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Tectonic Analysis of a Perseverant Disfigurement of a Zuma II Entry Route
Dikedi PN
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.