Hostname: page-component-cd9895bd7-dk4vv Total loading time: 0 Render date: 2024-12-28T13:47:52.291Z Has data issue: false hasContentIssue false
  • English
  • Français

XRD Identification of Two Coexisting Mixed Layer Expandable Minerals in Sedimentary Rocks

Published online by Cambridge University Press:  28 February 2024

M. Gharrabi ,
B. Velde  and
J. -P. Sagon
M. Gharrabi
Affiliation:
Laboratoire de Géologie, Ecole Normale Superieure, 24 rue Lhomond, 75231 Paris, France
B. Velde
Affiliation:
Laboratoire de Géologie, Ecole Normale Superieure, 24 rue Lhomond, 75231 Paris, France
J. -P. Sagon
Affiliation:
Laboratoire de Géologie Applique, Université de Paris VI, 4 pl Jussieu, 75252 Paris, France
Rights & Permissions [Opens in a new window]

Abstract

An abstract is not available for this content so a preview has been provided. As you have access to this content, a full PDF is available via the ‘Save PDF’ action button.
Image of the first page of this content. For PDF version, please use the ‘Save PDF’ preceeding this image.'

Keywords

DiagenesisExpandable interstratified mineralsX-ray diffraction
Type
Notes
Information
Clays and Clay Minerals , Volume 44 , Issue 3 , June 1996 , pp. 429 - 436
Copyright
Copyright © 1996, The Clay Minerals Society

References

Bailey, S.W., Brindley, G.W., Kodama, H. and Martin, R.T.. 1982. Report of clay minerals nomenclature committee. Clays & Clay Miner 30: 76–78.CrossRefGoogle Scholar
Garvie, L.A.. 1992. Diagenetic tosudoite from lowermost St. Maughan's Group, Lyney Harbour, Forest Dean, UK. Clay Miner 27: 507–513.CrossRefGoogle Scholar
Huggett, J.M.. 1992. Petrography, mineralogy and diagenesis of overpressured Tertiary and late Cretaceous mudrocks from East Shetland basin. Clay Miner 27: 487–506.CrossRefGoogle Scholar
Ichikawa, A. and Shimoda, S.. 1976. Tosudite from Hokuno mine, Hokuno, Gifu Pefecture, Japan. Clays & Clay Miner 24: 142–148.CrossRefGoogle Scholar
Lanson, B.. 1991. Decomprx decomposition program. ERM. University Poitiers, France.Google Scholar
Lanson, B.. 1990. Mise en évidence des mécanismes de transformation des interstratifiés illite/smectite au cours de la diagenèse. [Thése de Doctorat.] Paris: Université de Paris VI. 366 p.Google Scholar
Lanson, B. and Besson, G.. 1992. Characterization of the end of the smectite to illite transformation: Decomposition of X-ray patterns. Clays & Clay Miner 40: 40–52.CrossRefGoogle Scholar
Lanson, B. and Velde, B.. 1992. Decomposition of X-ray patterns: A convenient way to describe complex I/S diagenetic evolution. Clays & Clay Miner 40: 629–643.CrossRefGoogle Scholar
Reynolds, R.C.. 1985. NEWMOD a computer program for the calculation of one-dimensional diffraction powders of mixed-layer clays. Reynolds RC, 8 Brook Rd., Hanover, NH 03755 USA.Google Scholar
Velde, B. and Brusewitz, A.M.. 1986. Compositional variation in component layers in natural illite/smectite. Clays & Clay Miner 34: 651–657.CrossRefGoogle Scholar
Velde, B. and Vasseur, G.. 1992. Estimation of the diagenetic illite to smectite transformation in time-temperature space. Am Mineral 77: 967–976.Google Scholar
Walgenwitz, F., Pagel, M., Meyer, A., Maluski, H. and Monie, P.. 1990. Thermo-chronological approach to reservoir diagenesis in the offshore Angola Basin: A fluid inclusion, 409Ar-39-Ar and K-Ar investigation. Am Assoc Pet Geol Bull 74: 547–563.Google Scholar
Whitney, G. and Velde, B.. 1993. Changes in particle morphology during illitization: An experimental study. Clays & Clay Miner 41: 209–218.CrossRefGoogle Scholar