78.
[5] Xia Bing. The water drive characteristic curve should be taken in the calculation of reserves. A case study of Xin Wei 151 block in Dongxin oilfield [J]. China Science and technology information, 2005, (22): 116.
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| Paper Type | : | Research Paper |
| Title | : | Spatio-Temporal changes of Land use/Land cover of Pindrangi Village Using High Resolution Satellite Imagery |
| Country | : | India. |
| Authors | : | Dr.Gangaraju.M || Anitha.P || T.V.Krishna || A.Sravankumar |
|
: | 10.9790/0990-0504024044 |
Abstract: Interpretation of high resolution satellite imagery revealed various Land use/Land cover features in Pindrangi village , High resolution Satellite imagery was acquired from the goggle earth through Sasplanet software, The data were acquired for the years 1984, 1994, 2004 and 2014. High resolution Satellite imagery was processed in Arc Map 10.4.1. Further an analysis of the decadal sequence imagery pertaining to decadal aimed at detecting the land use / land cover change has indicated that the plantation has phenomenally increased by 235.20he during the study period,...........
Keywords: Land use/land cover, Temporal Changes, Arc Gis 10.4.1.
[1] Ali Mohammed (1978), 'Studies in Agricultural Geography', Rajesh Publications, New Delhi, 1978, pp-1-6.
[2] Nageswara Rao.K (2003)Remote Sensing and GIS Applications in the Identification of Aquaculture Hotspots at Village Level Journal of the Indian Society of Remote Sensing, Vol. 31, No. 2.
[3] Nageshwara Rao K. and Vaidyanathan R. (1981), 'Landuse capability studies from Arial Photo-Interpretation -A case study from Krishna Delha', India Geographical Review of India. Vol.43,
[4] No.3 pp-226-236.
[5] Vink, A. P. A. (1975): 'Land use in Advancing AgriculturalSpringer Verlag Berlin', Heidelberg, New York
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| Paper Type | : | Research Paper |
| Title | : | Delineating Ground Water Potential Zones in Khatra Block, Bankura District, West Bengal using MCE, RS and GIS Techniques |
| Country | : | India. |
| Authors | : | Pampiya Chowdhury || S.K.Nag |
|
: | 10.9790/0990-0504024560 |
Abstract: Groundwater is considered to be one of the most valuable natural resources that support human civilization. It is an immensely important and dependable source of water supply in all climatic regions over the world. Due to population explosion and improper management, the resource is depleting drastically and is accomplished by extensive withdrawal of groundwater. Groundwater is in demand in hard rock areas where surface water supply is inadequate. Owing to this geoscientists are employing various techniques to explore the potential zone amongst which Multi-Criteria Evaluation (MCE) technique seems to be more precise. Remote sensing and Geographic Information System...........
Keywords: Ground Water Potential zone, Multi Criteria Evaluation, Remote Sensing & GIS, Khatra Block.
[1] Assaf, H. and Saadeh, M. (2008). Geostatistical Assessment of Groundwater Nitrate Contamination with Reflection on DRASTIC Vulnerability Assessment: The Case of the Upper Litani Basin, Lebanon Resour Manag. V.23, pp.775–796.
[2] Agarwal, C.S..and Garg, P.K. (2000), 'Textbook on Remote Sensing in Natural Resources Monitoring and Management ' , Wheeler Publishing, New Delhi, pp.213.
[3] Asadi, S.S., Vuppala, P., Reddy, M.A. (2007). Remote sensing and GIS techniques for evaluation of groundwater quality in municipal corporation of Hyderabad (Zone-V), India. Int J Environ Res Public Health, v.4(1),pp. 45–52.
[4] Bahuguna, I.M., Nayak, S., Tamilarsan, V., Moses, J., (2003). Groundwater prospective zones in Basaltic terrain using remote sensing. J Indian Soc Remote Sens. V.31(2), pp.107–118.
[5] Basudeo, Rai., Tiwari, A., Dubey, V.S., (2005). Identification of groundwater prospective zones by using remote sensing and geoelectrical methods in Jarla and Raniganj coalfields, Dhanbad district, Jharkhand state. J of Earth System Scinces. V.114(5), pp.515-522.
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| Paper Type | : | Research Paper |
| Title | : | Hydrological Problems Associated With Mineralizations in the Middle Benue Trough: Implications for Mine Development and Possible Solutions |
| Country | : | Nigeria |
| Authors | : | Victor I. Vincent || Eyo E. Ntekim || Maimunatu Halilu || Fauziya Ahmed Rufai |
|
: | 10.9790/0990-0504026167 |
Abstract: The Benue Trough hosts a variety of metallic and non-metallic mineral deposits. The hydrologic conditions associated with the lithologic units hosting some of these deposits has presented substantial problems to its exploitation. This study was carried out in a bid to proffering viable methods of managing excessive water flow associated with the ore deposits as present mine development and water management practices seem inadequate. A combination of diversion and dewatering techniquesis seen as the best possible solution to handling hydrological conditions associated with mineralizations in the Benue Trough. It is hoped that incorporating these suggestions into mine design and groundwater inflow management during mining can help abate the problems.
[1] Akande, S.O., O.J. Ojo, Adekeye, O. A., and Egenhoff, S.O., 2011. Stratigraphic Evolution and Petroleum Potential of Middle Cretaceous Sediments in the Lower and Middle Benue Trough, Nigeria: Insights from New Source Rock Facies Evaluation.PTDF Journal July – Vol 1
[2] El-Nafaty, J.M., 2015. Rare earth element and stable sulphur (34 S) isotope study of baryte–copper mineralization in Gulani area, Upper Benue Trough, NE Nigeria. J. Afr. Earth Sci. http://dx.doi.org/10.1016/j.jafrearsci.2015.03.007
[3] Ene, E.G., and Okogbu, C.O., 2013. Stability Analysis of the Mine Pit Slopes in the Gabu-Alifokpa Barite Fields Southeastern Nigeria. Journal of Mining and Geology 101: 49(1) p21-30
[4] Morton, K.L. & van Merkerk, F.A., 1993. A Phased Approach to Mine Dewatering. Mine Water and the Environment 12:27. Doi: 10.1007/BF02914796
[5] Ngan, S.A., Reed, S.M. & Singh, R.N., 1984. Groundwater problems in Surface Mining in the United Kingdom. International Journal of Mine Water 3: 1. Doi:10.1007/BF02504588
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| Paper Type | : | Research Paper |
| Title | : | Solar Wind Periodicities in 24 Solar Maximum |
| Country | : | India. |
| Authors | : | Bidhu S S || Iren Sobia A || Dickson Benjamin |
|
: | 10.9790/0990-0504026873 |
Abstract: Solar wind carries solar fluctuations to the magnetosphere as the result of solar rotations. In the present work, we use Morlet wavelet technique to investigate the periodicities of solar wind parameters during maximum phase of 24 solar cycle. The solar wind parameters utilized for wavelet analysis in this work are the interplanetary magnetic field, solar wind speed, temperature and density. ACE observations are compared with WIND observations to verify the periodicities during solar maximum............
Keywords: Solar Wind density, Solar Wind magnetic field, Solar Wind temperature, Solar Wind velocity, Wavelet Spectrum
[1] Fligge, M., Solanki, S. K., & Beer, J. 1999, A&A, 346, 313
[2] Gonzalez. A.L.C and Gonzalez W.D., Periodicities in the IMF polarity, J.Geophys. Res., 92, 4357, 1987.
[3] Hapgood. M.A, M.Lockwood, G.A.Bowe and D.M.Wills., Variability in the interplanetary medium at 1 AU over 24 years. Planet.Space. Sci., 39, 411, 1991.
[4] Hapgood.M.A, A double solar cycle in the 27 day recurrence of geomagnetic activity. Ann. Geophys., 11,248, 1993.
[5] Howe, R., Christensen-Dalsgaard, J., Hill, F., et al. 2000, Science, 287,2456
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| Paper Type | : | Research Paper |
| Title | : | Aspects of Hydrocarbon Potential of the Tertiary Imo Shale Formation in Anambra Basin, Southeastern Nigeria |
| Country | : | Nigeria |
| Authors | : | Adeleye Mutiu Adesina || Adeniyi Vanessa Adeola || Oke, Abeeb Oladayo |
|
: | 10.9790/0990-0504027483 |
Abstract: The Tertiary Imo Shale Formation, a lithofacies equivalent of marine Akata Formation (prolific source rock) in subsurface Niger Delta, requires proper evaluation of its hydrocarbon generative potentials to complement organic geochemical data in Anambra Basin. This study attempts to evaluate aspects of the source rock potential for hydrocarbon generation of the Imo Shale Formation penetrated by the Akukwa-II and Nzam-I wells in Anambra basin. The sediments encountered at depth range of 120 to 240 m and 550 to 650 m in Akukwa-II and Nzam-1 wells respectively, are made up of shales, sandy shale and mudstones. The shales are fine grained, fissile and light to dark grey in colour, the sandy shale is medium grained and grey in colour while the mudstones are fine grained and brownish grey in colour...........
Keywords: Hydrocarbon potential, Imo Shale Formation, kerogen type, source rock, thermal maturity
[1] A. A. Avbovbo, and Ayoola, O, Petroleum prospects of the southern Nigeria's Anambra Basin. Oil and Gas Journal, 1981, 334-347.
[2] G. I. Unomah and Ekweozor, C. M, Petroleum source-rock assessment of the Campanian Nkporo Shale, Lower Benue Trough, Nigeria. NAPE Bull. 8 (2), 1993, 172-186.
[3] I. M. Akaegbobi, I. M. and Schmitt, M, Organic facies, hydrocarbon source potential and the reconstruction of depositional Paleoenvironment of Campano-Maastrichtian Nkporo shale in the Cretaceous Anambra Basin, Nigeria NAPE Bull. 13 (1), 1998, 1-19.
[4] Murat, R. C, Stratigraphy and paleogeography of the Cretaceous and Lower Tertiary in Southern Nigeria. In T.F. J. Dessauvigie and A.J. Whiteman eds. African Geology, University of Ibadan press, 1972, 635 - 648.
[5] Obaje.N. G., Ulu, O. K., and Petters, S. W.1999. Biostratigraphic and geochemical controls of hydrocarbon prospects in the Benue Trough and the Anambra basin, Nigeria. NAPE Bull. 14, 1999, 18-54.