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23.12.2024 - 01:26
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FLEKKEFJORD FM

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  • Generell informasjon

    Generell informasjon
    Attributt Verdi
    Litostrat. enhet
    Den litostratigrafiske enhetens offisielle navn.
    FLEKKEFJORD FM
    NPDID for litostrat. enhet
    Sokkeldirektoratets entydige nøkkel for litostratigrafiske enheter.
    43
    Nivå
    Angir den litostratigrafiske enhetens nivå. Lovlige verdier: GROUP, FORMATION, MEMBER.
    FORMATION
    Litostrat. enhet, forelder
    Den litostratigrafiske enhetens offisielle navn, refererer til forelder. Se også nivå. Vil være tom hvis Nivå = GROUP.
  • Nivå under

    Nivå under
    Litostrat. enhet
  • Beskrivelse

    Flekkefjord Formation

    Name
    From a town on the south-west coast of Norway. This formation was formerly included in the Valhall Formation of the Cromer Knoll Group (Deegan and Scull, 1977). The same unit was defined as the Flekkefjord Member by Rawson and Riley (1982), and is here elevated to formation status.
    Well type section
    Norwegian well 9/4-2 (Texaco) from 2155 m to 2208m, coord N 57°41'11.05", E 04°02'34.85" (Fig 3.38) .
    Well reference section
    Norwegian well 8/1-1 (Phillips) from 2379 m to 2425m, coord N 57°51'43.53", E 03° 12'27.64" (Fig 3.37) .
    Thickness
    In the type well it is 53 m, and in the reference well it is 46 m. This is also the approximate thickness in most wells within the Egersund Sub-Basin.
    Lithology
    The formation consists of dark grey shales which are variably carbonaceous, pyritic and may contain thin limestone stringers.
    Boundaries
    The lower boundary of the formation is clearly defined both on gamma and sonic logs by the contact with the more silty Sauda Formation . The upper boundary usually appears as a distinct log break, with higher radioactivity and higher interval transit times in the Flekkefjord Formation. In the Egersund Sub-Basin, which is situated closer to the source area, the boundary may be difficult to identify on logs.
    Distribution
    The formation is present in the Norwegian-Danish Basin. It is time-equivalent to the upper part of the Mandal Formation in the graben areas to the west and to the Fredrikshavn Unit C in the Danish sector to the east (Michelsen, 1978).
    Age
    Ryazanian.
    Depositional envitronment
    The Flekkefjord Formation was deposited in a marine, low-energy, basinal environment.
    Source
    • Vollset, J. and Doré, A. G. (eds.) 1984: A revised Triassic and Jurassic lithostratigraphic nomenclature for the Norwegian North Sea. NPD-Bulletin No. 3, 53 pp.
  • Brønnbaner som penetrerer

    Brønnbaner som penetrerer
    Brønnbane navn
    Dato for boreslutt
    Topp dyp [m]
    Bunn dyp [m]
    10.06.1969
    2598
    2643
    07.02.1972
    2379
    2425
    10.10.1966
    1628
    1658
    04.12.1982
    2025
    2075
    28.03.2013
    2176
    2205
    10.02.1976
    2103
    2123
    01.07.1969
    2775
    2793
    17.03.1980
    2657
    2667
    29.06.1975
    2807
    2835
    23.07.1971
    2574
    2607
    21.11.2011
    1934
    2060
    28.04.1987
    2483
    2550
    21.09.1987
    2381
    2447
    08.02.1990
    2625
    2799
    11.04.1994
    2730
    3075
    21.07.1995
    2595
    2706
    15.10.1996
    3297
    3800
    10.06.1997
    3062
    3182
    02.02.1998
    4762
    4995
    17.09.1999
    2710
    2823
    29.03.2010
    2101
    2180
    14.10.2019
    2530
    2602
    13.08.1996
    3758
    3865
    04.09.1986
    1446
    1488
    09.12.2005
    1970
    2072
    19.05.1968
    1985
    2047
    29.08.1970
    2155
    2208
    19.08.1972
    2200
    2250
    20.08.1977
    2310
    2395
    01.08.2006
    2300
    2387
    19.08.1971
    1957
    1966
    06.05.1969
    1905
    1948
    12.07.2015
    1842
    1937
    26.06.1976
    1275
    1335
    30.07.1992
    1298
    1386
    17.01.1971
    1367
    1393
    19.08.1969
    1655
    1672
    20.08.1995
    1875
    1980
    07.02.2011
    2020
    2116
    23.10.2021
    2297
    2346
    23.10.1973
    1933
    1954
    11.06.1974
    1933
    1954
    24.03.1969
    2515
    2544
    30.06.1968
    2083
    2101
    17.05.1976
    2410
    2422
    21.06.1972
    1902
    1946
    03.02.1980
    1957
    2010
    10.07.2009
    1992
    2017
    15.08.2009
    2142
    2175
    26.08.2009
    2101
    2134
    01.01.1980
    1991
    2046
    31.03.1974
    1609
    1650
  • Brønnbaner med kjerner

    Brønnbaner med kjerner
    Brønnbane navn
    Dato for boreslutt
    Kjernelengde [m]