Hostname: page-component-cd9895bd7-jn8rn Total loading time: 0 Render date: 2024-12-26T09:07:38.358Z Has data issue: false hasContentIssue false
  • English
  • Français

Clay minerals as records of temperature conditions and duration of thermal anomalies in the Paris Basin, France: a reply to the discussion by Spötl et al.

Published online by Cambridge University Press:  09 July 2018

N. Clauer ,
J. R. O'Neil ,
S. Furlan  and
J. R. Mossmann
N. Clauer
Affiliation:
Centre de Géochimie de la Surface (CNRS) 1 rue Blessig, 67084 Strasbourg, France
J. R. O'Neil
Affiliation:
Department of Geological Sciences, University of Michigan, Ann Arbor, Michigan 48109, USA
S. Furlan
Affiliation:
Department of Geology, Kansas State University, Manhattan, Kansas 66056, USA
J. R. Mossmann
Affiliation:
Bureau de Recherches Géologiques et Minièes, Avenue de Concyr, 45060 Orléans, France
Get access Rights & Permissions [Opens in a new window]

Abstract

Spötl et al. (1996) have re-examined studies published by us on clay materials of sandstones in the Paris Basin. They refute the XRD characterization, K-Ar dating and formation temperature of one of the interstratified illite-smectite phases identified and have provided an alternative explanation of the published results. However, the authors ignored some basic data provided in the publications under discussion, and they have not been able to explain readily why some of the data were discarded. Furthermore, part of their disagreement is unsubstantiated. We maintain that, on the basis of coherency and consistency of all the data obtained, as well as on independent published results, the most satisfactory interpretation for the thermal evolution of the Paris Basin is the one that we suggested in our publications.

Type
Research Article
Information
Clay Minerals , Volume 31 , Issue 2 , June 1996 , pp. 209 - 215
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1996

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

Brunet, M.F. & Le Pichon, X. (1982) Subsidence of the Paris Basin. J. Geophys. Res. 87, B10, 8547–8760.Google Scholar
Clauer, N. & Chaudhuri, S. (1995) Clays in Crustal Environments. Isotope Dating and Tracing. Springer Verlag, Heidelberg.Google Scholar
Clauer, N., Cocker, J.D. & Chaudhuri, S. (1992) Isotopic dating of diagenetic illites in reservoir sandstones: Influence of the investigator effect. Pp. 5–12 in: Origin, Diagenesis and Petrophysics of Clay Minerals in Sandstones (Houseknecht, D.W., editor). Soc. Econ. Paleont. and Mineral., Spec. Publ., 47.Google Scholar
Clauer, N., O'NEIL, J.R. & Furlan, S. (1995a) Clay minerals as record of temperature conditions and duration of thermal anomalies in the Paris Basin, France. Clay Miner. 30, 597–609.CrossRefGoogle Scholar
Clauer, N., Rais, N., Schaltegger, U. & Pique, A. (1995b) K-Ar systematics of clay-to-mica minerals in a multi-stage low-grade metamorphic evolution. Chem. GeoL, hot. Geosc. Section, 124, 305–316.Google Scholar
Clauer, N., Zwingmann, H. & Chaudhuri, S. (1996) Isotopic (K-Ar and oxygen) constraints on the extent and importance of the Liassic hydrothermal activity in Western Europe. Clay Miner, (in press).Google Scholar
Demars, C. & Paoel, M. (1994) Paleotemperatures et paleosalinites dans les gres du Keuper du Bassin de Paris: inclusions fluides dans les mineraux authigenes. C. R. Acad. Sci., Paris, 319, II, 427-434.Google Scholar
Dunoyer De Segonzac, G. (1969) Les mineraux argileux dans la diagenese. Passage au metamorphisme. Sci. Geol. Mem., Strasbourg, 29, 320 pp.Google Scholar
Girard, J.P., Savin, S.M. & Aronson, J.L. (1989) Diagenesis of the lower Cretaceous arkoses of the Angola margin: petrologic, K-Ar dating and 18O/16O evidence. J. Sed. Pet. 59, 519–538 Google Scholar
Guilhaumou, N. (1993) Paleotemperatures inferred from fluid inclusions in diagenetic cements: implications for the thermal history of the Paris Basin. Eur. J. Mineral. 5, 1217–1226.Google Scholar
Guilhaumou, N. & Gaulier, J.M. (1991) Determination de paleotemperatures dans les roches-meres du bassin de Paris: Etude d'inclusions fluides et implications pour l'histoire thermique du bassin. C. R. Acad. Sci, Paris, 313, II, 773-780.Google Scholar
Hunziker, J.C., FREY M, Clauer, N., Dallmeyer, R.D., Friedrichsen, H., Flehmig, W., Hochstrasser, K., Roggwiller, P. & Schwander, H. (1986) The evolution of illite to muscovite: mineralogical and isotopic data from the Glarus Alps, Switzerland. Contrib. Mineral. Pet. 92, 157–180.CrossRefGoogle Scholar
Ledesert, B. (1993) Fracturation et paleocirculations hydrothermales. Application au granite de Soultzsous- Foret. These, Univ. Poitiers, France.Google Scholar
Lee, M., Aronson, J.L. & Savin, S.M. (1989) Timing and conditions of Permian Rotliegendes sandstone diagenesis, southern North Sea: K/Ar and oxygen isotope data. Am. Assoc. Petrol. Geol. Bull., 73, 195–215.Google Scholar
Moore, D.M. & Reynolds, R.C. (1989) X-ray Diffraction and the Identification and Analysis of Clay Minerals. Oxford Univ. Press.Google Scholar
Mossmann, J.R. (1987) Conditions physico-chimiques d'evolution de reservoirs greseux. Approche petrologique, mineralogique et isotopique. Application aux gres rhetiens du bassin de Paris. These, Univ. Strasbourg, France.Google Scholar
Mossmann, J.R. (1991) K-Ar dating of authigenic illitesmectite clay material: application to complex mixtures of mixed-layer assemblages. Clay Miner. 26, 189–198.Google Scholar
Mossmann, J.R., Clauer, N. & Liewig, N. (1992) Dating thermal anomalies in sedimentary basins: the diagenetic history of clay minerals in the Triassic sandstones of the Paris Basin (France). Clay Miner. 27, 211–226.Google Scholar
Pagel, M. & Meyer, A. (1991) A fluid inclusion and fission track study in the Sancerre-Crouy deep drill hole. ECROFIXI (abstract), 10-12 April, Florence. Google Scholar
Reynolds, R.C. 1985. NEWMOD © a Computer Program for the Calculation of One-Dimensional Patterns of Mixed-Layer Clays. R.C. Reynolds, 8 Brook Road, Hannover, N.H. 03755, USA.Google Scholar
Spotl, C., Worden, R.H. & Walgenwitz, F. (1996) Clay minerals as records of temperature conditions and duration of thermal anomalies in the Paris Basin, France: discussion. Clay Miner. 31, 203–208.Google Scholar
Velde, B. (1985) Clay Minerals. A Physico-Chemical Explanation of their Occurrence. Elsevier, Amsterdam.Google Scholar
Winkler, H.G.F. (1965) Die Genese der Metamorphen Gesteine. Springer Verlag, Heidelberg, Berlin.Google Scholar
Walgenwitz, F. & Worden, R.H. (1993) Decoupling of thermal histories in the Paris Basin? Terra abstracts, suppl. n° 1 to Terra nova, 5, p 659.Google Scholar
Zwingmann, H. (1995) Etude des conditions de mise en place des gaz naturels dans les reservoirs greseux (Rotliegende d'Allemagne). Aspects mineralogiques, morphologiques, geochimiques et isotopiques. These, Univ. Strasbourg, France.Google Scholar