| ArcGIS REST Services Directory | Login | Get Token |
| Home > services > Factmaps > FactMapsED50UTM32 (OGCFeatureServer) > collections > 254 > items | API Reference |
| JSON |
General
Well 7324/10-1 was drilled on the Alpha structure in the Maud Basin on the Bjarmeland Platform. The main objective was to test the hydrocarbon potential in a prospect at the Base Anisian level (Top Klappmyss Formation). The secondary objective was to test sandstones below the Base Smithian level (Top Havert Formation). In addition the well should test the source rock potential in the Triassic, Base Snadd, and Base Kobbe Formations. Possible sand layers at 575 - and 695 m justified a shallow gas warning at these levels. Planned TD was at 3400 m in Late Permian.
Operations and results
Wildcat well 7324/10-1 was spudded with the semi-submersible rig Ross Rig 3 June 1989 and drilled to TD at 2919 m in the Early Triassic Havert Formation. TD was set approximately 500 m higher than prognosed due to lost circulation problems in the interval 1800 m to 2626 m. The well was drilled with seawater down to 558 m, with gypsum / polymer from 558 m to 2289 m, and with gel / lignosulphonate from 2289 m to TD. No shallow gas was encountered.
Minor gas was encountered in the Kobbe
Formation at 1607 m but the sandstones had very poor permeability and no RFT
samples were collected. The main target at Base Anisian/Klappmyss Formation at
1767 m in the prognosis, proved to be an intra Anisian seismic marker
encountered at 1822 m. At this level there was no reservoir developed, neither
was there any reservoir developed at the new Anisian seismic marker on 2272 m.
The secondary objective at top Havert Formation encountered at 2512 m had a
limited reservoir developed. Shows were recorded in the Snadd Formation from
617 m to 692 m and 1150 m to 1186 m. Organic rich shales were encountered in
Snadd, Kobbe, and Klappmyss Formations, but from organic geochemistry only a
thin sequences in the Snadd Formation could be classified as good, possibly
oil-prone source rocks. These were: a carbonaceous shale at 989 m and a thin
clay stone sequence at 1603 m t
wlbHistoryDateUpdated: 2016-07-06T00:00:00