{
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  "LayerId" : 254,
  "LayerName" : "Wellbore - History",
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    "wlbNpdidWellbore" : 2015,
    "wlbName" : "30/10-7",
    "wlbHistory" : "\r\n\u003cp\u003e\u003cb\u003eGeneral\u003c/b\u003e\u003c/p\u003e\r\n\r\n\u003cp\u003eThe exploration well 30/10-7 was\r\ndedicated to explore the hydrocarbon potential of the Paleocene Hermod\r\nFormation.\u003c/p\u003e\r\n\r\n\u003cp\u003eWell 30/10-7 is located in the\r\ncentral-northern part of block 30/10, and the Paleocene structure forms a\r\nmoundy/domal feature, with minor normal faults to the east and west of the well\r\nlocation. TD was planned at 2613 m in the Late Cretaceous Hardråde Formation.\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 30/10-7 was spudded 8 September\r\nby the semi-submersible installation Maersk Jutlander and drilled to TD at 2612\r\nm in the Late Cretaceous Hardråde Formation. The well was drilled with seawater\r\nand hi-vis pills down to 1270 m and with Gyp / Polymer mud from 1270 m to TD.\r\nThe well encountered sands with very good reservoir characteristics both in the\r\nHermod Formation and in the Heimdal Formation, but the reservoirs were water\r\nbearing. In the entire well bore no shows of any kind was observed. Two cores\r\nwere cut from 2207 m to 2227 m and recovered sands and mudstone from the Hermod\r\nand Sele Formations. No fluid samples were taken.\u003c/p\u003e\r\n\r\n\u003cp\u003eThe well was permanently abandoned on 17\r\nOctober 1992 as a dry hole.\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\r\n",
    "wlbHistoryDateUpdated" : "2026-02-24T00:00:00"
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}