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S-type ignimbrites with polybaric crystallisation histories: the Tolmie Igneous Complex, Central Victoria, Australia

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An Erratum to this article was published on 13 July 2011

Abstract

The Late Devonian Tolmie Igneous Complex (in north-eastern Victoria, Australia) contains S-type, intracaldera, rhyolitic ignimbrites with multiple generations of phenocrysts of biotite, garnet, cordierite and orthopyroxene; one unit also contains fayalitic olivine. Geothermometry and calculated phase relations indicate high-T deep- to mid-crustal origins for the magmas, with crystallisation at several levels. At least four separate magma groups make up the complex. Compositional variations within and between ignimbrites are adequately modelled by selective entrainment of peritectic garnet, ilmenite, orthopyroxene and plagioclase into the magmas. Neither crystal fractionation nor mafic-felsic magma mixing played a role. Chemical and isotope data suggest that the magma sources were once variably Ba-enriched arc greywackes with different proportions of clay. The deep origin of some of the Tolmie Complex magmas means that supracrustal rocks underlie parts of north-eastern Victoria at depths of around 35 km. This has important implications for understanding the region’s tectonic development.

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References

  • Barboza SA, Bergantz GW, Brown M (1999) Regional granulite facies metamorphism in the Ivrea zone: is the Mafic Complex the smoking gun or a red herring? Geology 27:447–450

    Article  Google Scholar 

  • Birch WD (1975) Mineralogy, geochemistry and petrogenesis of some Victorian Palaeozoic Rhyolites. PhD thesis (unpubl.), Melbourne University, Australia

  • Birch WD (1989) Alkali feldspars in Victorian Palaeozoic rhyolites. In: Le Maitre RW (ed) Pathways in geology—essays in Honour of Edwin Sherbon Hills. Blackwell Scientific Publications, Australia

  • Birch WD, Gleadow AJW (1974) The genesis of garnet and cordierite in acid volcanic rocks: evidence from the Cerberean Cauldron, Central Victoria, Australia. Contrib Mineral Petrol 45:1–13

    Article  Google Scholar 

  • Birch WD, Clemens JD, Phillips GN (1977) Devonian acid igneous complexes in central Victoria. National Museum of Victoria, Melbourne, p 29

    Google Scholar 

  • Cayley RA (2011) Exotic crustal block accretion to the eastern Gondwanaland margin in the Late Cambrian–Tasmania, the Selwyn Block, and implications for the Cambrian–Silurian evolution of the Ross, Delamerian, and Lachlan orogens. Gondwana Res 19:628–649

    Article  Google Scholar 

  • Chappell BW, White AJR (1974) Two contrasting granite types. Pacific Geol 8:173–174

    Google Scholar 

  • Chappell BW, White AJR (1992) I- and S-type granites in the Lachlan Fold Belt. Trans R Soc Edinburgh Earth Sci 83:1–26

    Google Scholar 

  • Chappell BW, White AJR (2001) Two contrasting granite types: 25 years later. Aust J Earth Sci 48:489–499

    Google Scholar 

  • Chappell BW, White AJR, Wyborn D (1987) The importance of residual source material (restite) in granite petrogenesis. J Petrol 28:1111–1138

    Google Scholar 

  • Clemens JD (1981) Origin and evolution of some Peraluminous Acid Magmas. PhD thesis (unpubl.), Monash University, Australia

  • Clemens JD (1982) The Tolmie Igneous Complex, Australia: high-T S-type rhyolites with polybaric crystallization histories. Geol Soc Am Abstr Prog 14:464–465

    Google Scholar 

  • Clemens JD (1984) Water contents of intermediate to silicic magmas. Lithos 17:273–287

    Article  Google Scholar 

  • Clemens JD (1989) The importance of residual source material (restite) in granite petrogenesis: a comment. J Petrol 30:1313–1316

    Google Scholar 

  • Clemens JD, Benn K (2010) Anatomy, emplacement and evolution of a shallow-level, post-tectonic laccolith: the Mt Disappointment pluton, SE Australia. J Geol Soc 167(5):915–941

    Article  Google Scholar 

  • Clemens JD, Wall VJ (1981) Crystallization and origin of some peraluminous (S-type) granitic magmas. Can Mineral 19:111–131

    Google Scholar 

  • Clemens JD, Wall VJ (1984) Origin and evolution of a peraluminous silicic ignimbrite suite: the Violet Town Volcanics. Contrib Mineral Petrol 88:354–371

    Article  Google Scholar 

  • Clemens JD, Watkins JM (2001) The fluid regime of high-temperature metamorphism during granitoid magma genesis. Contrib Mineral Petrol 140:600–606

    Article  Google Scholar 

  • Clemens JD, Petford N, Mawer CK (1997) Ascent mechanisms of granitic magmas: causes and consequences. In: Holness M (ed) Deformation-enhanced fluid transport in the earth’s crust and mantle. Chapman & Hall, London, pp 144–171

    Google Scholar 

  • Clemens JD, Helps PA, Stevens G (2010) Chemical structure in granitic magmas—a signal from the source?. Earth Environ Sci Trans R Soc Edinburgh 100(1–2): 159–172, doi:10.1017/s1755691009016053

  • Condie KC (1993) Chemical composition and evolution of the upper continental crust: contrasting results from surface samples and shales. Chem Geol 104:1–37

    Article  Google Scholar 

  • Connolly JAD (2009) The geodynamic equation of state: what and how. G3 10:Q10014, doi:10.1029/2009GC002540

  • Douglas GB (1985) Geology of the Tatong region, north east Victoria. BSc Hons thesis, Department of Geology, La Trobe University, Bundoora

  • Droop GTR (1987) A general equation for estimating Fe-3 + concentrations in ferromagnesian silicates and oxides from microprobe analyses, using stoichiometric criteria. Mineralog Mag 51:431–435

    Article  Google Scholar 

  • Finlayson DM, Wake-Dyster KD, Leven JH, Johnstone DW, Murray CG, Harrington HJ, Korsch RJ, Wellman P (1990) Seismic imaging of major tectonic features in the crust of Phanerozoic eastern Australia. Tectonophysics 173:221–230

    Google Scholar 

  • Finlayson DM, Leven JH, Johnstone DW, Korsch RJ, Glen RA (1998) Crustal architecture in the eastern Lachlan Orogen from deep seismic profiling at wide-angle and near-vertical incidence. Geol Soc Aust Abstracts 49:144

    Google Scholar 

  • Frost BR, Barnes CG, Collins WJ, Arculus RJ, Ellis DJ, Frost CD (2001) A geochemical classification for granitic rocks. J Petrol 42:2033–2048

    Article  Google Scholar 

  • Gaul AJ (1982) Geology of the Tolmie Highlands. MSc thesis (unpubl.), Monash University, Australia

  • Gaul AJ (1995) Geology of the Tolmie Highlands Igneous Complex. PhD thesis (unpubl.), Monash University, Australia

  • Gibson G, Wesson V, Cuthbertson R (1981) Seismicity of Victoria to 1980. J Geol Soc Aust 28:341–356

    Google Scholar 

  • Gray CM (1990) A strontium isotopic traverse across the granitic rocks of southeastern Australia: petrogenetic and tectonic implications. Aust J Earth Sci 37:331–349

    Article  Google Scholar 

  • Hills ES (1929) The geology and palaeontology of the Cathedral Range and Blue Hills in northwestern Gippsland. Proc R Soc Victoria 41:176–201

    Google Scholar 

  • Le Maitre RW, Bateman P, Dudek A, Keller J, Lameyre Le Bas MJ, Sabine PA, Schmid R, Sorensen H, Streckeisen A, Wolley AR, Zanettin B (1989) A classification of igneous rocks and glossary of terms. Blackwell, Oxford

    Google Scholar 

  • Long JA, Werdelin L (1986) A new Late Devonian bothriolepid (Placodermi, Antiarcha) from Victoria, with descriptions of other species from the state. Alcheringa 10:355–399

    Article  Google Scholar 

  • McCulloch MT, Chappell BW (1982) Nd isotopic characteristics of S- and I-type granites. Earth Planet Sci Lett 58:51–64

    Article  Google Scholar 

  • McDonough WF, Sun S-S (1995) Composition of the earth. Chem Geol 120:223–253

    Article  Google Scholar 

  • McDougall I, Compston W, Bofinger VM (1966) Isotopic age determinations on Upper Devonian rocks from Victoria, Australia: a revised estimate for the age of the Devonian–Carboniferous boundary. Geol Soc Am Bull 77:1075–1088

    Article  Google Scholar 

  • Montel J-M, Vielzeuf D (1997) Partial melting of metagreywackes, Part II. Compositions of minerals and melts. Contrib Mineral Petrol 128:176–196

    Article  Google Scholar 

  • Nisbet P (1978) Geology of the Mt Samaria region, Central Victoria. BSc (Hons) thesis (unpubl.) Monash University, Australia

  • Niu Y, Collerson K, Batiza R, Wendt J, Regelous M (1999) Origin of enriched-type mid-ocean ridge basalt at ridges far from mantle plumes: The East Pacific Rise at 11°20’N. J Geophys Res-solid Earth B104:7067–7087

    Article  Google Scholar 

  • O’Halloran GJ, Gaul AJ (1997) Sedimentary responses to sub-aerial felsic volcanism from the Late Devonian–early Carboniferous northern Macalister Synclinorium, southeastern Australia. Sed Geol 109:209–232

    Article  Google Scholar 

  • Patiño Douce AE, Beard JS (1996) Effects of P, f(O2) and Mg/Fe ratio on dehydration melting of model metagreywackes. J Petrol 37:999–1024

    Article  Google Scholar 

  • Phillips GN, Wall VJ, Clemens JD (1981) Petrology of the Strathbogie batholith: a cordierite-bearing granite. Can Mineral 19:47–64

    Google Scholar 

  • Putirka KD (2005) Igneous thermometers and barometers based on plagioclase + liquid equilibria: tests of some existing models and new calibrations. Am Mineral 90:336–346

    Article  Google Scholar 

  • Richards JR, Singleton OP (1981) Palaeozoic Victoria, Australia: igneous rocks, ages and their interpretation. J Geol Soc Aust 28:395–421

    Google Scholar 

  • Rickard MJ, Ward P (1981) Palaeozoic crustal thickness in the southern part of the Lachlan orogen deduced from volcano and pluton-spacing geometry. J Geol Soc Aust 28:19–32

    Google Scholar 

  • Scaillet B, Holtz F, Pichavant M (1998) Phase equilibrium constraints on the viscosity of silicic magmas—1. Volcanic-plutonic association. J Geophys Res-solid Earth 103:27257–27266

    Article  Google Scholar 

  • Stevens G, Clemens JD (2011) Titanium: a key to the processes that control granite chemistry. Nature (in press)

  • Stevens G, Clemens JD, Droop GTR (1997) Melt production during granulite-facies anatexis: experimental data from “primitive” metasedimentary protoliths. Contrib Mineral Petrol 128:352–370

    Article  Google Scholar 

  • Stevens G, Villaros A, Moyen JF (2007) Selective peritectic garnet entrainment as the origin of geochemical diversity in S-type granites. Geology 35:9–12

    Article  Google Scholar 

  • Taylor SR, McLennan SM (1995) The geochemical evolution of the continental crust. Rev Geophys 33:241–265

    Article  Google Scholar 

  • VandenBerg AHM, Willman CE, Maher S, Simons BA, Cayley RA, Taylor DH, Morand VJ, Moore DH, Radojkovic A (2000) The Tasman fold belt system in Victoria. Geological Survey of Victoria Special Publication, Melbourne, p 483

    Google Scholar 

  • Vielzeuf D, Montel J-M (1994) Partial melting of metagreywackes. 1. Fluid-absent experiments and phase relationships. Contrib Mineral Petrol 117:375–393

    Article  Google Scholar 

  • Villaros A, Stevens G, Moyen J-F, Buick IS (2009) The trace element compositions of S-type granites: evidence for disequilibrium melting and accessory phase entrainment in the source. Contrib Mineral Petrol 158:543–561

    Article  Google Scholar 

  • Waight TE, Dean AA, Maas R, Nicholls IA (2000a) Sr and Nd isotopic investigations towards the origin of feldspar megacrysts in microgranular enclaves in two I-type plutons of the Lachlan Fold Belt, southeast Australia. Aust J Earth Sci 47:1105–1112

    Article  Google Scholar 

  • Waight TE, Maas R, Nicholls IA (2000b) Fingerprinting feldspar phenocrysts using crystal isotopic composition stratigraphy: implications for crystal transfer and magma mingling in S-type granites. Contrib Mineral Petrol 139:227–239

    Article  Google Scholar 

  • Wall VJ, Clemens JD, Clarke DB (1987) Models for granitoid evolution and source compositions. J Geol 95:731–750

    Article  Google Scholar 

  • Wedepohl KH (1995) The composition of the continental crust. Geochim Cosmochim Acta 59:1217–1239

    Article  Google Scholar 

  • Whitney DL, Evans BW (2010) Abbreviations for names of rock-forming minerals. Am Mineral 95:185–187

    Article  Google Scholar 

  • Wohletz KH (1999) MAGMA: Calculates IUGS Volcanic Rock Classification, Densities, and Viscosities. Los Alamos National Laboratory computer code LA-CC 99-28, Los Alamos New Mexico

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Acknowledgments

This paper contains some whole-rock geochemical data on the TI, from unpublished work towards an MSc thesis that was being prepared, for Melbourne University, by the late Raymond Dudley. These data are included here by kind permission of Raymond’s widow Janice. Likewise, many whole-rock analyses reported here are also taken from the MSc and PhD theses of Dr Anthony Gaul. These data were made available to us through permission from both Tony and his former supervisor, Dr Ian Nicholls, at Monash University. We are grateful to these people for providing us with these data. Work for this paper was supported partly through NRF Incentive Funds and Stellenbosch University Establishment Funds awarded to JDC. We also acknowledge the valuable contributions made by Gary Stevens and another anonymous reviewer.

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Correspondence to J. D. Clemens.

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Communicated by J. Hoefs.

R. A. Dudley: deceased.

An erratum to this article can be found at http://dx.doi.org/10.1007/s00410-011-0666-8

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Clemens, J.D., Birch, W.D. & Dudley, R.A. S-type ignimbrites with polybaric crystallisation histories: the Tolmie Igneous Complex, Central Victoria, Australia. Contrib Mineral Petrol 162, 1315–1337 (2011). https://doi.org/10.1007/s00410-011-0652-1

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