Advances in reservoir geology by Michael Ashton, Geological Society of London

By Michael Ashton, Geological Society of London

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O. Box 488, 4001 Stavanger, Norway 3 Corrigan Associates, 2 The Drove, Ditchling, Sussex BN6 8TR, UK Abstract: The Rotliegendes Group in the Vanguard Field, UKCS, consists of a series of aeolian, fluvial, and reworked aeolian sediments, organized into four broadly correlatable lithostratigraphical units. Within these units, reservoir properties are strongly linked to lithofacies, with aeolian dune sandstones possessing the best porosity and permeability. A comparison of production log spinner profiles (PLT) with detailed sedimentological logs from three development wells shows that gas production is intimately associated with specific lithofacies and their spatial organization.

Displacive calcite and grain breakage in sandstones. Journal of Sedimentary Petrology, 59, 258-266. BRYANT, I. , KANTOROWlCZ, J. D. & LOVE, C. F. 1988. The origin and recognition of laterally continuous carbonate-cemented horizons in the Upper LiPs Sands of southern England. Marine and Petroleum Geology, 5, 108-133. GREY, D. I. 1987. Troll. In: SPENCER, A. M. ) Geology of Norwegian Oil and Gas Fields. Norwegian Petroleum Society, Oslo, 389-401. HALLAM, A. 1987. Eustatic cycles in the Jurassic. Palaeogeography, Palaeoclimatology, Palaeoecology, 23, 1-32.

The effect of this fluid was to dissolve K-feldspar, thereby facilitating compaction of the rock framework, illitization of chlorite, and ankerite formation. Wells Q04 and Q02 could have been located beneath a paleo-gas-water contact during this migration/alteration event, but we have no direct evidence for such an interpretation. The sandstones beneath the gas-water contact in wells Q01, Q03, and Q05 are petrographically similar to gas-saturated sandstones in the wells and do not resemble wells Q02 and Q04.

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