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Volcaniclastics as potential hydrocarbon reservoirs

Published online by Cambridge University Press:  09 July 2018

U. Seemann  and
M. Scherer
U. Seemann
Affiliation:
Shell UK Exploration & Production, Shell-Mex House, Strand, London WC2R 0DX
M. Scherer
Affiliation:
Shell UK Exploration & Production, Shell-Mex House, Strand, London WC2R 0DX
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Abstract

Volcaniclastics have not as yet been considered prime hydrocarbon exploration targets. This is because they contain a high proportion of mechanically and mineralogically unstable components which generally cause a faster deterioration in reservoir quality upon burial than is found in siliciclastics. Also, their complex mineralogical composition makes the burial-related diagenesis more difficult to understand. However, under favourable circumstances—such as devitrification at shallow depth, leaching of unstable particles, fracturing, or reworking—volcaniclastics may act as good reservoir rocks. Both favourable and unfavourable case histories are discussed.

Type
Research Article
Information
Clay Minerals , Volume 19 , Issue 3 , June 1984 , pp. 457 - 470
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1984

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References

Anonymous (1967) Case histories of gas fields recently developed in Niigata district Japan—ECAFA. Case Histories of Oil and Gas Fields in Asia and the Far East (2nd series). Minerals Resources Development Series 29. United Nations, New York.Google Scholar
Brobst, D.A. & Tucker, J.D. (1974) Composition and relation of analcime to diagenetic dawsonite in oil shale and tuff in the Green River Formation. Piceance Creek Basin, NW Colorado. J. Res, US Geol. Surv. 2/1, 35–39.Google Scholar
Carroll, R.D. (1968) Velocity-porosity logging in volcanic rocks. J. Petr. Techn. 22, 1371–1374.CrossRefGoogle Scholar
Coombs, D.S. (1974) Present status of the zeolite facies. Advances in Chemistry 101. America Chemical Society, 317 pp.Google Scholar
Davies, D.K. & William, R.A. (1978) Reservoir potential of volcanogenic sandstones. Bull. Am. Assoc. Petr. Geol. 62, 508 (abstract only).CrossRefGoogle Scholar
Fall, H.G., Gibb, F.G.F. & Kanaris-Sotiriou, R. (1982) Jurassic volcanic rocks of the northern North Sea. J. Geol.Soc. 139, 277–292.CrossRefGoogle Scholar
Fletcher, G.L. (1978) World energy development—Far East. Bull. Am. Assoc. Petr. Geol. 63, 1822.Google Scholar
Fletcher, G.L. (1979) World energy development—Far East. Bull. Am. Assoc. Petr. Geol. 64, 1888.Google Scholar
Fletcher, G.L. (1982) World energy development—Far East. Bull. Am. Assoc. Petr. Geol. 66, 2367–2368.Google Scholar
Galloway, W.E. (1979) Diagenetic control of reservoir quality in arc-derived sandstones implications for petroleum exploration. SEPM Spec. Pubi. 26, 251–262.Google Scholar
Helmhold, P.K. (1979) Diagenesis of Tertiary arkoses, Santa Ynez Mountains, Santa Barbara and Ventura Counties, California. Annual AAPG-SEPM Meeting (abstract).Google Scholar
Horton, R.C. (1965) Eastern Nevada is a gamble, but production is rising. World Oil, 84–89.Google Scholar
Khatchikian, A. & Lesta, P. (1973) Log evaluation of tuffites and tuffaceous sandstones in Southern Argentinia. SPWL 14th Ann. Logging Symp. Lafayette, 1–24.Google Scholar
Komatsu, N., Fujita, Y. & Satos, S. (1983) Cenozoic volcanic rocks as potential hydrocarbon reservoirs. Proc. 11th World Petr. Congr., London (preprint).Google Scholar
Loucks, R.G., Dodge, M.M. & Galloway, W.E. (1979) Importance of secondary leached porosity in lower Tertiary sandstones reservoir along the Texas Gulf Coast. Trans. Gulf Coast Ass. Geol. Soc. 29, 164–171.Google Scholar
Mumpton, F.A. & Sheppard, R.A. (1972) Zeolites. Geotimes March, 16–18.Google Scholar
Munson, R.A. & Sheppard, R.A. (1974) Natural zeolites; their properties, occurrences and uses. Miner. Sci. Eng. 6, 19–34.Google Scholar
Nagtegaal, P.J.C. (1979) Sandstone-framework instability as a function of burial diagenesis. J. Geol. Soc. 135, 101–105.CrossRefGoogle Scholar
Rateyev, M.A., Kheirov, M.B. & Shanter, A.A. (1967) Alteration of volcanic ash as a function of the physicochemical environment of diagenesis as illustrated by marine Miocene sediments of Western Kamchatka. Dokl. Akad. Nauk. SSSR 176, 176–179.Google Scholar
Stalder, P.J. (1979) Correlation between organic and inorganic metamorphism in the Taveyannaz sandstone from the Swiss Alps and in its equivalents in France and Italy. J. Sedim. Petrol. 49, 463–482.Google Scholar
Surdam, R.C. & Boles, J.R. (1979) Diagenesis of volcanic sandstones. Soc. Econ. Pal. Mineral. Spec. Pubi. 26. 227–242.Google Scholar
Sutan-Assin, N.D. (1972) Djatibarang, the discovery and development of a new oilfield: Proc. 1st Ann. Conv. IAP, Djakarta, 273–281.Google Scholar
Walton, W. (1975) Zeolitic diagenesis of Oligocene volcanic sediments, Trans-Pecos, Texas. Geol. Soc. Am. Bull. 86, 615–624.2.0.CO;2>CrossRefGoogle Scholar