6407/9-8
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General information
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Wellbore history
GeneralWildcat well 6407/9-8 was drilled on the Husmus East structure, situated east of the Draugen Field on the edge of the Trøndelag Platform on the Mid Norwegian Continental Shelf. The principal objective of the well was to test the hydrocarbon potential of the Late Jurassic Rogn Formation in a dip closure trap. Secondary objective was to test the potential for gas storage in the Rogn Formation and in the middle Jurassic Garn Formation. The well was also drilled to acquire additional stratigraphic information on the reservoir development of the Middle and Early Jurassic Ile and Tilje Formation.Operations and resultsWell 6407/9-8 was spudded with the semi-submersible installation West Vanguard on 14 August 1992 and drilled to TD at 2126 m in the Early Jurassic Tilje Formation. Operations went without significant problems. The well was drilled with seawater and bentonite down to 1120 m, with polymer/gypsum mud from 1120 m to 1582 m, and with KCl/polymer mud from 1582 m to TD.No potential reservoir zones were found above the Viking Group, which was penetrated from 1606.5 m to 1730 m. The Rogn Formation vas poorly developed as a thin (<1 m), well-cemented silty to very fine sandstone facies with low porosity and permeability. A well-developed Garn Formation in a sand facies vas encountered, with high porosities and permeabilities. The well vas terminated in sandstone of the Tilje Formation after penetration of Ile Formation sandstone. Both the Garn Formation and the Ile Formations appeared to be suitable for gas injection. The well was entirely water wet all through. This was evident from electrical logs, pressure gradients, and lack of shows on cores and cuttings. Post-well geochemical analyses of cores and cuttings confirmed general lack of migrated hydrocarbons. A total of seven cores were cut in the well with 105.95 m recovered. Cores 1 to 5 were cut from 1605 m to 1685 m in the Spekk and Rogn Formations. Cores 6 and 7 were cut from 1723 m to 1760.5 m in the Melke and Garn Formations. A dense FMT pressure-sampling programme confirmed a water-wet reservoir with a pressure gradient close to the theoretical gradient for the established Draugen Formation water. A number of attempts were made to take water samples at depths of 1731.5 m (Garn) and 1940 m (Ile). Some degree of filtrate contamination vas noted.The well was classified as dry and was suspended on 23 September 1992 as a possible future development well for the Draugen Field. It was re-entered on 14 August and taken in use as a gas injectorTestingNo 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]1130.002127.00 -
Cores at the Norwegian Offshore Directorate
Cores at the Norwegian Offshore Directorate Core sample numberCore sample - top depthCore sample - bottom depthCore sample depth - uom11605.01622.1[m ]21623.01633.1[m ]31633.51642.0[m ]41650.01666.0[m ]51666.01685.0[m ]61723.01741.9[m ]71742.01758.7[m ]Cores at the Norwegian Offshore Directorate Total core sample length [m]106.2Cores at the Norwegian Offshore Directorate Cores available for sampling?YES -
Core photos
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Lithostratigraphy
Lithostratigraphy Top depth [mMD RKB]Lithostrat. unit2522524387587581296129613351530153015981606160616991730173018331887200620062053 -
Composite logs
Composite logs Document nameDocument formatDocument size [MB]pdf0.48 -
Geochemical information
Geochemical information Document nameDocument formatDocument size [MB]pdf4.38 -
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]pdf43.91 -
Logs
Logs Log typeLog top depth [m]Log bottom depth [m]CORGUN286400CORGUN286400CORGUN11341578CORGUN15502110CORGUN16881852CORGUN18601933CORGUN19392098DIFL ACL BHC GR11101582DIFL BHC ACL GR2521113DIFL BHC ACL GR2521113DIFL BHC ACL GR11101582DIFL BHC ACL GR15531759DIFL BHC ACL GR15532120DIPLOG15502110DLL MLL GR15532115FMT16511920FMT17312096FMT18802105FMT19401940MWD252160SBT VDL GR14192086SPECTRALOG15532120VSP15532121ZDL CNL GR2521113ZDL CNL GR2521113ZDL CNL GR11101582ZDL CNL GR15531759ZDL CNL GR15532120ZDL FDC GR11101582 -
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 typeCONDUCTOR30309.736310.00.00LOTINTERM.18 5/81110.0261112.00.00LOTINTERM.13 3/81553.317 1/21555.01.62LOTINTERM.9 5/82118.012 1/42120.01.73LOT -
Drilling mud
Drilling mud Depth MD [m]Mud weight [g/cm3]Visc. [mPa.s]Yield point [Pa]Mud typeDate measured3101.02200.0WATER BASED3161.01200.0WATER BASED4771.02200.0WATER BASED6741.02200.0WATER BASED11171.02200.0WATER BASED11171.02200.0WATER BASED11201.02200.0WATER BASED11251.3960.0WATER BASED14001.3960.0WATER BASED15821.3982.0WATER BASED15981.1337.0WATER BASED16501.1439.0WATER BASED16661.1440.0WATER BASED17021.1540.0WATER BASED17421.1539.0WATER BASED18001.1639.0WATER BASED19621.1438.0WATER BCSED21261.1438.0WATER BASED -
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]PDF0.28