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Abstract: In recent years, ground penetrating radar (GPR) has been widely used as a technical means to understand the characteristics of subsurface geological deposition. However, there has not been any ground penetrating radar to recognize the internal configuration of the dam. The aim of this study is to form a composite dam with a point bar stack. Firstly, the highest resolution frequency of GPR is selected, and then the data are taken in the study area. And eliminate the influence of various factors on data volume. On the basis of the previous work, the location, the formation mechanism and the spatial distribution of the composite dam are determined by measuring the location of the point dam overlap and the dip angle, inclination and thickness of the lateral accretion.
Keywords: Ground penetrating radar; Field trench; the meandering river point bar; Point dam configuration.
[1]. Chenglong Zhao. Case Study of Ground Penetrating Radar for Geological Prediction in Qiyueshan Tunnel[A]. Science and Engineering Research Center.Proceedings of 2015 2nd International Conference on Green Materials and Environmental Engineering (GMEE2015)[C].Science and Engineering Research Center:,2015:4.
[2]. Baojin GE,Lianjun WANG,Yi LI,Danfeng LI School of Civil Engineering,Beijing Jiaotong University,Beijing 100044. APPLICATION OF GROUND PENETRATING RADAR IN SUBGRADE DEFECT DETECTION ON DA-QIN HEAVY HAUL RAILWAY[A]. Beijing Jiaotong University,China、Beijing Key Laboratory of Track Engineering.New Technologies of Railway Engineering[C].Beijing Jiaotong University,China、Beijing Key Laboratory of Track Engineering:,2012:4.
[3]. Jidong L Shijiazhuang University of Economics,Shijiazhuang,Hebei 050031,China. Urban underground drainage network investigation of ground penetrating radar[A]. Chinese Geophysical Society、National Natural Science Foundation of China、China University of Geosciences(CUG)、Chengdu University of Technology(CDUT).Near-Surface Geophysics and Geohazards--Proceedings of the 4~(th) International Conference on Environmental and Engineering Geophysics(Volume 2)[C].Chinese Geophysical Society、National Natural Science Foundation of China、China University of Geosciences(CUG)、Chengdu University of Technology(CDUT):,2010:5.
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Abstract: Miospore biozonation carried out on ditch cutting rock samples has been used to delineate the Upper Miocene/Pliocene sediments in well X, deep offshore, Niger delta. The rock succession is characterised by the alternation of sand and shale of variable thicknesses with lateral gradation in grain size. The base of the studied interval is made of Black shales intercalating with medium to coarse grained, sub rounded to rounded sandstone and siltstone at intervals representing the paralic Agbada formation while the top is made of Sub angular - sub rounded quartz pebble conglomerate, pebbly sandstone, medium - coarse grained, sub- rounded to well-rounded sandstone, intercalating with very thin lenses of grey shales typically...............
Keywords: Age, Biozonation, Formation, Miospore, Miocene, Pliocene
[1]. Reyment, R. A., 1965: Aspects of the Geology of Nigeria.Univ. Ibadan Press, Nigeria. 145pp.
[2]. Germeraad, J. B., Bopping, C. A..andMulIer, J., 1968. Palynology of Tertiary Sediments from Tropical areas. Rev. Paleobotan. Palynol., V. 6, P. 189 - 348.
[3]. Jan du Chene, R. E. Onyike, M. S. and Sowunmi, M. A., 1978C. Some new Eocene Pollen of the OgwashiAsaba Formation, Southern Nigeria. Revista Espanola De Micropaleontologia, V. X (2), P.285 – 322.
[4]. A Oloto, I. N., 1994. Nigerian Maastrichtian to Miocene dinoflagellate and MiosporeBiozonation - A summary. Journal of Mining and Geosciences.Society. (NMGS) V. 30(4), P. 61 - 73.
[5]. Evamy, B.D., Haremboure. J., Kamerling, P., Knaap, W.A., Molloy, F .A., and Rowlands, P .B., 1978. Hydrocarbon habitat of Tertiary Niger Delta.American Association of Petroleum Geologists Bulletin. v. 62, p.
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Abstract: Palynological investigation of the ditch cutting rock samples from well Z, offshore Niger Delta has been carried out. The rock succession is characterised by the alternation of fossilferous grey sandy shale with shells and shell fragments intercalating with medium - coarse grained, sub rounded to rounded sandstone with scattered mica flakes with appreciable thickness at the base and more paralic at the top, characteristically of the paralic Agbada Formation . palynological analysis yielded a well preserved and well distributed biostratigraphic relevant Miospores among which fifty...............
Keywords: Agbada, Age, Miocene, Miospore, Oligocene, Zones.
[1]. Germeraad, J. B., Bopping, C. A..andMulIer, J., 1968. Palynology of Tertiary Sediments from Tropical areas. Rev. Paleobotan. Palynol., V. 6, P. 189 - 348.
[2]. Jan du Chene, R. E. Onyike, M. S. and Sowunmi, M. A., 1978C. Some new Eocene Pollen of the OgwashiAsaba Formation, Southern Nigeria. Revista Espanola De Micropaleontologia, V. X (2), P.285 – 322.
[3]. Oloto, I. N., 1994. Nigerian Maastrichtian to Miocene dinoflagellate and MiosporeBiozonation - A summary. Journal of Mining and Geosciences.Society. (NMGS) V. 30(4), P. 61 - 73.
[4]. Evamy, B.D., Haremboure. J., Kamerling, P., Knaap, W.A., Molloy, F .A., and Rowlands, P .B., 1978. Hydrocarbon habitat of Tertiary Niger Delta.American Association of Petroleum Geologists Bulletin. v. 62, p.
[5]. Ajaegwu, N.E., Odoh, B.I., Akpunonu, E.O., Obiadi I.I. and Anakwuba, E.K., 2012.Late Miocene to Early Pliocene Palynostratigraphy and Palaeoenvironments of ANE-1 Well, Eastern Niger Delta, Nigeria. Journal of Mining and Geology Vol. 48(1) 2012, pp. 31–43.
