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Journal articles on the topic 'Greenstone belts – Zimbabwe'

Author: Grafiati

Published: 4 June 2021

Last updated: 14 February 2022

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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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11

Nisbet, E. G., N. T. Arndt, M. J. Bickle, et al. "Uniquely fresh 2.7 Ga komatiites from the Belingwe greenstone belt, Zimbabwe." Geology 15, no. 12 (1987): 1147. http://dx.doi.org/10.1130/0091-7613(1987)15<1147:ufgkft>2.0.co;2.

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12

Hofmann, A., P. H. G. M. Dirks, and H. A. Jelsma. "Clastic sedimentation in a late Archaean accretionary terrain, Midlands greenstone belt, Zimbabwe." Precambrian Research 129, no. 1-2 (2004): 47–69. http://dx.doi.org/10.1016/j.precamres.2003.09.017.

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13

Xenophontos, L., G. Stevens, and W. J. Przybylowicz. "Micro-PIXE elemental imaging of pyrites from the Bulawayan-Bubi Greenstone Belt, Zimbabwe." Nuclear Instruments and Methods in Physics Research Section B: Beam Interactions with Materials and Atoms 150, no. 1-4 (1999): 496–501. http://dx.doi.org/10.1016/s0168-583x(98)00945-8.

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14

Dirks, Paul H. G. M., Hielke A. Jelsma, and Axel Hofmann. "Thrust-related accretion of an Archaean greenstone belt in the Midlands of Zimbabwe." Journal of Structural Geology 24, no. 11 (2002): 1707–27. http://dx.doi.org/10.1016/s0191-8141(02)00002-0.

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15

Kusky, T. M., P. A. Winsky, W. S. F. Kidd, et al. "Ensialic origin for the Ngezi Group, Belingwe greenstone belt, Zimbabwe: Comment and Reply." Geology 22, no. 8 (1994): 766. http://dx.doi.org/10.1130/0091-7613(1994)022<0766:eoftng>2.3.co;2.

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16

Dirks, Paul H. G. M., Hielke A. Jelsma, Axel Hofmann, et al. "Continental extensional setting for the Archean Belingwe Greenstone Belt, Zimbabwe: Comment and Reply." Geology 27, no. 7 (1999): 667. http://dx.doi.org/10.1130/0091-7613(1999)027<0667:cesfta>2.3.co;2.

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17

Owen, R. J., O. Gwavava, and P. Gwaze. "Multi-electrode resistivity survey for groundwater exploration in the Harare greenstone belt, Zimbabwe." Hydrogeology Journal 14, no. 1-2 (2005): 244–52. http://dx.doi.org/10.1007/s10040-004-0420-7.

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18

Huizenga, Jan M. "Fluid evolution in the Pote Shear Zone Harare-Shamva-Bindura greenstone belt (northeast Zimbabwe)." Journal of African Earth Sciences 28, no. 2 (1999): 311–24. http://dx.doi.org/10.1016/s0899-5362(99)00006-8.

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19

Bolhar, Robert, Jon D. Woodhead, and Janet M. Hergt. "Continental setting inferred for emplacement of the 2.9–2.7 Ga Belingwe Greenstone Belt, Zimbabwe." Geology 31, no. 4 (2003): 295. http://dx.doi.org/10.1130/0091-7613(2003)031<0295:csifeo>2.0.co;2.

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20

Hofmann, Axel, Paul H. G. M. Dirks, and Heilke A. Jelsma. "Horizontal tectonic deformation geometries in a late Archaean sedimentary sequence, Belingwe greenstone belt, Zimbabwe." Tectonics 20, no. 6 (2001): 909–32. http://dx.doi.org/10.1029/2001tc900014.

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21

Zhou, Mei-Fu. "PGE distribution in 2.7-Ga layered komatiite flows from the Belingwe greenstone belt, Zimbabwe." Chemical Geology 118, no. 1-4 (1994): 155–72. http://dx.doi.org/10.1016/0009-2541(94)90174-0.

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22

Baldock, J. W., and J. A. Evans. "Constraints on the age of the Bulawayan group metavolcanic sequence, Harare Greenstone Belt, Zimbabwe." Journal of African Earth Sciences (and the Middle East) 7, no. 5-6 (1988): 795–804. http://dx.doi.org/10.1016/0899-5362(88)90022-x.

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23

Ranganai, Rubeni T. "Gravity and Aeromagnetic Studies of the Filabusi Greenstone Belt, Zimbabwe Craton: Regional and Geotectonic Implications." International Journal of Geosciences 03, no. 05 (2012): 1048–64. http://dx.doi.org/10.4236/ijg.2012.35106.

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24

Jelsma, H. A., P. A. van der Beek, and M. L. Vinyu. "Tectonic evolution of the Bindura-Shamva greenstone belt (northern Zimbabwe): Progressive deformation around diapiric batholiths." Journal of Structural Geology 15, no. 2 (1993): 163–76. http://dx.doi.org/10.1016/0191-8141(93)90093-p.

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25

Oberthür, T., and T. W. Weiser. "Gold-bismuth-telluride-sulphide assemblages at the Viceroy Mine, Harare-Bindura-Shamva greenstone belt, Zimbabwe." Mineralogical Magazine 72, no. 4 (2008): 953–70. http://dx.doi.org/10.1180/minmag.2008.072.4.953.

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AbstractGold mineralization at the Viceroy Mine is hosted in extensional veins in steep shear zones that transect metabasalts of the Archaean Arcturus Formation. The gold mineralization is generally made up of banded or massive quartz carrying abundant coarse arsenopyrite. However, most striking is a distinct suite of Au-Bi-Te-S minerals, namely joseite-A (Bi4TeS2), joseite-B (Bi4Te2S), hedleyite (Bi7Te3), ikunolite (Bi4S3), ‘protojoseite’ (Bi3TeS), an unnamed mineral (Bi6Te2S), bismuthinite (Bi2S3), native Bi, native gold, maldonite (Au2Bi), and jonassonite (AuBi5S4). The majority of the Bi-T

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26

Saager, Rudolf, Thomas Oberthuer, and Hans-Peter Tomschi. "Geochemistry and mineralogy of banded iron-formation-hosted gold mineralization in the Gwanda greenstone belt, Zimbabwe." Economic Geology 82, no. 8 (1987): 2017–32. http://dx.doi.org/10.2113/gsecongeo.82.8.2017.

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27

Herrington, R. J. "Late Archaean structure and gold mineralization in the Kadoma region of the Midlands greenstone belt, Zimbabwe." Geological Society, London, Special Publications 95, no. 1 (1995): 173–91. http://dx.doi.org/10.1144/gsl.sp.1995.095.01.11.

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28

Abell, P. I., J. McClory, A. Martin, and E. G. Nisbet. "Archaean stromatolites from the Ngesi Group, Belingwe greenstone belt, Zimbabwe; preservation and stable isotopes — preliminary results." Precambrian Research 27, no. 4 (1985): 357–83. http://dx.doi.org/10.1016/0301-9268(85)90094-4.

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29

Master, S., G. Henry, and G. Borg. "Geochemistry and mineralogy of banded iron-formation-hosted gold mineralization in the Gwanda greenstone belt, Zimbabwe; discussion." Economic Geology 84, no. 1 (1989): 194–97. http://dx.doi.org/10.2113/gsecongeo.84.1.194.

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30

Saager, R., and T. Oberthuer. "Geochemistry and mineralogy of banded iron-formation-hosted gold mineralization in the Gwanda greenstone belt, Zimbabwe; reply." Economic Geology 84, no. 1 (1989): 197–98. http://dx.doi.org/10.2113/gsecongeo.84.1.197.

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31

Hofmann, A., P. H. G. M. Dirks, and H. A. Jelsma. "Shallowing-Upward Carbonate Cycles in the Belingwe Greenstone Belt, Zimbabwe: A Record of Archean Sea-Level Oscillations." Journal of Sedimentary Research 74, no. 1 (2004): 64–81. http://dx.doi.org/10.1306/052903740064.

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32

Hofmann, A., P. H. G. M. Dirks, H. A. Jelsma, and N. Matura. "A tectonic origin for ironstone horizons in the Zimbabwe craton and their significance for greenstone belt geology." Journal of the Geological Society 160, no. 1 (2003): 83–97. http://dx.doi.org/10.1144/0016-764901-172.

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33

Hofmann, Axel, and Paul H. G. M. Dirks. "Continental setting inferred for emplacement of the 2.9–2.7 Ga Belingwe Greenstone Belt, Zimbabwe: Comment and Reply." Geology 31, no. 1 (2003): e30-e31. http://dx.doi.org/10.1130/0091-7613-31.1.e30.

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34

Bolhar, Robert, Jon D. Woodhead, and Janet M. Hergt. "Continental setting inferred for emplacement of the 2.9–2.7 Ga Belingwe Greenstone Belt, Zimbabwe: Comment and Reply." Geology 31, no. 1 (2003): e31-e31. http://dx.doi.org/10.1130/0091-7613-31.1.e31.

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35

Shimizu, Kenji, Eizo Nakamura, Katsura Kobayashi, and Shigenori Maruyama. "Discovery of Archean continental and mantle fragments inferred from xenocrysts in komatiites, the Belingwe greenstone belt, Zimbabwe." Geology 32, no. 4 (2004): 285. http://dx.doi.org/10.1130/g20162.1.

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36

Blenkinsop, T. G., T. Oberthür, and O. Mapeto. "Gold mineralization in the Mazowe area, Harare-Bindura-Shamva greenstone belt, Zimbabwe: I. Tectonic controls on mineralization." Mineralium Deposita 35, no. 2-3 (2000): 126–37. http://dx.doi.org/10.1007/s001260050011.

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37

Hofmann, A., PH GM Dirks, and H. A. Jelsma. "Late Archaean clastic sedimentary rocks (Shamvaian Group) of the Zimbabwe craton: first observations from the Bindura-Shamva greenstone belt." Canadian Journal of Earth Sciences 39, no. 11 (2002): 1689–708. http://dx.doi.org/10.1139/e02-074.

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The ~2.65 Ga old Shamvaian Group sedimentary rocks occur as a folded succession in the central part of the BinduraShamva greenstone belt of Zimbabwe. The strata comprise distinct, shear zone-bounded tectonostratigraphic units which may be stratigraphically arranged as follows. The lower part of the succession is represented by a transgressive, fining-upward sequence of alluvial fan conglomerate, overlain by fluvial braid-plain pebbly sandstone and marine shoreface sandstone. Detritus was derived from a mid-Archaean granitoid-gneiss terrain situated to the east. Sediment supply and subsidence

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38

GWAVAVA, O., and R. T. RANGANAI. "THE GEOLOGY AND STRUCTURE OF THE MASVINGO GREENSTONE BELT AND ADJACENT GRANITE PLUTONS FROM GEOPHYSICAL DATA, ZIMBABWE CRATON." South African Journal of Geology 112, no. 3-4 (2009): 277–90. http://dx.doi.org/10.2113/gssajg.112.3-4.277.

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39

Pirajno, F., and I. González-Álvarez. "A re-appraisal of the Epoch nickel sulphide deposit, Filabusi Greenstone Belt, Zimbabwe: A hydrothermal nickel mineral system?" Ore Geology Reviews 52 (August 2013): 58–65. http://dx.doi.org/10.1016/j.oregeorev.2012.11.005.

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40

Vinyu, M. L., and J. D. Kramers. "New Rb-Sr whole rock dates for some postorogenic granites (s.l.) from the Shamva-Harare Greenstone Belt, Zimbabwe." Chemical Geology 70, no. 1-2 (1988): 149. http://dx.doi.org/10.1016/0009-2541(88)90634-1.

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41

Fedo, Christopher M., Kenneth A. Eriksson, and Eirik J. Krogstad. "Geochemistry of shales from the Archean (~3.0 Ga) Buhwa Greenstone Belt, Zimbabwe: Implications for provenance and source-area weathering." Geochimica et Cosmochimica Acta 60, no. 10 (1996): 1751–63. http://dx.doi.org/10.1016/0016-7037(96)00058-0.

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42

Fedo, C. "Stratigraphic framework of the ∼ 3.0 Ga Buhwa Greenstone Belt: a unique stable-shelf succession in the Zimbabwe Archean Craton." Precambrian Research 77, no. 3-4 (1996): 161–78. http://dx.doi.org/10.1016/0301-9268(95)00053-4.

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43

Buchholz, P., P. Herzig, G. Friedrich, and R. Frei. "Granite-hosted gold mineralization in the Midlands greenstone belt: a new type of low-grade gold deposit in Zimbabwe." Mineralium Deposita 33, no. 5 (1998): 437–60. http://dx.doi.org/10.1007/s001260050162.

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44

Krogstad, Eirik J., Christopher M. Fedo, and Kenneth A. Eriksson. "Provenance ages and alteration histories of shales from the Middle Archean Buhwa greenstone belt, Zimbabwe: Nd and Pb isotopic evidence." Geochimica et Cosmochimica Acta 68, no. 2 (2004): 319–32. http://dx.doi.org/10.1016/s0016-7037(03)00206-0.

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45

Hickman-Lewis, K., and F. Westall. "A southern African perspective on the co-evolution of early life and environments." South African Journal of Geology 124, no. 1 (2021): 225–52. http://dx.doi.org/10.25131/sajg.124.0016.

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Abstract The Kaapvaal and Zimbabwe cratons host some of the earliest evidence for life. When compared to the contemporaneous East Pilbara craton, cherts and other metasedimentary horizons in southern Africa preserve traces of life with far greater morphological and geochemical fidelity. In spite of this, most fossiliferous horizons of southern Africa have received relatively limited attention. This review summarises current knowledge regarding the nature of early life and its distribution with respect to environments and ecosystems in the Archaean (&gt;2.5 Ga) of the region, correlating st

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46

SHIMIZU, KENJI, EIZO NAKAMURA, and SHIGENORI MARUYAMA. "The Geochemistry of Ultramafic to Mafic Volcanics from the Belingwe Greenstone Belt, Zimbabwe: Magmatism in an Archean Continental Large Igneous Province." Journal of Petrology 46, no. 11 (2005): 2367–94. http://dx.doi.org/10.1093/petrology/egi059.

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47

Sawada, Hikaru, Yusuke Sawaki, Shuhei Sakata, et al. "New geochronological constraints on the middle Archean Shurugwi greenstone belt toward an understanding of the crustal evolution of the Zimbabwe Craton." Journal of African Earth Sciences 173 (January 2021): 104021. http://dx.doi.org/10.1016/j.jafrearsci.2020.104021.

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48

Nutte, T. H. C., T. Oberth�r, R. Saager, and H. P. Tomschi. "The geology, mineralogy and geochemistry of the broomstock gold deposit, Kwekwe Greenstone Belt, Zimbabwe; Some implications for gold mineralization in jaspilite iron formations." Mineralogy and Petrology 39, no. 2 (1988): 145–62. http://dx.doi.org/10.1007/bf01184820.

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49

RANGANAI, R. T. "STRUCTURAL AND SUBSURFACE RELATIONSHIPS BETWEEN THE FORT RIXON-SHANGANI GREENSTONE BELT AND THE NALATALE PLUTON, ZIMBABWE CRATON, AS DERIVED FROM GRAVITY AND AEROMAGNETIC DATA." South African Journal of Geology 116, no. 2 (2013): 273–96. http://dx.doi.org/10.2113/gssajg.116.2.273.

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50

Hofmann, Axel, Robert Bolhar, Paul Dirks, and Hielke Jelsma. "The geochemistry of Archaean shales derived from a Mafic volcanic sequence, Belingwe greenstone belt, Zimbabwe: provenance, source area unroofing and submarine versus subaerial weathering." Geochimica et Cosmochimica Acta 67, no. 3 (2003): 421–40. http://dx.doi.org/10.1016/s0016-7037(02)01086-4.

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