Hostname: page-component-78c5997874-4rdpn Total loading time: 0 Render date: 2024-11-06T09:41:34.251Z Has data issue: false hasContentIssue false
  • English
  • Français

Features of mineral diagenesis in hydrocarbon reservoirs: An Introduction

Published online by Cambridge University Press:  09 July 2018

C. V. Jeans
C. V. Jeans*
Affiliation:
Department of Applied Biology, University of Cambridge, Pembroke Street, Cambridge CB2 3DX
Get access Rights & Permissions [Opens in a new window]

Abstract

An abstract is not available for this content so a preview has been provided. Please use the Get access link above for information on how to access this content.
Image of the first page of this content. For PDF version, please use the ‘Save PDF’ preceeding this image.'
Type
Introduction
Information
Clay Minerals , Volume 21 , Issue 4 , October 1986 , pp. 429 - 441
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1986

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

Brown, G., Catt, J.A. & Weir, A.H. (1969) Zeolites of the clinoptilolite-heulandite type in sediments of south-east England. Mineral. Mag. 37, 480–488.Google Scholar
Caschetto, S. & Wollast, R. (1979) Dissolved aluminium in interstitial waters of recent marine sediments. Geochim. Cosmochim. Acta 43, 425–428.Google Scholar
Correns, C.W. (1961) The experimental chemical weathering of silicates. Clay Miner. Bull. 4, 257–259.Google Scholar
Curtis, C.D. (1978) Possible links between sandstone diagenesis and depth-related geochemical reactions occurring in enclosing mudstone. J. Geol. Soc. Lond. 135, 107–117.Google Scholar
Curtis, C.D. (1983) Geochemistry of porosity enhancement and reduction in clastic sediments. Geol. Soc. Spec. Publ. 12, 113–125.Google Scholar
Holtzapffel, T. & Chamley, H. (1986) Les smectites latées du domaine Atlantique depuis le Jurassique superieur: gisement et signification. Clay Miner. 21, 133–148.Google Scholar
Jeans, C.V. (1978) Silicification and associated clay assemblages in the Cretaceous marine sediments of southern England. Clay Miner. 13, 101–126.CrossRefGoogle Scholar
Jeans, C.V. (1984) Patterns of mineral diagenesis: an introduction. Clay Miner. 19, 263–270.Google Scholar
Mackenzie, F.T., Stoffyn, M. & Wollast, R. (1978) Aluminium in seawater: control by biological activity. Science 199, 680–682.CrossRefGoogle ScholarPubMed
Milodowski, A.E., Martin, B. A. & Wilmot, R.D. (1982) Petrography of the Cretaceous core from the Harwell Research Site. Rep. Inst. Geol. Sci. ENPU 82-14, 83 pp.Google Scholar
Milodowski, A.E. & Wilmot, R.D. (1984) Diagenesis, porosity and permeability in the Corallian Beds (Upper Oxfordian) from the Harwell Research Site, South Oxfordshire, UK. Clay Miner. 19, 323–341.Google Scholar
Schmidt, V. & McDonald, D.A. (1979a) The role of secondary porosity in the course of sandstone diagenesis. Pp. 175–208 in: Aspects of Diagenesis (Scholle, P. A. & Schluger, P. R., editors). S.E.P.M. Spec. Publ. 26.Google Scholar
Schmidt, V. & McDonald, D.A. (1979b) Texture and recognition of secondary porosity in sandstones. Pp. 209– 225 in: Aspects of Diagenesis (Scholle, P. A. & Schluger, P. R., editors). S.E.P.M. Spec. Publ. 26.Google Scholar
Surdam, R.C. & Cressey, L.J. (1985) Organic-inorganic reactions during progressive burial: key to porosity and permeability enhancement and preservation. Phil. Trans. R. Soc. Lond. A315, 135–156.Google Scholar