NORWAY · WELLBORES · NPDID 6630

8/10-4 S

Exploration · Wildcat · P&A · Oil · Centrica Resources (Norge) AS · Oda · PL 405

2 documents: reports, logs, and plots →

8/10-4 S was cored 3 times, 69.4 m in all between 2,958 and 3,027.6 m.

3
cores
69.4
metres cored in all
19
palynology slides made from core
1
test or fluid sample across a core

SODIR FACTPAGES · PLACED BY DEPTH IN THIS WELLBORE

Core log

DEPTHFORMATIONCOREPHOTOSTHINSEC.SLIDESTESTS2,9582,9852,9602,9652,9702,9752,980Ula Fm, 2,958 to 2,985 mUla FmCore 1, 2,958 to 2,985 m. Open the core.Core 127 m3,003.82,9902,9953,000Ula Fm, 2,985 to 3,003.5 mUla FmSkagerrak Fm, 3,003.5 to 3,003.8 mCore 2, 2,985 to 3,003.8 m. Open the core.Core 218.8 m3,027.6 m3,0103,0153,0203,025Skagerrak Fm, 3,004 to 3,027.6 mSkagerrak FmCore 3, 3,004 to 3,027.6 m. Open the core.Core 323.6 m

Core by core

CoreTopBaseLengthInPhotosThin sectionsSlides from coreTestsSample available
Core 1 →2,958 m2,985 m27Ula Fm——21Yes
Core 2 →2,985 m3,003.8 m18.8Ula Fm, Skagerrak Fm——5—Yes
Core 3 →3,004 m3,027.6 m23.6Skagerrak Fm——12—Yes

Seeing the cores themselves

The cores are held by the Norwegian Offshore Directorate in its Geobank, which has rooms for viewing and sampling by booking.

The Directorate's Geobank: viewing and sampling →

About this data

Norwegian Offshore Directorate (Sodir) FactPages, mirrored nightly and used under the Norwegian Licence for Open Government Data (NLOD). The Directorate files each core as an interval and nothing against it. The log places everything else on file for the wellbore inside the core whose interval contains its depth: photographs by the interval in their title, thin sections and slides by their depth, tests by overlap, formations by this wellbore's own tops. Core depths are driller's depths, so a mark at the very edge of a core can belong to its neighbor. Only slides made from core are shown; slides from cuttings at the same depths are on the Samples tab.

Developers: this page as JSON is GET /v1/data/norway/wells/6630/cores, documented in the API reference.