LITHOLOGY AND STRUCTURAL ANALYSIS OF ZANGO-ANGWAN-LAMIDO ENVIRONS, KATSINA STATE, NORTHWESTERN NIGERIA

Authors

  • I. A. Kankara

DOI:

https://doi.org/10.33003/fjs-2023-0703-1982

Keywords:

Basement Complex, Lithology, Structural Analysis, South Katsina, Northwestern Nigeria

Abstract

The study of lithological types and structural analysis of rocks of Zango-Kankara-Angwan Lamido on a scale of 1:50,000, Katsina State, northwestern Nigeria at longitudes 70 15’ E and 70 30’E and latitudes 110 45’N and 120 00’N has been carried out. The area consist predominantly of migmatite, older granites and schist, associated with minor quartzite and gneisses. The methodology adopted for the study was mainly primary data in which extensive field visits were done and outlined structural analysis and field relationships were recorded between successive thermo-tectonic episodes  The area underwent three phases of tectonic deformation denoted as D1, D2 and D3, whose ages were shown to be Pan-African. At least two intense phases of ductile deformation were identified in the rocks. The rocks have been strongly foliated (especially the gneisses) with crystals showing strong preferred orientations.

References

Adeniyi J.O, Willoughby A.A, Adlmula I.A, Radicella S.M (2004). Preliminary ionosonde measurement at Ilorin, Nigeria. National Workshop on Basic Space science, CBSS, UNN.

Bailey G.J, Su Y.Z, Oyama K.I (2000). Yearly variations in the lower latitude topside ionosphere. Annales Geophysicae 18: 789–798.

Bremer J, Singer W (1976). Diurnal, seasonal and solar cycle variations of electron densities in the ionospheric D and E regions. J. Atmospheric and terrestrial phys. (39): 25 – 34.

Danilov A.D (2007). Time and spatial variations in the ratio of nighttime and daytime critical frequencies of the F 2 layer. Geomagnetism and Aeronomy 7: 710 -719.

Danilov A.D (2008). Long-term trends in the relation between daytime and nighttime values of foF2. Ann. Geophys., 26: 1199-1206.

Gwal A.K, Sharma N (2004). Study of variation in Electron Density over the Low-Latitude Station, Bhopal using Crabex Receiver, CBR 415. 35th COSPAR Scientific Assembly. Held 18 - 25 July 2004, in Paris, France p. 135.

Lakshmi D.R, Veenadhari B, Dabas R.S, Reddy B.M (1997). Sudden post-midnight decrease in equatorial F-region electron densities associated with severe magnetic storms. Annales Geophysicae 15(3): 306-313.

Marhamah M.S, R. Umar I, Hazim S,N, Zafar A.S, & Mat R. (2018). The influence of solar radiation on radio signal at UHF band. J Fundam Appl Sci. 2018, 10(1S), 268-277. http://dx.doi.org/10.4314/jfas.v10i1s.17.

Okeke, Francisca & Ebere, Onwuneme & Hanson, Esther. (2009). Investigation of electron density variation in some regions of the Ionosphere at Nsukka, Nigeria.

Pérez-de-Tejada H (2004). Plasma channels and electron density profiles near the midnight plane in the Venus nightside ionosphere, J. Geophys. Res., 109, A04106, doi:10.1029/2002JA009811.

Sabri, Nor & Azlan, A.W. & Umar, Roslan & Sulan, S.S. & Ibrahim, Z.A. & wan mokhtar, Wan. (2015). The effect of solar radiation on radio signal for radio astronomy purposes. 19. 1374-1381.

Tereshchenko V.D, Ogloblina O.F, Tereshchenko V.A, Kovalevich T.V (2002). Seasonal differences of electron density in polar ionosphere D-region determined by partial reflection techniques. Physics of Auroral Phenomena. Proc.xxv, Annual seminar, apatity pp. 115 – 117.

Published

2023-10-11

How to Cite

Kankara, I. A. (2023). LITHOLOGY AND STRUCTURAL ANALYSIS OF ZANGO-ANGWAN-LAMIDO ENVIRONS, KATSINA STATE, NORTHWESTERN NIGERIA. FUDMA JOURNAL OF SCIENCES, 7(3), 311 - 317. https://doi.org/10.33003/fjs-2023-0703-1982