Relevant bibliographies by topics / Geology – Swaziland / Journal articles
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Journal articles on the topic 'Geology – Swaziland'

Author: Grafiati
Published: 4 June 2021
Last updated: 30 January 2023

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1

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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2

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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3

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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4

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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5

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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6

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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7

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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8

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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9

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:
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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10

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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11

Kröner, A., and A. Tegtmeyer. "Gneiss-greenstone relationships in the Ancient Gneiss Complex of southwestern Swaziland, southern Africa, and implications for early crustal evolution." Precambrian Research 67, no. 1-2 (1994): 109–39. http://dx.doi.org/10.1016/0301-9268(94)90007-8.

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12

Trumbull, Robert B. "A petrological and RbSr isotopic study of an early Archean fertile granite-pegmatite system: The Sinceni Pluton in Swaziland." Precambrian Research 61, no. 1-2 (1993): 89–116. http://dx.doi.org/10.1016/0301-9268(93)90059-b.

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13

Hoffmann, J. Elis, Alfred Kröner, Ernst Hegner, et al. "Source composition, fractional crystallization and magma mixing processes in the 3.48–3.43Ga Tsawela tonalite suite (Ancient Gneiss Complex, Swaziland) – Implications for Palaeoarchaean geodynamics." Precambrian Research 276 (May 2016): 43–66. http://dx.doi.org/10.1016/j.precamres.2016.01.026.

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14

van Schijndel, Valby, Gary Stevens, Armin Zeh, Dirk Frei, and Cristiano Lana. "Zircon geochronology and Hf isotopes of the Dwalile Supracrustal Suite, Ancient Gneiss Complex, Swaziland: Insights into the diversity of Palaeoarchaean source rocks, depositional and metamorphic ages." Precambrian Research 295 (July 2017): 48–66. http://dx.doi.org/10.1016/j.precamres.2017.04.025.

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15

Hoffmann, J. Elis, Emmanuel Musese, Alfred Kröner, et al. "Hafnium-Neodymium isotope, trace element and U-Pb zircon age constraints on the petrogenesis of the 3.44–3.46 Ga Dwalile greenstone remnant, Ancient gneiss Complex, Swaziland." Precambrian Research 351 (December 2020): 105970. http://dx.doi.org/10.1016/j.precamres.2020.105970.

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16

Kro¨ner, A., C. Milisenda, W. Compston, A. Tegtmeyer, T. C. Liew, and W. Todt. "Combined use of single zircon ages and Sm-Nd isotopes in the analysis of early archaean crustal growth processes: The Ancient Gneiss Complex of Swaziland, Southern Africa." Chemical Geology 70, no. 1-2 (1988): 146. http://dx.doi.org/10.1016/0009-2541(88)90622-5.

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