Relevant bibliographies by topics / Granite emplacement – Namibia – Damara belt

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  1. Journal articles
  2. Dissertations / Theses

Academic literature on the topic 'Granite emplacement – Namibia – Damara belt'

Author: Grafiati
Published: 4 June 2021
Last updated: 16 February 2022

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Journal articles on the topic "Granite emplacement – Namibia – Damara belt"

1

Hall, Duncan, and Alexander Kisters. "From steep feeders to tabular plutons – Emplacement controls of syntectonic granitoid plutons in the Damara Belt, Namibia." Journal of African Earth Sciences 113 (January 2016): 51–64. http://dx.doi.org/10.1016/j.jafrearsci.2015.10.005.

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Kruger, Tolene, and Alexander Kisters. "Magma accumulation and segregation during regional-scale folding: The Holland’s dome granite injection complex, Damara belt, Namibia." Journal of Structural Geology 89 (August 2016): 1–18. http://dx.doi.org/10.1016/j.jsg.2016.05.002.

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Wang, Shengyun, Honghai Fan, Jinyong Chen, and Donghuan Chen. "Zircon U–Pb Geochronology, Whole-Rock Geochemistry and Petrogenesis of Biotite Granites in the Gaudeanmus Area, Namibia." Minerals 10, no. 1 (2020): 76. http://dx.doi.org/10.3390/min10010076.

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The Gaudeanmus area is located at the southern Central Zone of the Damara orogenic belt in south-western Africa. In this paper, we investigate the whole rock major and trace element compositions and Sr–Nd–Pb isotopic compositions of the biotite granite, and determine the age of the samples utilising U–Pb zircon dating methods. Our results provide an LA–collector inductively plasma mass spectrometer (ICP–MS) zircon U–Pb age for the biotite granite of 540 ± 4 Ma (i.e., earliest Cambrian). The biotite granites show the characteristics of metaluminous compositions belonging to high-K calc–alkaline
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Trumbull, R. B., M. S. Krienitz, B. Gottesmann, and M. Wiedenbeck. "Chemical and boron-isotope variations in tourmalines from an S-type granite and its source rocks: the Erongo granite and tourmalinites in the Damara Belt, Namibia." Contributions to Mineralogy and Petrology 155, no. 1 (2007): 1–18. http://dx.doi.org/10.1007/s00410-007-0227-3.

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Jung, S., A. Kröner, F. Hauff, and P. Masberg. "Petrogenesis of synorogenic diorite–granodiorite–granite complexes in the Damara Belt, Namibia: Constraints from U–Pb zircon ages and Sr–Nd–Pb isotopes." Journal of African Earth Sciences 101 (January 2015): 253–65. http://dx.doi.org/10.1016/j.jafrearsci.2014.09.015.

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Johnson, S. D., M. Poujol, and A. F. M. Kisters. "Constraining the timing and migration of collisional tectonics in the Damara Belt, Namibia: U-Pb zircon ages for the syntectonic Salem-type Stinkbank granite." South African Journal of Geology 109, no. 4 (2006): 611–24. http://dx.doi.org/10.2113/gssajg.109.4.611.

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Mondillo, Nicola, Maria Boni, Giuseppina Balassone, Nigel Forrester, Francesco Putzolu, and Licia Santoro. "Mineralogy and Genesis of the Kihabe Zn-Pb-V Prospect, Aha Hills, Northwest Botswana." Minerals 10, no. 8 (2020): 685. http://dx.doi.org/10.3390/min10080685.

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The Kihabe Zn-Pb-V > (Cu-Ag-Ge) prospect is located at the boundary between Namibia and Botswana (Aha Hills, Ngamiland District) in a strongly deformed Proterozoic fold belt, corresponding to the NE extension of the Namibian Damara Orogen. The Kihabe prospect contains Zn-Pb resources of 14.4 million tonnes at 2.84% zinc equivalent, Ag resources of 3.3 million ounces, and notable V-Ge amounts, still not evaluated at a resource level. The ores are represented by a mixed sulfide–nonsulfide mineralization. Sulfide minerals consist mainly of sphalerite, galena and pyrite in a metamorphic quartzw
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Dissertations / Theses on the topic "Granite emplacement – Namibia – Damara belt"

1

Owen, Geoffrey J. "Geology of the Kranzberg syncline and emplacement controls of the Usakos pegmatite field, Damara belt, Namibia." Thesis, Stellenbosch : University of Stellenbosch, 2011. http://hdl.handle.net/10019.1/6743.

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Thesis (MSc (Earth Sciences))--University of Stellenbosch, 2011.<br>ENGLISH ABSTRACT: The Central Zone (CZ) of the Damara belt in central Namibia is underlain by voluminous Pan-African granites and is host to numerous pegmatite occurrences, some of which have economic importance and have been mined extensively. This study discusses the occurrence, geometry, relative timing and emplacement mechanisms for the Usakos pegmatite field, located between the towns of Karibib and Usakos and within the core of the regional-scale Kranzberg syncline. Lithological mapping of the Kuiseb Formation in t
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2

Vietze, Martin Ernst. "Geology and emplacement controls of the Stinkbank granite in the south Central Zone of the Pan-African Damara Belt, Namibia." Thesis, Stellenbosch : University of Stellenbosch, 2010. http://hdl.handle.net/10019.1/4271.

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Thesis (MSc (Earth Sciences))--University of Stellenbosch, 2010.<br>ENGLISH SUMMARY: Regional mapping of the Stinkbank granite in the south Central Zone of the Damara Belt, focused on an area of ca. 150 km2 in the SW parts of the granite along well exposed sections of the Khan River to the SW of the town of Usakos. The granite forms part of the regionally widespread granite suite of Salem-type granites that intruded at ca. 550-540 Ma into amphibolite-facies rocks of the Damara Supergroup. The Stinkbank granite is intrusive into the regional-scale, NE-trending D2 Kransberg syncline, cored by sc
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3

McDermott, P. F. "Granite petrogenesis and crustal evolution studies in the Damara Pan-African orogenic belt, Namibia." Thesis, Open University, 1986. http://oro.open.ac.uk/57005/.

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Major and trace element data for Damara granitoids distinguish three geochemically distinct granitoid groups, - crustal-melt granitoids, calc-alkaline granitoids and within-plate granitoids. The overwhelming majority of the Oamara granitoids are peraluminous crustal-melt leucogranites which have elevated <sup>87</sup>Sr/<sup>86</sup>Sr ratios (> 0.710) and old model Nd ages (~ 2.0 Ga). Calc-alkaline diorites are metaluminous and have the lowest <sup>87</sup>Sr/<sup>86</sup>Sr ratios (0.704 - 0.707) and model Nd ages (OM) in the range 1.1 -1.7 Ga. Within-plate granitoids are characterised by el
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Freemantle, Guy George. "Primary uranium mineralisation of the central Damara Orogen, Namibia: a petrographic, geochemical and mineralogical account of the granite - hosted uranium deposits situated along the Swakop- and Khan River valleys." Thesis, 2017. http://hdl.handle.net/10539/23612.

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A thesis submitted to the Faculty of Science in fulfilment of the requirements for the degree of Doctor of Philosophy at the School of Geosciences University of the Witwatersrand, Johannesburg, 2017<br>Namibia, the 6th largest producer of uranium globally, has produced uranium from Pan African granite-hosted (primary) deposits since 1976, and from palaeochannel deposits since 2007; exporting 3 472 tonnes U in 2016. The large granite-hosted deposits at the Husab Mine are expected to add over 5 700 tonnes U/year at peak, while three large primary-hosted deposits remain in various stages of devel
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