Academic literature on the topic 'Swaziland geology'

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Journal articles on the topic "Swaziland geology"

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Scholten, T., P. Felix-Henningsen, and M. Schotte. "Geology, soils and saprolites of the Swaziland Middleveld." Soil Technology 11, no. 3 (1997): 229–46. http://dx.doi.org/10.1016/s0933-3630(97)00010-x.

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Mabuza, M., and R. J. Thomas. "16th international colloquium of African geology, Ezulwini, Swaziland, September 1993." Journal of African Earth Sciences 18, no. 4 (1994): 261. http://dx.doi.org/10.1016/0899-5362(94)90067-1.

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Turner, B. R., and W. E. L. Minter. "Diamond-bearing upper Karoo fluvial sediments in NE Swaziland." Journal of the Geological Society 142, no. 5 (1985): 765–76. http://dx.doi.org/10.1144/gsjgs.142.5.0765.

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Schoene, B., and S. A. Bowring. "Rates and mechanisms of Mesoarchean magmatic arc construction, eastern Kaapvaal craton, Swaziland." Geological Society of America Bulletin 122, no. 3-4 (2009): 408–29. http://dx.doi.org/10.1130/b26501.1.

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Hunter, D. R. "Geochemical heterogeneity of the bimodal suite, swaziland: Implications for crustal growth." Chemical Geology 70, no. 1-2 (1988): 145. http://dx.doi.org/10.1016/0009-2541(88)90618-3.

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de Villiers, S., and M. J. de Wit. "Sources of river water radiogenic strontium: examples from the Achaean granite dominated catchments of Swaziland." South African Journal of Geology 110, no. 2-3 (2007): 349–66. http://dx.doi.org/10.2113/gssajg.110.2-3.349.

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Knauth, L. Paul, and Donald R. Lowe. "High Archean climatic temperature inferred from oxygen isotope geochemistry of cherts in the 3.5 Ga Swaziland Supergroup, South Africa." Geological Society of America Bulletin 115 (May 2003): 566–80. http://dx.doi.org/10.1130/0016-7606(2003)115<0566:hactif>2.0.co;2.

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TAYLOR, J., G. STEVENS, and C. LANA. "AGE AND FIELD RELATIONSHIPS OF MAHAMBA ORTHOGNEISSES AND MKHONDO VALLEY METAMORPHIC SUITE PARAGNEISSES FROM THE MKHONDO RIVER, ANCIENT GNEISS COMPLEX, SWAZILAND." South African Journal of Geology 115, no. 3 (2012): 369–84. http://dx.doi.org/10.2113/gssajg.115.3.369.

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Goosmann, E. A., R. Buick, D. C. Catling, C. Luskin, and N. Nhleko. "Vesicle paleobarometry in the Pongola Supergroup: A cautionary note and guidelines for future studies." South African Journal of Geology 123, no. 1 (2020): 95–104. http://dx.doi.org/10.25131/sajg.123.0005.

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Abstract Earth’s global barometric pressure, currently 1 bar at sea level, may have changed over its 4.5-billion-year history. Proxy measurements, including N2/36Ar ratios in ~3.5 to 3.0 Ga hydrothermal quartz, ~2.7 Ga raindrop imprints, and ~2.7 Ga vesicle sizes in subaerial basalt lava flows indicate Archean air pressure could have been between 0.1 and 1.2 bar. However, some models argue air pressure in the Archean should have been much higher than now and could allow pressure broadening of greenhouse gas absorption lines to counteract the “Faint Young Sun”. Thus, additional paleobarometric
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Zeh, Armin, Axel Gerdes, and Leo Millonig. "Hafnium isotope record of the Ancient Gneiss Complex, Swaziland, southern Africa: evidence for Archaean crust–mantle formation and crust reworking between 3.66 and 2.73 Ga." Journal of the Geological Society 168, no. 4 (2011): 953–64. http://dx.doi.org/10.1144/0016-76492010-117.

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Dissertations / Theses on the topic "Swaziland geology"

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Kanya, Leo L. (Leo Linda) Carleton University Dissertation Earth Sciences. "Geology of Nhlangano-Mahamba area, Shiselweni Region, southwestern Swaziland." Ottawa, 1994.

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"The Pongola Supergroup in Swaziland." Thesis, 2009. http://hdl.handle.net/10210/1966.

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D.Phil.<br>The Mesoarchean Pongola Supergroup, cropping out in the southeastern region of the Kaapvaal craton, is one of the oldest known supracrustal successions in the world. It represents an erosional remnant of a once extensive cratonic cover sequence. The succession is subdivided into the lower Nsuze Group, a volcano sedimentary succession, and the Mozaan Group composed mainly of siliciclastics and minor volcanics. The Mozaan Group is host to the world’s oldest known glacial deposit. The Pongola Supergroup is well preserved both geochemically and structurally. Outcrops extend from the nor
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Jones, D. H. "Geology and gold mineralization of the Hhohho area, Northwestern Swaziland." Thesis, 2015. http://hdl.handle.net/10539/17470.

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Mabuza, Mbongeni Henry. "The geology and geochemistry of the volcanic rocks of the Pongola sequence in southern Swaziland." Thesis, 1993. http://hdl.handle.net/10413/7898.

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The ~3.0 Ga Pongola Sequence, comprising a lower dominantly volcanic Nsuze Group and an upper largely sedimentary Mozaan Group, crops out in the Mahlangatsha and Kubuta areas of southern Swaziland. The Nsuze Group consists of basaltic, andesitic, dacitic and rhyolitic rocks with intercalations of ferruginous shale and pyrophyllitic schists. The Mozaan Group comprises quartzites, ferruginous shales, basalts and minor amounts of andalusite and sericitic schists. In the study area in southern Swaziland the Pongola Sequence is represented by a northerly striking lens of metavolcanic basaltic rocks
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Nhleko, Noah. "Stratigraphy of the Archean Mozaan Group in the Kubuta-Mooihoek area, Swaziland." Thesis, 2012. http://hdl.handle.net/10210/6405.

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M.Sc.<br>Known outcrops of the supracrustal Mesoarchean Mozaan Group of the Pongola Supergroup occur in north-eastern Kwazulu-Natal and southern Mpumalanga in South Africa, and southern Swaziland. Outcrops of the Mozaan succession in Swaziland are preserved in the Ntungulu-Mahlangatsha and Kubuta-Mooihoek areas. The succession is composed of polymictic conglomerate, poorly sorted scour based quartzite, orthoquartzite, shale, iron-formation, polymictic diamictite and lava. In the Kubuta- Mooihoek area a 3000m thick succession is preserved and correlates almost bed for bed with that in the Hartl
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"An integrated field, geochemical and geochronological study of archaean rock units in Southern Swaziland." Thesis, 2015. http://hdl.handle.net/10210/13700.

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M.Sc. (Geology)<br>This study represents the first detailed field, geochemical and geochronological study of Archaean rock units that crop out along the Ncotshane River in the southern part of Swaziland. These rock units were mapped as Mahamba Gneiss in the geological map of Swaziland (Wilson, 1982). However, field examination indicated that the area consists of a heterogeneous assemblage of serpentinite, amphibolite, gabbroic gneiss, quartzite, meta-ironstone, augen gneiss, granitic gneiss and diorite, all of which are intimately associated with weakly foliated granite and dolerite. Serpentin
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Cole, Edward George. "Lithostratigraphy and depositional environment of the Archaean Nsuze Group, Pongola Supergroup." Thesis, 2014. http://hdl.handle.net/10210/11447.

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Books on the topic "Swaziland geology"

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M, Turner L., ed. A review of metamorphism in the Republic of South Africa and the kingdoms of Lesotho and Swaziland. Council for Geoscience, Geological Survey of South Africa, 1995.

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Visser, D. J. L. Expl anation of the 1:1 000 000 geological map, fourth edition, 1984: The geology of the Republics of South Africa, Transkei, Bophuthatswana, Venda, and Ciskei and the kingdoms of Lesotho and Swaziland. Geological Survey, 1989.

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Book chapters on the topic "Swaziland geology"

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Lowe, Donald R. "Petrology and sedimentology of cherts and related silicified sedimentary rocks in the Swaziland Supergroup." In Geologic Evolution of the Barberton Greenstone Belt, South Africa. Geological Society of America, 1999. http://dx.doi.org/10.1130/0-8137-2329-9.83.

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Walsh, Maud M., and Donald R. Lowe. "Modes of accumulation of carbonaceous matter in the early Archean: A petrographic and geochemical study of the carbonaceous cherts of the Swaziland Supergroup." In Geologic Evolution of the Barberton Greenstone Belt, South Africa. Geological Society of America, 1999. http://dx.doi.org/10.1130/0-8137-2329-9.115.

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