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    "wlbNpdidWellbore" : 202,
    "wlbName" : "6507/12-1",
    "wlbHistory" : "\r\n\u003cp\u003e\u003cb\u003eGeneral\u003c/b\u003e\u003c/p\u003e\r\n\r\n\u003cp\u003eWildcat well 6507/12-1 was the first well\r\nto be drilled offshore Mid-Norway. It was drilled to test the stratigraphic\r\nsequence between seabed and at least 500 m below "reflector E" as\r\ndefined in the licence agreement. The primary target was a mapped Intra\r\nJurassic seismic reflector at a depth of approximately 2575 m. This reflector\r\nwas interpreted to be associated with a Middle to Early Jurassic sandstone\r\nsequence. The secondary target was represented by possible sandstone sequences\r\nbetween the mapped Base Cretaceous reflector and the Intra Jurassic reflector.\r\nThirdly there was a small vertical closure in the basal part of the Tertiary\r\nsequence that could have prospective interest.\u003c/p\u003e\r\n\r\n\u003cp\u003eThe well is Type Well for the Båt Group,\r\nthe Tare Formation and the Naust Formation. It is Reference Well for the Fangst\r\nGroup.\u003c/p\u003e\r\n\r\n\u003cp\u003e\u003cb\u003eOperations and results\u003c/b\u003e\u003c/p\u003e\r\n\r\n\u003cp\u003eThe well was spudded with the\r\nsemi-submersible installation Byford Dolphin on 1 July 1980 in a water depth of\r\n225 m, and drilled to a total depth of 3713 m in Late Triassic Red Beds. The\r\nwell was drilled with spud mud down to 778 m, with Gypsum PAC mud from 778 m to\r\n1448 m, and with Lignosulfonate/PAC mud from 1448 m to TD.\u003c/p\u003e\r\n\r\n\u003cp\u003eThe well penetrated a section of 1105 m\r\nbelow reflector E and thus meets the requirement set in the work programme for\r\nlicence 059.\u003c/p\u003e\r\n\r\n\u003cp\u003eThe well encountered a Cenozoic sequence\r\nof 1679 m and the Tertiary succession was, at the time the well was drilled,\r\nsubdivided into lithostratigraphic units according to Deegan & Scull's\r\nnomenclature for the northern North Sea. The well proved a slightly thicker\r\nTertiary sequence than expected. The seismic leg interpreted to represent Base\r\nTertiary proved to be related to a tuff sequence (Tare Formation).\u003c/p\u003e\r\n\r\n\u003cp\u003eThe Top Cretaceous reflector was easily\r\ndetermined from acoustic and density logs. The base of the Cretaceous was\r\nencountered in the well at 2032 m. The prognosed depth was 1975 m. The\r\nCretaceous seque",
    "wlbHistoryDateUpdated" : "2026-02-24T00:00:00"
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