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By Michael Ashton, Geological Society of London

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Post-depositional faults acted as conduits for fluid which altered mineralogy, removed soluble components and, in one case, introduced anhydrite cement. The Vanguard Field is located in Block 49/16, approximately 45 miles east of Mablethorpe near the centre of the Sole Pit Basin, United Kingdom Continental Shelf (UKCS Fig. 1). The field was discovered in 1982 and brought into gas production as part of the Conoco-operated V-Fields development programme in October 1988. The field produces from the Leman Sandstone Member of the early Permian, Rotliegendes Group.

The core from this well contains abundant fractures and the sandstone is generally grey in colour. 1 mD permeability) are shown in Fig. 18. The sandstone is highly compacted, including crushed lithic fragments, and contains substantially more anhydrite than is typical for the Vanguard Field (Table 3). Authigenic illite appears more abundant (Fig. 19) than in well Q05. The data in Table 3 indicate that well Q02 contains less K-feldspar and has a lower chlorite/illite ratio than wells Q03 and Q05.

1977. Seismic stratigraphy and global changes of sea level, part 3: relative changes of sea level from coastal onlap. In: PAVTON, C. E. ) Seismic stratigraphy applications to hydrocarbon exploration. American Association of Petroleum Geologists Memoir 26, 63-97. VAN DER ZWAEN, C. J. 1989. Palynostratigraphical principles as applied in the Jurassic of the Troll and Draugen Fields, offshore Norway. In: COLLINSON, J. D. ) Correlation in hydrocarbon exploration. Norwegian Petroleum Society, Graham & Trotman, London, 357-365.

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