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Geochemistry, mineralogy and plate tectonic setting of a Late Cretaceous Sn-W Granite from Sumatra, Indonesia

Published online by Cambridge University Press:  05 July 2018

M. C. G. Clarke
Affiliation:
Overseas Directorate, British Geological Survey, Keyworth, Nottingham NG12 5GG, England
B. Beddoe-Stephens
Affiliation:
Geochemistry Directorate, British Geological Survey, Murchison House, West Mains Road, Edinburgh EH9 3LA, Scotland

Abstract

The Hatapang granite was discovered during geological mapping and mineral exploration in northern Sumatra by the British Geological Survey in conjunction with the Indonesian Directorate of Mineral Resources. The pluton comprises a two-mica granite which shows significant greisenization and veining around its margins associated with Sn and W mineralization. An Rb-Sr isochron derived for the pluton indicates an age of 80 Ma and an initial 87Sr/86Sr ratio of 0.7151. This together with major and trace element data show the Hatapang to be of clear S-type affinity.

The greisens are quartz-mica-topaz rocks and are almost totally deficient in Na. Trioctahedral mica compositions progress from biotite through siderophyllite to zinnwaldite during final differentiation and greisenization of the granite. Accompanying dioctahedral micas are phengitic. Associated with late-stage differentiation of the granite is the precipitation of tourmaline and various Nb-Ta oxides. Sn and W mineralization is manifested as cassiterite in the greisens, while wolframite tends to be related to quartz veining. A later and lower temperature sulphide event produced a suite of base metal sulphides and Ag-Bi-Pb sulphosalts. The identification of a Sn-W granite of Cretaceous age in northern Sumatra provides a link with occurrences of economically important Late Cretaceous Sn-W granites in Thailand and Burma and increases the potential of an area which until recently was thought to lie outside the SE Asian tin belt.

Type
Geochemistry
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1987

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Footnotes

*

Author for correspondence.

References

Atherton, M.P., McCourt, W.J., Sanderson, L.M., and Taylor, W.P. (1979) The geochemical character of the segmented Peruvian Coastal batholith and associated volcanics. In Origin of oranite batholiths—-geochemical evidence(Atherton, M., and Tarney, J., eds.). Shiva, 45-64.CrossRefGoogle Scholar
Bailey, J.C. (1977) Fluorine in granitic rocks and melts: a review. Chem. Geol. 19, 142.CrossRefGoogle Scholar
Ball, T.K., Fortey, N.J., and Shepherd, T.J. (1985) Mineralisation at the Carrock Fell tungsten mine, N.E.gland: Paragenetic, fluid inclusion and geochemical study. Mineral. Deposita, 20, 57-65.CrossRefGoogle Scholar
Beckinsale, R.D. (1979) Granite magmatism in the tin belt of Southeast Asia. In Origin of granite batholiths geochemical evidence(Atherton, M.P., and Tarney, J., eds.). Shiva, 34-44.CrossRefGoogle Scholar
Cameron, N.R., Clarke, M.C.G., Aldiss, D.T., Aspden, J.A., and Djunuddin, A. (1980) The geologic evolution of northern Sumatra. Proe. 9th Ann. Conf. Indon. Petrol. Assoc., Jakarta.149-87.Google Scholar
Chappell, B.W., and White, A.J.R. (1974) Two contrasting granite types. Pacific Geol. 8, 17-34.Google Scholar
Clarke, M.C.G., Ghazali, S.A., Harahap, H.K.syono, and Stephenson, B. (1982) The geology of the Pemantangsiantar Quadrangle, Sumatra (with map). Geol. Res. Dev. Centre, Bandung.Google Scholar
Coleman, R.G., and Donato, M.M. (1979) Oceanic plagiogranite revisited. In Trondjemites, dacites and related rocks (Barker, F., ed.). Elsevier, 149-68.CrossRefGoogle Scholar
Deer, W.A., Howie, R.A., and Zussman, J. (1962) Rock forming minerals. Vol. 3 (Sheet silicates). Longmans.Google Scholar
El Bouseily, A.M., and E1 Sokkary, A.A. (1975) The relation between Rb, Ba and Sr in granitic rocks. Chem. Geol. 16, 207-19.CrossRefGoogle Scholar
Eugster, H. (1985) Granites and hydrothermal ore deposits: a geochemical framework. Mineral. Mag. 49, 723.CrossRefGoogle Scholar
Exley, C.S., Stone, M., and Floyd, P.A. (1983) Composition and petrogenesis of the Cornubian granite batholith and post-orogenic volcanic rocks in Southwest England. In The Variscanfold belt in the British Isles (Hancock, P.L., ed.). Hilger, 153-77.Google Scholar
Graham, J., and Thornber, M.R. (1974) The crystal chemistry of complex niobium and tantalum oxides. 1: Structural classification. Am. Mineral. 59, 1026- 39.Google Scholar
Groves, D.I. (1972) The geochemical evolution of tinbearing granites in the Blue Tier Batholith, Tasmania. Econ. Geol. 67, 445-57.CrossRefGoogle Scholar
Groves, D.I. and Baker, W.E. (1972) The regional variation in composition of wolframites from Tasmania. Ibid. 67, 3628.CrossRefGoogle Scholar
Groves, D.I. and McCarthy, T.S. (1978) Fractional crystallisation and the origin of tin deposits in granitoids. Mineral. Deposita, 13, 11-26.CrossRefGoogle Scholar
Groves, D.I. and Taylor, R.G. (1973) Greisenisation and mineralisation at Anchor tin mine, northeast Tasmania. Trans. Inst. Mining Metall. 82, B13-546.Google Scholar
Hamidsyah, H., and Clarke, M.C.G. (1982) Discovery of primary tungsten and tin mineralisation in North Sumatra, Indonesia. In Symposium on tungsten geology (Hepworth, J.V., and Yu Hong Zhang, eds.). ESCAP/ RMRDC (UN), China, 49-58.Google Scholar
Hildreth, W. (1981) Gradients in silicic magma chambers: Implications for lithospheric magmatism. J. Geophys. Res. 86B, 1015–392.Google Scholar
Hosking, K.F.G. (1977) Known relationships between the ‘hard rock’ tin deposits and the granites of Southeast Asia. Geol. Soc. Malaysia Bull. 9, 141-57.CrossRefGoogle Scholar
Hutchinson, C.S., and Taylor, D. (1978) Metallogenesis in SE Asia. J. Geol. Soc. London, 135, 40728.Google Scholar
Imeokparia, E.G. (1983) Geochemical aspects of the evolution and mineralisation of the Amo Younger Granite Complex (northern Nigeria). Chem. Geol. 40, 293-312.CrossRefGoogle Scholar
Ishihara, S. (1977) The magnetite-series and ilmeniteseries granitic rocks. Min. Geol. Japan, 27, 293305.Google Scholar
Johari, S., Clarke, M.C.G., Djunuddin, A, and Stephenson, B. (1981) New evidence of tin and tungsten mineralisation in northern Sumatra. Proc. 4th Reg. Conf. Geol. SE Asia.Geol. Soc. Philippines, 497-508.Google Scholar
Leat, P.T., MacDonald, R., and Smith, R.L. (1984) Chemical evolution of the Menengai caldera volcano, Kenya. J. Geophys. Res. 89B, 857-192.Google Scholar
Lowell, G.R., and Gasparrini, C. (1982) Composition of arsenopyrite from topaz greisen veins in southeast Missouri. Mineral. Deposita, 17, 229-38.CrossRefGoogle Scholar
Manning, D.A.C., Hamilton, D.L., Henderson, C.M.B., and Dempsey, M.J. (1980) The probable occurrence of interstitial A1 in hydrous F-bearing and F-free aluminosilicate melts. Contrib. Mineral. Petrol. 75, 257-62.CrossRefGoogle Scholar
Metcalfe, I. (1983) Conodont faunas, age and correlation of the Alas Formation (Carboniferous), Sumatra. Geol. Mag. 120, 579-86.CrossRefGoogle Scholar
Mitchell, A.H.G. (1979) Rift, subduction and collision related tin belts. Geol. Soc. Malaysia Bull. 11, 81- 102.Google Scholar
Oen, I.S., Korpershoek, H.R., Kieft, C, and Lustenhouwer, W.J. (1982) A microprobe study of rutile, cassiterite, wolframite and sulphides in the Mono Potosi greisen, Rondonia, Brazil. Neues Jahrb. Mineral. Mh.175-91.Google Scholar
Page, B.G.N., Bennett, J.D., Cameron, N.R., Bridge, D.M.C., Jeffrey, D.H., Keats, W., and Thaib, J. (1978) Regional geochemistry and geological reconnaissance mapping and mineral exploration in northern Sumatra, Indonesia. Proc. llth Common. Min. Metall. Congr., Hongkong, 455-62.Google Scholar
Pitcher, W.S. (1983) Granite type and tectonic environment. In Mountain building processes (Hsu, K., ed.). Academic Press, 19-40.Google Scholar
Plant, J.A., Brown, G.C., Simpson, P.R., and Smith, R.T. (1980) Signatures of metalliferous granites in the Scottish Caledonides. Trans. Inst. Mining Metall. 89, B198-210.Google Scholar
Shepherd, T.J., and Waters, P. (1984) Fluid inclusion gas studies, Carrock Fell tungsten deposit, England: Implications for regional exploration. Mineral. Deposita, 19, 304-14.CrossRefGoogle Scholar
Stephenson, B., Ghazali, S.A., and Widjaja, H. (1982) Regional geochemical atlas series of Indonesia, 1. BGS, Keyworth, UK.Google Scholar
Steiger, R.H., and Jaeger, E. (1977) Subcommission on geochronology: Convention on the use of decay constants in geocosmochronology. Earth Planet. Sci. Lett. 36, 359-62.CrossRefGoogle Scholar
Streckeisen, A.L. (1976) To each plutonic rock its proper name. Earth Sci. Rev. 12, 133.CrossRefGoogle Scholar
Suryono, and Clarke, M.C.G. (1982) Primary tungsten occurrences in Sumatra and the Indonesian tin islands. In Symposium on tungsten geology(Hepworth, J.V., and Yu Hong Zhang, eds.). ESCAP/RMRDC (UN), China, 21731.Google Scholar
Tanelli, G. (1982) Geological setting, mineralogy and genesis of tungsten mineralisation in the Dayu district, Jiangxi (People's Republic of China): An outline. Mineral. Deposita, 17, 27994.CrossRefGoogle Scholar
Taylor, S.R. (1964) Abundance of chemical elements in the continental crust: A new table. Geochim. Cosmochim. Acta, 28, 127-385.Google Scholar
York, D. (1969) Least squares fitting of a straight line with correlated errors. Earth Planet. Sci. Lett. 5, 320-4.CrossRefGoogle Scholar