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General
Well 8/10-2 was drilled on the Sørvestlandet High about 20 km east of the Ula Field. The primary objective of the well was Jurassic sandstones expected to be 122 m thick. Secondary objective was Paleocene sandstones.
Operations and results
Wildcat well 8/10-2 was spudded with the semi-submersible installation Nortrym on 5 February 1980 and drilled to TD at 2997 m in the Late Permian Zechstein Group.
The first samples to the surface were
from Miocene - Oligocene. They were badly contaminated with cement from the
casing shoe at 461 m. First clean formation samples were collected at 503 m and
they consisted of a soft grey brown clay with minor amounts of fine to medium
grained sand and occasional fossil frogs. This gave way at 570 m to a totally
argillaceous section, and soft grey-brown, slightly calcareous, claystone was
found. This became the dominant lithology down to the 13 3/8" casing point
at 1198 m. After casing point, cement contamination of samples occurred for
about 10 m. The claystone gave way to a grey-green-brown, soft, sticky clay,
which had occasional traces of carbonaceous material. Top Hordaland Group is
set at 1265 m. At 1471 m a thin hard white limestone occurred with an
associated drop in drilling rate from 61 m to 46 m per hour. Background gas
also decreased during this interval. After 1494 m the dominant lithology became
soft grey-brown clay, some sections of which were slightly calcareous.
Occasional fossil fragments and pyrite nodules were also found in this section.
There was a slow increase in the claystone content and by 1801 m a light grey
claystone had become the dominant lithology. This claystone was moderately
hard, slightly calcareous and micro micaceous; traces of dolomite and shelly
fragments were also found. By 1951 m the soft clays had disappeared completely
and were replaced by light grey and dark brown claystones, both soft to firm,
the light grey claystone being non-calcareous and the
wlbHistoryDateUpdated: 2016-07-06T00:00:00