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7231/4-U-1

Partial source coverage. Status and company roles are reported by each source, not independently verified as current. Unknown does not mean zero.

Name / source ID
7231/4-U-1
Borehole / source record ID
1154
Sector
Oil and gas
Derived purpose group
Unclassified
Operator in source snapshot
IKU Petroleumsforskning SINTEF Gruppen
Recorded spud date
1987-08-22
Recorded completion date
1987-08-28
Latitude / longitude (WGS84)
72.738148 / 31.123531
Source-reported measurements
378 m MD · RKB
Status reported by source
P&A
Source accessed
2026-10-02
Source snapshot date
Not reported / not verified
Original coordinate reference system
ED50 / service geometry EPSG:4326

Company roles reported by source

Source-reported measurements
Source-reported measurementsValueReference
wlbTotalDepth378.00 mRKB
wlbWaterDepth280.00 mNot reported / not verified
Open source record ↗

Nearby wells and heat flow

These tools are descriptive: not forecasts, reserve estimates or investment advice. Source coverage is partial; unknown does not mean zero.

Nearby wells and heat flow
NameDistanceSource-reported measurementsSource catalogues
7231/1-U-11.73 km371 mNorwegian Offshore Directorate — Wellbores
7230/5-U-625.03 km383 mNorwegian Offshore Directorate — Wellbores
7230/5-U-525.07 km335 mNorwegian Offshore Directorate — Wellbores
7230/5-U-425.27 km362 mNorwegian Offshore Directorate — Wellbores
7230/5-U-325.46 km404 mNorwegian Offshore Directorate — Wellbores
7230/5-U-225.58 km412 mNorwegian Offshore Directorate — Wellbores
7230/5-U-927.91 km369 mNorwegian Offshore Directorate — Wellbores
7230/8-U-142.40 km30 mNorwegian Offshore Directorate — Wellbores

Subsurface temperature and heat flow

Compare bottom-hole temperatures with depth and see measured heat flow near wells: context for geothermal reuse.

Subsurface temperature and heat flow
NameDistanceSubsurface temperature and heat flowQuality flags
R24-P02288725.03 km104.00 mW/m2{"qualityScores":["Ux.Mx.-------"]}
R24-P02288842.40 km54.20 mW/m2{"qualityScores":["Ux.Mx.-------"]}
w.

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