Series-2 (Jan. – Feb. 2022)Jan. – Feb. 2022 Issue Statistics
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| Paper Type | : | Research Paper |
| Title | : | Study of Karst Topography Development in the Aranyak/Madarkonta Cave Area, Bastar Division, Chhattisgarh, India |
| Country | : | India |
| Authors | : | Swapna Gupta || Dr. Prashant Shrivastava || Dr. S.D. Deshmukh || Rahul Mahawar |
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: | 10.9790/0990-1001020117  |
Abstract: The study area belongs to Kanger formation of Indravati basin. The cave named as Aaranyak/Madarkonta cave is situated approximately 26km from Jagdalpur, Headquarter of Bastar Division. This cave is mainly developed in the limestone area. No systematic Geological study has been done regarding this cave. Therefore, an attempt has been made to collect proper and authentic Geomorphologic, Lithological and Structural information about the cave. The Coordinates of Aranyak/madarkonta cave are 18°56´2.51´´N, 81°51´33.01''E. And it lies.......
[1]. Gautam, P.K.,Origin and Evolution of Limestone Caves of Chhattisgarh and Orissa, India: Role of Geomorphology,Tectonic and Hydrological Processes, 2014
[2]. Geological map of India – 1:2 million, The Geological Survey of India,1988
[3]. Guhe, R., Geochemical Characteristics of Proterozoic Carbonate Lithofacies of Indravati Basin, Chhatisgarh, Central India: Implication of Depositional and Diagenetic History, Rearchgate, 2017[4]. Gupta, S., Shrivastava, P., Deshmukh, S.D., Significance of Geological Events in the Kangerdhara area with Special Reference to the Development of Kotamsar and Dandak Cave, international Journal of Innovative Research in Science, Engineering and Technology (IJIRSET), 2021
[5]. Jha, A.S.,Shettipnwar,V.S., (I.F.S.), and Jha A., (S.R.F), Indication of The Presence of Metazoan fossils from The Neo-Proterozoic of Indiravati Basin, International Journal of Multidisciplinary Research and Development, 2015
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| Paper Type | : | Research Paper |
| Title | : | Petrological and Geochemical Evaluation of the Otutu Rift Segment, Kenya |
| Country | : | Kenya |
| Authors | : | Erique O. Nyawir || Jacques Varet || Peter O. Omenda |
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: | 10.9790/0990-1001021828 |
Abstract: Otutu rift segment lies in between the Eburru and Elmenteita volcanic field within the Kenya Central Rift Valley. It is one of the areas within the Kenyan rift that has not been fully explored nor developed geothermally. Rock samples were collected from the study area with an intention of acquiring more information on the surface mineralogical and chemical characteristics of the volcanic lavas within the study area. The area was selected as a representative of an active rift segment of the Kenya Rift Valley (KRV). This information assisted in the understanding of the origin and evolution of the magmas. Magmatic events in geothermal areas provide irreplaceable tools to characterize heat sources which are one of the key things being looked for during geothermal prospecting:.......
[1]. Arevalo, R., and McDonough, W.F. (2010). Chemical variations and regional diversity observed in MORB, Chemical Geology, Volume 271, Issues 1–2, pp70-85.
[2]. Bailey, D.K., (1987). Mantle metasomatism-perspective and prospect, Geological Society, London, Special Publications, 30, pp1-13.
[3]. Barberi, F., Ferrara G., Santacroce R., Treuil M. and Varet J. (1975). A transitional basalt-pantellerite sequence of fractional cristallization, the Boina Centre (Afar Rift, Ethiopia), Journal of Petrology, 16, pp22-56
[4]. Calais, E., Ebinger, C., Hartnady, C. and Nocquet, J. M. (2006). Kinematics of the East African Rift from GPS and earthquake slip vector data. Geological Society, London, Special Publications, 259, pp9-22.
[5]. Chorowicz, J. (2005). The East African Rift System. Journal of African Earth Sciences, 43, pp379–410.
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| Paper Type | : | Research Paper |
| Title | : | Modélisation de l'irradiance solaire longue(IR) et Effet du Forcing solaire sur le réchauffement de l'air à Bukavu, au Sud Kivu |
| Country | : | Congo |
| Authors | : | Alfred CHUBAKA BASHIGE || Albert KABASELE YENGAYENGA || CIMBELA KABONGO Joseph || KAZADI TSHIAMALA |
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: | 10.9790/0990-1001022936 |
Abstract: Résumé :
Contexte : Le flux d'irradiation solaire courte perçu sur la surface de la terre ou irradiance incidente, une fois à la surface de la terre réfléchie une partie dans l'atmosphère sous forme d'irradiance longue ou infrarouge pendant que l'autre partie est absorbée par la terre. Cette différence d'irradiance longue et courte, dite forcing solaire selon le rapport de GIEC(2018), pourrait avoir d'effet sur l'évolution des températures de surface. D'autre part la maîtrise de la détermination de cette composante de l'irradiance en un lieu pourrait avoir d'importance capitale dans le cas de suivi des cultures, de température, qu'il est indispensable de l'évaluer et de déterminer le modèle de son estimation lorsqu'on connait l'irradiance globale ou irradiance incidente.
Matériels et méthodes : Dans:.......
[1]. DELAYGUE Gilles(2018), Variabilité de l'activité solaire et impacts climatiques : le cas des derniers siècles, Encyclopédie de l'Environnement,[en ligne ISSN 255-0950].https://www.encyclopédie de l'environnement.org. p.1748
[2]. G.Ameli L., Alfred BASHIGE et ali (2017) « mesure locale de l'irradiance solaire pour l'évaluation de la performance de l'unité photovoltaïque installée à l'ISP/ Bukavu, RDC, Afrique Science, 13(6)(2017) 338-348.
[3]. Alain Ricaud Jan(2011), Gisement solaire et transferts énergétiques, Cours au Master en Enérgies Renouvelables, Inédit, Université de CERGY-PONTOISE,p79.
[4]. Benbouza Naima(2008) , Etude du rayonnement dans la région de Batna, Inédit, Mémoire de Magistère
[5]. www.univ-grenoble-aples.fr
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| Paper Type | : | Research Paper |
| Title | : | Similutide Et Modelisation Sol/Atmosphere Des Eaux Souterraines Et Aeriennes Du Territoire De Walungu En Province Du Sud-Kivu/Rdc |
| Country | : | Congo |
| Authors | : | Ladislas MOSANGE KATIBIBI || Albert KABASELE YENGA YENGA || Joseph CIMBELA KABONGO || Bertin KAMGANG SIMPLICE || Evariste KAZADI TSHIAMALA |
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: | 10.9790/0990-1001023757 |
Abstract: RESUME
Contexte : Dans notre Publication intitulée' 'similitude et Modélisation Sol/ Atmosphère des Eaux Souterraines et des Aériennes en Territoire de Walungu,nous allons étudier les interactions entre les Aériennes et les Souterraines
Matériel et Méthodes : Cette étude nous amène à découvrir le comportement des 18 sources échantillon dans le Territoire de Walungu.En premier lieu on a eu à prélever les Coordonnées GPS des différentes Sources, les Analyses Physico-Chimiques et Bactériologiques, calculer les différents Débits aux différentes Saisons et Années
Nous utilisons la Télémétrie par Satellites des Données ASCII NOAA sur une Période allant de 1960 à 2020 Soit 60 ans. Les relations modélisées.......
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| Paper Type | : | Research Paper |
| Title | : | Interpretation of Airborne Radiometric Data of Part of Middle Benue Trough of Nigeria for Mineral Deposits |
| Country | : | Nigeria |
| Authors | : | Adonu I.I || Ugwu G.Z || Onyishi G.E. |
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: | 10.9790/0990-1001025862 |
Abstract: Aeroradiometric study of Makurdi, Gboko, Kastina-Ala and Akwana was carried out to delineate prominent radiometric anomalies within the study area. This study area which is in the Middle Benue trough of Nigeria lies within latitude.......
Keywords: Radiometric Anomalies, Total Count, Threshold Value, Ternary Map, Mineralization
[1]. Obi DA, Menkiti RC, Okereke CS. Aeromagnetic Anomalies Modeling and Their Tectonic Implications in the Middle Benue Trough, Nigeria. Journal of Environment and Earth Sciences. 2014; 4(7): 1-11.
[2]. Cratchley CR, Jones GP. An interpretation of geology and gravity anomalies of the Benue valley, Nigeria Geophysics Paper, Overseas Geol. Surv. London. 1965; 1: 1-26.
[3]. Offodile ME, Reyment RA. Stratigraphy of the Keana-Awe area of the Middle Benue region of Nigeria. Bull. Geol. Inst. Univ. Upsala. 1978; 2: 37-66.
[4]. Offodile ME. A review of the Geology of the Benue Valley, Geology of Nigeria. Elizabethan Publishing Company Lagos. 1976; 319-330.
[5]. Reyment RA. Aspects of Geology of Nigeria, Ibadan University Press. Bull. Geol. Surv. Nig. 1965; 1: 1-95.