1Department of Earth Sciences, University of Yaoundé I, P. O. Box 812 Yaounde, Cameroon
2Department of Geology, University of Buea, P. O. Box 63 Buea, Cameroon
Journal of Geosciences and Geomatics.
2016,
Vol. 4 No. 3, 61-72
DOI: 10.12691/jgg-4-3-3
Copyright © 2016 Science and Education PublishingCite this paper: Jonas Didero TAKODJOU WAMBO, Sylvestre GANNO, Aloysius AFAHNWIE NGAMBU, Emmanuel NOMO NEGUE, Joseph MVONDO ONDOA, Jean Paul NZENTI. Use of Landsat 7 ETM
+ Data for the Geological Structure Interpretation: Case Study of the Ngoura-Colomines Area, Eastern Cameroon.
Journal of Geosciences and Geomatics. 2016; 4(3):61-72. doi: 10.12691/jgg-4-3-3.
Correspondence to: Sylvestre GANNO, Department of Earth Sciences, University of Yaoundé I, P. O. Box 812 Yaounde, Cameroon. Email:
sganno@uy1.uninet.cmAbstract
Remote sensing and Geographical Information System (GIS) technology have opened a new era in the field of applied geology. In this study, combined field and remote sensing applications through the processing of the Landsat-7 Enhance Thematic Mapper Plus (ETM+) were used to monitor to geologic structures in Ngoura-Colomines area. This mapping approach led to the detection of 654 lineaments in which two main types have been distinguished. The type-I (15%) shows two main directions (NE-SW and NW-SE) and corresponds to large-scale or regional structures while type-II (85%) with dominant NE-SW-trends represents foliation trajectories. In addition, type-I lineaments are compatible with the Riedel fault system composed of P and P′ fractures oriented NE-SW and NNE-SSW respectively; E-W trending R fractures and R' fractures with NW-SE trends. Our findings provide the evidence of a polyphase ductile-brittle structures such as shear zone and faults. These structures constitute pathway for both mineralizing fluids and ground water circulation. Since several gold artisanal mines exist in Ngoura-Colomines area, the proposed mapping approach is an important guide for the identification of the structures that control the gold mineralisation in the area.
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