Relevant bibliographies by topics / Formations (Geology) – Zimbabwe

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  1. Journal articles
  2. Dissertations / Theses
  3. Book chapters

Academic literature on the topic 'Formations (Geology) – Zimbabwe'

Author: Grafiati
Published: 4 June 2021
Last updated: 18 February 2022

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Journal articles on the topic "Formations (Geology) – Zimbabwe"

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Nutte, T. H. C., T. Oberth�r, R. Saager, and H. P. Tomschi. "The geology, mineralogy and geochemistry of the broomstock gold deposit, Kwekwe Greenstone Belt, Zimbabwe; Some implications for gold mineralization in jaspilite iron formations." Mineralogy and Petrology 39, no. 2 (1988): 145–62. http://dx.doi.org/10.1007/bf01184820.

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Jelsma, H. A., R. W. Nesbitt, and C. M. Fanning. "Exploring our current understanding of the geological evolution and mineral endowment of the Zimbabwe Craton." South African Journal of Geology 124, no. 1 (2021): 279–310. http://dx.doi.org/10.25131/sajg.124.0020.

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Abstract A.M. Macgregor (1888-1961) is remembered for his enormous contribution to geology. His maps changed the course of geological thinking in southern Africa. Following in his footsteps we examine aspects of our current understanding of the geological evolution of the Zimbabwe Craton and, using new SHRIMP U-Pb ages of zircons from felsic volcanic and plutonic rocks from northern Zimbabwe and unpublished data related to the seminal paper by Wilson et al. (1995), a synthesis is proposed for the formation of the Neoarchaean greenstones. The data suggest marked differences (lithostratigraphy,
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Fedo, Christopher M., Kenneth A. Eriksson, and Tom G. Blenkinsop. "Geologic history of the Archean Buhwa Greenstone Belt and surrounding granite–gneiss terrane, Zimbabwe, with implications for the evolution of the Limpopo Belt." Canadian Journal of Earth Sciences 32, no. 11 (1995): 1977–90. http://dx.doi.org/10.1139/e95-151.

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The Buhwa Greenstone Belt (BGB) of southern Zimbabwe is the only major greenstone belt in the Archean Zimbabwe Craton directly adjacent to the granulite-facies rocks that constitute the Northern Marginal Zone of the Limpopo Belt. The deformational history and assembly of the BGB shed light on the evolution of the Northern Marginal Zone – Zimbabwe Craton transition. Assembly of the region began with deposition of the dominantly sedimentary cover succession at ~3.0 Ga on banded gneisses of the ~3.5 Ga Tokwe segment. At ~2.9 Ga the northern margin of the greenstone belt experienced kilometres of
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Abell, P. I., J. McClory, A. Martin, E. G. Nisbet, and T. K. Kyser. "Petrography and stable isotope ratios from Archaean stromatolites, Mushandike Formation, Zimbabwe." Precambrian Research 27, no. 4 (1985): 385–98. http://dx.doi.org/10.1016/0301-9268(85)90095-6.

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Horstwood, Matthew S. A., Robert W. Nesbitt, Stephen R. Noble, and James F. Wilson. "U-Pb zircon evidence for an extensive early Archean craton in Zimbabwe: A reassessment of the timing of craton formation, stabilization, and growth." Geology 27, no. 8 (1999): 707. http://dx.doi.org/10.1130/0091-7613(1999)027<0707:upzefa>2.3.co;2.

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Barrett, Paul M., Lara Sciscio, Pia A. Viglietti, et al. "The age of the Tashinga Formation (Karoo Supergroup) in the Mid-Zambezi Basin, Zimbabwe and the first phytosaur from mainland sub-Saharan Africa." Gondwana Research 81 (May 2020): 445–60. http://dx.doi.org/10.1016/j.gr.2019.12.008.

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WILSON, A. H. "The Geology of the Great Dyke, Zimbabwe: Crystallization, Layering, and Cumulate Formation in the P1 Pyroxenite of Cyclic Unit 1 of the Darwendale Subchamber." Journal of Petrology 33, no. 3 (1992): 611–63. http://dx.doi.org/10.1093/petrology/33.3.611.

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Chaumba, Jeff B., and Caston T. Musa. "Formation of the main sulfide zone at Unki Mine, Shurugwi Subchamber of the Great Dyke, Zimbabwe: Constraints from petrography and sulfide compositions." Geosphere 16, no. 2 (2020): 685–710. http://dx.doi.org/10.1130/ges02150.1.

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Abstract The major platinum group element (PGE) occurrence in the Great Dyke of Zimbabwe, the main sulfide zone, is a tabular stratabound layer hosted in pyroxenites, and it is broadly similar in form throughout the length of the Great Dyke. We conducted a petrographic and sulfide composition study on a sulfide-enriched zone from the contact of the mafic sequence–ultramafic sequence through the main sulfide zone at Unki Mine in the Shurugwi Subchamber to its underlying footwall rocks to place some constraints on the origin of the rocks. Pyrrhotite, pentlandite, chalcopyrite, and pyrite are the
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Johnson, S. P., and G. J. H. Oliver. "Mesoproterozoic oceanic subduction, island-arc formation and the initiation of back-arc spreading in the Kibaran Belt of central, southern Africa: evidence from the Ophiolite Terrane, Chewore Inliers, northern Zimbabwe." Precambrian Research 103, no. 3-4 (2000): 125–46. http://dx.doi.org/10.1016/s0301-9268(00)00075-9.

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Sciscio, Lara, Pia A. Viglietti, Paul M. Barrett, et al. "Sedimentology and palaeontology of the Upper Karoo Group in the Mid-Zambezi Basin, Zimbabwe: new localities and their implications for interbasinal correlation." Geological Magazine, October 26, 2020, 1–24. http://dx.doi.org/10.1017/s0016756820001089.

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Abstract The Triassic–Jurassic Upper Karoo Group of the Mid-Zambezi Basin (MZB; Zimbabwe) includes a thick succession of terrestrial sediments with high palaeontological potential that has been neglected since the 1970s. Here, we review the Upper Karoo Group stratigraphy, present detailed sedimentological work and identify new vertebrate-bearing sites at several measured sections along the southern shore of Lake Kariba. These fossil-bearing sites fall within the Pebbly Arkose and Forest Sandstone formations, and are the first to be recorded from the region since the discovery of Vulcanodon kar
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Dissertations / Theses on the topic "Formations (Geology) – Zimbabwe"

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Fisher, Nicola Jane. "Deformation induced fluid flow and gold precipitation in banded iron-formation, Zimbabwe." Thesis, University of Southampton, 1992. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.238887.

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Gilligan, Jonathan Mark. "The geology, geochemistry and genesis of gold mineralization associated with Archaean iron-formation, Lennox mine, Zimbabwe." Thesis, University of Southampton, 1990. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.292080.

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Landoll, John David. "The role of crustal interactions in the formation of cogenetic silica oversaturated and undersaturated syenites: evidence from the alkaline complexes of Abu Khruq (Egypt), Mt. Shefford (Quebec), and Marangudzi (Zimbabwe) /." The Ohio State University, 1994. http://rave.ohiolink.edu/etdc/view?acc_num=osu1487853913100352.

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Dittrich, Thomas. "Meso- to Neoarchean Lithium-Cesium-Tantalum- (LCT-) Pegmatites (Western Australia, Zimbabwe) and a Genetic Model for the Formation of Massive Pollucite Mineralisations." Doctoral thesis, Technische Universitaet Bergakademie Freiberg Universitaetsbibliothek "Georgius Agricola", 2017. http://nbn-resolving.de/urn:nbn:de:bsz:105-qucosa-228968.

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Lithium Cesium Tantalum (LCT) pegmatites are important resources for rare metals like Cesium, Lithium or Tantalum, whose demand increased markedly during the past decade. At present, Cs is known to occur in economic quantities only from the two LCT pegmatite deposits at Bikita located in Zimbabwe and Tanco in Canada. Host for this Cs mineralisation is the extreme rare zeolite group mineral pollucite. However, at Bikita and Tanco, pollucite forms huge massive, lensoid shaped and almost monomineralic pollucite mineralisations that occur within the upper portions of the pegmatite. In addition, bo
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Dittrich, Thomas. "Meso- to Neoarchean Lithium-Cesium-Tantalum- (LCT-) Pegmatites (Western Australia, Zimbabwe) and a Genetic Model for the Formation of Massive Pollucite Mineralisations." Doctoral thesis, 2016. https://tubaf.qucosa.de/id/qucosa%3A23157.

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Lithium Cesium Tantalum (LCT) pegmatites are important resources for rare metals like Cesium, Lithium or Tantalum, whose demand increased markedly during the past decade. At present, Cs is known to occur in economic quantities only from the two LCT pegmatite deposits at Bikita located in Zimbabwe and Tanco in Canada. Host for this Cs mineralisation is the extreme rare zeolite group mineral pollucite. However, at Bikita and Tanco, pollucite forms huge massive, lensoid shaped and almost monomineralic pollucite mineralisations that occur within the upper portions of the pegmatite. In addition, bo
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Book chapters on the topic "Formations (Geology) – Zimbabwe"

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Orpen, J. L., A. Martin, M. J. Bickle, and E. G. Nisbet. "The Mtshingwe Group in the west: Andesites, basalts, komatiites and sediments of the Hokonui, Bend and Koodoovale Formations." In The Geology of the Belingwe Greenstone Belt, Zimbabwe. CRC Press, 2020. http://dx.doi.org/10.1201/9781003077596-4.

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Nisbet, E. G., M. J. Bickle, J. L. Orpen, and A. Martin. "Controls on the formation of the Belingwe Greenstone Belt, Zimbabwe." In The Geology of the Belingwe Greenstone Belt, Zimbabwe. CRC Press, 2020. http://dx.doi.org/10.1201/9781003077596-9.

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Nisbet, E. G., M. J. Bickle, A. Martin, and J. L. Orpen. "Sedimentology of the Brooklands Formation, Zimbabwe: Development of an Archaean greenstone belt in a rifted graben." In The Geology of the Belingwe Greenstone Belt, Zimbabwe. CRC Press, 2020. http://dx.doi.org/10.1201/9781003077596-5.

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