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Experimental Clay-Mineral Formation from a Subvolcanic Rock by Interaction with 1 M NaOH Solution at Room Temperature

Published online by Cambridge University Press:  28 February 2024

A. Drief
Affiliation:
Departamento de Mineralogía y Petrología, Instituto Andaluz de Ciencias de la Tierra, Universidad de Granada-C.S.I.C, Av. Fuentenueva s/n, 18002 Granada, Spain
F. Nieto*
Affiliation:
Departamento de Mineralogía y Petrología, Instituto Andaluz de Ciencias de la Tierra, Universidad de Granada-C.S.I.C, Av. Fuentenueva s/n, 18002 Granada, Spain
A. Sanchez-Navas
Affiliation:
Departamento de Mineralogía y Petrología, Instituto Andaluz de Ciencias de la Tierra, Universidad de Granada-C.S.I.C, Av. Fuentenueva s/n, 18002 Granada, Spain
*
*E-mail address of corresponding author: fnieto@goliat.ugr.es

Abstract

The alteration process of a subvolcanic rock with calcic plagioclase, pyroxene, and olivine as major components was investigated by X-ray diffraction (XRD) and analytical and transmission electron microscopy (TEM/AEM). Experimental interaction with 1 M NaOH solution led to the formation of dioctahedral beidellite to Fe-rich montmorillonite after 1 and 3 d of reaction. This range of smectite composition is similar to that from natural subvolcanic-derived soil formed from the same parent material. After 14 d of reaction, a berthierine-smectite (B-S) interstratified clay had partially replaced the smectite. Although, the presence of smectite interlayers prevented analysis of pure berthierine, berthierine-rich BS interstratifications have a composition similar to pure berthierine. After 40 d, the alteration process led to a 7-Å S interstratification whose composition falls between greenalite and lizardite. A series of amorphous materials were also found in the 14 and 40-d experiments. The most abundant of these is a Si-CaFe-rich material, whose chemical composition approaches that of the starting rock. In contrast, two other amorphous materials had a smectitic composition.

Type
Research Article
Copyright
Copyright © 2001, The Clay Minerals Society

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References

Abad-Ortega, M.M. and Nieto, F., (1995) Genetic and chemical relationships between berthierine, chlorite and cordierite in nodules associated to granitic pegmatites of Sierra Albarrana (Iberian Massif, Spain) Contributions to Mineralogy and Petrology 120 327336 10.1007/BF00306511.CrossRefGoogle Scholar
Ahn, J.H. and Peacor, D.R., (1985) Transmission electron microscopic study of diagenetic chlorite in Gulf Coast argillaceous sediments Clays and Clay Minerals 33 228236 10.1346/CCMN.1985.0330309.Google Scholar
Amouric, M. Gianetto, I. and Proust, D., (1988) 7, 10, and 14 A mixed layer phyllosilicates studied structurally by TEM in pelitic rocks of the Piemontese zone (Venezuela) Bulletin de Minéralogie 111 2937.Google Scholar
Amouric, M. and Olives, J., (1998) Transformation mechanisms and interstratification in conversion of smectite to kaolinite: An HRTEM study Clays and Clay Minerals 46 521527 10.1346/CCMN.1998.0460505.Google Scholar
Amouric, M. Parron, C. Casalini, L. and Giresse, P., (1995) A (1:1) 7-A Fe phase and its transformation in recent sediments: An HRTEM and AEM study Clays and Clay Minerals 43 446454 10.1346/CCMN.1995.0430408.Google Scholar
Bailey, S.W., Brindley, G.W. and Brown, G., (1980) Structures of layer silicates Crystal Structure of Clay Minerals and Their X-ray Identification London Mineralogical Society 1123.Google Scholar
Banfield, J.F. and Eggleton, R.A., (1990) Analytical transmission electron microscope studies of plagioclase, muscovite and feldspar weathering Clays and Clay Minerals 38 7789 10.1346/CCMN.1990.0380111.Google Scholar
Banfield, J.E. Jones, B.F. and Veblen, D.R., (1991) An AEMTEM study of weathering and diagenesis, Albert Lake, Oregon: I. Weathering reactions in the volcanics Geochimica et Cosmochimica Acta 55 27812793 10.1016/0016-7037(91)90444-A.Google Scholar
Berner, R.A., Lasaga, A.C. and Kirkpatrick, R.J., (1984) Kinetics of weathering and diagenesis Kinetics of Geochemical Processes, Reviews in Mineralogy, Volume 8 Washington, D.C. Mineralogical Society of America 111134.Google Scholar
Bhattacharyya, D.P., (1983) Origin of berthierine in ironstones Clays and Clay Minerals 31 173182 10.1346/CCMN.1983.0310302.Google Scholar
Brindley, G.W., (1982) Chemical compositions of berthierines. A review Clays and Clay Minerals 30 153155 10.1346/CCMN.1982.0300211.Google Scholar
Christidis, G., (1989) Mineralogy, physical and chemical properties of deposits of Milos island, Greece UK M.S. thesis, University of Hull.Google Scholar
Drief, A. and Nieto, F., (2000) Chemical composition of smectites formed in clastic sediments. Implications for the smectite-illite transformation Clay Minerals 35 665678 10.1180/000985500547124.Google Scholar
Eggleton, R.A., (1987) Non-crystalline Fe-Si-Al-oxyhydroxides Clays and Clay Minerals 35 2937 10.1346/CCMN.1987.0350104.Google Scholar
Farmer, V.C. Krishnamurti, G.S.R. and Huang, P.M., (1991) Synthetic allophane and layer-silicate formation in Si02- Al203-FeO-Fe2O3-MgO-H2O systems at 23°C and 89°C in a calcareous environment Clays and Clay Minerals 39 561570 10.1346/CCMN.1991.0390601.Google Scholar
Farmer, V.C. McHardy, W.J. Palmieri, F. Violante, A. and Violante, P., (1991) Synthetic allophane formed in calcareous environments: Nature, conditions of formation, and transformations Soil Science Society of America Journal 55 11621166 10.2136/sssaj1991.03615995005500040044x.Google Scholar
Fritz, S.J. and Toth, T.A., (1997) An Fe-berthierine from a Cretaceous latente: Part II. Estimation of Eh, pH and pCO2 conditions of formation Clays and Clay Minerals 45 580586 10.1346/CCMN.1997.0450409.Google Scholar
Grauby, O. Petit, S. Decarreau, A. and Baronnet, A., (1993) The beidellite-saponite series: An experimental approach European Journal of Mineralogy 5 623635 10.1127/ejm/5/4/0623.Google Scholar
Guggenheim, S. and Eggleton, R.A., (1998) Modulated crystal structures of greenalite and caryopilite: A system with long-range, in-plane structural disorder in the tetrahedral sheet The Canadian Mineralogist 36 163179.Google Scholar
Guggenheim, S. Bailey, S.W. Eggleton, R.A. and Wilkes, P., (1982) Structural aspects of greenalite and related minerals The Canadian Mineralogist 20 118.Google Scholar
Güven, N. and Bailey, S.W., (1988) Smectite Hydrous Phyllosilicates, Reviews in Mineralogy, Volume 19 Washington, D.C. Mineralogical Society of America 497559 10.1515/9781501508998-018.Google Scholar
Hallam, A. and Bradshaw, M.J., (1979) Bituminous shales and oolitic ironstones as indicators of transgressions and regressions Journal of the Geological Society of London 136 157164 10.1144/gsjgs.136.2.0157.Google Scholar
Harder, H., (1978) Synthesis of iron layer silicate minerals under natural conditions Clays and Clay Minerals 26 6572 10.1346/CCMN.1978.0260108.Google Scholar
Hillier, S. and Velde, B., (1992) Chlorite interstratified with a 7 A mineral: An example from offshore Norway and possible implications for the interpretation of the composition of diagenetic chlorites Clay Minerals 27 475486 10.1180/claymin.1992.027.4.07.Google Scholar
Jahren, J.S. and Aagaard, P., (1989) Compositional variation in diagenetic chlorites and illites, and relationship with formation-water chemistry Clay Minerals 24 157170 10.1180/claymin.1989.024.2.04.Google Scholar
James, H.J. (1966) Chemistry of the Iron-Rich Sedimentary Rocks. U.S. Geological Survey Professional Paper 440-W, Washington, D.C., 59 pp.Google Scholar
Jiang, W.T. Peacor, D.R. and Slack, J.F., (1992) Microstructures, mixed layering, and polymorphism of chlorites and retrograde berthierine in the Kidd Creek Massive sulfide deposits, Ontario Clays and Clay Minerals 40 501514 10.1346/CCMN.1992.0400503.Google Scholar
Kawano, M. and Tomita, K., (1992) Formation of allophane and beidellite during hydrothermal alteration of volcanic glass below 200°C Clays and Clay Minerals 40 666674 10.1346/CCMN.1992.0400606.Google Scholar
Kawano, M. and Tomita, K., (1994) Growth of smectite from leached layer during experimental alteraction of albite Clays and Clay Minerals 42 717 10.1346/CCMN.1994.0420102.Google Scholar
Kloprogge, J.T. Jansen, J.B.H. and Geus, J.W., (1990) Characterization of synthetic Na-beidellite Clays and Clay Minerals 38 409414 10.1346/CCMN.1990.0380410.Google Scholar
Lee, H.H. and Peacor, D.R., (1983) Interlayer transitions in phyllosilicates of Martinsburg shale Nature 303 608609 10.1038/303608a0.Google Scholar
Leo Lunch, F. Make, L.E. and Land, L.S., (1997) Burial diagenesis of illite/smectite in shales and the origins of authigenic quartz and secondary porosity in sandstones Geochimica et Cosmochimica Acta 61 19952006 10.1016/S0016-7037(97)00066-5.Google Scholar
Li, G. Peacor, D.R. and Coombs, D.S., (1997) Transformation of smectite to illite in bentonite and associated sediments from Kaka Point, New Zealand: Contrast in rate and mechanism Clays and Clay Minerals 45 5467 10.1346/CCMN.1997.0450106.Google Scholar
Longstaffe, F.J. Racki, M.A. Ayalon, A., Kharaka, Y.K. and Maest, A.S., (1992) Stable isotope studies of diagenesis in berthierine-bearing oil sands, Clearwater Formation, Alberta Water Rock Interaction, Moderate and High Temperature Environments, Proceeding Seventh International Symposium on WaterRock Interaction Rotterdam AA Balkema 955958.Google Scholar
Lorimer, G.W. Cliff, G. and Wenk, H.R., (1976) Analytical electron microscopy of minerals Electron Microscopy in Mineralogy New York Springer-Verlag 506519 10.1007/978-3-642-66196-9_38.Google Scholar
Morata, D. Puga, E. Demant, A. and Aguirre, L., (1997) Geochemistry and tectonic setting of the “ophites” from the External Zones of the Betic Cordilleras (S. Spain) Estudios Geoldgicos 53 107120.Google Scholar
Nickel, E.H., (1992) Solid-solutions in mineral nomenclature Canadian Mineralogist 30 231234.Google Scholar
Olives, J., (1985) Biotites and chlorites as interlayered biotitechlorite crystals Bulleltin de Minéralogie 108 635641.Google Scholar
Olives, J. and Amouric, M., (1984) Biotite chloritization by interlayer brucitization as seen by HRTEM American Mineralogist 69 869871.Google Scholar
Plee, D. Gatineau, L. and Fripiat, J.J., (1987) Pillaring processes of smectites with and without tetrahedral substitution Clays and Clay Minerals 35 8188 10.1346/CCMN.1987.0350201.Google Scholar
Portugal-Ferreira, M. Morata, D. Puga, E. Demant, A. and Aguirre, L., (1995) Evolucion geoqufmica y temporal del magmatismo bâsico Mesozoico en las Zonas Externas de las Cordilleras Béticas Estudios Geoldgicos 51 109118.Google Scholar
Schiffman, P. and Southard, R.J., (1996) Cation exchange capacity of layer silicates and palagonitized glass in mafic volcanic rocks: A comparative study of bulk extraction and in situ techniques Clays and Clay Minerals 44 624634 10.1346/CCMN.1996.0440505.Google Scholar
Schultz, A. Stone, W.E.E. Poncelet, G. and Fripiat, J.J., (1987) Preparation and characterization of bidimensional zoolitic structures obtained from synthetic beidellite and hydroxy-aluminum solutions Clays and Clay Minerals 35 251261 10.1346/CCMN.1987.0350402.Google Scholar
Taylor, K.G., (1990) Berthierine from the non-marine Wealden (Early Cretaceous) sediments of south-east England Clay Minerals 25 391399 10.1180/claymin.1990.025.3.13.Google Scholar
Tazaki, K. and Fyfe, W.S., (1987) Primitive clay precursors formed on feldspar Canadian Journal of Earth Sciences 24 506527 10.1139/e87-051.Google Scholar
Toth, T.A. and Fritz, S.J., (1997) An Fe-berthierine from a Cretaceous latérite: Part I. Characterization Clays and Clay Minerals 45 564579 10.1346/CCMN.1997.0450408.Google Scholar