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General
Well 7120/7-2 is located in the Snøhvit Field area. The primary of the well was to test possible hydrocarbon accumulations in sandstones of Middle to Early Jurassic age.
Operations and results
Wildcat well 7120/7-2 was spudded with the semi-submersible rig West Vanguard on 26 May 1983 and drilled to TD at 2523 m, 5 meters into Late Triassic rocks. Due to boulders at the spud location the rig was moved 11 m north and respudded. A sand body with shallow gas was encountered at 378 m to 382.5 m and it was decided to set the 20" casing shoe above this sand. After setting this casing the rig was shut down due to strike from 3 June at 2400 hrs to 18 June at 1125 hrs. The well was drilled using gel mud down to 815 m, with gypsum/polymer mud from 815 m to 1515, and dispersed to a lignosulphonate (Unical) mud from 1515 m to TD.
Hydrocarbon accumulations were discovered
in the Middle Jurassic Stø Formation sandstone sequence from 2149.5 m down to a
gas/water contact at 2228 m. Shows were recorded below 1809 m in the Cretaceous
Kolje Formation. Organic geochemical analyses showed that TOC increases down
through the Cretaceous, but generally the Cretaceous mudstones were regarded as
immature, poor source rocks with a primary potential for gas. Entering into the
silty shales and mudstones of the Late Jurassic Hekkingen Formation at 2107 m
TOC increases abruptly above 3%. TOC continues to increase to 9 % at the base
of the Hekkingen Formation. These shales are potentially very good source rocks
for gas and condensate above ca 2120 metres and rich sources for light oil and
gas below this depth. Maturity evaluation was difficult due to reworked
material and cavings, but most likely the well is immature all through,
possibly marginally mature below ca 2000 m. Five cores were cut in the
sandstones from 2168 m to 2244 m. Four RFT samples were taken. Sample 1 was
taken at 2150 m (gas, mud filtrate and film of condensate), sample 2 at 2
wlbHistoryDateUpdated: 2016-05-19T00:00:00