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Journal articles on the topic 'Geology – Ghana'

Author: Grafiati

Published: 4 June 2021

Last updated: 6 February 2022

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1

Appiah, H. "Geology and mine exploration trends of Prestea Goldfields, Ghana." Journal of African Earth Sciences (and the Middle East) 13, no. 2 (January 1991): 235–41. http://dx.doi.org/10.1016/0899-5362(91)90008-m.

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2

Amponsah, Prince Ofori, Stefano Salvi, Didier Béziat, Luc Siebenaller, Lenka Baratoux, and Mark W. Jessell. "Geology and geochemistry of the shear-hosted Julie gold deposit, NW Ghana." Journal of African Earth Sciences 112 (December 2015): 505–23. http://dx.doi.org/10.1016/j.jafrearsci.2015.06.013.

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3

Dzigbodi-Adjimah, Komla. "Geology and geochemical patterns of the Birimian gold deposits, Ghana, West Africa." Journal of Geochemical Exploration 47, no. 1-3 (April 1993): 305–20. http://dx.doi.org/10.1016/0375-6742(93)90073-u.

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4

Bowell, R. J. "Sulfide Oxidation and Production of Gossans, Ashanti Mine, Ghana." International Geology Review 36, no. 8 (August 1994): 732–52. http://dx.doi.org/10.1080/00206819409465485.

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5

Boamah, Daniel, and Christian Koeberl. "Geology and geochemistry of shallow drill cores from the Bosumtwi impact structure, Ghana." Meteoritics & Planetary Science 38, no. 8 (August 2003): 1137–59. http://dx.doi.org/10.1111/j.1945-5100.2003.tb00304.x.

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6

Tunks, Andrew J., David Selley, Jamie R. Rogers, and Gary Brabham. "Vein mineralization at the Damang Gold Mine, Ghana: controls on mineralization." Journal of Structural Geology 26, no. 6-7 (June 2004): 1257–73. http://dx.doi.org/10.1016/j.jsg.2003.11.005.

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7

Jones, W. B. "The origin of the Bosumtwi Crater, Ghana—an historical review." Proceedings of the Geologists' Association 96, no. 3 (January 1985): 275–84. http://dx.doi.org/10.1016/s0016-7878(85)80009-2.

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8

Nzulu, Gabriel K., Babak Bakhit, Hans Högberg, Lars Hultman, and Martin Magnuson. "Elucidating Pathfinding Elements from the Kubi Gold Mine in Ghana." Minerals 11, no. 9 (August 24, 2021): 912. http://dx.doi.org/10.3390/min11090912.

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X-ray photoelectron spectroscopy (XPS) and energy dispersive X-ray spectroscopy (EDX) are applied to investigate the properties of fine-grained concentrates on artisanal, small-scale gold mining samples from the Kubi Gold Project of the Asante Gold Corporation near Dunwka-on-Offin in the Central Region of Ghana. Both techniques show that the Au-containing residual sediments are dominated by the host elements Fe, Ag, Al, N, O, Si, Hg, and Ti that either form alloys with gold or with inherent elements in the sediments. For comparison, a bulk nugget sample mainly consisting of Au forms an electrum, i.e., a solid solution with Ag. Untreated (impure) sediments, fine-grained Au concentrate, coarse-grained Au concentrate, and processed ore (Au bulk/nugget) samples were found to contain clusters of O, C, N, and Ag, with Au concentrations significantly lower than that of the related elements. This finding can be attributed to primary geochemical dispersion, which evolved from the crystallization of magma and hydrothermal liquids as well as the migration of metasomatic elements and the rapid rate of chemical weathering of lateralization in secondary processes. The results indicate that Si and Ag are strongly concomitant with Au because of their eutectic characteristics, while N, C, and O follow alongside because of their affinity to Si. These non-noble elements thus act as pathfinders for Au ores in the exploration area. This paper further discusses relationships between gold and sediments of auriferous lodes as key to determining indicator minerals of gold in mining sites.

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9

Agomor, A. K., V. V. Gordiyenko, and V. G. Lazarenkov. "REGIONAL MINERALOGICAL AND GEOCHEMICAL ZONING OF A PEGMATITE FIELD IN SOUTHERN GHANA." International Geology Review 29, no. 2 (February 1987): 151–59. http://dx.doi.org/10.1080/00206818709466132.

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10

Yidana, Sandow Mark. "Groundwater classification using multivariate statistical methods: Southern Ghana." Journal of African Earth Sciences 57, no. 5 (July 2010): 455–69. http://dx.doi.org/10.1016/j.jafrearsci.2009.12.002.

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11

Christiansen, Flemming G. "Review of Survey activities 2010." Geological Survey of Denmark and Greenland (GEUS) Bulletin 23 (July 15, 2011): 1–8. http://dx.doi.org/10.34194/geusb.v23.4775.

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This Review of Survey activities presents a selection of 19 papers reflecting the wide spectrum of activities of the Geological Survey of Denmark and Greenland, from the microscopic to the plate-tectonic level. The Survey's activities in Denmark and surrounding areas are illustrated by 12 articles covering petroleum geology, groundwater geology, applied marine geology, Quaternary stratigraphy, sea-level changes, disposal of radioactive waste and the use of satellite radar data to detect elevation changes. The depth of two earthquakes has been determined using data from array stations in Canada and Niger. Activities in Greenland are covered by six papers dealing with mineral and petroleum exploration. One paper comes with further evidence that the controversial Wegener Fault is a myth. The influence of recent climate change on the Greenland ice sheet is the subject of another article; 2010 was the warmest year ever recorded in Greenland, and the ice sheet is losing mass at an accelerating rate. The Survey's international activities are the subject of a paper dealing with quality control of geophysical data in Ghana.

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12

AMPONSAH, P. E., B. K. BANOENG-YAKUBO, G. F. PANZA, and F. VACCARI. "DETERMINISTIC SEISMIC GROUND MOTION MODELLING OF THE GREATER ACCRA METROPOLITAN AREA, SOUTHEASTERN GHANA." South African Journal of Geology 112, no. 3-4 (December 1, 2009): 317–28. http://dx.doi.org/10.2113/gssajg.112.3-4.317.

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13

Wagner, T., and T. Pletsch. "No major thermal event on the mid-Cretaceous Cote d'Ivoire-Ghana Transform Margin." Terra Nova 13, no. 3 (December 2001): 165–71. http://dx.doi.org/10.1046/j.1365-3121.2001.00333.x.

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14

CLIFT, P. D., J. LORENZO, A. CARTER, and A. J. HURFORD. "Transform tectonics and thermal rejuvenation on the Côte d’Ivoire-Ghana margin, west Africa." Journal of the Geological Society 154, no. 3 (May 1997): 483–89. http://dx.doi.org/10.1144/gsjgs.154.3.0483.

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15

Bigot-Cormier, Florence, Christophe Basile, Gérard Poupeau, Jean-Pierre Bouillin, and Erika Labrin. "Denudation of the Côte d'Ivoire-Ghana transform continental margin from apatite fission tracks." Terra Nova 17, no. 2 (April 8, 2005): 189–95. http://dx.doi.org/10.1111/j.1365-3121.2005.00605.x.

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16

Yao, Y. "Gold mineralization in Palaeoproterozoic granitoids at Obuasi, Ashanti region, Ghana: Ore geology, geochemistry and fluid characteristics." South African Journal of Geology 103, no. 3-4 (December 1, 2000): 255–78. http://dx.doi.org/10.2113/1030255.

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17

Mwanzia, Dorothy Kanini, Peace Zowa, Dennis Achoki, Ozotta Ogochukwu, Chioma Onwumelu, and Antony Hiuhu Mwangi. "Student Zone." Leading Edge 40, no. 1 (January 2021): 74–75. http://dx.doi.org/10.1190/tle40010074.1.

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More than 80 young professionals and students from around the world attended the 1st Virtual African Young Professionals and Students Geoscience Week, which took place 21–26 September 2020. Participants were from Argentina, Brazil, Congo, Germany, Ghana, Indonesia, Kenya, Malawi, Mexico, Nigeria, Rwanda, South Africa, Tanzania, Uganda, Ukraine, the United States, and Zimbabwe. Figure 1 shows a distribution map of the represented locations. A total of 12 speakers presented on a variety of interesting topics throughout the week.

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18

Chudasama, Bijal, Alok Porwal, Oliver P. Kreuzer, and Kris Butera. "Geology, geodynamics and orogenic gold prospectivity modelling of the Paleoproterozoic Kumasi Basin, Ghana, West Africa." Ore Geology Reviews 78 (October 2016): 692–711. http://dx.doi.org/10.1016/j.oregeorev.2015.08.012.

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19

Lutz, Alexandra, James M. Thomas, Greg Pohll, and W. Alan McKay. "Groundwater resource sustainability in the Nabogo Basin of Ghana." Journal of African Earth Sciences 49, no. 3 (October 2007): 61–70. http://dx.doi.org/10.1016/j.jafrearsci.2007.06.004.

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20

Blarez, E., and J. Mascle. "Shallow structures and evolution of the Ivory Coast and Ghana transform margin." Marine and Petroleum Geology 5, no. 1 (February 1988): 54–64. http://dx.doi.org/10.1016/0264-8172(88)90039-6.

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21

Amegbey, N. A., and A. A. Adimado. "Incidents of cyanide spillage in Ghana." Mineral Processing and Extractive Metallurgy 112, no. 2 (August 2003): 126–30. http://dx.doi.org/10.1179/037195503225002808.

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22

Amoateng, Paul, C. Max Finlayson, Jonathon Howard, and Ben Wilson. "A multi-faceted analysis of annual flood incidences in Kumasi, Ghana." International Journal of Disaster Risk Reduction 27 (March 2018): 105–17. http://dx.doi.org/10.1016/j.ijdrr.2017.09.044.

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23

Nyame, Frank K., Katsuo Kase, and Masahiro Yamamoto. "Spessartine Garnets in a Manganiferous Carbonate Formation from Nsuta, Ghana." Resource Geology 48, no. 1 (March 1998): 13–22. http://dx.doi.org/10.1111/j.1751-3928.1998.tb00003.x.

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24

Atta-Peters, D., and M. B. Salami. "Aptian–Maastrichtian palynomorphs from the offshore Tano Basin, western Ghana." Journal of African Earth Sciences 46, no. 4 (November 2006): 379–94. http://dx.doi.org/10.1016/j.jafrearsci.2006.07.002.

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25

Bowell, R. J. "Mineralogy and geochemistry of tropical rain forest soils: Ashanti, Ghana." Chemical Geology 106, no. 3-4 (June 1993): 345–58. http://dx.doi.org/10.1016/0009-2541(93)90036-i.

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26

Curt Stager, Jay, Kenneth Alton, Christopher H. Martin, David T. King, Lucille W. Petruny, Brendan Wiltse, and Daniel A. Livingstone. "On the Age and Origin of Lake Ejagham, Cameroon, and Its Endemic Fishes." Quaternary Research 89, no. 1 (July 20, 2017): 21–32. http://dx.doi.org/10.1017/qua.2017.37.

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AbstractLake Ejagham is a small, shallow lake in Cameroon, West Africa, which supports five endemic species of cichlid fishes in two distinct lineages. Genetic evidence suggests a relatively young age for the species flocks, but supporting geologic evidence has thus far been unavailable. Here we present diatom, geochemical, mineralogical, and radiocarbon data from two sediment cores that provide new insights into the age and origin of Lake Ejagham and its endemic fishes. Radiocarbon ages at the base of the longer core indicate that the lake formed approximately 9 ka ago, and the diatom record of the shorter core suggests that hydroclimate variability during the last 3 millennia was similar to that of other lakes in Cameroon and Ghana. These findings establish a maximum age of ca. 9 cal ka BP for the lake and its endemic species and suggest that repeated cichlid speciation in two distinct lineages occurred rapidly within the lake. Local geology and West African paleoclimate records argue against a volcanic, chemical, or climatic origin for Lake Ejagham. Although not conclusive, the morphometry of the lake and possible signs of impact-induced effects on quartz grains are instead more suggestive of a bolide impact.

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27

Tsidzi, K. E. N. "An engineering geological approach to road cutting slope design in Ghana." Geotechnical and Geological Engineering 15, no. 1 (March 1997): 31–45. http://dx.doi.org/10.1007/bf00881237.

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28

Antonio, Paul Yves Jean, Lenka Baratoux, Ricardo Ivan Ferreira Trindade, Sonia Rousse, Anani Ayite, Cristiano Lana, Mélina Macouin, et al. "West Africa in Rodinia: High quality paleomagnetic pole from the ~ 860 Ma Manso dyke swarm (Ghana)." Gondwana Research 94 (June 2021): 28–43. http://dx.doi.org/10.1016/j.gr.2021.02.010.

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29

Acquah, P. C., and A. Boateng. "Planning for mine closure: Some case studies in Ghana." Minerals & Energy - Raw Materials Report 15, no. 1 (January 2000): 23–30. http://dx.doi.org/10.1080/14041040009362548.

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30

Nsiah, Emmanuel, Emmanuel K. Appiah-Adjei, and Kwaku A. Adjei. "Hydrogeological delineation of groundwater potential zones in the Nabogo basin, Ghana." Journal of African Earth Sciences 143 (July 2018): 1–9. http://dx.doi.org/10.1016/j.jafrearsci.2018.03.016.

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31

Duah, Anthony A., Bismark A. Akurugu, Philip K. Darko, Evans Manu, and Patrick A. Mainoo. "Groundwater recharge and potential exploitation in the Densu basin, Southwestern Ghana." Journal of African Earth Sciences 183 (November 2021): 104332. http://dx.doi.org/10.1016/j.jafrearsci.2021.104332.

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32

Anani, Chris Y., Richard O. Anim, Benjamin N. Armah, Joseph F. Atichogbe, Patrick Asamoah Sakyi, Edem Mahu, and Daniel K. Asiedu. "Petrography of detrital zircons from sandstones of the Lower Devonian Accraian Formation, SE Ghana: Implications on provenance." Geological Journal 55, no. 5 (August 22, 2019): 3716–31. http://dx.doi.org/10.1002/gj.3633.

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33

Hall, A. M., M. F. Thomas, and M. B. Thorp. "Late Quaternary alluvial placer development in the humid tropics: the case of the Birim Diamond Placer, Ghana." Journal of the Geological Society 142, no. 5 (September 1985): 777–87. http://dx.doi.org/10.1144/gsjgs.142.5.0777.

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34

Adu-Gyamfi, Bismark, Rajib Shaw, and Wanglin Yan. "Assessment of housing exposure to accelerated coastal erosion in Keta Municipality of Ghana." International Journal of Disaster Risk Reduction 44 (April 2020): 101450. http://dx.doi.org/10.1016/j.ijdrr.2019.101450.

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35

Abass, Kabila, Daniel Buor, Kwadwo Afriyie, Gift Dumedah, Alex Yao Segbefi, Lawrence Guodaar, Emmanuel Kofi Garsonu, et al. "Urban sprawl and green space depletion: Implications for flood incidence in Kumasi, Ghana." International Journal of Disaster Risk Reduction 51 (December 2020): 101915. http://dx.doi.org/10.1016/j.ijdrr.2020.101915.

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36

Anani, Chris. "Sandstone petrology and provenance of the Neoproterozoic Voltaian Group in the southeastern Voltaian Basin, Ghana." Sedimentary Geology 128, no. 1-2 (October 1999): 83–98. http://dx.doi.org/10.1016/s0037-0738(99)00063-9.

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37

Dzigbodi-Adjimah, Komla. "The mineralogy and petrography of the ferruginous manganese rocks at Mankwadzi, Ghana." Journal of African Earth Sciences 38, no. 3 (February 2004): 293–315. http://dx.doi.org/10.1016/j.jafrearsci.2003.08.001.

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38

Hammond, Napoleon Q., and Hidehiko Shimazaki. "Geology and Geochemical Aspects of Ore Formation at the Prestea Mesothermal Vein Gold Deposit in the Birimian System of Ghana." International Geology Review 36, no. 8 (August 1994): 715–31. http://dx.doi.org/10.1080/00206819409465484.

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39

OSAE, Shiloh, Katsuo KASE, and Masahiro YAMAMOTO. "Ore Mineralogy and Mineral Chemistry of the Ashanti Gold Deposit at Obuasi, Ghana." Resource Geology 49, no. 1 (March 1999): 1–11. http://dx.doi.org/10.1111/j.1751-3928.1999.tb00027.x.

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40

Yidana, Sandow Mark, Samuel Ganyaglo, Bruce Banoeng-Yakubo, and Thomas Akabzaa. "A conceptual framework of groundwater flow in some crystalline aquifers in Southeastern Ghana." Journal of African Earth Sciences 59, no. 2-3 (February 2011): 185–94. http://dx.doi.org/10.1016/j.jafrearsci.2010.10.005.

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41

Jianping, Liu, Pan Xiaohua, Ma Jun, Tian Zuoji, and Wan Lunkun. "Exploration targets in the Côte d'Ivoire-Ghana transform margin in Equatorial West Africa." Petroleum Exploration and Development 37, no. 1 (February 2010): 43–50. http://dx.doi.org/10.1016/s1876-3804(10)60013-4.

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42

Sakyi, Patrick Asamoah, Johnson Manu, Ben‐Xun Su, Daniel Kwayisi, Prosper M. Nude, and Samuel Boakye Dampare. "Geochemical and Sm–Nd isotopic evidence for the composition of the Palaeoproterozoic crust of the West African Craton in Ghana." Geological Journal 54, no. 6 (November 28, 2018): 3940–57. http://dx.doi.org/10.1002/gj.3387.

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43

Dampare, Samuel B., Tsugio Shibata, Daniel K. Asiedu, Osamu Okano, Shiloh K. D. Osae, David Atta‐Peters, and Patrick A. Sakyi. "Ultramafic–mafic and granitoids supra‐subduction magmatism in the southern Ashanti volcanic belt, Ghana: Evidence from geochemistry and Nd isotopes." Geological Journal 55, no. 4 (April 2020): 2495–531. http://dx.doi.org/10.1002/gj.3512.

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44

Achaegakwo, Christopher A., and David Atta‐Peters. "Palynofacies analysis and depositional environments of Upper Cretaceous sediments in the ST‐9H well, offshore South Tano Basin, Western Ghana." Geological Journal 56, no. 6 (February 14, 2021): 3225–40. http://dx.doi.org/10.1002/gj.4097.

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45

Kuma, D. O. K. "The use of low-grade and unsound crushed rock aggregates in Ghana for construction." Geotechnical and Geological Engineering 13, no. 4 (December 1995): 217–25. http://dx.doi.org/10.1007/bf00422211.

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46

Frempong, E. M. "Field compaction control studies on road bases in a new settlement area in Ghana." Geotechnical and Geological Engineering 13, no. 4 (December 1995): 227–41. http://dx.doi.org/10.1007/bf00422212.

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47

Sakyi, Patrick Asamoah, Ben-Xun Su, Johnson Manu, Daniel Kwayisi, Chris Y. Anani, Melesse Alemayehu, Sanjeewa P. K. Malaviarachchi, Prosper M. Nude, and Ben-Can Su. "Origin and tectonic significance of the metavolcanic rocks and mafic enclaves from the Palaeoproterozoic Birimian Terrane, SE West African Craton, Ghana." Geological Magazine 157, no. 8 (March 12, 2020): 1349–66. http://dx.doi.org/10.1017/s001675681900150x.

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AbstractThe Palaeoproterozoic Birimian Supergroup of the West African Craton (WAC) consists of volcanic belts composed predominantly of basaltic and andesitic rocks and intervening sedimentary basins composed predominantly of wackes and argillites. Mafic metavolcanic rocks and granitoid-hosted enclaves from the Palaeoproterozoic Lawra Belt of Ghana were analysed for geochemical and Sr–Nd isotopic data to constrain the geological evolution of the southeastern part of the WAC. The metavolcanic rocks display mainly tholeiitic signatures, whereas the enclaves show calc-alkaline signatures. The high SiO2 contents (48.6–68.9 wt%) of the enclaves are suggestive of their evolved character. The high Th/Yb values of the samples relative to that of the mantle array may indicate derivation of their respective magmas from subduction-modified source(s). The rocks show positive εNd values of +0.79 to +2.86 (metavolcanic rocks) and +0.79 to +1.82 (enclaves). These signatures and their Nd model ages (TDM2) of 2.31–2.47 Ga (metavolcanic rocks) and 2.39–2.47 Ga (enclaves) suggest they were probably derived from juvenile mantle-derived protoliths, with possible input of subducted pre-Birimian (Archean?) rocks in their source(s). Their positive Ba–Th and negative Nb–Ta, Zr–Hf and Ti anomalies may indicate their formation through subduction-related magmatism consistent with an arc setting. We propose that the metavolcanic rocks and enclaves from the Lawra Belt formed in a similar island-arc setting. We infer that the granitoids developed through variable degrees of mixing/mingling between basic magma and granitic melt during subduction, when blobs of basic to intermediate parental magma became trapped in the granitic magma to form the enclaves.

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48

Anani, C. Y., S. Bonsu, D. Kwayisi, and D. K. Asiedu. "Geochemistry and provenance of Neoproterozoic metasedimentary rocks from the Togo structural unit, Southeastern Ghana." Journal of African Earth Sciences 153 (May 2019): 208–18. http://dx.doi.org/10.1016/j.jafrearsci.2019.03.002.

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49

Adu-Gyamfi, Bismark, Rajib Shaw, and Bernice Ofosu. "Identifying exposures of health facilities to potential disasters in the Greater Accra Metropolitan Area of Ghana." International Journal of Disaster Risk Reduction 54 (February 2021): 102028. http://dx.doi.org/10.1016/j.ijdrr.2020.102028.

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50

Moomen, Abdul-Wadood, and Ashraf Dewan. "Assessing the spatial relationships between mining and land degradation: evidence from Ghana." International Journal of Mining, Reclamation and Environment 31, no. 7 (May 23, 2016): 505–18. http://dx.doi.org/10.1080/17480930.2016.1188253.

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