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Mafic Phyllosilicates in Low-Grade Metabasites. Characterization Using Deconvolution Analysis

Published online by Cambridge University Press:  09 July 2018

D. Robinson
Affiliation:
Department of Geology, University of Bristol, Bristol BS8 1RJ, and Department of Geology, National Museum of Wales, Cardiff CF1 3NP, UK
R. E. Bevins
Affiliation:
Department of Geology, University of Bristol, Bristol BS8 1RJ, and Department of Geology, National Museum of Wales, Cardiff CF1 3NP, UK

Abstract

The <2 µm clay fractions from low-grade metabasalts of eastern North Greenland are mixtures of mafic phyllosilicates and celadonite that show complex X-ray diffraction (XRD) patterns. Interpretation of such patterns is difficult and subjective using only visual examination of peak positions and shapes. Deconvolution analysis offers a less subjective means of identifying peak positions for overlapping peaks and is applied to several composite peaks in a pattern; the peaks identified are then rationalized in terms of specific mixed-layer phases. Comparison against NEWMOD patterns of the identified clay mixture provides an additional constraint on the phases identified. Three mafic phyllosilicates, discrete chlorite and two chlorite-smectites with 60:40 and 80:20 proportions are demonstrated in the same XRD pattern. Modelling using NEWMOD of a mechanical mixture between these mineral shows an excellent match to the observed XRD pattern. The recognition in low-grade metabasalts of chlorite and random and different varieties of regular mixed-layer chlorite-smectite offers support for the classical model of a tri-smectite to chlorite transition. This is in contrast to an alternative model proposing smectite and chlorite end-members with corrensite as a discrete phase crystallizing directly without intervening mixed-layer chlorite-smectite.

Type
Research Article
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1994

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References

Bailey, S.W. (1982) Nomenclature for regular interstratifications. Am. Miner, 67, 394398.Google Scholar
Bevins, R.E., Rowbotham, G. & Robinson, D. (1991a) Zeolite facies metamorphism of the late Proterozoic ZigZag Dal Basalt Formation, eastern North Greenland. Litho, 27, 155165.Google Scholar
Bevins, R.E., Robinson, D. & Rowbotham, G. (1991b) Compositional variation in mafic phyllosilicates from regional low grade metabasites and application of the chlorite geothermometer. J. Met. Geol, 9, 711721.Google Scholar
Brown, G. & Brindley, G.W. (1980) X-ray diffraction procedures for clay mineral identification. Pp. 305-359 in: Crystal Structures of Clay Minerals and their X-ray Identification. (G.W. Brindley & G. Brown, editors) Mineralogical Society, London.Google Scholar
Cathelineau, M. & Nievā D. (1985) A chlorite solid solution geothermometer. The Los Azufres geothermal system (Mexico). Contr. Miner. Petr, 91, 235244.Google Scholar
Frey, M., de Capitani, C. & Liou, I.G. (1991) A new petrogenetic grid for low grade metabasites. J. Met. Geol, 9, 497509.CrossRefGoogle Scholar
Howard, S.A. & Preston, K.D. (1989) Profile fitting of powder diffraction patterns. Pp. 217-275 in: Modern Powder Diffraction (D.L. Bish & J.E. Post, editors). Reviews in Mineralogy, 20, Mineralogical Society of America, Washington.Google Scholar
Hower, J. (1981) X-ray identification of mixed-layer clay minerals. Pp. 39-59 in: Clays and the Resource Geologist. (F.J. Longstaffe, editor) Short Course Handbook, 7, Mineralogical Association of Canada.Google Scholar
Jenkins, R. & Schreiner, M.N. (1986) Consideration in the design of goniometers for use in X-ray powder diffraction. Powder Diffractio, 7, 305319.CrossRefGoogle Scholar
Kristmansdéttir, H. (1979) Alteration of basaltic rocks by hydrothermal activity at 100-300°C. Proc. 6th Int. Clay Conf. Oxford, 359-367.Google Scholar
Lanson, B. & Champion, D. (1991) The I/S-to-illite reaction in the late stage diagenesis. Amer. J. Sci, 291, 473506.Google Scholar
Lanson, B. & Velde, B. (1992) Decomposition of X-ray diffraction patterns: a convenient way to describe complex I/S diagenetic evolution. Clays Clay Miner, 40, 629643.Google Scholar
Liou, J.G., Maruyama, S. & Cho, M. (1985) Phase equilibria and mineral parageneses of metabasites in low grade metamorphism. Mineral. Mag, 49, 321333.CrossRefGoogle Scholar
Reynolds, R.C. (1980) Interstratified clay minerals. Pp. 249-303 in: Crystal Structures of Clay Minerals and their X-ray Identification. (G.W. Brindley & G. Brown, editors) Mineralogical Society, London.Google Scholar
Reynolds, R.C. (1985) NEWMOD© a Computer program for the Calculation of One-Dimensional Diffraction Patterns of Mixed Layered Clay Minerals. R.C. Reynolds, 8 Brook Rd, Hanover, New Hampshire, 03755, USA.Google Scholar
Reynolds, R.C. (1988) Mixed layer chlorite minerals. Pp. 601-629 in: Hydrous Phyllosilicates (Exclusive of Micas). (S.W. Bailey, editor). Reviews in Mineralogy, 19, Mineralogy Society of America, Washington.Google Scholar
Roberson, H.E. (1987) Corrensite and chlorite in subsea floor hydrothermal altered basalts. Abstracts Clay Minerals Society, 24th Annual General Meeting. Google Scholar
Roberson, H.E. (1988) Random mixed-layer chlorite- smectite: does it exist? Abstract, Clay Minerals Society, 25th Annual General Meeting. Google Scholar
Robinson, D., Bevins, R.E. & Rowbotham, G. (1983) The characterization of mafic phyllosilicates in low grade metabasites from eastern North Greenland. Am. Miner, 78, 377390.Google Scholar
Schreiner, W.N. & Jenkins, R. (1980) A second derivative algorithm for identification of peaks in powder diffraction. Adv. X-ray Analysis, 23, 287293.Google Scholar
Schreiner, W.N. & Jenkins, R. (1983) Profile fitting for quantitative analysis in X-ray powder diffraction. Adv. X-ray Analysi, 26, 6669.Google Scholar
Shau, Y.-H. & Peacor, D.R. (1992) Phyllosilicates in hydrothermally altered basalts from DSDP Hole 504B, Leg 83-a TEM and AEM study. Contr. Miner. Petr, 112, 119133.Google Scholar
Shau, Y.-H., Peacor, D.R. & EsseneE.J. (1990) Corrensite and mixed-layer chlorite/corrensite in metabasalt from northern Taiwan: TEM/AEM, EMPA, XRD and optical studies. Contr. Miner. Petr, 105, 123142.Google Scholar
Stern, W.B., Mullis, J., Rahn, M. & Frey, M. (1991) Deconvolution of the first ‘illite’ basal reflection. Schweiz Mineral. Petrogr. Mitt, 71, 453–162.Google Scholar
Tomasson, J. & KristmansdOttir, H. (1972) High temperature alteration minerals and thermal brines, Reykjanes, Iceland. Contr. Miner. Petr, 36, 123134.Google Scholar