7/7-1
Eksport: PDF
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Generell informasjon
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Brønnhistorie
GeneralWell 7/7-1 was the first well in license 148, and was designed to drill a tilted block on the Jæren High close to the UK border. Early/Middle Jurassic events resulted in uplift and erosion, such that Jurassic sediments at the well location are missing. Due to the Tertiary uplift and eastward tilting of the Shetland Platform, along with a relative drop in sea level, this tilting gave rise to an eastward drainage pattern. Submarine fan sandstones derived from deltaic and barrier bar complexes in the Morray Firth area were deposited in the Central Graben and on to the Jæren High. Several lobe systems developed, giving rise to continuous and periodic sandstone deposition as the lobes migrated laterally. The eastern pinch out of these systems occurs in blocks 7/4 and 7/7. The primary objective of this well was an anticlinal closure at the Base Cretaceous Unconformity level, the C-prospect, Triassic sandstones. The secondary objective was the B-prospect, Paleocene sandstones, a possible closure along a pinch out of a sandy sequence consisting of distal turbidites. Some high amplitude anomalies indicated shallow gas between 241 to 395 m. The nearest one at 308 m was situated approximately 300 m east of the well location. Sticky and swelling "gumbo" clays are common in the area.Operations and resultsWildcat well 7/7-1 was spudded with the semi-submersible installation Deepsea Bergen 30 December 1989 and drilled to TD at 3500 m in the Triassic Smith Bank Formation. The well was drilled with seawater and gel down to 572 m, with gypsum/polymer mud from 572 m to 3263 m, and with bentonite/lignosulphonate mud from 3263 m to TD. Apart from some tight hole problems, drilling went without severe problems. No shallow gas was encountered. The well was drilled approximately 200 m into the Triassic, which consisted of brick red sandstones, interbedded with siltstone / claystone. The Paleocene sandstones came in nearly 60 m below the prognosed depth, and only minor amounts of sand was encountered (Andrew Formation). No indication of hydrocarbons was seen in this well. Two conventional cores were cut, one from 2786 m to 2803 m in the Paleocene Andrew Formation and a second from 3286 m to 3313.5 m driller's depth (3291.5 m to 3319 m loggers depth) in the Smith Bank Formation. A total of 125 sidewall cores were attempted, and 118 sidewall cores were recovered. No fluid samples were taken. The well was permanently abandoned on 20 February 1990 as a dry hole.TestingNo drill stem test was performed -
Borekaks i Sokkeldirektoratet
Borekaks i Sokkeldirektoratet Borekaks tilgjengelig for prøvetaking?YESBorekaks i Sokkeldirektoratet Borekaksprøve, topp dybde [m]Borekaksprøve, bunn dybde [m]590.003500.00 -
Borekjerner i Sokkeldirektoratet
Borekjerner i Sokkeldirektoratet Kjerneprøve nummerKjerneprøve - topp dybdeKjerneprøve - bunn dybdeKjerneprøve dybde - enhet12786.02803.0[m ]23296.03313.5[m ]Borekjerner i Sokkeldirektoratet Total kjerneprøve lengde [m]34.5Borekjerner i Sokkeldirektoratet Kjerner tilgjengelig for prøvetaking?YES -
Kjernebilder
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Foringsrør og formasjonsstyrketester
Foringsrør og formasjonsstyrketester Type utforingUtforing diam.
[tommer]Utforing dybde
[m]Brønnbane diam.
[tommer]Brønnbane dyp
[m]LOT/FIT slam eqv.
[g/cm3]Type formasjonstestCONDUCTOR30167.036168.00.00LOTINTERM.20567.026580.01.64LOTINTERM.13 3/82548.0182565.01.86LOTINTERM.9 5/83251.012 1/43263.01.63LOTOPEN HOLE3500.08 1/23500.00.00LOT -
Logger
Logger Type loggTopp dyp for logg [m]Bunn dyp for logg [m]CBL VDL GR13332554CBL VDL GR19033253DIFL ACL CDL CNL GR25483260DIFL ACL CDL CNL GR32533502DIFL ACL CDL GR5672567DIPS GR32543499FMT GR32903317MLL SPL32533505MWD5723500SWC GR20212566SWC GR26493258SWC GR32603503VSP1003490 -
Litostratigrafi
Litostratigrafi Topp Dyb [mMD RKB]Litostrat. enhet106125626262626266027582780280828302830292531083243324332883288 -
Spleisede logger
Spleisede logger Dokument navnDokument formatDokumentstørrelse [MB]pdf0.57 -
Geokjemisk informasjon
Geokjemisk informasjon Dokument navnDokument formatDokumentstørrelse [MB]pdf0.23 -
Dokumenter – rapportert av utvinningstillatelsen (frigitt ihht til regelverk)
Dokumenter – rapportert av utvinningstillatelsen (frigitt ihht til regelverk) Dokument navnDokument formatDokumentstørrelse [MB]pdf18.43 -
Dokumenter – eldre Sokkeldirektoratets WDSS rapporter og andre relaterte dokumenter
Dokumenter – eldre Sokkeldirektoratets WDSS rapporter og andre relaterte dokumenter Dokument navnDokument formatDokumentstørrelse [MB]pdf0.19pdf0.18 -
Boreslam
Boreslam Dybde MD [m]Egenvekt, slam [g/cm3]Viskositet, slam [mPa.s]Flytegrense [Pa]Type slamDato, måling5761.03WATER BASED05.01.19905801.03WATER BASED05.01.19905801.03WATER BASED08.01.199025651.5629.06.0WATER BASED16.01.199025651.5626.06.0WATER BASED16.01.199025651.5625.05.0WATER BASED17.01.199025681.5021.05.0WATER BASED24.01.199026851.5022.04.0WATER BASED25.01.199026901.5021.04.5WATER BASED26.01.199027641.5022.06.0WATER BASED29.01.199027861.5021.05.0WATER BASED29.01.199028031.5023.05.0WATER BASED29.01.199029031.5024.06.5WATER BASED30.01.199029971.5027.06.0WATER BASED31.01.199030471.5027.05.5WATER BASED02.02.199030541.5025.04.5WATER BASED05.02.199031141.5025.05.0WATER BASED06.02.199032631.5025.05.5WATER BASED07.02.199032631.5023.05.0WATER BASED07.02.199032631.5027.05.0WATER BASED08.02.199032841.5545.06.0WATER BASED12.02.199032841.5543.06.5WATER BASED14.02.199032841.5542.05.0WATER BASED14.02.199032841.5543.05.5WATER BASED15.02.199032941.5540.012.5WATER BASED20.02.199032941.5540.010.0WATER BASED20.02.199032941.5543.05.5WATER BASED16.02.199032941.5542.010.5WATER BASED20.02.199033651.5543.06.5WATER BASED14.02.1990 -
Palynologiske preparater i Sokkeldirektoratet
Palynologiske preparater i Sokkeldirektoratet Prøve dybdeDybde enhetPrøve typeLaboratorie2022.0[m]SWCSTATO2074.0[m]SWCSTATO2111.0[m]SWCSTATO2122.0[m]SWCSTATO2135.0[m]SWCSTATO2143.2[m]SWCSTATO2175.0[m]SWCSTATO2225.0[m]SWCSTATO2275.0[m]SWCSTATO2310.0[m]SWCSTATO2325.0[m]SWCSTATO2344.0[m]SWCSTATO2360.0[m]SWCSTATO2382.2[m]SWCSTATO2400.0[m]SWCSTATO2415.0[m]SWCSTATO2431.0[m]SWCSTATO2450.0[m]SWCSTATO2464.0[m]SWCSTATO2479.0[m]SWCSTATO2500.0[m]SWCSTATO2513.5[m]SWCSTATO2530.0[m]SWCSTATO2545.0[m]SWCSTATO2560.0[m]SWCSTATO2580.0[m]DCRRI2595.0[m]DCRRI2610.0[m]DCRRI2625.0[m]DCRRI2640.0[m]DCRRI2649.5[m]SWCSTATO2658.5[m]SWCSTATO2679.0[m]DCRRI2694.0[m]DCRRI2706.0[m]SWCSTATO2724.0[m]DCRRI2739.0[m]DCRRI2742.0[m]SWCSTATO2753.0[m]SWCSTATO2758.3[m]SWCSTATO2769.0[m]DCRRI2790.2[m]SWCSTATO2793.0[m]SWCSTATO2795.3[m]SWCSTATO2798.1[m]SWCSTATO2801.9[m]SWCSTATO2826.0[m]DCRRI2832.0[m]DCRRI2958.0[m]SWCSTATO3433.2[m]SWCSTATO3503.9[m]SWCSTATO