2/3-4
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General information
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Wellbore history
GeneralWell 2/3-4 was drilled by Gulf Oil Corporation - Norway Branch as a non-obligatory well on behalf of the participants in Production Licence 022. All obligatory work had been previously been done. The well is situated 275 km SSW of Stavanger. Geologically, the location was chosen on the "Ula Trend" on the NE flank of the Central Graben in the southern Norwegian North Sea. The principal objective of the well was to test structural closure of Upper Jurassic Ula Formation sandstone. This formation was believed to exist within 100 m below the nearest representative mappable seismic reflection, the Base Cretaceous Unconformity. The well was also planned to penetrate an Oligocene sand down-dip from a very small gas accumulation defined by a seismic flat spot anomaly, and which was therefore believed to be water wet at the location. The chalk reservoir was not predicted to be hydrocarbon bearing, nor was the well located within its mapped closure.Operations and resultsExploration well 2/3-4 was spudded with the jack-up installation Glomar Moray Firth I on 28 may 1984 and drilled to a total depth of 3386.3 m in Permian (Zechstein) evaporites. The well was drilled with seawater and gel down to 651 m and with Safemul oil based mud from 651 m to TD. Some swelling of the Miocene clay occurred during drilling of the 17 1/2" hole, otherwise no major problems occurred. Well 2/3-4 was the first exploration well for which NPD approved that conventional wire line logs was replaced with a suite of MWD logs.The primary objective, Ula Formation sands, was penetrated at 3006 m and was 207 m thick. The porosity of particularly the uppermost 170 m was excellent, generally between 25% and 30%. Electric logs, and a formation fluid sample (from FMT), indicated that the reservoir was water bearing throughout. Shows detection was made difficult due to the mud used. However, spectrofluorometric analyses on cuttings samples while drilling indicated that real shows could be present in the interval between 3045 m and 3006 m. The formation pressure gradient of 1.51 psi/m (0.46 psi/ft) within the reservoir further confirmed that the pore fluid was water, and that no vertical permeability barriers were present. Two segregated FMT samples were taken at 3011.5 m and 3073 m, both contained water. One core was cut from 3125.3 m to 3144.3 m in the Ula Formation sandstone. An anomalous high gamma ray peak was observed at 3030.6 m. The well was permanently abandoned as a dry well on 24 July 1984.TestingNo drill stem test was performed -
Cuttings at the Norwegian Offshore Directorate
Cuttings at the Norwegian Offshore Directorate Cuttings available for sampling?YESCuttings at the Norwegian Offshore Directorate Cutting sample, top depth [m]Cutting samples, bottom depth [m]200.003386.00 -
Cores at the Norwegian Offshore Directorate
Cores at the Norwegian Offshore Directorate Core sample numberCore sample - top depthCore sample - bottom depthCore sample depth - uom13125.43144.0[m ]Cores at the Norwegian Offshore Directorate Total core sample length [m]18.6Cores at the Norwegian Offshore Directorate Cores available for sampling?YES -
Core photos
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Palynological slides at the Norwegian Offshore Directorate
Palynological slides at the Norwegian Offshore Directorate Sample depthDepth unitSample typeLaboratory1400.0[m]DCRRI1450.0[m]DCRRI1500.0[m]DCRRI1550.0[m]DCRRI1600.0[m]DCRRI1650.0[m]DCRRI1700.0[m]DCRRI1710.0[m]DCRRI1720.0[m]DCRRI1740.0[m]DCRRI1750.0[m]DCRRI1780.0[m]DCRRI1790.0[m]DCRRI1810.0[m]DCRRI1820.0[m]DCRRI1830.0[m]DCRRI1840.0[m]DCRRI1850.0[m]DCRRI1870.0[m]DCRRI1880.0[m]DCRRI1900.0[m]DCRRI1905.0[m]DCRRI1915.0[m]DCRRI1920.0[m]DCRRI1930.0[m]DCRRI1945.0[m]DCRRI1950.0[m]DCRRI1960.0[m]DCRRI1970.0[m]DCRRI1975.0[m]DCRRI1990.0[m]DCRRI2005.0[m]DCRRI2020.0[m]DCRRI2035.0[m]DCRRI2050.0[m]DCRRI2060.0[m]DCRRI2065.0[m]DCRRI2080.0[m]DCRRI2095.0[m]DCRRI2105.0[m]DCRRI2110.0[m]DCRRI2125.0[m]DCRRI2140.0[m]DCRRI2155.0[m]DCRRI2160.0[m]DCRRI2170.0[m]DCRRI2185.0[m]DCRRI2190.0[m]DCRRI2200.0[m]DCRRI2215.0[m]DCRRI2230.0[m]DCRRI2245.0[m]DCRRI2260.0[m]DCRRI2270.0[m]DCRRI2275.0[m]DCRRI2290.0[m]DCRRI2300.0[m]DCRRI2305.0[m]DCRRI2320.0[m]DCRRI2335.0[m]DCRRI2350.0[m]DCRRI2365.0[m]DCRRI2380.0[m]DCRRI2395.0[m]DCRRI2400.0[m]DCRRI2410.0[m]DCRRI2425.0[m]DCRRI2440.0[m]DCRRI2450.0[m]DCRRI2455.0[m]DCRRI2470.0[m]DCRRI2485.0[m]DCRRI2500.0[m]DCRRI2505.0[m]DCRRI2515.0[m]DCRRI2525.0[m]DCRRI2530.0[m]DCRRI2535.0[m]DCRRI2545.0[m]DCRRI2560.0[m]DCRRI2575.0[m]DCRRI2590.0[m]DCRRI2600.0[m]DCRRI2605.0[m]DCRRI2610.0[m]DCRRI2620.0[m]DCRRI2650.0[m]DCRRI2660.0[m]DCRRI2670.0[m]DCRRI2675.0[m]DCRRI2680.0[m]DCRRI2690.0[m]DCRRI2695.0[m]DCRRI2710.0[m]DCRRI2785.0[m]DCRRI2800.0[m]DCRRI3000.0[m]DCRRI3006.0[m]DCRRI3034.0[m]DCRRI3060.0[m]DCRRI3113.0[m]DCRRI3135.5[m]DCRRI3142.0[m]DCRRI3144.0[m]DCRRI3180.0[m]DCRRI3188.0[m]DCRRI3204.0[m]DCRRI3236.0[m]DCRRI3248.0[m]DCRRI3256.0[m]DCRRI3268.0[m]DCRRI3302.0[m]DCRRI3322.0[m]DCRRI3334.0[m]DCRRI3342.0[m]DCRRI -
Lithostratigraphy
Lithostratigraphy Top depth [mMD RKB]Lithostrat. unit9614342527252725482592261327192719279629252925293030053005300630063215333233323377 -
Composite logs
Composite logs Document nameDocument formatDocument size [MB]pdf0.52 -
Geochemical information
Geochemical information Document nameDocument formatDocument size [MB]pdf0.40 -
Documents – reported by the production licence (period for duty of secrecy expired)
Documents – reported by the production licence (period for duty of secrecy expired) Document nameDocument formatDocument size [MB]pdf1.98pdf23.56 -
Logs
Logs Log typeLog top depth [m]Log bottom depth [m]DIFL ACL CDL CN GR CAL16852965DIFL ACL CDL CN GR CAL29593139DIFL ACL CDL CN GR CAL30603381DIFL ACL CDL GR CAL6111764DIPLOG29593382FMT00MWD - GR6441780MWD - GR18282959MWD - GR RES195644TEMP20620TEMP5002940VELOCITY6113381VSP16003370XY CAL GR157648 -
Casing and leak–off tests
Casing and leak–off tests Casing typeCasing diam.
[inch]Casing depth
[m]Hole diam.
[inch]Hole depth
[m]LOT/FIT mud eqv.
[g/cm3]Formation test typeCONDUCTOR30183.536335.30.00LOTSURF.COND.20644.526650.51.49LOTINTERM.13 3/81770.617 1/21786.01.74LOTINTERM.9 5/82963.912 1/42967.81.92LOTOPEN HOLE3386.08 1/23386.00.00LOT -
Drilling mud
Drilling mud Depth MD [m]Mud weight [g/cm3]Visc. [mPa.s]Yield point [Pa]Mud typeDate measured1281.43WATER BASED29.05.19842011.32WATER BASED31.05.19842011.32WATER BASED31.05.19842011.04WATER BASED04.06.19846391.14330.0200.0OIL BASED15.06.19846511.056.029.0WATER BASED05.06.198412131.2631.022.0OIL BASED17.06.198417711.3837.025.0OIL BASED25.06.198421571.4032.025.0OIL BASED28.06.198425631.4139.027.0OIL BASED02.07.198427951.4134.011.1OIL BASED04.07.198428891.4132.010.6OIL BASED04.07.198429681.4935.015.4OIL BASED06.07.198430011.5336.014.9OIL BASED11.07.198431251.5636.014.9OIL BASED13.07.1984 -
Thin sections at the Norwegian Offshore Directorate
Thin sections at the Norwegian Offshore Directorate DepthUnit3136.00[m ] -
Pressure plots
Pressure plots The pore pressure data is sourced from well logs if no other source is specified. In some wells where pore pressure logs do not exist, information from Drill stem tests and kicks have been used. The data has been reported to the NPD, and further processed and quality controlled by IHS Markit.Pressure plots Document nameDocument formatDocument size [MB]pdf0.23