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    "wlbName" : "16/3-3",
    "wlbHistory" : "\r\n\r\n\u003cp\u003e\u003cb\u003eGeneral\u003c/b\u003e\u003c/p\u003e\r\n\r\n\u003cp\u003eWell 16/3-3 is located on the eastern\r\nmargin of the Utsira High in the North Sea. The primary objective of the well\r\nwas to test the reservoir and hydrocarbon potential of the Paleocene Heimdal\r\nsands in the Havørn Prospect. The prospect sands pinches out to the east and\r\nsouth combined with a structural dip to the northwest. The source kitchen was\r\nexpected to be the Late Jurassic Draupne Formation in the Southern Viking\r\nGraben. Top seal for the sands were prognosed to be the Late Paleocene- and the\r\nEocene marine shales.\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 16/3-3 was spudded with the\r\nsemi-submersible installation Vildkat Explorer on 24 July 1989 and drilled to\r\nTD at 1566 m in the Late Cretaceous Tor Formation. No significant problems occurred\r\nduring the operations. The well was drilled with seawater down to 445 m and\r\nwith lignosulphonate/seawater and gel from 445 m to TD.\u003c/p\u003e\r\n\r\n\u003cp\u003eLate Cretaceous rocks were encountered at\r\n1488 m, underlying 1341 meters of Cenozoic claystones. The Late Cretaceous\r\nsediments (+ 78 m) consisted of white-creamy chalk. The Heimdal Formation sands\r\nwere absent. No reservoir intervals were penetrated. No shows were recorded. \u003c/p\u003e\r\n\r\n\u003cp\u003eNo cores were cut and no fluid samples\r\ntaken in this well.\u003c/p\u003e\r\n\r\n\u003cp\u003eThe well was permanently abandoned on 6\r\nAugust 1989 as a dry well.\u003c/p\u003e\r\n\r\n\u003cp\u003e\u003cb\u003eTesting\u003c/b\u003e\u003c/p\u003e\r\n\r\n\u003cp\u003eNo drill stem test was performed\u003c/p\u003e\r\n\r\n",
    "wlbHistoryDateUpdated" : "2026-02-24T00:00:00"
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