THE GEOLOGY OF SOUTHERN AKOR AND ITS ENVIRONMENT | Blazingprojects Postgraduate Thesis
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THE GEOLOGY OF SOUTHERN AKOR AND ITS ENVIRONMENT

 

Table Of Contents


Chapter ONE

INTRODUCTION

  • 1.1Introduction
  • 1.2Background of study
  • 1.3Problem Statement
  • 1.4Objective of study
  • 1.5Limitation of study
  • 1.6Scope of study
  • 1.7Significance of study
  • 1.8Structure of the research
  • 1.9Definition of terms

Chapter TWO

LITERATURE REVIEW

  • 2.1Overview of Geology
  • 2.2Geological History of Southern Akor
  • 2.3Rock Formations in the Region
  • 2.4Mineral Resources in Southern Akor
  • 2.5Environmental Impact of Geological Features
  • 2.6Geographical Features of Southern Akor
  • 2.7Climate and Weather Patterns
  • 2.8Biodiversity in the Region
  • 2.9Human Interaction with Geological Features
  • 2.10Future Trends in Geology of Southern Akor

Chapter THREE

RESEARCH METHODOLOGY

  • 3.1Research Design and Strategy
  • 3.2Data Collection Methods
  • 3.3Sampling Techniques
  • 3.4Data Analysis Procedures
  • 3.5Research Ethics and Integrity
  • 3.6Research Limitations
  • 3.7Research Validity and Reliability
  • 3.8Timeframe and Budget for the Study

Chapter FOUR

DATA PRESENTATION AND ANALYSIS

  • 4.1Overview of Research Findings
  • 4.2Geological Features Analysis
  • 4.3Environmental Impact Assessment
  • 4.4Comparison with Previous Studies
  • 4.5Discussion on Mineral Resources
  • 4.6Climate Change Implications
  • 4.7Biodiversity Conservation Strategies
  • 4.8Recommendations for Future Research

Chapter FIVE

SUMMARY, CONCLUSION AND RECOMMENDATIONS

  • 5.1Conclusion and Summary
  • 5.2Summary of Findings
  • 5.3Implications for Geology and Environment
  • 5.4Contribution to Existing Knowledge
  • 5.5Recommendations for Policy and Practice

Thesis Abstract

The study area is located within latitude 050 271 4611N and longitude 0080 431 46E, and the elevation of the place is 156m. The major rock types encountered in the area include gneisses, quartzite, amphibolites and marbles. These are intruded by pegmatite, quartz vein and aplite. The latest metamorphic episode occurred during the Pan-African Orogeny (600 ± 15ma) and the deformation left a structural trend of NS and NE-SW on the rocks. The occurrence of NW-SE structural trend are also shown on some rocks indicating that the Pan-African event did not completely alter earlier structural imprints. The study area is highly forested, undulating in slope and is a characteristic of a tropical rain forest in the area.  



Thesis Overview

<p> </p><p><strong>INTRODUCTION</strong></p><p>The geology of southern Akor and its environs lies within the Oban Massif, a component of the crystalline basement of Nigeria. The Nigeria crystalline basement in turn forms a part of the African crystalline basement and covers over 50% of the total land surface of Nigeria . The rock assemblages encountered and identified consists of mainly schists, gneisses, Amphibolite, Charnockite, Marble and Quartzites and pegmatite, Quartz vein and Aplite emerging as Igneous intrusive rocks. The area mapped and studied (Akor) is predominated by intrusive rocks and these rocks are very well exposed where the topographyis slopy along streams and river channels.</p><p>Ekwueme et al (1992) proposed that charnockite rock's occur in both the eastern and western Oban Massif. The rocks occur as large coarse-grained, rounded and, massive bodies deformed together with the bounded gneisses. Ekwueme (1992) has shown that the diorities and charnockite are similar in composition and that the former may be retrogressive product of the latter.</p><p>The occurrences of weathering and tectonic activities were observed to have greatly affected the exposed outcrop and such effects from wet season had deformed these outcrops to boulders with reference to their shapes and sizes.</p><p><strong>1.1 &nbsp; Location and accessibility</strong></p><p>The area is located in the Eastern part of Akamkpa local Government area of theCross River State of Nigeria. It covers an estimated area of about 85sq.KM and constitutes part of the Oban Massif of the South-eastern Nigeria. The map area is largely made up of Ntebachot Akor. New Ntebeji and Ayip Eku all located in Akamkpa Local Government area of Cross River state. </p><p>&nbsp;</p><p>About 90 percent of the area is inaccessible due to thick vegetation, steep valleys and hilly terrains. The only access road across the area is the Calabar-Ekang Road while hunters tracks provide minimal access into the area.</p> <br><p></p>

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