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    "wlbNpdidWellbore" : 1411,
    "wlbName" : "7324/10-1",
    "wlbHistory" : "\r\n\r\n\u003cp\u003e\u003cb\u003eGeneral\u003c/b\u003e\u003c/p\u003e\r\n\r\n\u003cp\u003eWell 7324/10-1 was drilled on the Alpha\r\nstructure in the Maud Basin on the Bjarmeland Platform. The main objective was\r\nto test the hydrocarbon potential in a prospect at the Base Anisian level (Top\r\nKlappmyss Formation). The secondary objective was to test sandstones below the\r\nBase Smithian level (Top Havert Formation). In addition the well should test\r\nthe source rock potential in the Triassic, Base Snadd, and Base Kobbe\r\nFormations. Possible sand layers at 575 - and 695 m justified a shallow gas\r\nwarning at these levels. Planned TD was at 3400 m in Late Permian.\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 7324/10-1 was spudded with\r\nthe semi-submersible rig Ross Rig 3 June 1989 and drilled to TD at 2919 m in\r\nthe Early Triassic Havert Formation. TD was set approximately 500 m higher than\r\nprognosed due to lost circulation problems in the interval 1800 m to 2626 m.\r\nThe well was drilled with seawater down to 558 m, with gypsum / polymer from\r\n558 m to 2289 m, and with gel / lignosulphonate from 2289 m to TD. No shallow\r\ngas was encountered.\u003c/p\u003e\r\n\r\n\u003cp\u003eMinor gas was encountered in the Kobbe\r\nFormation at 1607 m but the sandstones had very poor permeability and no RFT\r\nsamples were collected. The main target at Base Anisian/Klappmyss Formation at\r\n1767 m in the prognosis, proved to be an intra Anisian seismic marker\r\nencountered at 1822 m. At this level there was no reservoir developed, neither\r\nwas there any reservoir developed at the new Anisian seismic marker on 2272 m.\r\nThe secondary objective at top Havert Formation encountered at 2512 m had a\r\nlimited reservoir developed. Shows were recorded in the Snadd Formation from\r\n617 m to 692 m and 1150 m to 1186 m. Organic rich shales were encountered in\r\nSnadd, Kobbe, and Klappmyss Formations, but from organic geochemistry only a\r\nthin sequences in the Snadd Formation could be classified as good, possibly\r\noil-prone source rocks. These were: a carbonaceous shale at 989 m and a thin\r\nclay stone sequence at 1603 m t",
    "wlbHistoryDateUpdated" : "2026-02-24T00:00:00"
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