Faktasider Sokkeldirektoratet
Faktasider Sokkeldirektoratet
sodir.no          English
04.11.2024 - 01:25
Tidspunkt for siste synkronisering med Sokkeldirektoratets interne systemer

TAU FM

Eksport: PDF ikon PDF
  • Generell informasjon

    Generell informasjon
    Attributt Verdi
    Litostrat. enhet
    Den litostratigrafiske enhetens offisielle navn.
    TAU FM
    NPDID for litostrat. enhet
    Sokkeldirektoratets entydige nøkkel for litostratigrafiske enheter.
    164
    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

    Tau Formation

    Name
    From a village within the Boknfjord area in Rogaland. The formation represents only the lowermost, radioactive part of the Børglum Member as defined by Deegan and Scull (1977).
    Well type section
    Norwegian well 9/4-3 (Conoco) from 2400 m to 2437 m, coord N 57°36'54.5", E 04°18'57.7" (Fig 3.36) .
    Well reference section
    Norwegian well 8/1-1 (Phillips) from 2551 m to 2606 m, coord N 57°51'43.53'', E 03°12'27.64" (Fig 3.37) .
    Thickness
    37 m in the type well and 55 m in the reference well.
    Lithology
    The Tau Formation consists of dark grey to black, pyritic, fissile, organic-rich slightly to non-calcareous shales.
    Boundaries
    This formation is highly radioactive and the boundaries are characterized by prominent log breaks. The underlying Egersund Formation is less radioactive and has a lower interval transit time than the Tau Formation. The upper boundary may be more gradational but shows a marked increase in radioactivity compared to the overlying unit.
    Distribution
    The formation is confined to the central part of the type area of the Boknfjord Group , and grades laterally into the Børglum unit southwards and eastwards.
    Age
    Kimmeridgian to Early Volgian.
    Depositional environment
    The Tau Formation was deposited in an anaerobic marine environment with high organic productivity and restricted bottom water circulation.
    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]
    07.02.1972
    2551
    2606
    10.10.1966
    1831
    1890
    04.12.1982
    2200
    2290
    25.07.1977
    2351
    2397
    28.03.2013
    2260
    2314
    23.07.1971
    2661
    2663
    21.11.2011
    2262
    2332
    28.04.1987
    2993
    3097
    21.09.1987
    2957
    3062
    08.02.1990
    3098
    3188
    11.04.1994
    3875
    3993
    21.07.1995
    3021
    3078
    15.10.1996
    4627
    4714
    10.06.1997
    3683
    3784
    02.02.1998
    5689
    5769
    17.09.1999
    3551
    3669
    29.03.2010
    2492
    2574
    14.10.2019
    2825
    2932
    13.08.1996
    4478
    4560
    04.09.1986
    1686
    1749
    09.12.2005
    2503
    2607
    19.05.1968
    2200
    2251
    29.08.1970
    2396
    2435
    19.08.1972
    2400
    2437
    20.08.1977
    2598
    2668
    01.08.2006
    2603
    2654
    19.08.1971
    1993
    2005
    12.07.2015
    2215
    2245
    30.07.1992
    1486
    1539
    17.01.1971
    1451
    1464
    12.09.2007
    1107
    1141
    31.10.1967
    2124
    2142
    31.10.1967
    2152
    2165
    23.07.1973
    2127
    2202
    20.08.1995
    2311
    2339
    07.02.2011
    2489
    2542
    23.10.2021
    2393
    2417
    23.10.1973
    2165
    2205
    11.06.1974
    2165
    2205
    24.03.1969
    2640
    2675
    30.06.1968
    2180
    2195
    17.05.1976
    2495
    2513
    21.06.1972
    2167
    2215
    03.02.1980
    2236
    2288
    10.07.2009
    2149
    2198
    15.08.2009
    2358
    2438
    26.08.2009
    2309
    2377
    01.01.1980
    2277
    2319
    31.03.1974
    1747
    1800
  • Brønnbaner med kjerner

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