{
  "type" : "Feature",
  "links" : [
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      "rel" : "collection",
      "type" : "application/geo+json",
      "title" : "The collection document"
    },
    {
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      "title" : "This document as JSON"
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  "LayerId" : 254,
  "LayerName" : "Wellbore - History",
  "id" : "326",
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    "wlbNpdidWellbore" : 331,
    "wlbName" : "15/12-2",
    "wlbHistory" : "\u003cp\u003e\u003cb\u003eGeneral\u003c/b\u003e\u003c/p\u003e\r\n\r\n\u003cp\u003eWell 15/12-2 was drilled in order to\r\nevaluate Jurassic formations on a seismic structure located in the eastern part\r\nof block 15/12. The principal objective of the 15/12-2 well was to test the\r\nDogger (Hugin Formation) sandstone, where oil shows had been encountered in the\r\n15/12-1 well. A secondary object was a possible sand in the Paleocene. \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 15/12-2 was spudded with the\r\nsemi-submersible installation Ross Rig on 7 January 1976 and drilled to TD at\r\n2924 m in Late Permian Zechstein anhydrite. The well was drilled with a\r\nlignosulphonate mud system. \u003c/p\u003e\r\n\r\n\u003cp\u003eNo sand was found in the Paleocene. The\r\nHugin Formation sandstone was found 304 meters higher than in the 15/12-1 well.\r\nThe sandstone proved to have very good reservoir qualities, but was completely\r\nwater bearing. There were sandstone stringers in the lower part of the Heather\r\nFormation. The Hugin Formation sand was cored from 2823 m to 2835.4 m, with no\r\nshow. No fluid sampling was attempted in the well.\u003c/p\u003e\r\n\r\n\u003cp\u003eThe well was permanently abandoned as a\r\ndry well on 27 February 1976.\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"
  }
}