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Quartz cementation inhibited by crestal oil charge: Miller deep water sandstone, UK North Sea

Published online by Cambridge University Press:  09 July 2018

A. M. E. Marchand ,
R. S. Haszeldine ,
C. I. Macaulay ,
R. Swennen  and
A. E. Fallick
A. M. E. Marchand*
Affiliation:
Fysico-Chemische Geologie, K.U. Leuven, Celestijnenlaan 200C, B-3001 Heverlee, Belgium Department of Geology and Geophysics, The University of Edinburgh, Grant Institute, West Mains Road, Edinburgh EH9 3JW, UK
R. S. Haszeldine
Affiliation:
Department of Geology and Geophysics, The University of Edinburgh, Grant Institute, West Mains Road, Edinburgh EH9 3JW, UK
C. I. Macaulay
Affiliation:
Department of Geology and Geophysics, The University of Edinburgh, Grant Institute, West Mains Road, Edinburgh EH9 3JW, UK
R. Swennen
Affiliation:
Fysico-Chemische Geologie, K.U. Leuven, Celestijnenlaan 200C, B-3001 Heverlee, Belgium
A. E. Fallick
Affiliation:
Scottish Universities Research and Reactor Centre, Isotope Geosciences Unit, East-Kilbride, G75 0QF, UK
*
*E-mail: ann.marchand@glg.ed.ac.uk
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Abstract

In the Miller Field, diagenetic quartz abundance, isotopic compositions and salinities of quartz-cementing fluids display a distinct pattern which is related to the structural depth of the reservoir sandstones. Quartz cement volumes increase from the crest of the field (average 6.0±1.5%) towards the flanks of the field (average 13.2±2.1%) and directly reduce reservoir porosity. By integrating petrographic observations with results of fluid inclusion measurements and O isotope analyses of diagenetic quartz, the pattern of quartz cementation is seen to be related to the reservoir filling history. Oil filled the crest of the reservoir first and prevented extensive quartz cementation. At greater depth in the reservoir oil zone, quartz overgrowths continued to precipitate until inhibited by the developing oil column. Oxygen isotope compositions of diagenetic quartz imply that quartz cement continued to precipitate in the water zone of the reservoir up to the present day.

Keywords

quartz cementationMiller deep water sandstoneNorth Seadiagenetic quartz
Type
Research Article
Information
Clay Minerals , Volume 35 , Issue 1 , March 2000 , pp. 201 - 210
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 2000

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References

Aplin, A.C., Warren, E.A., Grant, S.M. & Robinson, A.G. (1993) Mechanisms of quartz cementation in North Sea reservoir sandstones: constraints from fluid composition. Pp. 7-22 in: Diagenesis and Basin Development (Horbury, A. & Robinson, A., editors). Am. Assoc. Petrol. Geol. Stud. Geol., 36.Google Scholar
Baldwin, B. & Butler CO. (1985) Compaction curves. Am. Assoc. Petr. Geol. Bull. 69, 69–622.Google Scholar
Brint, J.F., Hamilton, P.J., Haszeldine, R.S., Fallick, A.E. & Brown, S. (1991) Oxygen isotope analysis of diagenetic quartz overgrowths from the Brent sands: A comparison of two preparation methods. J. Sed. Pet. 61, 61–527.Google Scholar
Clayton, R.N., Friedman, I., Graf, D.L., Mayeda, T.K., Meents, W.F. & Shimp, N.F. (1966) The origin of saline formation waters. J. Geophys. Res. 71, 71–3869.Google Scholar
Egeberg, P.K. & Aagaard, P. (1989) Origin and evolution of formation waters from oil fields on the Norwegian shelf. Appl. Geochem. 4, 4–131.CrossRefGoogle Scholar
Emery, D., Smalley, P.C. & Oxtoby, N.H. (1993) Synchronous oil migration and cementation in sandstone reservoirs demonstrated by quantitative description of diagenesis. Phil. Trans. R. Soc. London, 344, 344–115.Google Scholar
Friedman, I. & O'Neil, J.R. (1977) Compilation of stable isotope fractionation factors of geochemical interest In: Data of Geochemistry, 6th edition (Fleischer, M., editor). US Geol. Survey Prof. Paper, 440-kk.Google Scholar
Garland, C.A. (1993) Miller Field: reservoir stratigraphy and its impact on development. Pp. 401-414 in: Petroleum Geology of Northwest Europe: Proc. 4th Conf. (Parker, J.R., editor). Geological Society, London.Google Scholar
Gluyas, J.G., Robinson, A.G., Emery, D., Grant, S.M. & Oxtoby, N.H. (1993) The link between petroleum emplacement and sandstone cementation. Pp. 1395-1402 in: Petroleum Geology of Northwest Europe: Proc. 4th Conf. (Parker, J.R., editor). Geological Society, London.Google Scholar
Hamilton, P.J., Fallick, A.E., Macintyre, R.M. & Elliott, S. (1987) Isotopic tracing of the provenance and diagenesis of Lower Brent Group sands, North Sea. Pp. 939-949 in: Petroleum Geology of Northwest Europe (Brooks, J. & Glennie, K., editors). Graham & Trotman, London.Google Scholar
Hanor, I.S. (1980) Dissolved methane in sedimentary brines: Potential effect on the PVT properties of fluid inclusions. Econ. Geol. 75, 75–603.Google Scholar
Haszeldine, R.S. & Osborne, M. (1993) Fluid inclusion temperatures in diagenetic quartz reset by burial: implications for oilfield cementation. Pp. 35-46 in: Diagenesis and Basin Development (Horbury, A. & Robinson, A., editors). Am. Assoc. Petrol. Geol. Stud. Geol. 36.Google Scholar
Hudson, J.D. & Andrews, JE. (1987) The diagenesis of the Great Estuarine Group, Middle Jurassic, Inner Hebrides, Scotland. Pp 259-276 in: Diagenesis of Sedimentary Sequences (Marshall, J.D., editor). Blackwell, Oxford, UK.Google Scholar
Lee, M. & Savin, S.M. (1985) Isolation of diagenetic overgrowths on sand grains for oxygen isotope analysis. Geochim. Cosmochim. Acta, 49, 49–497.Google Scholar
McBride, E.F. (1963) A classification of common sandstones. J. Sed. Pet. 33, 33–664.Google Scholar
McLaughlin, O.M., Haszeldine, R.S., Fallick, A.E. & Rogers, G. (1994) The case of the missing clay, aluminium loss and secondary porosity, South Brae oilfield, North Sea. Clay Miner. 29, 29–651.CrossRefGoogle Scholar
McLaughlin, O.M., Haszeldine, R.S. & Fallick, A.E. (1996) Quartz diagenesis in layered fluids in the South Brae oilfield, North Sea. SEPM Spec. Publ. 55, 55–103.Google Scholar
Osborne, M. & Haszeldine, R.S. (1993) Evidence for resetting of fluid inclusion temperatures from quartz cements in oilfield. Marine Petrol. Geol. 10, 10–271.Google Scholar
Rooksby, S.K. (1991) The Miller Field, blocks 16/7b, 16/8b UK North Sea. Pp. 159-164 in: United Kingdom Oil and Gas Fields, 25 years Commemorative vol. (Abbotts, I.L., editor). Geological Society Memoir 14.Google Scholar
Saigal, G.C., Bjørlykke, K. & Larter, S. (1992) The effects of oil emplacement on diagenetic processes - examples from the Fulmar reservoir sandstones, central North Sea. Am. Assoc. Petr. Geol. Bull. 76, 76–1024.Google Scholar
Shackleton, N.J. & Kennett, J.P. (1975) Paleotemperature history of the Cenozoic and the initiation of Antarctic glaciation: Oxygen and carbon analyses in DSDP sites 277, 279, 281. Pp. 653-659 in: Initial Report DSDP 24 (Kennett, J.P. & Howtz, R.E., editors), Washington.Google Scholar
Sharp, Z.D. (1990) A laser-based microanalytical method for the in-situ determination of oxygen isotope ratios in silicates and oxides. Geochim. Cosmochim. Acta, 54, 54–1353.Google Scholar
Smalley, P.C. & Warren, E.A. (1994) The Miller Field. P. 52 in: North Sea Formation Waters Atlas (Warren, E.A. & Smalley, P.C., editors). Geological Society London, Memoir 15.Google Scholar
Suchecki, R.N. & Land, L.S. (1983) Isotopic geochemistry of burial-metamorphosed volcanogenic sediments, Great Valley sequence, California. Geochim. Cosmochim. Acta, 47, 47–1487.CrossRefGoogle Scholar
Thermie (1994) Miller field demonstration. P. 42 in: Thermie Reservoir Geochemistry Project report. Newcastle Research Group in Fossil Fuels and Environmental Geochemistry (University of Newcastle, UK), BP Exploration (Sunbury-on- Thames, UK), Geolab Nor (Trondheim, Norway), Institut Français du Pétrole (France), Department of Geology (University of Manchester, UK).Google Scholar
Turner, C.C., Cohen, J.M., Connell, E.R. & Cooper, D.M. (1987) A depositional model for the South Brae oilfield. Pp. 853-864 in: Petroleum Geology of Northwest Europe (Brooks, J. & Glennie, K., editors). Graham & Trotman, London.Google Scholar
Walderhaug, O. (1990) A fluid inclusion study of quartzcemented sandstones from offshore mid-Norway–possible evidence for continued quartz cementation during oil emplacement. J. Sed. Pet. 60, 60–302.Google Scholar
Walderhaug, O. (1994) Temperatures of quartz cementation in Jurassic sandstones from the Norwegian continental shelf–evidence from fluid inclusions. J. Sed. Res. A64, 64–311.Google Scholar
Wilkinson, M., Crowley, S.F. & Marshall, J.D. (1992). Model for the evolution of oxygen isotope ratios in the porefluids of mudrocks during burial. Marine Petrol. Geol. 9, 9–98.Google Scholar
Worden, R.H., Warren, E.A., Smalley, P.C., Primmer, T.J. & Oxtoby, N.H. (1995) Discussion of ‘Evidence for resetting of fluid inclusion temperatures from quartz cements in oilfields’ by Osborne and Haszeldine (1993). Marine Petrol. Geol. 12, 12–566.Google Scholar
Worden, R.H. (1996) Controls on halogen concentrations in sedimentary formation waters. Mineral. Mag. 60, 60–259.Google Scholar
Worden, R.H., Oxtoby, N.H. & Smalley, P.C. (1998) Can oil emplacement prevent quartz cementation in sandstones. Petrol. Geosci. 4, 4–129.Google Scholar