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Research Articles

Integrated geophysical study of the Subika Gold Deposit in the Sefwi Belt, Ghana

, ORCID Icon, & | (Reviewing editor)
Article: 1585406 | Received 19 Jun 2017, Accepted 18 Feb 2019, Published online: 03 Apr 2019

References

  • Airo, M. L. (2002). Aeromagnetic and aeroradiometric response to hydrothermal alteration. Surveys in Geophysics, 23, 1–16. doi:10.1023/A:1015556614694
  • Airo, M. L. (2005). Aerogeophysics in Finland 1972 – 2004: Methods, system characteristics and applications. Geological Survey of Finland Special Paper, 39, 1-197.
  • Allibone, A. H., McCuaig, T. C., Harris, D., Etheridge, M., Munroe, S., Byrne, D., Gyapong, W. (2002). Structural controls on gold mineralization at the Ashanti gold deposit (Vol. 9, pp. 65–93). Obuasi, Ghana: Society of Economic Geologists, Special Publication.
  • Anand, R. R., Wildman, J. E., Varga, Z. S., & Phang, C. (2001). Regolith evolution and geochemical dispersion in transported and residual regolith—bronzewing gold deposit. Geochemistry: Exploration, Environment, Analysis, 1(12), 256–276. doi:10.1144/geochem.1.3.265
  • Boadi, B., Wemegah, D. D., & Preko, K. (2013). Geological and structural interpretation of the Konongo area of the Ashanti gold belt of Ghana from aeromagnetic and radiometric data. International Research Journal of Geology and Mining, 3(3), 124–135. ISSN 2276-6618.
  • Clark, D. A. (1997). Magnetic petrophysics and magnetic petrology: Aids to geological interpretation of magnetic surveys. AGSO Journal of Australian Geology and Geophysics, 17(2), 83–103.
  • Connell, S., Hunt, P., & Li, J. (2004). Electrical conductivity mechanism of graphitic shale from the Astarte River Formation, Piling Group, Baffin Island, Nunavut’. Geological Survey of Canada Current Research, C5, 1–9.
  • Connell, S., Scromeda, N., Katsube, T. J., & Mwenifumbo, J. (2000). The electricalcharacteristics of mineralised and non-mineralised rocks from Giant and Con mine areas. Northwest Territories: Geological Survey of Canada, Current Research 2000E.
  • Cook, K. (2007) Aeromagnetic data interpretation of Ahafo District. doi:10.1094/PDIS-91-4-0467B
  • Griffis, R. J., & Agezo, F. L. (2000). Mineral occurrence and exploration potential of northern Ghana. Mineral Commission Report.132–1133, Accra.
  • Griffis, J., Barning, K., Agezo, F. L., & Akosa, F. (2002). Gold deposits of Ghana prepared on behalf of Ghana mineral commission. Ghana: Accra, 432.
  • Groves, D. I., Goldfarb, R. J., Gebre-Mariam, M., Hagemann, S. G., & Robert, F. (1998). Orogenic gold deposits: A proposed classification in the context of their crustal distribution and relationship to other gold deposit types. Ore Geology Reviews, 13, 7–27. doi:10.1016/S0169-1368(97)00012-7
  • Jessell, M. W., Amponsah, P. O., Baratoux, L., Asiedu, D. K., Loh, G. K., & Ganne, J. (2013). Crustal-scale transcurrent shearing in the Paleoproterozoic Sefwi-Sunyani-Comoe region, West Africa. Precambrian Research, 212–213, 155–168.
  • Kesse, G. O. (1985). The rock and mineral resources of Ghana. Rotterdam: A. A. Balkema.
  • Lawrence, D. M., Treloar, P. J., Rankin, A. H., Harbidge, P., & Holliday, J. (2013). The Geology and Mineralogy of the Loulo Mining District, Mali, West Africa: Evidence for two distinct styles of orogenic gold mineralization. Economic Geology, 108, 199–227. doi:10.2113/econgeo.108.2.199
  • Mumin, A. H., Fleet, M. E., & Chryssoulis, S. L. (1994). Gold mineralization in As-rich mesothermal gold ores of the Bogosu-Prestea mining district of the Ashanti Gold Belt, Ghana: Remobilization of “invisible” gold. Mineral Deposita, 29, 445–460. doi:10.1007/BF00193506
  • Newmont Mining Corporation, Annual report 2003
  • Newmont Mining Corporation, Annual report 2004
  • Scromeda, N., Connell, S., & Katsube, T. J. (2000). Petrophysical properties of mineralized and nonmineralized rocks from Giant and Con mine areas, Northwest Territories; in: Current Research 2000 (pp. 7). Geological Survey of Canada, Calgary, Canada.
  • Tsiboah, T., & Grant, T. (2009). Application of geophysics to gold exploration in Ghana: Examples from Newmont. ASEG Extended Abstracts 2009: 20th Geophysical Conference, pp.1–5, ASEG 20th Geophysical Conference and Exhibition, February, Adelaide. doi:10.1071/ASEG2009ab089.
  • Wemegah, D. D., Preko, K., Noye, R. M., Boadi, B., Menyeh, A., Danuor, S. K., & Amenyoh, T. (2015). Geophysical Interpretation of possible gold mineralization zones in Kyerano, South-Western Ghana using aeromagnetic and radiometric datasets. Journal of Geoscience and Environment Protection, 2015(3), 67–82. doi:10.4236/gep.2015.340
  • White, A. J. R., Waters, D. J., & Robb, L. J. (2015). Exhumation-driven devolatilization as a fluid source for orogenic gold mineralization at the damang deposit, Ghana. Economic Geology. Economic Geology, 110, 1009–1025. doi:10.2113/econgeo.110.4.1009
  • Wilford, J. R., Bierwirth, P. N., & Craig, M. A. (1997). Application of airborne gamma-ray spectrometry in soil regolith mapping and applied geomorphology. AGSO Journal of Australian Geology and Geophysics, 17(2), 201–216.