{
  "type" : "Feature",
  "links" : [
    {
      "href" : "https://factmaps.sodir.no/api/rest/services/Factmaps/FactMapsWGS84/OGCFeatureServer/collections/254/items?f=application%2fjson",
      "rel" : "collection",
      "type" : "application/geo+json",
      "title" : "The collection document"
    },
    {
      "href" : "https://factmaps.sodir.no/api/rest/services/Factmaps/FactMapsWGS84/OGCFeatureServer/collections/254/items/605?f=json",
      "rel" : "self",
      "type" : "application/geo+json",
      "title" : "This document as JSON"
    },
    {
      "href" : "https://factmaps.sodir.no/api/rest/services/Factmaps/FactMapsWGS84/OGCFeatureServer/collections/254/items/605?f=text/html",
      "rel" : "alternate",
      "type" : "text/html",
      "title" : "This document as text/html"
    },
    {
      "href" : "https://factmaps.sodir.no/api/rest/services/Factmaps/FactMapsWGS84/OGCFeatureServer/collections/254/items/605?f=application/geo+json",
      "rel" : "alternate",
      "type" : "application/geo+json",
      "title" : "This document as application/geo+json"
    }
  ],
  "LayerId" : 254,
  "LayerName" : "Wellbore - History",
  "id" : "605",
  "properties" : {
    "OBJECTID" : 605,
    "wlbNpdidWellbore" : 1140,
    "wlbName" : "7122/6-1",
    "wlbHistory" : "\r\n\u003cp\u003e\u003cb\u003eGeneral\u003c/b\u003e\u003c/p\u003e\r\n\r\n\u003cp\u003eWildcat well 7122/6-1 was designed to\r\ndrill a prospect located in the central part of the block, located in the\r\neastern part of the Hammerfest Basin. The purpose of well 7122/6-1 was to test\r\nthe hydrocarbon potential of the Middle Jurassic to Upper Triassic sandstones\r\nin the main structure of the block.\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 7122/6-1 was spudded with\r\nPolar Frontier Drilling semi-submersible installation Polar Pioneer on 6\r\nSeptember 1987 and drilled to TD at 2707 m in the Middle - Late Triassic Snadd\r\nFormation.\u003c/p\u003e\r\n\r\n\u003cp\u003eThe structure penetrated by the well is a\r\nlarge tilted block dipping southwards. The northern closure is a major WNW-ESE\r\nfault. Top of the main markers were encountered higher than prognosed: top Stø\r\nFormation came in 71 m higher, and top Trias came in 183 m higher than\r\nexpected. The Jurassic reservoirs were found water bearing, however, some oil\r\nrecovered by RFT indicated the presence of a thin (1.5 m) oil zone at the top\r\nof the Stø formation. The late Triassic Snadd Formation proved gas and\r\ncondensate in a 71.5 m gross thickness reservoir. Weak shows were recorded in\r\ncuttings from the Hekkingen shale. Strong whitish yellow direct fluorescence\r\nwas observed in the cored sandstones all through the Stø Formation down to 2040\r\nm. Weak shows were recorded on the cored sandstones in the Nordmela, Tubåen,\r\nand Fruholmen Formations. Below this level, in the Triassic section, weak oil\r\nshows were recorded in sandstones, including the reservoir section between 2400\r\nto 2450 m that produced gas and condensate in the DST.\u003c/p\u003e\r\n\r\n\u003cp\u003eA very dense geochemical screening in\r\nthis well showed only very lean source rocks (< 1% TOC) above 1340 m.\r\nBetween 1340 m and 1931 m, the average TOC is around 1% with a somewhat richer\r\ninterval between 1750 m and 1900 m (TOC 1.5 to 3%), but with HI generally lower\r\nthan 100 mg/g. Between 1931 m and 2015 m, high organic content (TOC 10 to 15%)\r\nand high HI (280 - 350 mg/g) indicate a very",
    "wlbHistoryDateUpdated" : "2026-02-24T00:00:00"
  }
}