Abstract
Textures of Bushveld chromite from thin seams and accessory disseminations in the Platreef and the northernmost Waterberg Project area were compared with textures of xenocrystic chromite from mantle xenoliths found in Neogene basalt in the Kurile Island Arc. The sieve-textured to symplectic rims around the resorbed chromite in the Kurile samples resulted from the reaction between chromite and chromite-undersaturated basaltic melt, with the inclusions in chromite being entrapped during episodes of chromite primary growth, chemical dissolution, and reprecipitation or secondary growth. The relics of the lattice-oriented etch tunnels suggest that the dissolution preferentially developed along the crystallographic planes and defects. The Bushveld chromites exhibiting similar textures are interpreted as reaction-textured chromites, by analogy with the Kurile samples. The Bushveld sieve-textured, fish-hook to symplectic and amoeboidal to atoll-like chromites, are believed to have been formed due to coupled dissolution-reprecipitation of the earlier cumulus or xenocrystic chromite during interaction with chromite-undersaturated evolved melt. The electron backscattered diffraction data confirm the same single-crystal crystallographic orientation of all domains of the reaction-textured chromites as well as their clustered semi-dissolved relics. Therefore, Bushveld inclusion-rich chromite might have captured different populations of melt inclusions during its discontinuous out-of-equilibrium growth with fast episodic resorption and regeneration. The occurrence of reaction-textured chromites indicates a zone of interaction between dynamic magmatic influxes where chemical equilibrium was not achieved whereas a complete re-equilibration between chromite and the stagnant and sequestered interstitial liquid was attained during the formation of the massive chromitites.
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References
Akmaz RM, Uysal I, Saka S (2014) Compositional variations of chromite and solid inclusions in ophiolitic chromitites from the southeastern Turkey: implications for chromitite genesis. Ore Geol Rev 58:208–224
Anderson ED, Moecher DP (2007) Omphacite breakdown reactions and relation to eclogite exhumation rates. Contrib Mineral Petrol 154:253–277
Arai S, Kadoshima K, Morishita T (2006) Widespread arc-related melting in mantle section of the northern Oman ophiolite as inferred from detrital chromian spinels. J Geol Soc London 163:1–11
Ballhaus CG, Stumpfl EF (1986) Sulfide and platinum mineralization in the Merensky Reef: evidence from hydrous silicates and fluid inclusions. Contrib Mineral Petrol 94:193–204
Ballhaus C, Fonseca ROC, Munker C, Kirchenbaur M, Zirner A (2015) Spheroidal textures in igneous rocks—Textural consequences of H2O saturation in basaltic melts. Geochim Cosmochim Acta 167:241–252
Barnes SJ (1998) Chromite in komatiites, 1. Magmatic controls on crystallisation and composition. J Petrol 39:1689–1720
Barnes S-J, Maier WD (2002) Platinum-group elements and microstructures of normal Merensky reef from Impala Platinum Mines, Bushveld Complex. J Petrol 43:109–128
Barnes SJ, Roeder PL (2001) The range of spinel compositions in terrestrial mafic and ultramafic rocks. J Petrol 42:2279–2302
Barnes S-J, Pagé P, Prichard HM, Zientek ML, Fisher PC (2016) Chalcophile and platinum-group element distribution in the Ultramafic series of the Stillwater Complex, MT, USA—implications for processes enriching chromite layers in Os, Ir, Ru, and Rh. Miner Deposita 51:25–47
Borisova AY, Ceuleneer G, Kamenetsky VS, Arai S, Abily B, Bindeman IN, Polve M, De Parceval P, Aigouy T, Pokrovski GS (2012) A new view on the petrogenesis of the Oman ophiolite chromitites from microanalyses of chromite-hosted inclusions. J Petrol 53:2411–2440
Cameron EN (1975) Postcumulus and subsolidus equilibration of chromite and coexisting silicates in the Eastern Bushveld Complex. Geochim Cosmochim Acta 39:1021–1033
Cawthorn RG, Eales HV, Walraven F, Uken R, Watkeys MR (2006) The Bushveld Complex. In: Johnson MR, Anhaeusser CR, Thomas RJ (eds) The geology of South Africa, Johannesburg-Pretoria, Geol Soc S Afr, pp 261–282
Clark JN, Ihli J, Schenk AS, Kim Y-Y, Kulak AN, Campbell JM, Nisbet G, Meldrum FC, Robinson IK (2015) Three-dimensional imaging of dislocation propagation during crystal growth and dissolution. Nat Mater 14(8):780–784
Danyushevsky LV, Leslie RAJ, Crawford AJ, Durance P (2004) Melt inclusions in primitive olivine phenocrysts: the role of localized reaction processes in the origin of anomalous compositions. J Petrol 45:2531–2553
Dick HJB, Bullen T (1984) Chromian spinel as a petrogentic indicator in abyssal and alpine-type peridotites and spatially associated lavas. Contrib Mineral Petrol 86:54–76
Distler VV, Kryachko VV, Yudovskaya MA (2008) Ore petrology of chromite-PGE mineralization in the Kempirsai ophiolite complex. Mineral Petrol 92:31–58
Eales HV (2000) Implications of the chromium budget of the western limb of the Bushveld Complex. S Afr J Geol 103:141–150
Eales HV, Reynolds IM (1986) Cryptic variations within chromitites of the Upper Critical Zone, northwestern Bushveld Complex. Econ Geol 81:1056–1066
Erdmann S, Scaillet B, Kellett DA (2012) Textures of peritectic crystals as guides to reactive minerals in magmatic systems: new insights from melting experiments. J Petrol 53:2231–2258
Elardo SM, Francis M, McCubbin FM, Charles K, Shearer CK (2012) Chromite symplectites in Mg-suite troctolite 76535 as evidence for infiltration metasomatism of a lunar layered intrusion. Geochim Cosmochim Acta 87:154–177
Erdmann S, Scaillet B, Martel C, Cadoux A (2014) Characteristic textures of recrystallized, peritectic, and primary magmatic olivine in experimental samples and natural volcanic rocks. J Petrol 55:2377–2402
Ghiorso MS, Sack RO (1995) Chemical mass-transfer in magmatic processes IV. A revised and internally consistent thermodynamic model for the interpolation and extrapolation of liquid-solid equilibria in magmatic systems at elevated temperatures and pressures. Contrib Mineral Petrol 119:197–212
Godel B, Barnes SJ, Barnes SJ, Maier WD (2007) Platinum-group elements in sulfide minerals, platinum-group minerals, and whole-rocks of the Merensky Reef (Bushveld Complex, South Africa): implications for the formation of the reef. J Petrol 48:1569–1604
Grobler DF, Brits JAN, Maier WD, Crossingham A (2018) Litho- and chemostratigraphy of the Flatreef PGE deposit, northern Bushveld Complex. Miner Deposita 54:3–28
Holness MB, Stripp G, Humphrey CS, Veksler IV, Nielsen TF, Tegner C (2011) Silicate liquid immiscibility within the crystal mush: late-stage magmatic microstructures in the Skaergaard intrusion, East Greenland. J Petrol 52:175–222
Holwell DA, McDonald I, Butler IB (2011) Precious metal enrichment in the Platreef, Bushveld Complex, South Africa: evidence from homogenized magmatic sulfide melt inclusions. Contrib Mineral Petrol 161:1011–1026
Howarth GH, Prevec SA (2013) Hydration vs. oxidation: modelling implications for Fe–Ti oxide crystallisation in mafic intrusions, with specific reference to the Panzhihua intrusion, SW China. Geosci Frontiers 4:555–569
Hulbert LJ, von Gruenewaldt G (1985) Textural and compositional features of chromite in the lower and critical zones of the Bushveld Complex south of Potgietersrus. Econ Geol 80:872–895
Hutchinson D, Foster J, Prichard H, Gilbert S (2015) Concentration of particulate platinum-group minerals during magma emplacement; a case study from the Merensky Reef, Bushveld Complex. J Petrol 56:113–159
Huthmann FM, Yudovskaya MA, Frei D, Kinnaird JA (2016) Geochronological evidence for an extension of the Northern Lobe of the Bushveld Complex, Limpopo Province, South Africa. Precam Res 280:61–75
Huthmann FM, Yudovskaya MA, Kinnaird JA, McCreesh M, McDonald I (2018) Geochemistry and PGE of the lower mineralized Zone of the Waterberg Project, South Africa. Ore Geol Rev 92:161–185
Irvine TN (1967) Chromian spinel as a petrogenetic indicator Part 2. Petrologic applications. Can J Earth Sci 4:71–103
Johan Z, Martin R, Ettler V (2017) Fluids are bound to be involved in the formation of ophiolitic chromite deposits. Eur J Mineral 29:543–555
Kamenetsky VS, Crawford AJ, Meffre S (2001) Factors controlling chemistry of magmatic spinel: an empirical study of associated olivine, Cr-spinel and melt inclusions from primitive rocks. J Petrol 42:655–671
Kapsiotis A, Rassios AE, Antonelou A, Tzamos E (2016) Genesis and multi-episodic alteration of zircon-bearing chromitites from the Ayios Stefanos Mine, Othris massif, Greece: assessment of an unconventional hypothesis on the origin of zircon in ophiolitic chromitites. Minerals 6:124
Kinnaird JA, Kruger FJ, Nex PAM, Cawthorn RG (2002) The chromitite formation- a key to understand processes of formation and platinum enrichment. Appl Earth Sci 111:23–35
Kinnaird JA, Yudovskaya M, McCreesh M, Huthmann F, Botha TJ (2017) The Waterberg platinum group element deposit: atypical mineralization in mafic-ultramafic rocks of the Bushveld Complex, South Africa. Econ Geol 112:1367–1394
Leblanc M (1980) Chromite growth, dissolution and deformation from a morphological view point: SEM investigations. Mineral Deposita 15:201–210
Leuthold J, Blundy JD, Brooker RA (2015) Experimental petrology constraints on the recycling of mafic cumulate: a focus on Cr-spinel from the Rum Eastern layered intrusion, Scotland. Contrib Mineral Petrol 170:12. https://doi.org/10.1007/s00410-015-1165-0
Li C, Ripley EM, Sarkar A, Shin D, Maier WD (2005) Origin of phlogopite-orthopyroxene inclusions in chromites from the Merensky Reef of the Bushveld Complex, South Africa. Contrib Mineral Petrol 150:119–130
Liu J, Hattori K, Wang J (2017) Mineral inclusions in chromite from the chromite deposit in the Kudi ophiolite, Tibet, Proto-Tethys. Acta Geol Sinica 91:469–485
Lorand JP, Ceuleneer G (1989) Silicate and base-metal sulfide inclusions in chromites from the Maqsad area (Oman ophiolite, Gulf of Oman): a model for entrapment. Lithos 22:173–190
Maier WD, de Klerk L, Blaine J, Manyeruke T, Barnes S-J, Stevens MVA, Mavrogenes JA (2008) Petrogenesis of contact-style PGE mineralisation in the northern lobe of the Bushveld Complex: comparison of data from the farms Rooipoort, Townlands, Drenthe and Nonnenwerth. Mineral Deposita 43:255–280
Manzini M, Bouvier A-S, Baumgartner LP, Müntener O, Rose-Koga EF, Schiano P, Escrig S, Meibom A, Shimizu N (2017) Weekly to monthly time scale of melt inclusion entrapment prior to eruption recorded by phosphorus distribution in olivine from mid-ocean ridges. Geology 45:1059–1062
Martynov YA, Khanchuk AI, Kimura JI, Rybin AV, Martynov AY (2010) Geochemistry and petrogenesis of volcanic rocks in the Kuril island arc. Petrology 18:489–513
Mathez EA, Kinzler RJ (2017) Metasomatic chromitite seams in the Bushveld and Rum layered intrusions. Elements 13(6):397–402
Matveev S, Ballhaus C (2002) Role of water in the origin of podiform chromitite deposits. Earth Planet Sci Lett 203:235–243
McElduff B, Stumpfl EF (1991) The chromite deposits of the Troodos Complex, Cyprus—evidence for the role of a fluid phase accompanying chromite formation. Mineral Deposita 26:307–318
Melcher F, Grum W, Simon G, Thalhammer TV, Stumpfl EF (1997) Petrogenesis of the ophiolitic giant chromite deposits of Kempirsai, Kazakhstan: a study of solid and fluid inclusions in chromite. J Petrol 38:1419–1458
Mitchell AA, Scoon RN (2007) The Merensky Reef at Winnaarshoek, Eastern Bushveld Complex: a primary magmatic hypothesis based on a wide reef facies. Econ Geol 102:971–1009
Mondal SK, Mukherjee R (2017) Chromite: petrogenetic indicator to ore deposits. Ore Geol Rev 90:63–64. https://doi.org/10.1016/j.oregeorev.2017.07.005
Naldrett AJ, Wilson A, Kinnaird J, Yudovskaya M, Chunnett G (2012) The application of MELTS to the formation of chromitites and related PGE mineralization in the Bushveld Complex and elsewhere. Mineral Deposita 47:209–232
Nielsen JW, Foster FG (1960) Unusual etch pits in quartz crystals. Amer Mineral 45:299–310
O’Driscoll B, Emeleus CH, Donaldson CH, Daly JS (2010) Cr-spinel seam petrogenesis in the Rum layered suite, NW Scotland: cumulate assimilation and in situ crystallization in a deforming crystal mush. J Petrol 51(6):1171–1201
Pan S, Zheng J, Yin Z, Griffin WL, Xia M, Lin A, Zhang H (2018) Spongy texture in mantle clinopyroxene records decompression-induced melting. Lithos 320–321:44–154
Plank T, Kelley KA, Zimmer MM, Hauri EH, Wallace PJ (2013) Why do mafic arc magmas contain ~ 4 wt% water on average? Earth Planet Sci Lett 364:168–179
Plechov PY, Shishkina TA, Ermakov VA, Portnyagin MV (2008) Formation conditions of allivalites, olivine–anorthite crystal enclaves, in the volcanics of the Kuril-Kamchatka Arc. Petrology 16:232–260
Prichard HM, Barnes SJ, Godel B, Reddy SM, Vukmanovic Z, Halfpenny A, Neary CR, Fisher PC (2015) The structure of and origin of nodular chromite from the Troodos ophiolite, Cyprus, revealed using high-resolution X-ray computed tomography and electron backscatter diffraction. Lithos 218–219:87–98
Pushkarev EV, Kamenetsky VS, Morozova AV, Khiller VV, Glavatskykh SP, Rodemann T (2015) Ontogeny of ore Cr-spinel and composition of inclusions as indicators of the pneumatolytic–hydrothermal origin of PGM-bearing chromitites from Kondyor massif, the Aldan Shield. Geol Ore Deposits 57:352–380
Roeder PL, Reynolds I (1991) Crystallization of chromite and chromium solubility in basaltic melts. J Petrol 32:909–934
Roeder PL, Poustovetov AA, Oskarsson N (2001) Growth forms and composition of chromian spinel in MORB magma: diffusion controlled crystallization of chromian spinel. Can Mineral 39:397–416
Satsukawa T, Piazolo S, González-Jiménez JM, Colás V, Griffin WL, O’Reilly SY, Gervilla F, Fanlo I, Kerestedjian TN (2015) Fluid-present deformation aids chemical modification of chromite: insights from chromites from Golyamo Kamenyane, SE Bulgaria. Lithos 228–229:78–89
Schiano P, Clocchiatti R, Lorand JP, Massare D, Deloule E, Chaussidon M (1997) Primitive basaltic melts included in podiform chromites from the Oman ophiolite. Earth Planet Sci Lett 146:489–497
Schiano P, Bourdon B, Clocchiatti R, Massare D, Varela ME, Bottinga Y (1998) Low-degree partial melting trends recorded in upper mantle minerals. Earth Planet Sci Lett 160:537–550
Schwarzer RA, Field DP, Adams BL, Kumar M, Schwartz AJ (2009) Present state of electron backscatter diffraction and prospective developments. In: Schwartz AJ (ed) Electron backscatter diffraction in materials science. Springer, New York, pp 1–20. https://doi.org/10.1007/978-0-387-88136-2
Scoon RN, Costin G (2018) Chemistry, morphology and origin of magmatic-reaction chromite stringers associated with anorthosite in the Upper Critical zone at Winnaarshoek, eastern limb of the Bushveld Complex. J Petrol 59:1551–1578. https://doi.org/10.1093/petrology/egy071
Scoon RG, Teigler B (1994) Platinum group element mineralisation in the Critical Zone of the western Bushveld Complex: 1. Sulphide-poor chromitites below the UG2. Econ Geol 89:1094–1121
Shaw CSJ, Dingwell DB (2008) Experimental peridotite–melt reaction at one atmosphere: a textural and chemical study. Contrib Mineral Petrol 155:199–214
Shaw CSJ, Edgar AD (1997) Post-entrainment mineral-melt reactions in spinel peridotite xenoliths from Inver, Donegal, Ireland. Geol Mag 134:771–779
Smith PM, Asimow PD (2005) Adiabat_1ph: a new public front-end to the MELTS, pMELTS, and pHMELTS models. Geochem Geophys Geosys 6:Q02004
Spandler C, Mavrogenes J, Arculus R (2005) Origin of chromitites in layered intrusions: evidence from chromite-hosted melt inclusions from the Stillwater complex. Geology 33:893–896
Suwas S, Ray RK (2014) Crystallographic texture of materials, engineering materials and processes. Springer, London
Tingle TN, Roeder E, Green HW II (1992) Formation of fluid inclusions and etch tunnels in olivine at high pressure. Am Mineral 77:296–302
van der Merwe MJ (1978) The geology of the basic and ultramafic rocks of the Potgietersrus limb of the Bushveld Complex. Unpublished PhD thesis, Johannesburg, University of Witwatersrand, p 176
Vukmanovic Z, Barnes SJ, Reddy SM, Godel B, Fiorentini ML (2013) Morphology and microstructure of chromite crystals in chromitites from the Merensky Reef (Bushveld Complex, South Africa). Contrib Mineral Petrol 165:1031–1050
Welsch B, Faure F, Famin V, Baronnet A, Bache’lery P (2013) Dendritic crystallization: a single process for all the textures ofolivine in basalts? J Petrol 54:539–574
Yudovskaya MA, Kinnaird JA (2010) Chromite in the Platreef (Bushveld Complex, South Africa): occurrence and evolution of its chemical composition. Mineral Deposita 45:369–391
Yudovskaya MA, Kinnaird JA, Grobler DF, Costin G, Abramova VD, Dunnett T, Barnes S-J (2017) Zonation of Merensky-style platinum mineralization in Turfspruit thick reef facies (northern limb of the Bushveld Complex). Econ Geol 112:1333–1365
Zeh A, Ovtcharova M, Wilson AH, Schaltegger U (2015) The Bushveld Complex was emplaced and cooled in less than one million years—results of zirconology, and geotectonic implications. Earth Planet Sci Lett 418:103–114
Zhou M-F, Robinson PT, Su B-X, Gao J-F, Li J-W, Yang J-S, Malpas J (2014) Compositions of chromite, associated minerals, and parental magmas of podiform chromite deposits: the role of slab contamination of asthenospheric melts in suprasubduction zone environments. Gondwana Res 26:262–283
Acknowledgements
The authors thank Ivanplats South Africa (SA) and Platinum Group Metals (PTM SA) for generous access to borehole cores and cooperation in all aspects of our research. This study was carried out using equipment at the Sankt-Petersburg State University (SPSU) Resource Centers “Geomodel” and “Nanophotonics”. Maksim Lozhkin is acknowledged for assistance during Ar etching at SPSU. The work was supported by the Russian Foundation for Basic Research (grant 18-05-70073) and the Centre of Excellence for Intergrated Mineral and Resource Analysis (CIMERA) in South Africa. The discussions with Dima Kamenetsky, Paul Nex and Florian Huthmann were fruitful throughout the study. Thorough reviews by Brian O’Driscoll and Roger Scoon helped to improve the earlier version of the paper. Editorial handling and critical comments by Chris Ballhaus as well as advice from Othmar Müntener are appreciated.
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Yudovskaya, M.A., Costin, G., Shilovskikh, V. et al. Bushveld symplectic and sieve-textured chromite is a result of coupled dissolution-reprecipitation: a comparison with xenocrystic chromite reactions in arc basalt. Contrib Mineral Petrol 174, 74 (2019). https://doi.org/10.1007/s00410-019-1613-3
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DOI: https://doi.org/10.1007/s00410-019-1613-3