Abstract
We describe the petrography and mineral chemistry of sixteen eclogite and garnet pyroxenite xenoliths from the reworked Boshof road dump (Kimberley) and define three groups that stem from different depths. Group A, the shallowest derived, has low HREE (heavy rare earth element) abundances, flat middle to heavy REE patterns and high Mg# [= 100·Mg/(Mg + Fe)]. Their protoliths probably were higher pressure cumulates (~ 0.7 GPa) of mainly clinopyroxene (cpx) and subordinate orthopyroxene (opx) and olivine (ol). Group B1 xenoliths, derived from the graphite/diamond boundary and below show similarities to present-day N-MORB that were modified by partial melting (higher Mg# and positively inclined MREE (middle REE) and HREE (heavy REE) patterns of calculated bulk rocks). Group B2 samples from greatest depth are unique amongst eclogites reported so far worldwide. The calculated bulk rocks have humped REE patterns with very low La and Lu and prominent maxima at Sm or Eu and anomalously high Na2O (up to 5 wt%) which makes protolith identification difficult. The complex trace element signatures of the full spectrum of Kimberley eclogites belie a multi-stage history of melt depletion and metasomatism with the introduction of new phases especially of phlogopite (phlog). Phlogopite appears to be characteristic for Kimberley eclogites and garnet peridotites. Modelling the metasomatic overprint indicates that groups A and B1 were overprinted by volatile- and potassium-rich melts probably by a process of chromatographic fractionation. Using constraints from other metasomatized Kimberley mantle rocks suggest that much of the metasomatic phlogopite in the eclogites formed during an intense episode of metasomatism that affected the mantle beneath this region 1.1 Gyr ago.
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References
Armstrong JT (1991) Quantitative elemental analysis of individual microparticles with electron beam instruments. In: Heinrich KFJ, Newbury DE (eds) Electron probe quantitation. Plenum Press, New York, London, pp 261–315
Armstrong JT (1995) CITZAF: a package of correction programs for the quantitative electron microbeam X-ray analysis of thick polished materials, thin films, and particles. Microb Anal 4:177–200
Aulbach S, Jacob DE (2016) Major- and trace-elements in cratonic mantle eclogites and pyroxenites reveal heterogeneous sources and metamorphic processing of low-pressure protoliths. Lithos 262:586–605
Aulbach S, Viljoen KS (2015) Eclogite xenoliths from the Lace kimberlite, Kaapvaal craton: from convecting mantle source to palaeo-ocean floor and back. Earth Planet Sci Lett 431:274–286
Barth M, Rudnick RL, Horn I, McDonough WF, Spicuzza M, Valley JW, Haggerty SE (2001) Geochemistry of xenolithic eclogites from West Africa, part I: a link between low MgO eclogites and Archean crust formation. Geochim Cosmochim Acta 65:1499–1527
Basaltic Volcanism Study Project (1981) Basaltic volcanism on the Terrestrial planets. The Lunar and Planetary Institute, Houston. Pergamon Press, New York, 1286 pp
Bulatov VK, Brey GP, Girnis AV, Gerdes A, Höfer HE (2014) Carbonated sediment–peridotite interaction and melting at 7.5–12 GPa. Lithos 200-201:368–385
Casey JF (1997) Comparison of major and trace element geochemistry of abyssal peridotites and mafic plutonic rocks with basalts from the MARK region of the mid-Atlantic ridge. In: Karson JA, Cannat M, Miller DJ, Elthon D (eds) Proceedings of the ocean drilling program, scientific results. 153, pp 181–241
Coleman RG, Lrt DE, Bnamv LB, Bnalwocr WW (1965) Eclogites and eclogites; their differences and similarities. Geol Soc Am BulI 76:83–508
Dawson JB, Smith JV (1977) MARID (mica-amphibole–rutile–ilmenite–diopside) suite of xenoliths in kimberlite. Geochim Cosmochim Acta 41(2):309–323
de Capitani C, Petrakakis K (2010) The computation of equilibrium assemblage diagrams with Theriak/Domino software. Am Mineral 95:1006–1016
Dongrea AN, Jacob DE, Stern RA (2015) Subduction-related origin of eclogite xenoliths from Wajrakarur kimberlite field, Eastern Dharwar craton, Southern India: Constraints from petrology and geochemistry. Geochim Cosmochim Acta 166(1):165–188
Erlank AJ, Waters FG, Hawkesworth CJ, Haggerty SE, Allsopp HL, Rickard RS, Menzies MA (1987) Evidence for mantle metasomatism in peridotite nodules from the Kimberley pipes, South Africa. In: Menzies MA, Hawkesworth CJ (eds) Mantle Metasomatism. Academic Press, London, pp 221–311
Girnis A, Bulatov VK, Brey GP, Gerdes A, Höfer EH (2013) Trace element partitioning between mantle minerals and silicate–carbonate melts at 6-12 GPa and applications to mantle metasomatism and kimberlite genesis. Lithos 160-161:183–200
Grassi D, Schmidt MW (2011) Melting of carbonated pelites at 8–13 GPa: generating K-rich carbonatites for mantle metasomatism. Contrib Mineral Petrol 162:169–191
Green DH, Ringwood AE (1967) The genesis of basaltic magmas. Contrib Mineral Petrol 15:103–190
Green TH, Blundy JD, Adam J, Yaxley GM (2000) SIMS determination of trace element partition coefficients between garnet, clinopyroxene and hydrous basaltic liquids at 2–7.5 GPa and 1080–1200 °C. Lithos 53:165–187
Harte B, Kirkley MB (1997) Partitioning of trace elements between clinopyroxene and garnet: data from mantle eclogites. Chem Geol 136:1–24
Heaman LM, Creaser RA, Cookenboo HO, Chacko T (2006) Multi-stage modification of the Northern Slave mantle lithosphere: evidence from zircon- and diamond-bearing eclogite xenoliths entrained in Jericho kimberlite, Canada. J Petrol 47:821–858
Hellman PL, Henderson P (1977) Are rare earth elements mobile during spilitisation? Nature 267:38–40
Hopp J, Trieloff M, Brey GP, Woodland AB, Simon NSC, Wijbrans JR, Siebel W, Reitter E (2008) 40Ar/39Ar-ages of phlogopite in mantle xenoliths from South African kimberlites: evidence for metasomatic mantle impregnation during the Kibaran orogenic cycle. Lithos 106, 3-4:351–364
Ionov DA, Bodinier J-L, Mukasa SB, Zanetti A (2002) Mechanisms and sources of mantle metasomatism: major and trace element compositions of peridotite xenoliths from Spitsbergen in the context of numerical modelling. J Petrol 43(12):2219–2259
Jacob DE (2004) Nature and origin of eclogite xenoliths from kimberlites. Lithos 77:295–316
Jacob DE, Jagoutz E, Lowry D, Mattey D, Kudrjavtseva G (1994) Diamondiferous eclogites from Siberia: remnants of Archean oceanic crust. Geochim Cosmochim Acta 58:5191–5207
Jacob DE, Bizimis M, Salters VJM (2005) Lu/Hf and geochemical systematics of recycled ancient oceanic crust: evidence from Roberts Victor eclogites. Contrib Mineral Petrol 148(6):707–720
Jacob DE, Viljoen KS, Grassineau NV (2009) Eclogite xenoliths from Kimberley, South Africa -a case study of mantle metasomatism in eclogites. Lithos 112:1002–1013
Jenner FE, O’Neill HS (2012) Analysis of 60 elements in 616 ocean floor basaltic glasses. Geochem Geophys Geosyst 13(1):1–11
Jerde EA, Taylor LA, Crozaz G, Sobolev NV (1993) Exsolution of garnet within clinopyroxene of mantle eclogites: major- and trace-element chemistry. Contrib Mineral Petrol 114:148–159
Jochum KP, Willbold M, Raczek I, Stoll B, Herwig K (2005) Chemical characterisation of the USGS reference glasses GSA-1G, GSC-1G, GSD-1G, GSE-1G, BCR-2G, BHVO-2G and BIR-1G using EPMA, ID-TIMS, ID-ICPMS and LA-ICPMS. Geostand Geoanal Res 29:285–302
Klemme S, Blundy JD, Wood BJ (2002) Experimental constraints on major and trace element partitioning during partial melting of eclogite. Geochim Cosmochim Acta 66:3109–3123
Konzett J, Ulmer P (1999) The stability of hydrous potassic phases in lherzolitic mantle—an experimental study to 9·5 GPa in simplified and natural bulk compositions. J Petrol 4:629–652
Konzett J, Armstrong RA, Günther D (2000) Modal metasomatism in the Kaapvaal craton lithosphere: constraints on timing and genesis from U-Pb zircon dating of metasomatized peridotites and MARID-type xenoliths. Contrib Mineral Petrol 139:704–719
Krogh EJ (1988) The garnet-clinopyroxene Fe-Mg geothermometer - a reinterpretation of existing experimental data. Contrib Mineral Petrol 99:44–48
Lazarov M (2008) Archean to present day evolution of the lithospheric mantle beneath the Kaapvaal craton—processes recorded in subcalcic garnets, peridotites and polymict breccia. PhD thesis Goethe-University Frankfurt. http://publikationen.ub.uni-frankfurt.de/files/6873/LazarovMarina.pdf
Liu YS, Hu ZC, Gao S, Günther D, Xu J, Gao CG, Chen HH (2008) In situ analysis of major and trace elements of anhydrous minerals by LA-ICP-MS without applying an internal standard. Chem Geol 257(1–2):34–43
Liu YS, Gao S, Hu ZC, Gao CG, Zong KQ, Wang DB (2010) Continental and oceanic crust recycling-induced melt-peridotite interactions in the Trans-North China Orogen: U-Pb dating, Hf isotopes and trace elements in zircons of mantle xenoliths. J Petrol 51(1–2):537–571
Mather KA, Pearson DG, McKenzie D, Kjarsgaard B, Priestley K (2011) Constraining the depth and thermal history of cratonic lithosphere using peridotite xenolith and xenocryst thermobarometry and seismology. Lithos 125:729–742
Nowell GM, Pearson DG, Bell DR, Carlson RW, Smith CB, Kempton PD, Noble SR (2004) Hf isotope systematics of kimberlites and their megacrysts: new constraints on their source regions. J Petrol 45:1583–1612
Pearson DG (1999) The age of continental roots. Lithos 48:171–194
Perk NW, Coogan LA, Karson JA, Klein EM, Hanna HD (2007) Petrology and geochemistry of primitive lower oceanic crust from Pito Deep: implications for the accretion of the lower crust at the Southern East Pacific Rise. Contrib Mineral Petrol 154:575–590
Presnall DC, Dixon SA, Dixon JR, O’Donnel TH, Brenner NL, Schrock RL, Dycus DW (1978) Liquidus phase relations on the join Diopside-Forsterite-Anorthite from 1 atm to 20 kbar. Their bearing on the generation and crystallization of basaltic magma. Contrib Mineral Petrol 66:203–220
Purwin H, Lauterbach S, Brey GP, Woodland AB, Kleebe H-J (2012) An experimental study of the Fe oxidation states in garnet and clinopyroxene as a function of temperature in the system CaO–FeO–Fe2O3–MgO–Al2O3–SiO2: implications for garnet–clinopyroxene geothermometry. Contrib Mineral Petrol 165:623–639
Ringwood AE (1975) Composition and petrology of the earth’s mantle. Mac Graw Hill, New York
Schmickler B, Jacob DE, Foley SF (2004) Eclogite xenoliths from the Kuruman kimberlites, South Africa: geochemical fingerprinting of deep subduction and cumulate processes. Lithos 75(1–2):173–207
Schulze DJ (1989) Constraints on the abundance of eclogite in the upper mantle. J Geophys Res 94:4205–4212
Shu Q, Brey GP (2015) Ancient mantle metasomatism recorded in subcalcic garnet xenocrysts: temporal links between mantle metasomatism, diamond growth and crustal tectonomagmatism. Earth Planet Sci Lett 418:27–39
Shu Q, Brey GP, Hoefer HE, Zhao ZD, Pearson DG (2016) Kyanite/corundum eclogites from the Kaapvaal Craton: subducted troctolites and layered gabbros from the Mid to Early Archean. Contrib Mineral Petrol 171:1
Simon NSC, Carlson RW, Pearson DG, Davies G (2007) The origin and evolution of the Kaapvaal cratonic lithospheric mantle. J Petrol 48(3):589–625
Smyth JR, Hatton CJ (1977) Coesite-sanidine grospydite from Roberts-Victor kimberlite. Earth Planet Sci Lett 34:284–290
Sommer H, Jacob DE, Stern RA, Petts D, Mattey DP, Pearson DG (2017) Fluid-induced transition from banded kyanite- to bimineralic eclogite and implications for the evolution of cratons. Geochim Cosmochim Acta 207:19–42
Stachel T, Viljoen KS, Brey GP, Harris JW (1998) Metasomatic processes in lherzolitic and harzburgitic domains of diamondiferous lithospheric mantle: REE in garnets from xenoliths and inclusions in diamonds. Earth Planet Sci Lett 159:1–12
Sun S-S, McDonough WF (1989) Chemical and isotopic systematics of oceanic basalts: implications for mantle compositions and processes. In: Saunders AD, Norris MJ (eds) Magmatism in the ocean basins. Geol Soc Spec Publ, pp 313–345
Taylor LA, Neal CR (1989) Eclogites with oceanic crustal and mantle signatures from the Bellsbank kimberlite, South Africa, part 1: mineralogy, petrography, and whole rock chemistry. J Geol 97:551–567
Waters FG (1987) A suggested origin of MARID xenoliths in kimberlites by high pressure crystallization of an ultrapotassic rock such as lamproite. Contrib Mineral Petrol 95:523–533
Weiss Y, McNeill J, Pearson GD, Nowell GM, Ottley CJ (2015) Highly saline fluids from a subducting slab as the source for fluid-rich diamonds. Nature 524:339–344
Williams-Jones AE (2015) The hydrothermal mobility of the rare earth elements. British Columbia Geological Survey, Paper 2015-3:119–123
Acknowledgements
The authors profited from the continuous help and support in the laboratory, in the field, and through discussions by Heidi E. Hoefer, Jan Heliosch, Vlad Matjuschkin, Yan Luo, Sarah Woodland, Chiranjeeb Sarkar and Jeffrey W. Harris. We particularly appreciate Jock Robey’s help and support in making contact in the right places and in collecting the valuable specimens with us. Dr. Zhaochu Hu provided the opportunity and help for the trace element analysis of phlogopites at the State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences (Wuhan). The valuable input of Sébastien Pilet and two anonymous reviewers, the guest editor David B. Snyder and the editor-in-chief Lutz Nasdala is highly appreciated. This research was supported by funding from the Canada Excellence Research Chairs program and by the Deutsche Forschungsgemeinschaft (BR1012/33-1).
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Shu, Q., Brey, G.P. & Pearson, D.G. Eclogites and garnet pyroxenites from Kimberley, Kaapvaal craton, South Africa: their diverse origins and complex metasomatic signatures. Miner Petrol 112 (Suppl 1), 43–56 (2018). https://doi.org/10.1007/s00710-018-0595-6
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DOI: https://doi.org/10.1007/s00710-018-0595-6