Hostname: page-component-8448b6f56d-c47g7 Total loading time: 0 Render date: 2024-04-24T04:20:38.879Z Has data issue: false hasContentIssue false
  • English
  • Français

Clay diagenesis, overpressure and reservoir quality: an introduction

Published online by Cambridge University Press:  09 July 2018

C. V. Jeans
C. V. Jeans*
Affiliation:
Department of Earth Sciences, Downing Street, Cambridge CB2 3EQ, UK
Get access Rights & Permissions [Opens in a new window]

Abstract

The interplay of overpressure and diagenesis is an important factor in developing reservoir quality and controlling the movement of pore-fluids and hydrocarbons within sedimentary basins. The first part of this introduction deals with petrographic features by which certain highly overpressured reservoirs can be recognised. The second part considers the 20 papers, presented at the 1993 Cambridge Conference, published in this special issue of Clay Minerals and how they fit into the broader context of the subject.

Type
Research Article
Information
Clay Minerals , Volume 29 , Issue 4 , October 1994 , pp. 415 - 423
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1994

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

Bjørlykke, K. (1993) Fluid flow in sedimentary basins. Sed. Geol., 86, 137–158.CrossRefGoogle Scholar
Bjørlykke, K. (1994) Fluid flow processes and diagenesis in sedimentary basins. Pp. 127-140 in: Geofluids: Origin, Migration and Evolution of Fluids in Sedimentary Basins (Parnell, J., editor). Geol. Soc. Spec. Publ. No. 78.Google Scholar
Jeans, C.V. (1978) The origin of the Triassic clay assemblages of Europe with special reference to the Keuper Marl and Rhaetic of parts of England. Phil. Trans. Roy. Soc., Series A, 549-639.Google Scholar
Jeans, C.V. (1986) Features of mineral diagenesis in hydrocarbon reservoirs: an introduction. Clay Miner. 21, 429–441.Google Scholar
Jeans, C.V. (1989) Clay diagenesis in sandstones and shales: an introduction. Clay Miner., 24, 127–136.Google Scholar
Jeans, C.V. & Fisher, M.J. (1986) Diagenesis in Upper Jurassic marine sandstones from the North Sea Well 14/26-1 and its significance. Clay Miner., 21, 513–535.CrossRefGoogle Scholar
Mcaulay, G.E., Burley, S.D. & Johnes, L.H. (1993) Silicate mineral authigenesis in the Hutton And, N.W. Hutton fields: implications for subsurface porosity development. Pp. 1377-1394 in: Petroleum Geology of NW Europe (Parker, J., editor). Geol. Soc. London.Google Scholar
Prieto, M., Putnis, A. & Fernandez-Diaz, L. (1990) Factors controlling the kinetics of crystallization: supersaturation evolution in a porous medium. Application to barite crystallization. Geol. Mag., 127, 485–495.CrossRefGoogle Scholar
Putnis, A., Prieto, M. & Fernanoez-Diaz, L. (1994) Fluid supersaturation and crystallization in porous media. Geol. Mag. (in press).Google Scholar
Stewart, D.J. (1986) Diagenesis of the shallow marine Fulmar Formation in the Central North Sea. Clay Miner., 21, 537–564.CrossRefGoogle Scholar