Near Surface Fractures Evidence from Audio-Magnetotelluric (AMT) Investigation in Ayos-Nguelemendouka Area (Eastern Cameroon)

Abstract

The current study deals with an interpretation of audio-magnetotelluric (AMT) data collected in the Ayos/Nguelemendouka area, using a Stratagem EH4 unit. The study’s objective is to provide a better understanding of the area’s subsurface structure. Thus, AMT soundings were realised through seven profiles NE30° oriented, each profile made up of four stations. Data modelling highlights a SW-NE tectonic unevenness which seems to correlate with the Centre Cameroon Shear Zone. Moreover, this interpretation put into evidence an uplift of the basement at Lamba 2, a tabular structure at depth and an absence of discontinuities beneath 300 mdepth.

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A. Meying, T. Mbarga, D. Gouet and P. Stéphane, "Near Surface Fractures Evidence from Audio-Magnetotelluric (AMT) Investigation in Ayos-Nguelemendouka Area (Eastern Cameroon)," International Journal of Geosciences, Vol. 4 No. 2, 2013, pp. 480-493. doi: 10.4236/ijg.2013.42045.

Conflicts of Interest

The authors declare no conflicts of interest.

References

[1] J. P. Nzenti, P. Barbey, J. Macaudiere and D. Soba, “Origin and Evolution of the Precambrian High Grade Yaounde Gneiss (Cameroon),” Precambrian Research, Vol. 38, No. 2, 1988, pp. 91-109. doi:10.1016/0301-9268(88)90086-1
[2] P. Rolin, “La Zone de Décrochement Panafricain des Oubanguides en République Centrafricaine,” Comptes rendus de l'Académie des Sciences, Paris, Vol. 320, No. 2A, 1995, pp. 63-69.
[3] S. F. Toteu, J. Penaye and D. Y. Poudjom, “Geodynamic Evolution of the Panafrican Belt in Central Africa with Reference to Cameroon,” Canadian Journal of Earth Sciences, Vol. 41, No. 1, 2004, pp. 73-85. doi:10.1139/e03-079
[4] A. Meying, T. Ndougsa-Mbarga and E. Manguelle-Dicoum, “Evidence of Fractures from the Image of the Subsurface in the Akonolinga-Ayos Area (Cameroon) by Combining the Classical and the Bostick Approaches in the Interpretation of Audio-Magnetotelluric Data,” Journal of Geology and Mining Research, Vol. 1, No. 8, 2009, pp. 159-171.
[5] J. M. Tadjou, R. Nouayou, J. Kamguia, H. L. Kande and E. Manguelle-Dicoum, “Gravity Analysis of the Boundary between the Congo Craton and the Pan-African Belt of Cameroon,” Austrian Journal of Earth Science, Vol. 102, 2009, pp. 71-79.
[6] T. Ndougsa-Mbarga, A. Meying, D. Bisso, D. Y. Layou, K. K. Sharma and E. Manguelle-Dicoum, “Audiomagne-totellurics (AMT) Soundings Based on the Bostick Approach and Evidence of Tectonic Features along the Northern Edge of the Congo Craton, in the Messamena/ Abong-Mbang Area (Cameroon),” Journal of Indian Geophysical Union, Vol. 15, No. 3, 2011, pp. 145-159.
[7] S. Mbom-Abane, “Investigation Géophysique en Bordure du Craton du Congo (Région D’Abong-Mbang/Akono-linga, Cameroun) et Implications Structurales,” Thèse Doctorat d’Etat ès Sciences, Faculté des Sciences, Université de Yaoundé I, 1997, 187 p.
[8] T. Ndougsa-Mbarga, I. K. Njilah, J. Nni and J. Nana, “Note on the Review of Earthquakes on Cameroon Territory,” Journal of Civil Protection, Ministry of Territorial Administration, Vol. 3, 2010, pp. 65-67.
[9] J. M. Regnoult, “Synthèse Géologique du Cameroun,” Ministère des Mines et de l'énergie, 1986, p. 119.
[10] H. Mvondo, S. W. J. Den-Brok and J. Mvondo-Ondoa, “Evidence for Symmetric Extension and Exhumation of the Yaoundé Nappe (Pan-African Fold Belt, Cameroon),” Journal of African Earth Sciences, Vol. 36, No. 3, 2003, pp. 215-231. doi:10.1016/S0899-5362(03)00017-4
[11] H. Mvondo, S. Owona, J. Mvondo-Ondoa and J. Essono, “Tectonic Evolution of the Yaoundé Segment of the Neo-proterozoic Central African Orogenic Belt in Southern Cameroon,” Canadian Journal of Earth Sciences, Vol. 44, No. 4, 2007, pp. 433-444. doi:10.1139/e06-107
[12] J. Penaye, S. F. Toteu, W. R. Van Schmus and J. P. Nzenti, “U-Pb and Sm-Nd Preliminary Geochronologic Data on the Yaounde Series, Cameroun: Re-Interpretation of the Granulitic Roks as the Suture of a Collision in the Central Africa Belt,” Comptes rendus de l'Académie des Sciences, Paris, Vol. 317, No. 2, 1993, pp. 789-794.
[13] J. B. Olinga, J. E. Mpesse, D. Minyem, V. Ngako, T. Ndougsa-Mbarga and G. E. Ekodeck, “The Awaé—Ayos Strike-Slip Shear Zones (Southern-Cameroon): Geometry, Kinematics and Significance in the Late Panafrican Tectonics,” Neues Jahrbuch für Geologie und Palaontologie—Abhandlungen, Vol. 257, No. 1, 2010, pp. 1-11.
[14] M. Vignès-Adler, A. Le Page and P. M. Alder, “Fractal Analysis of Fracturing in Two African Regions from Sattelite Imagery to Ground Scale,” Tectonophysics, Vol. 196, No. 1-2, 1991, pp. 69-86. doi:10.1016/0040-1951(91)90290-9
[15] L. Cagniard, “Basic Theory of the Magneto Telluric Method of Geophysical Prospecting,” Geophysics, Vol. 18, No. 3, 1953, pp. 605-635. doi:10.1190/1.1437915
[16] K. Vozoff, “Magnetotelluric Principles and Practice,” Proceedings of the Indian Academy of Sciences—Earth and Planetary Sciences, Vol. 99, No. 4, 1990, pp. 441-471.
[17] K. Vozoff, “The Magnetotellurics Method in the Exploration of Sedimentary Basins,” Geophysics, Vol. 37, No. 1, 1972, pp. 98-141.
[18] M. S. Zhdanov, “Magnetotelluric and Magnetovariational Methods,” Geophysical Electromagnetic Theory and Methods, Vol. 45, 2009, pp. 545-645.
[19] F. X. Bostick, “A Simple Almost Exact Method of MT Analysis,” Workshop on Electrical Methods in Geothermal Exploration US Geological Survey, Contract No. 14080001-8, Vol. 359, pp. 174-183.
[20] M. Ritz, “Etude Régionale M.T. des Structures de la Conductivité Electrique sur la Bordure Occidentale du Craton Ouest Africain en République du Sénégal,” Canadian Journal of Earth Sciences, Vol. 19, 1982, pp. 1408-1416.
[21] A. G. Jones, “On the Equivalence of the Niblett and Bostick Transformation in the Magnetotelluric Method,” Geophysic, Vol. 53, 1983, pp. 72-73.
[22] E. Manguelle-Dicoum, A. S. Bokossah and T. E. Kwende-Mbanwi, “Geophysical Evidence for a Major Precam-brian Schist-Granite Boundary in Southern Cameroon,” Tectonophysics, Vol. 205, No. 4, 1992, pp. 437-446. doi:10.1016/0040-1951(92)90447-E
[23] E. Manguelle-Dicoum, R. Nouayou, A. S. Bokossah and T. E. Kwende-Mbanwi, “Audiomagnetotelluric Soundings on the Basement-Sedimentary Transition Zone around the Eastern Margin of the Douala Basin in Cameroun,” Journal of African Earth Sciences, Vol. 17, No. 4, 1993, pp. 487-496. doi:10.1016/0899-5362(93)90006-C
[24] J. O. Campos-Enriquez, J. A. Arzate, J. Urrutia-Fuccugauchi and O. Delgado-Rodriguez, “The Subsurface Structure of the Chicxulub Crater (Yucatan, Mexico): Preliminary Results of a Magnetotelluric Study,” The Leading Edge, Vol. 16, No. 12, 1997, pp. 1774-1777.
[25] O. Delgado-Rodrigez, J. O. Campos-Enriquez, J. Urrutia-Fuccugauchi and J. A. Arzate, “Occam and Bostick 1D Inversion of Magnetotelluric Soundings in the Chixulub Impact Crater, Yucatan, Mexico,” Geofisica Internacional, Vol. 40, 2001, pp. 271-283.
[26] Geometrics, “Operation Manual for Stratagem Systems Running IMAGEM Ver. 2.16,” Geometrics San Jose Californi, 2000.
[27] T. Ndougsa-Mbarga, E. Manguelle-Dicoum, S. Mbom-Abane and C. T. Tabod, “Deep Crustal Structures along the North Eastern Margin of the Congo Craton in the Abong-Mbang/Bertoua Region Cameroon Based on Gravity Data,” Electronics Memories of the 2nd Cuban Geophysical Congress and the 4th Latin American Geophysical Conference, 2002, 15 p.

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