ISSN: 2157-7617

Journal of Earth Science & Climatic Change
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  • Research Article   
  • J Earth Sci Clim Change,
  • DOI: 10.4172/2157-7617.1000501

Tectonic Analysis of a Perseverant Disfigurement of a Zuma II Entry Route

Dikedi PN*
Department of Pure and Applied Physics, College of Natural and Applied Sciences, Veritas University, Abuja, Nigeria
*Corresponding Author : Dikedi PN, Department of Pure and Applied Physics, College of Natural and Applied Sciences, Veritas University, Abuja, Nigeria, Tel: 09021374449, Email: pdikedi@yahoo.co.uk

Received Date: Dec 04, 2018 / Accepted Date: Dec 20, 2018 / Published Date: Dec 27, 2018

Abstract

This research probe centers on unravelling the cause of a perseverant disfigurement of a Zuma II entry route from the tectonic standpoint. Seismic, magnetometry, and gravimetry approaches are employed in the tectonic analysis of the region under investigation. Traffic and Satellite maps of Bwari and study area is generated; data of magnetic and gravity intensity against location are tabulated; eleven seismograms of Earthquake magnitude on the Richter Scale are produced; graphs of gravitational intensity and magnetic intensity each against distance, are plotted. Conclusions, robust enough for this analysis, are drawn. Magnetic intensity peaked as much as 58 μT indicative of electromagnetic radiation escape. The repeated 4.3 Richter magnitude scale readings is indicative of the fragility and motion of the region. The folds are indicative of intense tectonic activities within the subsurface.

Keywords: Seismograms; Gravitational intensity; Magnetic intensity; Richter Magnitude Scale

Citation: Dikedi PN (2018) Tectonic Analysis of a Perseverant Disfigurement of a Zuma II Entry Route. J Earth Sci Clim Change 9: 501. Doi: 10.4172/2157-7617.1000501

Copyright: © 2018 Dikedi PN. This is an open-access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.

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