Relevant bibliographies by topics / Kaapval

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  1. Journal articles
  2. Dissertations / Theses
  3. Books
  4. Book chapters
  5. Conference papers

Academic literature on the topic 'Kaapval'

Author: Grafiati
Published: 14 June 2025
Last updated: 2 August 2025

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Journal articles on the topic "Kaapval"

1

Cuney, Michel. "Felsic magmatism and uranium deposits." Bulletin de la Société Géologique de France 185, no. 2 (2014): 75–92. http://dx.doi.org/10.2113/gssgfbull.185.2.75.

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Abstract The strongly incompatible behaviour of uranium in silicate magmas results in its concentration in the most felsic melts and a prevalence of granites and rhyolites as primary U sources for the formation of U deposits. Despite its incompatible behavior, U deposits resulting directly from magmatic processes are quite rare. In most deposits, U is mobilized by hydrothermal fluids or ground water well after the emplacement of the igneous rocks. Of the broad range of granite types, only a few have U contents and physico-chemical properties that permit the crystallization of accessory mineral
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Baptiste, V., and A. Tommasi. "Petrophysical constraints on the seismic properties of the Kaapvaal craton mantle root." Solid Earth Discussions 5, no. 2 (2013): 963–1005. http://dx.doi.org/10.5194/sed-5-963-2013.

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Abstract. We calculated the seismic properties of 47 mantle xenoliths from 9 kimberlitic pipes in the Kaapvaal craton based on their modal composition, the crystal preferred orientations (CPO) of olivine, ortho- and clinopyroxene, and garnet, the Fe content of olivine, and the pressures and temperatures at which the rocks were equilibrated. These data allow constraining the variation of seismic anisotropy and velocities with depth. The fastest P wave and fast split shear wave (S1) polarization direction is always close to olivine [100] maximum. Changes in olivine CPO symmetry result in minor v
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Rasmussen, Birger, Jian-Wei Zi, and Janet R. Muhling. "U-Pb evidence for a 2.15 Ga orogenic event in the Archean Kaapvaal (South Africa) and Pilbara (Western Australia) cratons." Geology 47, no. 12 (2019): 1131–35. http://dx.doi.org/10.1130/g46366.1.

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Abstract There is geological evidence for widespread deformation in the Kaapvaal craton, South Africa, between 2.2 and 2.0 Ga. In Griqualand West, post-Ongeluk Formation (ca. 2.42 Ga) and pre-Mapedi Formation (>1.91 Ga) folding, faulting, and uplift have been linked to the development of a regional-scale unconformity, weathering horizons, and extensive Fe-oxide mineralization. However, the lack of deformational fabrics and the low metamorphic temperatures (<300 °C) have hampered efforts to date this event. Here we show that metamorphic monazite in Neoarchean shales from four stratigraphi
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Moore, A. E., T. G. Blenkinsop, R. M. Key, W. D. Maier, and R. B. M. Mapeo. "Tectonic triggers for the intrusion of the Great Dyke (Zimbabwe) and Bushveld Complex (South Africa)." South African Journal of Geology 128, no. 1 (2025): 73–90. https://doi.org/10.25131/sajg.128.0002.

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Abstract Two of the world’s largest layered igneous complexes – the Great Dyke in Zimbabwe (2 575 ± 0.7 Ma) and the Bushveld Complex in South Africa (2 056 ± 1 Ma) were intruded broadly coeval with major compressive events associated with orogenic belts along the margins of their host cratons (the Zimbabwe and Kaapvaal cratons, respectively). Thus, the Northern Marginal Zone of the Limpopo Belt, which bounds the Zimbabwe Craton in the south, experienced a major north-northwest shortening event at some time between 2.74 and 2.57 Ga, with a metamorphic peak at ~2.59 Ga. Therefore, this time span
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Rollinson, H. R. "A terrane interpretation of the Archaean Limpopo Belt." Geological Magazine 130, no. 6 (1993): 755–65. http://dx.doi.org/10.1017/s001675680002313x.

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AbstractThe Limpopo Belt is a zone of thickened Archaean crust whose origin is currently explained by a late Archaean continent-continent collision between the Kaapvaal and Zimbabwe cratons. This review shows that the two cratons have fundamentally different geological histories and that the Zimbabwe Craton was unlikely to have behaved as a stable ‘cratonic’ block at the time of the Limpopo Belt collision. The geological histories of the Zimbabwe Craton, the North Marginal, Central and South Marginal zones of the Limpopo Belt and the Kaapvaal Craton are shown to be sufficiently different from
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Baptiste, V., and A. Tommasi. "Petrophysical constraints on the seismic properties of the Kaapvaal craton mantle root." Solid Earth 5, no. 1 (2014): 45–63. http://dx.doi.org/10.5194/se-5-45-2014.

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Abstract. We calculated the seismic properties of 47 mantle xenoliths from 9 kimberlitic pipes in the Kaapvaal craton based on their modal composition, the crystal-preferred orientations (CPO) of olivine, ortho- and clinopyroxene, and garnet, the Fe content of olivine, and the pressures and temperatures at which the rocks were equilibrated. These data allow constraining the variation of seismic anisotropy and velocities within the cratonic mantle. The fastest P and S2 wave propagation directions and the polarization of fast split shear waves (S1) are always subparallel to olivine [100] axes of
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Hofmann, A., H. Xie, L. Saha, and C. Reinke. "Granitoids and greenstones of the White Mfolozi Inlier, south-east Kaapvaal Craton." South African Journal of Geology 123, no. 3 (2020): 263–76. http://dx.doi.org/10.25131/sajg.123.0019.

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Abstract A Palaeoarchaean greenstone fragment and associated granitoid gneisses from an area south of Ulundi in KwaZulu-Natal is described. The fragment consists of an association of garnetiferous amphibolite and calc-silicate that was intruded at 3388 ± 4 Ma by tonalite and at 3275 ± 4 Ma by trondhjemite. Strong ductile deformation of the greenstones and granitoids under amphibolite facies conditions (7 kbar and 600 to 650°C) took place prior to uplift and emplacement of a granite batholith at ~3.25 Ga ago in which the granitoid gneiss-greenstone domain is now found. Magmatism 3.27 to 3.25 Ga
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de Wit, M. J. "Kaapvaal Craton special volume- An introduction." South African Journal of Geology 107, no. 1-2 (2004): 1–6. http://dx.doi.org/10.2113/107.1-2.1.

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Herzberg, Claude T. "Lithosphere peridotites of the Kaapvaal craton." Earth and Planetary Science Letters 120, no. 1-2 (1993): 13–29. http://dx.doi.org/10.1016/0012-821x(93)90020-a.

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Jones, M. Q. W. "Heat flow in the Bushveld Complex, South Africa: implications for upper mantle structure." South African Journal of Geology 120, no. 3 (2017): 351–70. http://dx.doi.org/10.25131/gssajg.120.3.351.

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Abstract Geothermal measurements in South Africa since 1939 have resulted in a good coverage of heat flow observations. The Archaean Kaapvaal Craton, in the central part of South Africa, is the best-studied tectonic domain, with nearly 150 heat flow measurements. The greatest density of heat flow sites is in the Witwatersrand Basin goldfields, where geothermal data are essential for determining refrigeration requirements of deep (up to 4 km) gold mines; the average heat flow is 51 ± 6mWm-2. The Bushveld Complex north of the Witwatersrand Basin is an extensive 2.06 Ga ultramafic-felsic intrusiv
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Dissertations / Theses on the topic "Kaapval"

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Chugunov, Aleksandr. "L'évolution de la composition du manteau de l'Archeen : les preuves du magmatisme du craton du Kaapval." Electronic Thesis or Diss., Université Grenoble Alpes, 2025. http://www.theses.fr/2025GRALU002.

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Les komatiites proviennent des laves les plus chaudes et les plus magnésiennes de la Terre et ont été utilisées comme sondes de l'évolution séculaire du manteau terrestre. Les phénocristaux d'olivine trouvés dans les komatiites archéennes se sont révélés être des conteneurs efficaces pour préserver les matières fondues de l'environnement extérieur. L'olivine étant le premier minéral à cristalliser dans la fonte komatiitique, les inclusions d'olivine à haute teneur en magnésium fournissent des informations uniques sur le manteau terrestre primitif.Cette thèse caractérise les fontes komatiitique
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Bekker, Andrey. "Chemostratigraphy of the Early Paleoproterozoic carbonate successions (Kaapvaal and Wyoming cratons)." Diss., Virginia Tech, 2001. http://hdl.handle.net/10919/28965.

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Evidence of three glaciations in Paleoproterozoic successions of North America and at least one on three other continents, suggests that these glaciations were of global extent. In common with the Neoproterozoic record, carbonates cap the glacials. However, the relationship between biogeochemical cycling of carbon and ice ages has not been fully appreciated. This research involved the sedimentology and isotope stratigraphy of carbonates and shales in Paleoproterozoic glacially-influenced successions of Wyoming and South Africa. Carbonates of the Vagner Formation cap the middle of three dia
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Larson, Angela Marie. "S-wave velocity structure beneath the Kaapvaal Craton from surface-wave inversions compared with estimates from mantle xenoliths." Thesis, Virginia Tech, 2004. http://hdl.handle.net/10919/34200.

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Results from two-station surface-wave inversions across the Archean Kaapvaal craton of southern Africa are compared with seismic velocities estimated from approximately 100 mantle xenoliths brought to the surface in kimberlite pipes. As the xenoliths represent a snapshot of the mantle at the time of their eruption, comparison with recently recorded seismic data provides an opportunity to compare and contrast the independently gained results. These cratonic xenoliths from the southern Kaapvaal, all less than 100Ma in age, have been analyzed geothermobarometrically to obtain the equilibrium P-T
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Burger, Erasmus Petrus. "An Investigation of the carbonatites of the Kaapvaal Craton and their tectonic context." Diss., University of Pretoria, 2013. http://hdl.handle.net/2263/43297.

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Carbonatites are exotic rocks which usually occur in discrete intrusions. Considering the association of carbonatites with rifting environments, this dissertation proposes that: carbonatites occur in extensional tectonic settings and therefore carbonatite occurrence can be used to constrain an extensional setting for related occurrences. In order to give context in which to consider this hypothesis, the formation of carbonatites is reviewed. This work favours the direct mantle melting model as it is most relevant and consistent with observations of Kaapvaal Craton carbonatites. However t
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Schoene, Robert Blair. "A thermotectonic framework for the growth and stabilization of the eastern Kaapvaal craton, southern Africa." Thesis, Massachusetts Institute of Technology, 2006. http://hdl.handle.net/1721.1/38251.

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Thesis (Ph. D.)--Massachusetts Institute of Technology, Dept. of Earth, Atmospheric, and Planetary Sciences, 2006.<br>Includes bibliographical references.<br>Continents are an amalgamation of crust and mantle lithosphere assembled over -4 Gyr and are therefore our best record of the early Earth. Exposures of rocks -3.0-3.7 Ga cover -20,000 km2 of eastern S. Africa and Swaziland, and provide a record of the continental assembly and subsequent stabilization of the eastern Kaapvaal craton. This thesis uses structural, geochronological, thermochronological and isotopic constraints to examine the t
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Tinker, Justine. "Stratigraphic and structural interpretation of seismic reflection data across selected sections of the Kaapvaal Craton." Master's thesis, University of Cape Town, 2001. http://hdl.handle.net/11427/9739.

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Includes bibliography.<br>The Kaapvaal Craton is one of the best preserved of all Archean cratons. It is partially covered by the supracrustal sequences of the Witwatersrand, Ventersdorp and Transvaal Basin (and correlated Griqualand West Basin), which span almost a billion years (~3.1 to 2.2 Ga). This thesis describes and interprets eight newly available seismic reflection profiles, acquired by the vibroseis method to 6 seconds TWT, and totaling ~720 km in length. New stratigraphic and structural features are identified across three main regions: the Kaapvaal Craton's western margin, the north
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Sonwa, Cyrille Stephane Tsakou. "Analysis of the structural geology of the high-grade metamorphic rocks in part of the Kakamas terrane of an area adjacent to the Neusspruit shear zone South of the orange river, Northern Cape, South Africa." University of the Western Cape, 2021. http://hdl.handle.net/11394/8257.

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>Magister Scientiae - MSc<br>The Proterozoic Namaqua-Natal Province comprises highly deformed rocks of medium to high grade metamorphism and is bordering the Archean Kaapvaal Craton to the west, south and east in South Africa. The sector to the west of the Craton, namely the Namaqua Sector, is structurally complex and subdivided from west to east into the Bushmanland Subprovince, the Kakamas and Areachap terranes of the Gordonia Subprovince and the Kheis Subprovince. The prominent Neusberg Mountain Range, with exposures to the north and south of the Orange River in the Kakamas Terrane constitu
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Smildzins, V. (Viesturs). "Using mineral chemistry to constrain P-T conditions for mantle xenoliths from the Kaapvaal craton, South Africa." Master's thesis, University of Oulu, 2016. http://urn.fi/URN:NBN:fi:oulu-201611233107.

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Kimberlites are igneous rocks that originate by small degrees of melting of the mantle. Notably, kimberlites carry large variety of crustal and mantle xenoliths. Geochemical data on xenoliths can provide insights into the processes occurring in the subcontinental lithosphere (SCLM) and deeper. The Kaapvaal craton in South Africa hosts one of the best-studied kimberlite populations on Earth. In this thesis, a total of 24 thin sections of peridotite xenoliths from Group I Letlhakane, Letseng, Premier and Frank Smith kimberlites were investigated to constrain the pressure, temperature and depth
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Nethenzheni, Sedzani Shane. "The geochemistry, geochronology and petrogenetic characteristics of two granitic suites on the eastern margin of the Namaqua Sector, Namaqua-Natal Mobile Belt, South Africa." Thesis, University of the Western Cape, 2016. http://hdl.handle.net/11394/5209.

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>Magister Scientiae - MSc<br>The group of granites on the eastern margin of the Mesoproterozoic Namaqua sector of the polydeformed and highly metamorphosed Namaqua-Natal Province of southern Africa is known as the Keimoes Suite. The suite includes mixtures of diverse rock types not belonging to a single intrusive series and so it should be subdivided into more than one intrusive suite. The exact definition, extent, distribution and petrogenesis of these granites have been poorly defined in the past, with various authors defining the suite differently due to the lack of proper geochronology and
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Coetzee, Megan. "Geochemistry of selected South African group I, group II and transitional kimberlites located on and off the Kaapvaal craton." Master's thesis, University of Cape Town, 2004. http://hdl.handle.net/11427/4192.

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Includes bibliographical references.<br>Eighteen Jurassic to Cretaceous South African kimberlites representative of group 1, group 11 and transitional varieties that have been emplaced through both the Archean Kaapvall craton (on-craton) and Proterozoic Namaqua-Natal belt (off-craton), have been selected for a comparative study aimed at characterising their geochemistry and source region compositions, as well as understanding the petrogenetic processes that have affected them. The petrography of the analysed kimberlites is similar to typical group 1 and group 11 kimberlites, characterised by d
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Books on the topic "Kaapval"

1

Truswell, J. F. Early Proterozoic red beds on the Kaapvaal craton. University of the Witwatersrand, 1990.

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Kröner, Alfred, and Axel Hofmann, eds. The Archaean Geology of the Kaapvaal Craton, Southern Africa. Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-319-78652-0.

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Dr, Jones Alan G., Carlson R. W. 1954-, and Grutter Herman, eds. A tale of two cratons: The Slave-Kaapvaal workshop. Elsevier, 2004.

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Weilers, B. F. A review of the Pongola Supergroup and its setting on the Kaapvaal Craton. University of the Witwatersrand, 1990.

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Hofmann, Axel, and Alfred Kröner. The Archaean Geology of the Kaapvaal Craton, Southern Africa. Springer, 2019.

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(Editor), A. G. Jones, R. W. Carlson (Editor), and H. Grutter (Editor), eds. A Tale of Two Cratons: The Slave Kaapvaal Workshop. Elsevier Science, 2004.

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Gutenberg-Universität, Johannes, ed. Zur Genese des oberen Erdmantels unterhalb des Kaapvaal Kratons, Folgerungen aus isotopischen Untersuchungen an Niedrigtemperatur-Mantelxenolithen. 1993.

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Jaeckel, Petra. U-Pb Zirkon Datierungen von magmatischen und metamorphen Gesteinen der Zentralzone des Limpopo Gürtels und des nordöstlichen Kaapvaal Kratons, Südafrika. 1997.

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The Distribution of radioelements in Archaean granites of the Kaapvaal Craton, with implications for the source of uranium in the Witwatersrand Basin. University of the Witwatersrand, 1989.

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Book chapters on the topic "Kaapval"

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Arndt, Nicholas. "Kaapvaal Craton, South Africa." In Encyclopedia of Astrobiology. Springer Berlin Heidelberg, 2015. http://dx.doi.org/10.1007/978-3-662-44185-5_1894.

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Arndt, Nicholas. "Kaapvaal Craton, South Africa." In Encyclopedia of Astrobiology. Springer Berlin Heidelberg, 2011. http://dx.doi.org/10.1007/978-3-642-11274-4_1894.

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Arndt, Nicholas. "Kaapvaal Craton, South Africa." In Encyclopedia of Astrobiology. Springer Berlin Heidelberg, 2023. http://dx.doi.org/10.1007/978-3-662-65093-6_1894.

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Arndt, Nicholas. "Kaapvaal Craton, South Africa." In Encyclopedia of Astrobiology. Springer Berlin Heidelberg, 2021. http://dx.doi.org/10.1007/978-3-642-27833-4_1894-4.

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Arndt, Nicholas. "Kaapvaal Craton, South Africa." In Encyclopedia of Astrobiology. Springer Berlin Heidelberg, 2014. http://dx.doi.org/10.1007/978-3-642-27833-4_1894-3.

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Kröner, Alfred, J. Elis Hoffmann, Jean M. Wong, et al. "Archaean Crystalline Rocks of the Eastern Kaapvaal Craton." In Regional Geology Reviews. Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-319-78652-0_1.

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Luskin, Casey, Allan Wilson, Digby Gold, and Axel Hofmann. "The Pongola Supergroup: Mesoarchaean Deposition Following Kaapvaal Craton Stabilization." In Regional Geology Reviews. Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-319-78652-0_9.

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Hofmann, Axel, Carl R. Anhaeusser, John Dixon, et al. "Archaean Granitoid–Greenstone Geology of the Southeastern Part of the Kaapvaal Craton." In Regional Geology Reviews. Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-319-78652-0_2.

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Wabo, H., F. Humbert, M. O. de Kock, et al. "Constraining the Chronology of the Mashishing Dykes from the Eastern Kaapvaal Craton in South Africa." In Springer Geology. Springer Singapore, 2018. http://dx.doi.org/10.1007/978-981-13-1666-1_6.

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Glikson, Andrew Y. "Pre-3.2 Ga Evolution and Asteroid Impacts of the Barberton Greenstone Belt, Kaapvaal Craton, South Africa." In The Archaean: Geological and Geochemical Windows into the Early Earth. Springer International Publishing, 2014. http://dx.doi.org/10.1007/978-3-319-07908-0_7.

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Conference papers on the topic "Kaapval"

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de Wit, M. J., and C. M. Doucouré. "A feedback from the Kaapvaal Craton Project." In 7th SAGA Biennial Technical Meeting and Exhibition. European Association of Geoscientists & Engineers, 2001. http://dx.doi.org/10.3997/2214-4609-pdb.143.17.1.

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Durrheim, R. J., and R. W. E. Green. "Seismic Velocity Structure Of The Central Kaapvaal Craton." In 1st SAGA Biennial Conference and Exhibition. European Association of Geoscientists & Engineers, 1989. http://dx.doi.org/10.3997/2214-4609-pdb.222.015.

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Webb, S. J. "Gravity And Geoid Investigations Of The Kaapvaal Craton." In 5th SAGA Biennial Conference and Exhibition. European Association of Geoscientists & Engineers, 1997. http://dx.doi.org/10.3997/2214-4609-pdb.223.022.

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Heckel, Catharina, Alan Woodland, Jolien Linckens, and Sally A. Gibson. "Different types of sheared peridotites from Lesotho (Kaapvaal craton)." In Goldschmidt2022. European Association of Geochemistry, 2022. http://dx.doi.org/10.46427/gold2022.10998.

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Smit, Karen V., Kaydi O. Govender, Kananelo Letete, and Fezeka Dliwako. "Transitional pyroxenitic-lherzolitic xenoliths from Roberts Victor, Kaapvaal craton." In International Kimberlite Conference. University of Alberta, 2024. http://dx.doi.org/10.29173/ikc4157.

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Corner, B. "The Nature Of The Deep Crust Of The Kaapvaal Craton." In 3rd SAGA Biennial Conference and Exhibition. European Association of Geoscientists & Engineers, 1993. http://dx.doi.org/10.3997/2214-4609-pdb.224.011.

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Tinker, J. H., and M. J. de Wit. "Seismic Stratigraphy of Neoarchean-Paleoproterozoic Cover of the Kaapvaal Craton." In 7th SAGA Biennial Technical Meeting and Exhibition. European Association of Geoscientists & Engineers, 2001. http://dx.doi.org/10.3997/2214-4609-pdb.143.19.3.

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Wright, C., S. J. Webb, and T. K. Nguuri. "Broadband Seismological Studies On The Kaapvaal Craton Data Acquisition And Research Objectives." In 5th SAGA Biennial Conference and Exhibition. European Association of Geoscientists & Engineers, 1997. http://dx.doi.org/10.3997/2214-4609-pdb.223.052.

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Chatu, A., M. Q. W. Jones, and S. J. Webb. "Thermal Modelling of The Kaapvaal Lithosphere: Implications for the Bushveld Tomographic Anomaly." In 8th SAGA Biennial Technical Meeting and Exhibition. European Association of Geoscientists & Engineers, 2003. http://dx.doi.org/10.3997/2214-4609-pdb.144.16.

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Wang, Hao, and Jin-Hui Yang. "Widespread Magmatism and Metamorphism at 3.2 Ga in the Eastern Kaapvaal Craton, Southern Africa." In Goldschmidt2020. Geochemical Society, 2020. http://dx.doi.org/10.46427/gold2020.2724.

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