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Relevant bibliographies by topics / Greenstone belts – Zimbabwe

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Journal articles

Academic literature on the topic 'Greenstone belts – Zimbabwe'

Author: Grafiati

Published: 4 June 2021

Last updated: 14 February 2022

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Journal articles on the topic "Greenstone belts – Zimbabwe"

1

Yoshihara, Arata, and Yozo Hamano. "Paleomagnetic constraints on the Archean geomagnetic field intensity obtained from komatiites of the Barberton and Belingwe greenstone belts, South Africa and Zimbabwe." Precambrian Research 131, no. 1-2 (2004): 111–42. http://dx.doi.org/10.1016/j.precamres.2004.01.003.

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2

Neil Phillips, G. "Metamorphic fluids and gold." Mineralogical Magazine 57, no. 388 (1993): 365–74. http://dx.doi.org/10.1180/minmag.1993.057.388.02.

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AbstractLow-salinity fluids (T > 200°C reduced S, modest CO2) and high geothermal gradients are common to many gold deposits and provinces. In contrast, host rocks, hosting structures, depth of formation (in the crust during deposition), subsequent metamorphic overprint, alteration mineralogy and isotopic signatures can vary dramatically within single deposits or provinces. Gold deposits with co-product base metals are an exception to the above comments, and probably relate to saline fluids.The low salinity fluids inferred for major gold-only deposits are not easily explained by seawater, b

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3

Fedo, Christopher M., Kenneth A. Eriksson, and Tom G. Blenkinsop. "Geologic history of the Archean Buhwa Greenstone Belt and surrounding granite–gneiss terrane, Zimbabwe, with implications for the evolution of the Limpopo Belt." Canadian Journal of Earth Sciences 32, no. 11 (1995): 1977–90. http://dx.doi.org/10.1139/e95-151.

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The Buhwa Greenstone Belt (BGB) of southern Zimbabwe is the only major greenstone belt in the Archean Zimbabwe Craton directly adjacent to the granulite-facies rocks that constitute the Northern Marginal Zone of the Limpopo Belt. The deformational history and assembly of the BGB shed light on the evolution of the Northern Marginal Zone – Zimbabwe Craton transition. Assembly of the region began with deposition of the dominantly sedimentary cover succession at ~3.0 Ga on banded gneisses of the ~3.5 Ga Tokwe segment. At ~2.9 Ga the northern margin of the greenstone belt experienced kilometres of

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4

Kusky, Timothy M., and Pamela A. Winsky. "Structural relationships along a greenstone/shallow water shelf contact, Belingwe greenstone belt, Zimbabwe." Tectonics 14, no. 2 (1995): 448–71. http://dx.doi.org/10.1029/94tc03086.

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5

Hofmann, A., P. H. G. M. Dirks, and H. A. Jelsma. "Late Archaean foreland basin deposits, Belingwe greenstone belt, Zimbabwe." Sedimentary Geology 141-142 (June 2001): 131–68. http://dx.doi.org/10.1016/s0037-0738(01)00072-0.

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6

Vinyu, M. L., H. A. Jelsma, and R. Frei. "Timing between granitoid emplacement and associated gold mineralization: examples from the ca. 2.7 Ga Harare–Shamva greenstone belt, northern Zimbabwe." Canadian Journal of Earth Sciences 33, no. 7 (1996): 981–92. http://dx.doi.org/10.1139/e96-074.

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Structurally controlled Late Archaean gold mineralizations associated with felsic plutons in the Harare–Shamva greenstone belt, Zimbabwe, are synchronous with the emplacement of their hosts. The ages of these mineralizations are identical to those reported from other mesothermal gold deposits elsewhere in the Zimbabwe Craton. The Pb and Nd isotopic signatures of the host plutons are compatible with a direct mantle or a short crustal residence period for the protoliths to the host intrusions. The coincidence of the Pb-isotope data from ore minerals with the whole-rock trends (errorchrons) of th

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7

Huizenga, Jan M., and Jacques L. R. Touret. "Fluid inclusions in shear zones: The case of the Umwindsi shear zone in the Harare-Shamva-Bindura greenstone belt, NE Zimbabwe." European Journal of Mineralogy 11, no. 6 (1999): 1079–90. http://dx.doi.org/10.1127/ejm/11/6/1079.

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8

Kusky, T. M., and W. S. F. Kidd. "Remnants of an Archean oceanic plateau, Belingwe greenstone belt, Zimbabwe." Geology 20, no. 1 (1992): 43. http://dx.doi.org/10.1130/0091-7613(1992)020<0043:roaaop>2.3.co;2.

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9

Blenkinsop, Tom G., Christopher M. Fedo, Michael J. Bickle, et al. "Ensialic origin for the Ngezi Group, Belingwe greenstone belt, Zimbabwe." Geology 21, no. 12 (1993): 1135. http://dx.doi.org/10.1130/0091-7613(1993)021<1135:eoftng>2.3.co;2.

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10

Hunter, M. A., M. J. Bickle, E. G. Nisbet, A. Martin, and H. J. Chapman. "Continental extensional setting for the Archean Belingwe Greenstone Belt, Zimbabwe." Geology 26, no. 10 (1998): 883. http://dx.doi.org/10.1130/0091-7613(1998)026<0883:cesfta>2.3.co;2.

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