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Green ferric clay in non-marine sandstones of the Rewan Group, southern Bowen Basin, Eastern Australia

Published online by Cambridge University Press:  09 July 2018

J. C. Baker
J. C. Baker*
Affiliation:
Centre for Microscopy and Microanalysis, The University of Queensland, Brisbane, Queensland, 4072, Australia, and K.R. Martin Pty. Ltd., P.O. Box 22, Kenmore, Queensland, 4069, Australia
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Abstract

Accessory green ferric clay occurs in fluvial litharenites of the Early Triassic Rewan Group. Although resembling glauconitic minerals in thin-section, electron microprobe analyses indicate that the green ferric clay is mainly ferric illite. The ferric illite may have formed in a small hypersaline lake or well drained, flood-plain soil, and its presence in the Rewan Group cannot be used to support a notion that the unit is partly marine influenced. Identification of the ferric illite by electron microprobe analysis shows that some green ferric clays, particularly those that resemble glauconitic minerals optically, may require precise quantitative elemental analysis before they can be used as a basis for environmental interpretation. Green ferric clay in the Rewan Group also includes detrital celadonite that most likely originated in a volcanic arc setting.

Type
Research Article
Information
Clay Minerals , Volume 32 , Issue 4 , December 1997 , pp. 499 - 506
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1997

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References

Baker, J.C., Kassan, J. & Hamilton, P.J. (1996) Early diagenetic siderite as an indicator of depositional environment in the Triassic Rewan Group, southern Bowen Basin, eastem Australia. Sedimentology 43, 77–88.Google Scholar
Berg-Madsen, V. (1983) High-alumina glaucony from the Middle Cambrian of Oland and Bornholm, southern Baltoscandia. J. Sed. Pet. 53, 875–893.Google Scholar
Cundill Meyers Resources Ltd. (1983) Tiggrigie Creek No. 1. Geological report, Open file, held by Queensland Department of Minerals and Energy.Google Scholar
Dasgupta, S., Chaudhuri, A.K. & Fukuoka, M. (1990) Compositional characteristics of glauconitic alterations of K-feldspar from India and their implications. J. Sed. Pet. 60, 277–281.Google Scholar
Deconinck, J.F., Strasser, A. & Debrabant, P. (1988) Formation of illitic minerals at surface temperatures in Purbeckian sediments (Lower Berriasian, Swiss and French Jura). Clay Miner. 23, 91–103.CrossRefGoogle Scholar
Fielding, C.R., Caritat, P. de, Baker, J.C. & Wilkinson, M.M. (1994) Permian to mid-Triassic evolution of sandstone composition in a complex back-arc extensional to foreland basin: the Bowen Basin, eastern Queensland, Australia. Pp. 109-117 in: Proc. 29th Int. Geol. Cong. (Part A) Sandstone Petrology in Relation to Tectonics (Kumon, F. & Yu, K.M., editors).Google Scholar
Fielding, C.R., Stephens, C.J., Kassan, J. & Holcombe, R.J. (1995) Revised palaeogeographic maps for the Bowen Basin, central Queensland. Pp. 7–15 in: Proc. Bowen Basin Symp. 1995 (Follington, I.J., Beeston, J.W. & Hamilton, L.H., editors).Google Scholar
Folk, R.L., Andrews, P.B. & Lewis, D.W. (1970) Detrital sedimentary rock classification and nomenclature for use in New Zealand. N. Z. J. Geol. Geophys. 13, 947–968.Google Scholar
Hekel, H. (1983) Palynology and biostratigraphy of core and cuttings samples from COE Tiggriggie Creek 1. Company Report, Open File, held by Queensland Department of Minerals and Energy.Google Scholar
Ireland, B.J., Curtis, C.D. & Whiteman, J.A. (1983) Compositional variation within some glauconites and illites and implications for their stability and origins. Sedimentology 30, 769–786.Google Scholar
Jeans, C.V., Mitchell, J.G., Scherer, M. & Fisher, M.J. (1994) Origin of the Permo-Triassic clay mica assemblage. Clay Miner. 29, 575–589.Google Scholar
Jensen, A.R. (1975) Permo-Triassic stratigraphy and sedimentation in the Bowen Basin, Queensland. Bull. Bur. Miner. Resour. Geol. Geophys. Aust. 154.Google Scholar
Kassan, J. (1993) Basin analysis of the Triassic succession, Bowen Basin. PhD thesis, Queensland Univ., Australia.Google Scholar
Kassan, J. & Fielding, C.R. (1996) Aspects of Triassic sedimentation in the Bowen Basin, Queensland. Geol. Soc. Aust. Ext. Absts. 43, 292–301.Google Scholar
Kossovskaya, A.G. & Drits, V.A. (1970) The variability of micaceous minerals in sedimentary rocks. Sedimentology 15, 83–101.CrossRefGoogle Scholar
Martin, K.R. (1992) Sedimentology, petrology and reservoir quality of the Bandanna Formation to Showgrounds Sandstone interval in Namarah no. 3, Bowen-Surat Basin. Report to Oil Company of Australia, Brisbane, Australia.Google Scholar
McConchie, D.M. & Lewis, D.W. (1980) Varieties of glauconite in late Cretaceous and early Tertiary rocks of the South Island of New Zealand, and new proposals for classification. N. Z. J. Geol. Geophys. 23, 413–437.Google Scholar
Newman, A.C.D. & Brown, G. (1987) The chemical constitution of clays. Pp. 1 – 128 in: Chemistry of Clays and Clay Minerals (Newman, A.C.D., editor), Mineralogical Society, London.Google Scholar
Norrish, K. & Picketing, J.G. (1983) Clay minerals. Pp. 281–308 in: Soils: an Australian Viewpoint, Division of Soils, CSIRO, Melbourne/Academic Press, London.Google Scholar
Odin, G.S. & Fullagar, P.D. (1988) Geological significance of the glaucony facies. Pp. 295–332 in: Green Marine Clays (Odin, G.S., editor), Dev. SedimentoL 45.Google Scholar
Odin, G.S., Desprairies, P.D., Fullagar, P.D., Bellon, H., Decarreau, A., Fröhlich, F. & Zelvelder, M. (1988) Nature and geological significance of celadonite. Pp. 337-398 in: Green Marine Clays (Odin, G.S., editor), Dev. Sedimentol. 45.Google Scholar
Odom, I.E. (1984) Glauconite and celadonite minerals. Pp. 545-572 in: Micas (Bailey, S.W., editor), Rev. Mineralogy 13, Mineralogical Society of America, Washington, D.C..Google Scholar
Porrenga, D.H. (1968) Non-marine glauconitic illite in the lower Oligocene of Aardebrug, Belgium. Clay Miner. 7, 421–430.Google Scholar
Van Houten, F.B. & Purucker, M.E. (1984) Glauconitic peloids and chamositic ooids - favourable factors, constraints, and problems. Earth Sci. Rev. 20, 211–243.Google Scholar
Wise, W.S. & Eugster, H.P. (1964) Celadonite: synthesis, thermal stability and occurrence. Am. Miner. 49, 1031–1083.Google Scholar