30/10-1
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General information
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Wellbore history
GeneralWell 30/10-1 is located on the Northern apex of the Frigg field. The well was drilled as a wildcat, primarily to evaluate the Lower Eocene sand ("Frigg Field Clastic Tongue") in the area. Secondly, the well should evaluate the Paleocene sands and the Late Cretaceous limestone. The plan was to set the 9 5/8 inch casing in the top of a high-pressure zone (Cretaceous Shale) prior to moving the rig Saipem Due to another location. The hole should then be re-entered with another rig and drill deeper to evaluate a deep-seated structural closure.Operations and resultsWell 30/10-1 was spudded with the vessel Saipem Due on 5 May 1973 and drilled to TD at 2917 m in Late Cretaceous (Maastrichtian) shale. Initial drilling from the sea floor to 1067 m was with seawater and gel. Below 1067 m a fresh water Spersene XP 20 (lignosulphonate) mud system was used.The thickness of the pay section of the Frigg Clastic Tongue (Primary objective) was disappointing in that it was very thin. A green shale unit replaced the expected pay section. Formation interval test and logs indicate that approximately 4 m of the Frigg Clastic sand contained gas and approximately 6 m could possibly be oil bearing. No other good hydrocarbon shows were encountered below the Frigg Clastic Tongue. in the rogaland Group almost 200 m of sand were present, however, the sand was void of hydrocarbons, with the exception of some scattered fluorescence in the upper portion. Five cores were cut in the Frigg sand in the interval 1974 m to 2010 m. No sidewall cores were taken. Four Formation Interval Tests (FITs) were taken in the Frigg sand. FIT No 1 at 1960.5 m recovered, 29 cubic feet of gas, 5 litres water and 0.5 litres mud. FIT No. 2 at 1989.5 m recovered 10 litres water. FIT No. 3 at 1974.5 m recovered 7 litres liquid (mud and water) and 100 cc oil. FIT No. 4 at 1966 m recovered 6.5 cubic feet gas, 2.25 litres oil, 300 cc mud, and 4.75 litres of water. Oil gravity was 29.7 deg API.Due to a pressure zone encountered between 2905 m and 2917 m and subsequent loss of circulation the well was junked. The well was abandoned as an oil and gas appraisal well.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]167.642916.94 -
Cores at the Norwegian Offshore Directorate
Cores at the Norwegian Offshore Directorate Core sample numberCore sample - top depthCore sample - bottom depthCore sample depth - uom16482.06490.0[ft ]26490.06521.0[ft ]36534.06545.0[ft ]46545.06563.0[ft ]56578.06593.0[ft ]Cores at the Norwegian Offshore Directorate Total core sample length [m]25.3Cores at the Norwegian Offshore Directorate Cores available for sampling?YES -
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 typeCONDUCTOR30156.036160.00.00LOTSURF.COND.20362.026365.00.00LOTINTERM.13 3/81063.017 1/21065.01.43LOTOPEN HOLE2917.012 1/42917.00.00LOT -
Logs
Logs Log typeLog top depth [m]Log bottom depth [m]BHC S GRC1171088BHC S GRC10642036CAL10631570DIL10642038GR NEU10632905IEL3631088TEMP15242659 -
Lithostratigraphy
Lithostratigraphy Top depth [mMD RKB]Lithostrat. unit1294536606608421960207620762115216021702202228923402374246026212640264026792834 -
Composite logs
Composite logs Document nameDocument formatDocument size [MB]pdf0.21 -
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]pdf6.46 -
Drilling mud
Drilling mud Depth MD [m]Mud weight [g/cm3]Visc. [mPa.s]Yield point [Pa]Mud typeDate measured10961.17water/spers19761.17water/spers23561.18water/spers25651.19water/spers29161.49water/spers -
Palynological slides at the Norwegian Offshore Directorate
Palynological slides at the Norwegian Offshore Directorate Sample depthDepth unitSample typeLaboratory3010.0[ft]DC3100.0[ft]DC3190.0[ft]DC3310.0[ft]DC3400.0[ft]DC3490.0[ft]DC3600.0[ft]DC3690.0[ft]DC3810.0[ft]DC3900.0[ft]DC3990.0[ft]DC4110.0[ft]DC4200.0[ft]DC4290.0[ft]DC4410.0[ft]DC4500.0[ft]DC4620.0[ft]DC4710.0[ft]DC4800.0[ft]DC4890.0[ft]DC5010.0[ft]DC5100.0[ft]DC5190.0[ft]DC5280.0[ft]DC5370.0[ft]DC5460.0[ft]DC5550.0[ft]DC5640.0[ft]DC5730.0[ft]DC5820.0[ft]DC5910.0[ft]DC6030.0[ft]DC6120.0[ft]DC6210.0[ft]DC6330.0[ft]DC6360.0[ft]DC6390.0[ft]DC6420.0[ft]DC6486.0[ft]C6489.0[ft]C6493.0[ft]C6498.0[ft]C6501.0[ft]C6508.0[ft]C6545.0[ft]C6548.0[ft]C6550.0[ft]DC6555.0[ft]DC6600.0[ft]DC6691.0[ft]DC6780.0[ft]DC6870.0[ft]DC6900.0[ft]DC6930.0[ft]DC6960.0[ft]DC7070.0[ft]DC7160.0[ft]DC7225.0[ft]DC7270.0[ft]DC7280.0[ft]DC7290.0[ft]DC7300.0[ft]DC7310.0[ft]DC7320.0[ft]DC7330.0[ft]DC7340.0[ft]DC7350.0[ft]DC7360.0[ft]DC7370.0[ft]DC7470.0[ft]DC7570.0[ft]DC7670.0[ft]DC7770.0[ft]DC7870.0[ft]DC7970.0[ft]DC7990.0[ft]DC8010.0[ft]DC8030.0[ft]DC8050.0[ft]DC8070.0[ft]DC8170.0[ft]DC8270.0[ft]DC8370.0[ft]DC8470.0[ft]DC8570.0[ft]DC8620.0[ft]DC8670.0[ft]DC8680.0[ft]DC8720.0[ft]DC8770.0[ft]DC8870.0[ft]DC8970.0[ft]DC9070.0[ft]DC9170.0[ft]DC9270.0[ft]DC9370.0[ft]DC9470.0[ft]DC9570.0[ft]DC