Abstract
The Barberton Greenstone Belt hosts abundant structurally controlled gold mineralisation of Mesoarchaean age. More than 300 gold occurrences have been reported, although most of the gold production so far (>350 tonnes Au) has come from a handful of deposits located along the northern margin of the greenstone belt. Most deposits are hosted by greenschist-facies metasedimentary and metamafic rocks, with the notable exception of the amphibolite-facies rocks at New Consort mine. Mineralisation is associated with quartz–carbonate veins that truncate major compressional structures at the greenstone belt scale. The age of mineralisation is loosely constrained at circa 3080–3030 Ma, based on U–Pb dating of hydrothermal rutile and titanite. In greenschist-facies deposits, the ore assemblage is dominated by pyrite and arsenopyrite, which contain up to thousands of ppm of ‘invisible’ gold, Ni–As–Sb sulphides and native gold. At New Consort mine, mineralisation includes massive replacement-style ore and vein-hosted or disseminated types. Both structural studies in the field and microstructural observation point to a multistage ore deposition process, which is reflected in the re-activation of brittle to ductile structures and the overprinting of sulphide assemblages. The presence of mass-independently fractionated S isotopes (Δ33S = –0.6 to +1.0‰) in pyrite from Sheba and Fairview mines suggests that hydrothermal fluids mobilised S from volcanic and sedimentary rocks of the greenstone belt and places constraints on the origin of the Au itself.
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Notes
- 1.
The Zwartkoppie Formation is not recognised by SACS and its use is informal.
References
Agangi A, Hofmann A, Przybyłowicz W (2014) Trace element zoning of sulfides and quartz at Sheba and Fairview gold mines: clues to Mesoarchean mineralisation in the Barberton Greenstone Belt, South Africa. Ore Geol Rev 56:94–114
Agangi A, Przybyłowicz W, Hofmann A (2015) Trace element map** of pyrite from Archean gold deposits—A comparison between PIXE and EPMA. Nucl Instrum Methods Phys Res, Sect B 348:302–306
Agangi A, Hofmann A, Eickmann B, Marin-Carbonne J, Reddy SM (2016) An atmospheric source of S in Mesoarchaean structurally-controlled gold mineralisation of the Barberton Greenstone Belt. Precambr Res 285:10–20
Altigani MAH, Merkle RKW, Dixon RD (2016) Geochemical identification of episodes of gold mineralisation in the Barberton Greenstone Belt, South Africa. Ore Geol Rev 75:186–205
Anhaeusser CR (1976) Archean metallogeny in southern Africa. Econ Geol 71:16–43
Anhaeusser CR (1984) Structural elements of Archaean granite-greenstone terranes as exemplified by the Barberton Mountain Land, Southern Africa. In: Kröner A, Greiling R (eds) Precambrian Tectonics Illustrated. E. Schweizerbart’sche Verlagsbuchhandlung, Stuttgart, pp 57–58
Anhaeusser CR (1986) Archaean gold mineralization in the Barberton Mountain Land. In: Anhaeusser CR, Maske S (eds) Mineral deposits of southern Africa, Geological Society of South Africa, pp 113–154
Anhaeusser CR (2001) The anatomy of an extrusive-intrusive Archaean mafic-ultramafic sequence: the Nelshoogte Schist Belt and Stolzburg Layered Ultramafic Complex, Barberton Greenstone Belt, South Africa. S Afr J Geol 104:167–204
Armstrong RA, Compston W, Retief EA, Williams IS, Welke HJ (1991) Zircon ion microprobe studies bearing on the age and evolution of the Witwatersrand triad. Precambr Res 53:243–266
Bao H, Rumble D III, Lowe DR (2007) The five stable isotope compositions of Fig Tree barites: implications on sulfur cycle in ca. 3.2-Ga oceans. Geochimica et Cosmochimica Acta 71:4868–4879
Barberton Gold Mines (2010) Mineral resources and technical short form report. www.panafricanresources.com. Consulted Nov 2012
Barberton Gold Mines (2014) Mineral resources and mineral reserve report. www.panafricanresources.com. Consulted Feb 2017
Bath AB, Walshe JL, Cloutier J, Verrall M, Cleverley JS, Pownceby MI, Macrae CM, Wilson NC, Tunjic J, Nortje GS, Robinson P (2013) Biotite and apatite as tools for tracking pathways of oxidized fluids in the Archean East Repulse gold deposit, Australia. Econ Geol 108:667–690
Cabri LJ, Chryssoulis SL, de Villiers JPR, Laflamme JHG, Buseck PR (1989) The nature of “invisible” gold in arsenopyrite. The Canadian Mineralogist 27:353–362
Cutts KA, Stevens G, Hoffmann JE, Buick IS, Frei D, Münker C (2014) Paleo- to Mesoarchean polymetamorphism in the Barberton Granite-Greenstone Belt, South Africa: Constraints from U-Pb monazite and Lu-Hf garnet geochronology on the tectonic processes that shaped the belt. Geol Soc Am Bull 126:251–270
de Boorder H (2012) Spatial and temporal distribution of the orogenic gold deposits in the late Palaeozoic Variscides and Southern Tianshan: how orogenic are they? Ore Geol Rev 46:1–31
de Ronde CEJ, de Wit MJ (1994) Tectonic history of the Barberton greenstone belt, South Africa: 490 million years of Archean crustal evolution. Tectonics 13:983–1005
de Ronde CEJ, Kamo SL (2000) An Archaean arc-arc collisional event: a short-lived (ca 3 Myr) episode, Weltevreden area, Barberton greenstone belt, South Africa. J Afr Earth Sc 30:219–248
de Ronde CEJ, Kamo S, Davis DW, de Wit MJ, Spooner ETC (1991) Field, geochemical and U-Pb isotopic constraints from hypabyssal felsic intrusions within the Barberton greenstone belt, South Africa: implications for tectonics and the timing of gold mineralization. Precambr Res 49:261–280
de Ronde CEJ, Spooner ETC, de Wit MJ, Bray CJ (1992) Shear zone-related, Au quartz vein deposits in the Barberton greenstone belt, South Africa; field and petrographic characteristics, fluid properties, and light stable isotope geochemistry. Econ Geol 87:366–402
Diener JFA, Stevens G, Kisters AFM, Poujol M (2005) Metamorphism and exhumation of the basal parts of the Barberton greenstone belt, South Africa: constraining the rates of Mesoarchaean tectonism. Precambr Res 143:87–112
Dirks PHGM, Charlesworth EG, Munyai MR (2009) Cratonic extension and Archaean gold mineralisation in the Sheba-Fairview mine, Barberton greenstone belt, South Africa. S Afr J Geol 112:291–316
Dirks PHGM, Charlesworth EG, Munyai MR, Wormald R (2013) Stress analysis, post-orogenic extension and 3.01 Ga gold mineralisation in the Barberton Greenstone Belt, South Africa. Precambrian Res 226:157–184
Doublier MP, Thébaud N, Wingate MTD, Romano SS, Kirkland CL, Gessner K, Mole DR, Evans N (2014) Structure and timing of Neoarchean gold mineralization in the Southern Cross district (Yilgarn Craton, Western Australia) suggest leading role of late Low-Ca I-type granite intrusions. J Struct Geol 67, Part B: 205–221
Drabon N, Lowe DR, Byerly G, Harrington JA (2017) Detrital zircon geochronology of sandstones of the 3.6–3.2 Ga Barberton greenstone belt: no evidence for older continental crust. Geology 45:803–806
Dziggel A, Kisters AFM (2019) Chapter 26—Tectono-metamorphic controls on Archean gold mineralization in the Barberton Greenstone Belt, South Africa. In: Van Kranendonk RH, Bennet VC Hoffmann E (eds) Earth’s oldest rocks 2nd Ed, Elsevier, pp 655–674
Dziggel A, Stevens G, Poujol M, Anhaeusser CR, Armstrong RA (2002) Metamorphism of the granite-greenstone terrane south of the Barberton greenstone belt, South Africa: an insight into the tectono-thermal evolution of the lower portions of the Onverwacht Group. Precambr Res 114:221–247
Dziggel A, Armstrong RA, Stevens G, Nasdala L (2005) Growth of zircon and titanite during metamorphism in the granitoid-gneiss terrane south of the Barberton greenstone belt, South Africa. Mineral Mag 69:1019–1036
Dziggel A, Knipfer S, Kisters AFM, Meyer FM (2006) P-T and structural evolution during exhumation of high-T, medium-P basement rocks in the Barberton Mountain Land, South Africa. J Metamorph Geol 24:535–551
Dziggel A, Otto A, Kisters AFM, Meyer FM (2007) Chapter 5.8 Tectono-metamorphic controls on Archean gold mineralization in the Barberton Greenstone Belt, South Africa: an example from the New Consort gold mine. In: Van Kranendonk, MJ, Smithies, RH & Bennet, VC (eds) Earth’s oldest rocks, Elsevier, Amsterdam, pp 699–727
Dziggel A, Poujol M, Otto A, Kisters AFM, Trieloff M, Schwarz WH, Meyer FM (2010) New U-Pb and 40Ar/39Ar ages from the northern margin of the Barberton greenstone belt, South Africa: implications for the formation of Mesoarchaean gold deposits. Precambr Res 179:206–220
Farquhar J, Bao H, Thiemens M (2000) Atmospheric influence of Earth’s earliest sulfur cycle. Science 289:756–758
Fougerouse D, Micklethwaite S, Ulrich S, Miller J, Godel B, Adams DT, McCuaig TC (2016) Evidence for two stages of mineralisation in west Africa’s largest gold deposit: Obuasi, Ghana. Econ Geol 112:2–33
Frimmel HE, Groves DI, Kirk J, Ruiz J, Chesley J, Minter WEL (2005) The formation and preservation of the Witwatersrand goldfields, the world’s largest gold province. Econ Geol 100th Anniversary Volume:769–698
Fu B, Touret JLR (2014) From granulite fluids to quartz-carbonate megashear zones: the gold rush. Geosci Front 5:747–758
Gaboury D (2013) Does gold in orogenic deposits come from pyrite in deeply buried carbon-rich sediments?: insight from volatiles in fluid inclusions. Geology 41:1207–1210
Goldfarb RJ, Groves DI (2015) Orogenic gold: common or evolving fluid and metal sources through time. Lithos 233:2–26
Grosch EG, McLoughlin N (2013) Paleoarchean sulfur cycle and biogeochemical surface conditions on the early Earth, Barberton, South Africa. Earth Planet Sci Lett 377–378:142–154
Groves DI, Goldfarb RJ, Knox-Robinson CM, Ojala J, Gardoll S, Yun GY, Holyland P (2000) Late-kinematic timing of orogenic gold deposits and significance for computer-based exploration techniques with emphasis on the Yilgarn Block, Western Australia. Ore Geol Rev 17:1–38
Groves DI, Goldfarb RJ, Robert F, Hart CJR (2003) Gold deposits in metamorphic belts: overview of current understanding, outstanding problems, future research, and exploration significance. Econ Geol 98:1–29
Harris PD, Robb LJ, Tomkinson MJ (1995) The nature and structural setting of rare-element pegmatites along the northern flank of the Barberton greenstone belt, South Africa. S Afr J Geol 98:82–94
Hazarika P, Mishra B, Pruseth KL (2017) Trace-element geochemistry of pyrite and arsenopyrite: ore genetic implications for late Archean orogenic gold deposits in southern India. Mineral Mag 81:661
Hegner E, Kröner A, Hofmann AW (1984) Age and isotope geochemistry of the Archaean Pongola and Usushwana suites in Swaziland, Southern Africa: a case for crustal contamination of mantle-derived magma. Earth Planet Sci Lett 70:267–279
Heubeck C, Engelhardt J, Byerly GR, Zeh A, Sell B, Luber T, Lowe DR (2013) Timing of deposition and deformation of the Moodies Group (Barberton Greenstone Belt, South Africa): very-high-resolution of Archaean surface processes. Precambr Res 231:236–262
Heubeck C, Bläsing S, Grund M, Drabon N, Homann M, Nabhan S (2016) Geological constraints on Archean (3.22 Ga) coastal-zone processes from the Dycedale Syncline, Barberton greenstone belt. S Afr J Geol 119:495
Hofmann A (2005) The geochemistry of sedimentary rocks from the Fig Tree Group, Barberton greenstone belt: implications for tectonic, hydrothermal and surface processes during mid-Archaean times. Precambr Res 143:23–49
Hofmann A, Pitcairn I, Wilson A (2017) Gold mobility during Palaeoarchaean submarine alteration. Earth Planet Sci Lett 462:47–54
Hronsky J, Groves D, Loucks R, Begg G (2012) A unified model for gold mineralisation in accretionary orogens and implications for regional-scale exploration targeting methods. Miner Deposita 47:339–358
Johnston DT (2011) Multiple sulfur isotopes and the evolution of Earth’s surface sulfur cycle. Earth Sci Rev 106:161–183
Kakegawa T, Ohmoto H (1999) Sulfur isotope evidence for the origin of 3.4 to 3.1 Ga pyrite at the Princeton gold mine, Barberton greenstone belt, South Africa. Precambr Res 96:209–224
Kamo SL, Davis DW (1994) Reassessment of Archean crustal development in the Barberton Mountain Land, South Africa, based on U-Pb dating. Tectonics 13:167–192
Kendrick MA, Honda M, Walshe J, Petersen K (2011) Fluid sources and the role of abiogenic-CH4 in Archean gold mineralization: Constraints from noble gases and halogens. Precambr Res 189(3–4):313–327
Kirk J, Ruiz J, Chesley J, Walshe J, England G (2002) A major Archean, gold- and crust-forming event in the Kaapvaal Craton, South Africa. Science 297:1856–1858
Kisters AFM, Stevens G, Dziggel A, Armstrong RA (2003) Extensional detachment faulting and core-complex formation in the southern Barberton granite-greenstone terrain, South Africa: evidence for a 3.2 Ga orogenic collapse. Precambr Res 127:355–378
Kisters AFM, Belcher RW, Poujol M, Dziggel A (2010) Continental growth and convergence-related arc plutonism in the Mesoarchaean: evidence from the Barberton granitoid-greenstone terrain, South Africa. Precambr Res 178:15–26
Kolb J, Dziggel A, Bagas L (2015) Hypozonal lode gold deposits: a genetic concept based on a review of the New Consort, Renco, Hutti, Hira Buddini, Navachab, Nevoria and the granites deposits. Precambr Res 262:20–44
Kositcin N, Krapez B (2004) Relationship between detrital zircon age-spectra and the tectonic evolution of the late Archaean Witwatersrand Basin, South Africa. Precambr Res 129:141–168
Kröner A, Hegner E, Wendt JI, Byerly GR (1996) The oldest part of the Barberton granitoid-greenstone terrain, South Africa: evidence for crust formation between 3.5 and 3.7 Ga. Precambr Res 78:105–124
Kröner A, Anhaeusser CR, Hoffmann JE, Wong J, Geng H, Hegner E, **e H, Yang J, Liu D (2016) Chronology of the oldest supracrustal sequences in the Palaeoarchaean Barberton Greenstone Belt, South Africa and Swaziland. Precambr Res 279:123–143
Lana C, Tohver E, Cawood P (2010) Quantifying rates of dome-and-keel formation in the Barberton granitoid-greenstone belt, South Africa. Precambr Res 177:199–211
Lowe DR (1999) Geologic evolution of the Barberton Greenstone Belt and vicinity. Geological Society of America Special Papers 329:287–312
Lowe DR, Byerly GR (1999) Stratigraphy of the west-central part of the Barberton Greenstone Belt, South Africa. Geological Society of America Special Papers 329:1–36
Lowe DR, Byerly GR (2007) An overview of the geology of the Barberton Greenstone Belt and vicinity: implications for early crustal development. In: Van Kranendonk MJ, Smithies RH, Bennett VC (eds) Earth’s oldest rocks. Elsevier, Amsterdam, pp 481–524
Lowe, DR, Byerly, GR, Heubeck, C (2012) Geologic Map of the west-central Barberton greenstone belt. In: South Africa, scale 1:25,000: Geological Society of America Map and Chart Series No. 103
Maphalala R, Kröner A (1993) Pb-Pb single zircon ages for the younger Archaean granitoids of Swaziland, southern Africa. In: Maphalala R, Mabuza M (eds) 16th Colloquium of African Geology. Swaziland Geological Survey and Mines 2: 201–206
Matsumura R (2014) The petrogenesis of the Nelshoogte pluton: the youngest and most compositionally variable TTG pluton in the Barberton Granite-Greenstone Terrain. Unpublished MSc thesis, Stellenbosch University, 108 p
Mishra B, Pruseth KL, Hazarika P, Chinnasamy SS (2017) Nature and source of the ore-forming fluids associated with orogenic gold deposits in the Dharwar Craton. Geosci Front 9:715–726
Montinaro A, Strauss H, Mason PRD, Roerdink D, Münker C, Schwarz-Schampera U, Arndt NT, Farquhar J, Beukes NJ, Gutzmer J, Peters M (2015) Paleoarchean sulfur cycling: multiple sulfur isotope constraints from the Barberton greenstone belt, South Africa. Precambr Res 267:311–322
Morey AA, Tomkins AG, Bierlein FP, Weinberg RF, Davidson GJ (2008) Bimodal distribution of gold in pyrite and arsenopyrite: examples from the Archean Boorara and Bardoc shear systems, Yilgarn Craton, Western Australia. Econ Geol 103:599–614
Moyen J-F, Stevens G, Kisters A (2006) Record of mid-Archaean subduction from metamorphism in the Barberton terrain, South Africa. Nature 442:559–562
Munyai MR, Dirks PHGM, Charlesworth EG (2011) Archaean gold mineralisation during post-orogenic extension in the New Consort gold mine, Barberton greenstone belt, South Africa. S Afr J Geol 114:121–144
Murphy RCL (2015) Stabilising a craton: the origin and emplacement of the 3.1 Ga Mpuluzi Batholith. Unpublished PhD thesis, Macquarie University, Sydney, Australia, 489p
Ono S, Eigenbrode JL, Pavlov AA, Kharecha P, Rumble D III, Kasting JF, Freeman KH (2003) New insights into Archean sulfur cycle from mass-independent sulfur isotope records from the Hamersley Basin, Australia. Earth Planet Sci Lett 213:15–30
Otto A, Dziggel A, Kisters A, Meyer F (2007) The New Consort Gold Mine, Barberton greenstone belt, South Africa: orogenic gold mineralization in a condensed metamorphic profile. Miner Deposita 42:715–735
Pearton T, Viljoen M (2017) Gold on the Kaapvaal Craton, outside the Witwatersrand Basin, South Africa. S Afr J Geol 120:101–132
Philippot P, van Zuilen M, Rollion-Bard C (2012) Variations in atmospheric sulphur chemistry on early Earth linked to volcanic activity. Nat Geosci 5:668–674
Phillips GN, Powell R (2009) Formation of gold deposits: review and evaluation of the continuum model. Earth Sci Rev 94:1–21
Pokrovski GS, Akinfiev NN, Borisova AY, Zotov AV, Kouzmanov K (2014) Gold speciation and transport in geological fluids: insights from experiments and physical-chemical modelling. Geol Soc Spec Pub 402:9–70
Poujol M, Robb LJ, Respaut J-P, Anhaeusser CR (1996) 3.07–2.97 Ga greenstone belt formation in the northeastern Kaapvaal Craton; implications for the origin of the Witwatersrand Basin. Econ Geol 91:1455–1461
Qiu Y, McNaughton NJ (1999) Source of Pb in orogenic lode-gold mineralisation: Pb isotope constraints from deep crustal rocks from the southwestern Archaean Yilgarn Craton, Australia. Mineralium Deposita 34(4):366–381
Reich M, Kesler SE, Utsunomiya S, Palenik CS, Chryssoulis SL, Ewing RC (2005) Solubility of gold in arsenian pyrite. Geochimica et Cosmochimica Acta 69:2781–2796
Roerdink DL, Mason PRD, Farquhar J, Reimer T (2012) Multiple sulfur isotopes in Paleoarchean barites identify an important role for microbial sulfate reduction in the early marine environment. Earth Planet Sci Lett 331–332:177–186
Roerdink DL, Mason PRD, Whitehouse MJ, Reimer T (2013) High-resolution quadruple sulfur isotope analyses of 3.2 Ga pyrite from the Barberton Greenstone Belt in South Africa reveal distinct environmental controls on sulfide isotopic arrays. Geochimica et Cosmochimica Acta 117:203–215
SACS (1980) Stratigraphy of South Africa Part 1: Lithostratigraphy of the Republic of South Africa, South West Africa/Namibia and the Republics of Bophuthatswana, Transkei and Venda. Geological Survey of South Africa, 690p
Sahoo PR, Venkatesh AS (2015) Constraints of mineralogical characterization of gold ore: implication for genesis, controls and evolution of gold from Kundarkocha gold deposit, eastern India. J Asian Earth Sci 97, Part A: 136–149
Salier BP, Groves DI, McNaughton NJ, Fletcher IR (2005) Geochronological and stable isotope evidence for widespread orogenic gold mineralization from a deep-seated fluid source at ca 2.65 Ga in the Laverton Gold Province, Western Australia. Econ Geol 100:1363–1388
Schoene B, de Wit MJ, Bowring SA (2008) Mesoarchean assembly and stabilization of the eastern Kaapvaal craton: a structural-thermochronological perspective. Tectonics 27:TC5010
Schouwstra RP (1995) Wall-rock alteration as a guide to gold-bearing fracture zones in the Zwartkoppie Section, Sheba gold mine, South Africa. S Afr J Geol 98:399–414
Schouwstra RP, De Villier J (1998) Gold mineralization and associated wallrock alteration in the Main Reef Complex at Sheba Mine, South Africa. Appl Earth Sci IMM Trans Sect B:B158–B170
Selvaraja V, Fiorentini ML, Jeon H, Savard DD, LaFlamme CK, Guagliardo P, Caruso S, Bui T-H (2017) Evidence of local sourcing of sulfur and gold in an Archaean sediment-hosted gold deposit. Ore Geol Rev 89:909–930
Sibson RH, Robert F, Poulsen KH (1988) High-angle reverse faults, fluid-pressure cycling, and mesothermal gold-quartz deposits. Geology 16:551–555
Stiegler MT, Cooper M, Byerly GR, Lowe DR (2012) Geochemistry and petrology of komatiites of the pioneer ultramafic complex of the 3.3 Ga Weltevreden formation, Barberton greenstone belt, South Africa. Precambr Res 212:1–12
Tomkins AG (2013) On the source of orogenic gold. Geology 41:1255–1256
Van Kranendonk MJ, Kröner A, Hegner E, Connelly J (2009) Age, lithology and structural evolution of the c. 3.53 Ga Theespruit Formation in the Tjakastad area, southwestern Barberton greenstone belt, South Africa, with implications for Archaean tectonics. Chem Geol 261:115–139
Viljoen MJ, Viljoen RP (1969) Introduction to the geology of the Barberton granite-greenstone terrain. Geological Society of South Africa Special Publication 2:9–28
Wang LG, McNaughton NJ, Groves DI (1993) An overview of the relationship between granitoid intrusions and gold mineralisation in the Archaean Murchison Province, Western Australia. Mineralium Deposita 28(6):482–494
Ward JHW (1995) Geology and metallogeny of the Barberton greenstone belt: a survey. J Afr Earth Sc 21:213–240
Ward JHW (1999) The metallogeny of the Barberton greenstone belt, South Africa and Swaziland. Geological Survey of South Africa Memoir 86, 108p
Wilson AH, Zeh A (2019) U-Pb and Hf isotopes of detrital zircons from the Pongola Supergroup: constraints on deposition ages, provenance and Archean evolution of the Kaapvaal craton. Precambrian Research 305 (Supplement C): 177–196
Wit De et al (2019) Paleoarchean bedrock lithologies across the Makhonjwa Mountains of South Africa and Swaziland linked to geochemical, magnetic and tectonic data reveal early plate tectonic genes flanking subduction margins. Geosci Front 9:603–665
Zeh A, Gerdes A, Heubeck C (2013) U-Pb and Hf isotope data of detrital zircons from the Barberton greenstone belt: constraints on provenance and Archaean crustal evolution. J Geol Soc 170:215–223
Acknowledgements
This research was funded by SIEF (Science and Industry Endowment Fund), the NRF (National Research Foundation of South Africa), and the DST-NRF Centre of Excellence for Integrated Mineral and Energy Resource Analysis (CIMERA). JMC thanks the CNRS-INSU Programme National de Planétologie for their support. We acknowledge Chris Rippon (Barberton Mines (Pty) Limited) for providing sample material.
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Agangi, A., Hofmann, A., Eickmann, B., Marin-Carbonne, J. (2019). Mesoarchaean Gold Mineralisation in the Barberton Greenstone Belt: A Review. In: Kröner, A., Hofmann, A. (eds) The Archaean Geology of the Kaapvaal Craton, Southern Africa. Regional Geology Reviews. Springer, Cham. https://doi.org/10.1007/978-3-319-78652-0_7
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