Hostname: page-component-78c5997874-8bhkd Total loading time: 0 Render date: 2024-11-10T13:39:40.379Z Has data issue: false hasContentIssue false

Modelling of dissolution–reprecipitation ion-exchange reactions for the development of flame perthite in a suite of sheared alkaline rocks: an example from Chimakurthy, Eastern Ghats, India

Published online by Cambridge University Press:  05 July 2018

Sudip Bhattacharyya*
Affiliation:
Petrology Division, Eastern Region, Geological Survey of India, Kolkata-700091, India
P. Sengupta
Affiliation:
Department of Geological Sciences, Jadavpur University, Kolkata-700032, India
*

Abstract

A suite of sheared syenites occurring along the western margin of the Eastern Ghats Belt, India have developed extensive flame perthite in K-feldspar. Albite flames show large variation in size, shape and abundance. Field, petrographic and chemical evidence suggests complex interplay between differential stress, recycling of K-Na-Ca and supply of Na by infiltration for the development of flame perthite. Partial replacement of pyroxenes, plagioclase and alkali feldspar by amphibole, biotite, nepheline and calcite causes internal recycling of Na-Ca-K in a closed system. Representative compositions of the minerals are used to constrain the model dissolution–reprecipitation ion-exchange reactions involving Na and K either as reactants and/or as products. A substantial proportion of Na+ required for the development of the albite flames, originates from Na metasomatism accompanied by ductile shearing in the feldspathic rocks, providing an ideal open system wherein both the differential stress and Na+ are made available for the development of the flame perthites. This process probably augmented the replacement of K-feldspar grains by flame albite and the K+ released was carried away by the fluid or, possibly, augmented the biotite-forming reactions in the associated quartz-poor syenites and, hence, trigger the Na-K cycle in these rocks.

Type
Research Article
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 2014

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Allison, I. and La Tour, T.E., (1977) Brittle deformation of hornblende in a mylonite: direct geometrical analogue of ductile deformation by translation gliding. Canadian Journal of Earth Sciences, 14, 19531958.CrossRefGoogle Scholar
Anderson, D.J., Lindsley, D.H., and Davidson, P.M., (1993) QUILF: A Pascal program to assess equilibria among Fe-Mg-Mn-Ti oxides, pyroxenes, olivine and quartz. Computers and Geosciences, 19, 13331350.CrossRefGoogle Scholar
Bhattacharyya, S. (2000) Geology and geochemistry of a suite of alkaline rocks from Chimakurthy, Prakasam district, Andhra Pradesh. Unpublished PhD thesis, Jadavpur University, Calcutta, India.Google Scholar
Bhattacharya, A., Krishnakumar, K.R., Raith, M. and Sen, S.K., (1991) An improved set of a-x parameters for the Fe-Mg-Ca garnets and refinements of the orthopyroxene-garnet thermometer and the orthopyroxene- garnet-plagioclase-quartz barometer. Journal of Petrology, 32, 629656.CrossRefGoogle Scholar
Blundy, J.D., and Holland, T.J.B. (1990) Calcic amphibole equilibria and a new amphibole-plagioclase geothermometer. Contributions to Mineralogy and Petrology, 104, 208228.CrossRefGoogle Scholar
Brown, W.L., and Parsons, I. (1993) Storage and release of elastic strain energy: the driving force for low temperature reactivity and alteration of alkali feldspar. Pp. 267290 in: Defects and Processes in the Solid State: Geoscience Applications – The McLaren volume (J. Bonald and J.D Fitz Gerald, editors). Elsevier Science Publishers BV, Amsterdam.Google Scholar
Dasgupta, S., Ehl, J., Raith, M.M., Sengupta, Pr. and Sengupta, P. (1997) Mid-crustal contact metamorphism around the Chimakurthy mafic-ultramafic complex, Eastern Ghats Belt, India. Contributions to Mineralogy and Petrology, 129, 182197.CrossRefGoogle Scholar
Dasgupta, S., Sengupta, P., Sengupta, Pr. and Ehl, J. (1999) Petrology of the gedrite-bearing rocks in midcrustal ductile shear zones from the Eastern Ghats Belt, India. Journal of Metamorphic Geology, 17, 765778.CrossRefGoogle Scholar
Dobmeier, C.J., and Raith, M.M., (2003) Crustal architecture and evolution of the Eastern Ghats Granulite Belt, India. Pp. 145168 in: Proterozoic East Gondwana: Supercontinent Assembly and Breakup (M.Yoshida, B.F.Windley and S. Dasgupta editors). Geological Society, London, Special Publications, 206. The Geological Society, London.Google Scholar
Ellis, D.J., and Green, D.H., (1979) An experimental study of the effect of Ca upon garnet-clinopyroxene Fe-Mg exchange equilibrium, Contributions to Mineralogy and Petrology, 71, 1322.Google Scholar
Graham, C.M., and Powell, R. (1984) A garnethornblende geothermometer: California. Journal of Metamorphic Geology, 2, 1331.CrossRefGoogle Scholar
Guidotti, C.V., and Johnson, S.E., (2002) Pseudomorphs and associated microstructures of western Maine, USA. Journal of Structural Geology, 24, 1139–56.CrossRefGoogle Scholar
Hammerstrom, J.M., and Zen, E-an. (1986) Aluminium in hornblende: An empirical igneous geobarometer. American Mineralogist, 71, 12971313.Google Scholar
Helz, R.T., (1973) Phase relations of basalts in their melting range at PH2O=5 Kb as a function of oxygen fugacity. Part-I. Mafic phases, Journal of Petrology, 14, 249302.CrossRefGoogle Scholar
Hirth, G. and Tullis, J. (1992) Dislocation creep regimes in quartz aggregates. Journal of Structural Geology, 14, 145–60.CrossRefGoogle Scholar
Hollister, L.S., Grisson, G.C., Peters, E.K., Stowell, H.H., and Sisson, V.B., (1987) Confirmation of empirical correlation of Al in hornblende with pressure of solidification of calc-alkaline plutons. American Mineralogist, 72, 231239.Google Scholar
Johnson, M.C., and Rutherford, M.J., (1989) Experimental calibration of the aluminium-in-hornblende geobarometer with application to Long Valley caldera (California). Geology, 17, 837841.2.3.CO;2>CrossRefGoogle Scholar
Kohn, M.J., and Spear, F.S., (1990) Two new geobarometers for garnet ammphibolites, with application to Southeastern Vermont. American Mineralogist, 75, 8996.Google Scholar
Kretz, R. (1982) Transfer and exchange equilibria in a portion of the pyroxene quadrilateral as deduced from natural and experimental data. Geochimica et Cosmochimica Acta, 46, 411422.CrossRefGoogle Scholar
Kroll, H., Evangalakakis, C. and Voll, G. (1993) Two feldspar geothermometry, review and revision for slowly cooled rocks. Contributions to Mineralogy and Petrology, 114, 510518.CrossRefGoogle Scholar
Kruhl, J.H., (1998) Prism- and basal-plane parallel subgrain boundaries in quartz: a microstructural geothermobarometer: Reply. Journal of Metamorphic Geology, 16, 142146.Google Scholar
Leake, B.E., Woolley, A.R., Arps, C.E.S., Birch, W.D., Gilbert, M.C., Grice, J.D., Hawthorne, F.C., Kato, A., Kisch, H.J., Krivovichev, V.G., Linthout, K., Laird, J., Mandarino, J., Maresch, W.V., Nickel, E.H., Rock, N.M.S., Smith, D.C., Stephenson, N.C.N., Whittaker, E.J.W. and Youzhi, G. (1997) Nomenclature of Amphiboles: Report of the Subcommittee on Amphiboles of the International Mineralogical Association Commission on New Minerals and Mineral Names. Mineralogical Magazine, 61, 295321.CrossRefGoogle Scholar
Lee, M.R., and Parsons, I. (1997) Dislocation, formation and albitization in alkali feldspars from the Shap granite. American Mineralogist, 82, 557570.CrossRefGoogle Scholar
Leelanandam, C. (1989) The Prakasam alkaline province in Andhra Pradesh, India. Journal of Geological Society of India, 34, 2545.Google Scholar
Mezger, K. and Cosca, M.A., (1999) The thermal history of the Eastern Ghats Belt (India) as revealed by U-Pb and 40Ar/39Ar dating of metamorphic and magmatic minerals: implications for the SWEAT correlation. Precambrian Research, 94, 251271.CrossRefGoogle Scholar
Miller, R.B., and Paterson, S.R., (1994) The transition from magmatic to high-temperature solid-state deformation: implications from the Mount Stuart batholith, Washington. Journal of Structural Geology, 16, 853865.CrossRefGoogle Scholar
Moecher, D.P., Essene, E.J., and Anovitz, L.M., (1988) Calculation and application of clinopyroxene-garnet-plagioclase- quartz geobarometers. Contributions to Mineralogy and Petrology, 100, 92106.CrossRefGoogle Scholar
Mongkoltip, P. and Ashworth, J.R., (1983) Quantitative estimation of an open-system symplectite-forming reaction: restricted diffusion of Al and Si in coronas around olivine. Journal of Petrology, 24, 635–61.CrossRefGoogle Scholar
Mukhopadhyay, A., Bhattacharya, A. and Mohanty, L. (1992) Geobarometers involving clinopyroxene, garnet, plagioclase, ilmenite, rutile, sphene and quartz: estimation of pressure in quartz-absent assemblages. Contributions to Mineralogy and Petrology, 110, 346354.CrossRefGoogle Scholar
Nyman, M.W., Law, R.D., and Smelik, E. (1992) Cataclastic deformation mechanism for the development of core-mantle structures in amphibole. Geology, 20, 455458.2.3.CO;2>CrossRefGoogle Scholar
Passchier, C.W., (1985) Water-deficient mylonite zones – an example from the Pyrenees. Lithos, 18, 115127.CrossRefGoogle Scholar
Passchier, C.W., and Trouw, R.A.J. (1996) Microtectonics. Springer, Berlin. Pouchou, J.L., and Pichoir, F. (1985) ‘PAP’ (j-r-Z) procedure for improved quantitative microanalysis. Pp. 104106 in: Microbeam Analysis (J.T. Armstrong, editor). San Francisco Press, San Francisco.Google Scholar
Pryer, L.L., and Robin, P.-Y.F. (1995) Retrograde metamorphic reactions in deforming granites and the origin of flame perthite. Journal of Metamorphic Geology, 13, 645658.CrossRefGoogle Scholar
Pryer, L.L., and Robin, P.-Y.F. (1996) Differential stress control on the growth and orientation of flame perthite: a palaeostress indicator. Journal of Structural Geology, 18, 11511166.CrossRefGoogle Scholar
Putnis, A. (2002) Mineral replacement reactions: from macroscopic observations to microscopic mechanisms. Mineralogical Magazine, 66, 689708.CrossRefGoogle Scholar
Richard, L.R., (1995) Minpet – mineralogical and petrological data processing system, version 2.02. Minpet Geological Software, Quebec, Canada.Google Scholar
Rosenberg, C.L., and Stünitz, H. (2003) Deformation and recrystallization of plagioclase along a temperature gradient: an example from the Bergell tonalite. Journal of Structural Geology, 25, 389408.CrossRefGoogle Scholar
Sengupta, P., Dasgupta, S., Bhattacharya, P.K., and Hariya, Y. (1989) Mixing behaviour in quaternary garnet solid solution and an extended Ellis and Green garnet-clino pyrox ene geo thermometer. Contributions to Mineralogy and Petrology, 103, 223227.CrossRefGoogle Scholar
Sengupta, P., Sen, J., Dasgupta, S., Raith, M.M., Bhui, U.K., and Ehl, J. (1999) Ultra high temperature metamorphism of meta-pelitic granulites from Kondapalle, Eastern Ghats Belt: Implications for the Indo-Antartic correlation. Journal of Petrology, 40, 10651087.CrossRefGoogle Scholar
Simpson, C. and Wintsch, R.P., (1989) Evidence for deformation-induced K-feldspar replacement by myrmekite. Journal of Metamorphic Geology, 7, 261275.CrossRefGoogle Scholar
Spear, F.S., (1993) Metamorphic Phase Equilibria and Pressure-Temperature-Time Paths. Mineralogical Society of America, Washington, DC.Google Scholar
Tribe, I.R., and D’Lemos, R.S., (1996) Significance of a hiatus in down-temperature fabric development within syn-tectonic quartz diorite complexes, Channel Islands, UK. Journal of the Geological Society of London, 153, 127138.CrossRefGoogle Scholar
Tullis, J.A., (1983) Deformation of feldspars. Pp. 297324 in: Feldspar Mineralogy (P.H. Ribbe editor). Reviews in Mineralogy, 2, 2nd edition. Mineralogical Society of America, Washington, DC.Google Scholar
Vernon, R.H., (1996) Problems with inferring P-T-t paths in low-P granulite facies rocks. Journal of Metamorphic Geology, 14, 143153.CrossRefGoogle Scholar
Vernon, R.H., (1999) Flame perthite in metapelitic gneiss at Cooma S. Australia. American Mineralogist, 84, 17601765.CrossRefGoogle Scholar
White, J.C., and Mawer, C.K., (1988) Dynamic recrystallisation and associated exsolution in perthites: evidence for deep crustal thrusting. Journal of Geophysical Research, 93, 325337.CrossRefGoogle Scholar
Wirth, R. and Voll, G. (1987) Cellular intergrowth between quartz and sodium-rich plagioclase (myrmekite) – an analogue of discontinuous precipitation in metal alloys. Journal of Materials Science, 22, 1913–18.CrossRefGoogle Scholar
Yund, R.A., and Davidson, P. (1978) Kinetics of lamellar coarsening in cryptoperthites. American Mineralogist, 63, 470477.Google Scholar
Yund, R.A., and Tullis, I.A., (1986) The effect of ductile deformation on plagioclase breakdown kinetics. Geological Society of America Abstracts with Programs, 18, 799.Google Scholar