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    "wlbNpdidWellbore" : 1135,
    "wlbName" : "9/2-2",
    "wlbHistory" : "\"\r\n\r\n\u003cp\u003e\u003cb\u003eGeneral\u003c/b\u003e\u003c/p\u003e\r\n\r\n\u003cp\u003eWildcat well 9/2-2 was drilled on a\r\nfault-induced dome-formed structural trap (the Alpha structure) in the\r\nnorthwestern part of the block. The primary objective for the well was to test\r\nthe Jurassic sandstones of the Sandnes- and Bryne Formations in the structure.\r\nIn addition the well should test the structural and geophysical\r\ninterpretations, and improve the geological, geochemical and paleontological\r\nunderstanding of the area. The well was programmed and designed as a possible future\r\nproducer.\u003c/p\u003e\r\n\r\n\u003cp\u003e\u003cb\u003eOperations and results\u003c/b\u003e\u003c/p\u003e\r\n\r\n\u003cp\u003eWildcat well 9/2-2 was spudded with the\r\nsemi-submersible installation Ross Isle 8 august 1987 and drilled to TD at 3550\r\nm in the Triassic Skagerrak Formation. Drilling went on with some minor\r\nproblems in the interval 2400 - 3000 m. Inclination increased in the 8\r\n1/2" section towards TD and was 11.1° at 3539 m. The well was drilled with\r\nseawater and gel down to 363 m, with gypsum/polymer mud from 363 m to 2871 m,\r\nand with gel/lignosulphonate mud from 2871 m to TD.\u003c/p\u003e\r\n\r\n\u003cp\u003eTop Sandnes and Bryne sandstones were\r\nreached at 3131 m and 3230 m respectively. From the logs the Middle Jurassic\r\nsandstones were interpreted as water bearing. The results of the log\r\ninterpretation indicated some low hydrocarbon saturations in the lower part of\r\nthe Sandnes formation and in major parts of the Bryne formation. Some residual\r\nhydrocarbons may be present, but the major part of the hydrocarbon saturations,\r\nparticular in the Bryne formation, is unrealistic due to organic material and\r\ncoal layers affecting the logs. The first show in the well was recorded at 3114\r\nm and the deepest near TD at 3544 m. The shows were generally seen in shales\r\nand coals or in sandstones interbedded with shales and coals. The strongest and\r\nmost continuous shows were seen in shales from 3114 m to 3234 m (base Egersund\r\nFormation - upper Sandnes Formation), and in interbedded sands, shales, and\r\ncoals in the interval 3417 m to 3498 m (base Bryne Formation and",
    "wlbHistoryDateUpdated" : "2026-02-24T00:00:00"
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