Relevant bibliographies by topics / Petrology – Zimbabwe

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

Academic literature on the topic 'Petrology – Zimbabwe'

Author: Grafiati
Published: 4 June 2021
Last updated: 1 February 2022

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Journal articles on the topic "Petrology – Zimbabwe"

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JOHNSON, S. P. "High fO2 Metasomatism During Whiteschist Metamorphism, Zambezi Belt, Northern Zimbabwe." Journal of Petrology 43, no. 2 (February 1, 2002): 271–90. http://dx.doi.org/10.1093/petrology/43.2.271.

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Laurs, Brendan M., and Nathan D. Renfro. "Amethyst from Zimbabwe." Journal of Gemmology 36, no. 8 (2019): 682. http://dx.doi.org/10.15506/jog.2019.36.8.682.

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RENNER, R., E. G. NISBET, M. J. CHEADLE, N. T. ARNDT, M. J. BICKLE, and W. E. CAMERON. "Komatiite Flows from the Reliance Formation, Belingwe Belt, Zimbabwe: I. Petrography and Mineralogy." Journal of Petrology 35, no. 2 (April 1, 1994): 361–400. http://dx.doi.org/10.1093/petrology/35.2.361.

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Sweetman, Thorley M., and Paul L. Tromp. "Radiate, bladed quartz from Zimbabwe." Mineralogical Magazine 55, no. 378 (March 1991): 138–40. http://dx.doi.org/10.1180/minmag.1991.055.378.13.

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Manyeruke, Tawanda D., Thomas G. Blenkinsop, Peter Buchholz, David Love, Thomas Oberthür, Ulrich K. Vetter, and Donald W. Davis. "The age and petrology of the Chimbadzi Hill Intrusion, NW Zimbabwe: first evidence for early Paleoproterozoic magmatism in Zimbabwe." Journal of African Earth Sciences 40, no. 5 (December 2004): 281–92. http://dx.doi.org/10.1016/j.jafrearsci.2004.12.003.

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Tsunogae, T., T. Miyano, and J. Ridley. "Metamorphic P-T profiles from the Zimbabwe Craton to the Limpopo Belt, Zimbabwe." Precambrian Research 55, no. 1-4 (March 1992): 259–77. http://dx.doi.org/10.1016/0301-9268(92)90027-l.

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Grew, Edward S., Martin G. Yates, Charles K. Shearer, and Michael Wiedenbeck. "Werdingite from the Urungwe District, Zimbabwe." Mineralogical Magazine 61, no. 408 (October 1997): 713–18. http://dx.doi.org/10.1180/minmag.1997.061.408.11.

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LUAIS, B. A., and C. J. HAWKESWORTH. "The Generation of Continental Crust: An Integrated Study of Crust-Forming Processes in the Archaean of Zimbabwe." Journal of Petrology 35, no. 1 (February 1, 1994): 43–94. http://dx.doi.org/10.1093/petrology/35.1.43.

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9

Chinyama, A., R. Ncube, and W. Ela. "Critical pollution levels in Umguza River, Zimbabwe." Physics and Chemistry of the Earth, Parts A/B/C 93 (June 2016): 76–83. http://dx.doi.org/10.1016/j.pce.2016.03.008.

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Boudreau, A. E., C. Love, and M. D. Prendergast. "Halogen geochemistry of the Great Dyke, Zimbabwe." Contributions to Mineralogy and Petrology 122, no. 3 (December 11, 1995): 289–300. http://dx.doi.org/10.1007/s004100050128.

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Dissertations / Theses on the topic "Petrology – Zimbabwe"

1

Birch, Graham John. "Petrology of the Madziwa Mafic Intrusion, Zimbabwe." Thesis, Imperial College London, 1985. http://hdl.handle.net/10044/1/37640.

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Mason-Apps, Alexander Dymoke. "The petrology and geochemistry of the lower pyroxenite succession of the Great Dyke in the Mutorashanga area." Thesis, Rhodes University, 1998. http://hdl.handle.net/10962/d1005602.

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This thesis focuses on the petrology and geochemistry of the lower Pyroxenite Succession of the Great Dyke of Zimbabwe in an area to the south ofMutorashanga. Particular emphasis is placed upon the economically important chromitite C5, and on the pervasive serpentinization of olivinerich rocks. An overview of the Great Dyke, including the Satellite Dykes, the structure and stratigraphy of the Great Dyke, the economic resources of the Great Dyke, and the evolution of the Great Dyke magma, is given. A review of the geodynamic history of the Zimbabwe Archaean craton, which culminated in widespread cratonisation and emplacement of the Great Dyke is also provided. The silicate rocks of the lower Pyroxenite Succession are highly adcumulate dunites and orthopyroxenites, with well-developed granular textures and a restricted mineral assemblage of olivine and pyroxene, with very minor plagioclase and clinopyroxene. Within cyclic units, the silicate rocks commonly display a textural and modal progression from granular dunite through poikilitic harzburgite, granular harzburgite, and olivine orthopyroxenite, to granular orthopyroxenite. Chromitites commonly occur at the base of each cyclic unit, these are thin, massive, coarse-grained layers, and are shown to be modified, texturally and compositionally, by postcumulus annealing processes. The olivine-rich rocks are pervasively serpentinized to a depth of over 300 metres. The serpentites typically display well-developed pseudomorphic mesh textures, with a slight overprint of nonpseudomorphic interpenetrating textures and late-stage cross-cutting veins. X-Ray diffraction studies indicate that chrysotile is the dominant serpentine mineral, and also reveal the presence of a nickeliferous magnesium hydroxide, occurring as an intimate admixture with serpentine, and believed to be a nickel-bearing analogue of brucite. Mineral and whole rock compositions of chromitite and silicate rocks highlight the strongly magnesian nature of the Ultramafic Sequence. Studies ofthe footwall chromites below chromitite C5 are consistant with a model of replenishment of primitive magma into the Great Dyke magma chamber, at the base of each cyclic unit. The magma injection and subsequent mixing with the evolved resident magma gives rise to chromitite fonnation, and a causes a reversal of the fractionation trend, resulting in a return to more primitive compositions in the silicate rocks. The silicates display an overall fractionation trend that reflects the evolving composition of the parental magma.
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Book chapters on the topic "Petrology – Zimbabwe"

1

Wilson, A. H. "The Great Dyke of Zimbabwe." In Developments in Petrology, 365–402. Elsevier, 1996. http://dx.doi.org/10.1016/s0167-2894(96)80013-3.

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