| ArcGIS REST Services Directory | Login | Get Token |
| Home > services > Factmaps > FactMapsED50UTM32 (OGCFeatureServer) > collections > 254 > items | API Reference |
| JSON |
General
Well 7120/2-2 was designed to test the Mesozoic rocks on a down-faulted position, south of the Loppa High. Well 7120/1-2 about 12.5 km to the southwest had tested minor amounts of oil in the Early Cretaceous. This was a new play concept on the Barents Shelf related to structural/stratigraphic combination traps as a result of wedge sedimentation in conjunction with the Kimmeridgian tectonic phase. The main objectives of the well were to test the prospectivity of the Early Cretaceous fan systems (wedge I and II) in an optimal position, and to test the prospectivity of the Middle Jurassic Stø Formation. The pore pressure was expected to be normal throughout the well. Shallow gas warnings were given for two levels down to 1437 m. A fault with displacement less than 10 m was seen at the planned well location at depth ca 565 m.
Operations and results
Wildcat well 7120/2-2 was spudded with the semi-submersible rig Polar Pioneer on 27 January 1991 and drilled to TD at 2800 m in Early Jurassic sandstones of the Stø Formation. The well was drilled with spud mud down to 800 m and with KCl polymer mud from 800 m to TD. No shallow gas intervals were penetrated. No major problems were experienced while drilling the hole.
The first wedge, in the Kolmule
Formation, was penetrated at 1712 m. The second wedge, expected to be
sandstones of the Knurr Formation, was penetrated at 2125 m. Oil shows, mostly
weak, were recorded from the top of this wedge and down to ca 2700 m. The
strongest shows were recorded on a core from 2393 m to 2403 m. Geochemical
analyses proved a ten metre claystone sequence with excellent source rock
potential at 2120 m on top of the wedge; around 6% TOC and Hydrogen Index
around 480 mg HC/g TOC. Vitrinite reflectance in the sequence is in the range
0.55 to 0.60 % Ro and Tmax around 434 deg C, corresponding to early oil window
maturity. A second excellent source interval was penetrated in the Late
Jurassic Hekkingen Fo
wlbHistoryDateUpdated: 2016-07-06T00:00:00