DRAUPNE FM

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• General information

  General information

  Attribute	Value
  Lithostrat. unit The lithostratigraphic unit's official name.	DRAUPNE FM
  NPDID lithostrat. unit Norwegian Offshore Directorate's unique id for lithostratigraphic units.	28
  Level Indicates the lithostratigraphic unit's level. Legal values: GROUP, FORMATION, MEMBER.	FORMATION
  Lithostrat. unit, parent The parent lithostratigraphic unit's official name. See also level. Will be empty if Level = GROUP.	VIKING GP

• Level below

  Level below

  Lithostrat. unit

• Description

  Draupne Formation
  
  Name

  From a gold ring owned by Odin (the mythologic Viking God) which "dripped" 7 new rings, of the same weight as the original, every 9th day. The name is considered particularly appropriate in view of the Draupne Formation's role as a prolific hydrocarbon source in the Northern North Sea. It replaces the name "Kimmeridge Clay Formation" as used by Deegan and Scull (1977) in the Northern North Sea (see remarks).

  Well type section

  Norwegian well 30/6-5 (Norsk Hydro) from 2452 m to 2615 m, coord N 60°41 '20.6", E 02°57'11.09", (Fig 3.22) .

  Well reference sections

  UK wells 211/21-1A (Shell) from 2729.5 m to 2810 m, coord N 61°11'09.6", E 01°06'45", (Fig 3.18) . and 210/30-1 (Arpet), from 3330 m to 3717.5 m, coord N 61°04'05.4", E 00°54'14.4'', (Fig 3.20) .
  Norwegian wells 33/9-1 (Mobil) from 2443 m to 2450 m, coord N 61°15'07.5", E 01°50'25.8", (Fig 3.11) . 15/9-2 (Statoil) from 3397 m to 3478 m, coord. N 58°25'34.06", E 01°42'28.2", (Fig 3.26) . and 15/3-1 S (Elf) from 3947 m to 4754 m, coord N 58°50'57.00", E01°43'13.25", (Fig 3.19) .

  Thickness

  163 m in the type well, 80,5 m in 211/21-1A, 387,5 m in 210/30-1, 7 m in 33/9-1, 81 m in 15/9-2 and 807 m in 15/3-1 S .

  Lithology

  The formation consists of dark grey-brown to black, usually non-calcareous, carbonaceous, occasionally fissile claystone. It is characterized by very high radioactivity (often above 100 API units) which is a function of organic carbon content. It has anomalously low velocity, density and high resistivity. Minor limestone streaks and concretions occur throughout the formation. In addition interbedded sandstones and siltstones can cause a reduction in gamma ray response. The reference well 15/3-1 S is an atypical example of the Draupne Formation which has been chosen to illustrate these arenaceous intercalations.
  An informal three-fold subdivision has been identified, and is best recognizable along the basin rim areas where a middle high gamma ray zone separates two zones of lower gamma ray response (e.g. 210/30-1).

  Boundaries

  These are marked by distinct log breaks due to the very high gamma ray response and low velocity shown by the Draupne Formation.
  In basinal areas the formation generally has a diachronous contact with the Heather Formation . On marginal highs the formation onlaps pre-Upper Jurassic rocks. On the northern Horda Platform, Upper Jurassic sandstones of the Sognefjord Formation mark the base of the Draupne Formation.
  The upper boundary is often an unconformity or discontinuity, usually overlain by Cretaceous sediments which have a higher velocity and lower gamma ray response than the Draupne Formation. The importance and regional validity of this unconformity is under debate; see for example Rawson and Riley (1982).

  Distribution

  The formation is found in the East Shetland Basin, the Viking Graben and over the Horda Platform.

  Age

  The formation ranges from Oxfordian to Ryazanian in age.

  Depositional environment

  The Draupne Formation was deposited in a marine environment with restricted bottom circulation and often with anaerobic conditions. In places the formation may contain sandstones which are generally considered to be of turbiditic origin (De`Ath and Schuyleman, 1981; Harms et al, 1981).

  Remarks

  The Norwegian Lithostratigraphic Nomenclature Committee formally proposes abandonment of the name "Kimmeridge Clay Formation" for Upper Jurassic claystones encountered north of the Mid-North Sea High. The committee further recommends substitution of the names "Mandal Formation" (in the Central Graben area) and "Draupne Formation" (in the Northern North Sea) for intervals formerly termed Kimmeridge Clay Formation in those areas. The principal reasons for this revision are:

  1. distance from type area
  2. change in meaning of the term "Kimmeridge Clay Formation" from area to area

  The type area for the Kimmeridge Clay Formation is Kimmeridge Bay in Dorset, southern England (e.g. Arkell 1947). There the unit consists of dark, organic-rich claystones of Kimme-ridgian to Volgian age (using Boreal stage terminology). The term was extended by Rhys (1974 and 1975) into the Southern North Sea to describe a unit of comparable age overlying Oxfordian limestones (Corallian Formation) in type well 47/15-1. Deegan and Scull (1977) further extended the Kimmeridge Clay into the Northern North Sea to denote a generally highly radioactive, generally low velocity claystone sequence. The age range of the formation was broadened to include part of the Oxfordian and Ryazanian. It was remarked that the sediments in the Southern North Sea were less radioactive (less than 60 A.P.I, units compared with 100-200 A.P.I, units in the north). However, the low seismic velocities shown by both units were considered sufficient grounds to justify a correlation.
  Deegan and Scull did not specifically discuss the application of the term "Kimmeridge Clay" to the Central Graben region of the Central North Sea. Nevertheless, the name is in common usage there (e.g. Ofstad, 1983). It has, among other meanings, been taken to denote:

  1. all claystones of Upper Jurassic age regardless of log character, or more usually
  2. only the upper, most highly radioactive claystone unit of Volgian-Ryazanian age

  To the northwest, in the Norwegian-Danish Basin, a similar deposit is present (the Tau Formation , described in this publication). This unit has never been referred to the Kimmeridge Clay Formation but is nevertheless a typical Upper Jurassic organic shale. It is of Kimmeridgian — Volgian age and occupies a lower relative position in the overall Upper Jurassic shale sequence than the Central Graben "hot shales". (Table 3.4). A connection between the two deposits across the Southern Vestland Arch is most unlikely.
  In extending the Kimmeridge Clay Formation from the type area to the Northern North Sea (a distance of approximately 1300 km) the stratigraphic meaning of the name has varied considerably (Table 3.5). It is recognised that deposits of this type were laid down over a very wide area in intervals of the late Jurassic, the widespread deoxygenated bottom conditions reflecting the combined effect of paleo-geography with general sea level rise (e.g. Tyson et al., 1979; Ziegler 1982). However, acceptance of this overall regime should not alone be taken as a basis for lithostratigraphic classification. The nature and timing of the organic shales appears to have varied according to the evolution of individual basins. Use of the generic term Kimmeridge Clay Formation is a potential cause of mistaken correlation and does not further understanding of inter-basin relationships. Replacement of the name is a more palatable alternative to its continued extension northwards to the Arctic and Russia, where alternative nomenclature already exists.
  It therefore seems appropriate to limit the "Kimmeridge Clay Formation" of the North Sea to to the area south of the Mid-North Sea High, as described by Rhys (1974). The Norwegian Lithostratigraphic Nomenclature Committee proposes substitution of the name "Draupne Formation" for the "Kimmeridge Clay Formation" of the Northern North Sea as defined by De-egan and Schull (1977). It is suggested that the name "Mandal Formation" should be applied specifically to the "hot" shales of Volgian — Ryazanian age in the Central Graben region (Table 4), following the precedent set by Hamar et al., (1982).

  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.

• Wellbores penetrating

  Wellbores penetrating

  Wellbore name	Wellbore completion date	Top depth [m]	Bottom depth [m]
  6/3-1	01.02.1985	2963	2965
  6/3-2	10.03.1986	3008	3017
  15/2-1	24.02.1982	3878	4211
  15/3-1 S	06.07.1975	3947	4754
  15/3-2	24.01.1977	4236	4258
  15/3-2 R	27.11.1977	4236	4352
  15/3-3	09.08.1979	4017	4225
  15/3-4	30.03.1982	3675	3742
  15/3-5	13.05.1984	3808	3881
  15/3-7	01.09.2001	4049	4218
  15/3-7	01.09.2001	4230	4330
  15/3-7	01.09.2001	4398	4502
  15/3-8	11.04.2006	3933	4073
  15/3-8	11.04.2006	4392	4474
  15/3-9	13.08.2010	3975	4322
  15/3-11	09.08.2018	3717	3798
  15/3-12 S	20.01.2020	3573	3603
  15/5-1	08.04.1978	3492	3558
  15/5-2	16.12.1978	3759	3831
  15/5-3	07.12.1980	3665	3800
  15/5-7	07.09.2008	3666	3762
  15/5-7 A	13.10.2008	3728	3870
  15/6-2 R	01.08.1974	3438	3523
  15/6-4	16.08.1976	3157	3187
  15/6-5	29.11.1977	3361	3385
  15/6-6	09.06.1982	3398	3418
  15/6-7	08.06.1993	3233	3292
  15/6-8 S	05.04.1997	3090	3118
  15/6-9 A	13.06.2007	3487	3518
  15/6-9 B	23.07.2007	3582	3776
  15/6-9 S	27.05.2007	3511	3616
  15/6-10	06.04.2009	3461	3497
  15/6-11 A	13.03.2011	3967	4009
  15/6-11 S	19.12.2010	3612	3725
  15/6-12	09.02.2011	3669	3780
  15/6-13	15.05.2015	3401	3429
  15/6-13 A	03.06.2015	3673	3785
  15/6-13 B	29.06.2015	3603	3638
  15/6-14 S	26.12.2017	4526	4613
  15/6-15	02.06.2019	3389	3452
  15/6-16 S	28.06.2019	3783	3872
  15/8-1	07.01.1982	3535	3605
  15/8-2	21.10.2011	3763	3839
  15/9-1	30.05.1977	3377	3485
  15/9-2	17.06.1978	3396	3478
  15/9-3	03.04.1979	3364	3466
  15/9-4	14.06.1979	3274	3421
  15/9-5	11.04.1980	3432	3526
  15/9-6	07.09.1980	3470	3700
  15/9-7	29.04.1981	3412	3505
  15/9-8	25.05.1981	3290	3427
  15/9-9	14.07.1981	2625	2627
  15/9-10	07.11.1981	3004	3059
  15/9-11	23.12.1981	2752	2766
  15/9-12	27.02.1982	3400	3498
  15/9-13	27.05.1982	2741	2762
  15/9-14	27.06.1982	3176	3212
  15/9-15	01.08.1982	2751	2806
  15/9-17	30.03.1983	2712	2715
  15/9-18	02.03.1984	3108	3213
  15/9-19 A	09.11.1997	3667	3706
  15/9-19 B	02.02.1998	3768	3780
  15/9-19 SR2	25.07.1997	4307	4313
  15/9-19 SR	29.04.1993	4304	4310
  15/9-20 S	20.03.1994	3247	3249
  15/9-21 S	23.05.1998	4431	4700
  15/9-22	13.03.2006	3400	3548
  15/9-23	03.01.2010	2938	3038
  15/12-1	06.09.1975	3006	3027
  15/12-2	27.02.1976	2703	2765
  15/12-3	22.12.1980	2998	3142
  15/12-4	31.10.1984	2784	2892
  15/12-5	04.05.1986	2841	2888
  15/12-6 S	04.11.1990	2746	2834
  15/12-7 S	07.01.1991	3008	3025
  15/12-8	14.07.1991	2829	2838
  15/12-8 A	29.07.1991	2827	2838
  15/12-9 S	08.10.1992	3304	3385
  15/12-11 S	19.05.1997	3241	3322
  15/12-12	09.02.2001	2793	2861
  15/12-13	11.05.2003	2856	2944
  15/12-13 B	11.06.2003	2877	2939
  15/12-14	31.12.2003	2992	3015
  15/12-15	21.12.2004	2956	2962
  15/12-16 S	31.03.2006	2802	2834
  15/12-17 A	23.03.2007	3175	3356
  15/12-17 S	04.02.2007	3162	3246
  15/12-18 S	07.11.2007	3210	3351
  15/12-19	20.05.2008	2969	2973
  15/12-20 S	01.07.2008	3791	3797
  15/12-21	21.05.2009	2887	2916
  15/12-21 A	21.06.2009	3088	3285
  15/12-22	16.05.2010	2764	2799
  15/12-23	29.05.2010	2966	3013
  15/12-23 A	18.07.2010	4345	4428
  15/12-24 S	20.05.2015	2887	2898
  15/12-26	13.05.2021	2610	2650
  16/1-7	28.05.2004	2747	2918
  16/1-11	26.04.2010	2267	2318
  16/1-11 A	09.05.2010	2320	2396
  16/1-12	08.09.2009	1912	1913
  16/1-14	30.11.2010	2251	2392
  16/1-16	07.12.2012	2176	2357
  16/1-16 A	01.01.2013	2179	2424
  16/1-21 A	20.04.2015	2972	3155
  16/1-21 S	03.03.2015	2294	2462
  16/1-22 A	04.06.2015	2618	2740
  16/1-22 B	14.06.2015	2940	3049
  16/1-22 S	27.05.2015	2412	2487
  16/1-24	16.03.2015	2198	2223
  16/1-26 A	24.04.2016	4135	4601
  16/1-26 S	14.04.2016	4331	4787
  16/1-30 S	01.07.2019	1999	2004
  16/1-33 S	05.08.2020	2625	2766
  16/1-34 S	31.07.2021	2260	2261
  16/2-6	20.09.2010	1926	1931
  16/2-6	20.09.2010	1938	1942
  16/2-7	01.09.2011	1936	1940
  16/2-7 A	29.09.2011	2011	2014
  16/2-9 S	24.09.2011	1934	1935
  16/2-9 S	24.09.2011	1941	1949
  16/2-11	29.03.2012	1889	1890
  16/2-11 A	04.05.2012	2181	2185
  16/2-13 A	29.09.2012	2583	2597
  16/2-13 S	30.08.2012	1915	1925
  16/2-16	12.12.2012	1946	1952
  16/2-16 A	07.02.2013	2324	2327
  16/2-19	03.04.2014	1932	1945
  16/2-19 A	03.05.2014	2265	2283
  16/2-20 A	16.02.2014	2105	2125
  16/2-20 S	21.11.2013	2006	2027
  16/2-21	07.06.2013	1932	1935
  16/2-22 S	28.01.2017	1935	1950
  16/2-U-18	28.11.2016	1947	1954
  16/3-2	08.03.1976	1955	1975
  16/3-4	28.06.2011	1914	1926
  16/3-4 A	18.07.2011	2066	2077
  16/3-5	07.03.2013	1910	1918
  16/3-6	16.07.2013	1924	1940
  16/3-7	08.11.2013	1937	1950
  16/3-8 A	01.04.2014	1960	1966
  16/3-8 S	16.03.2014	1959	1965
  16/3-U-1	24.12.2016	1938	1950
  16/3-U-1 A	10.01.2017	2578	2763
  16/3-U-1 B	15.01.2017	2515	2598
  16/4-2	29.07.1990	2961	3113
  16/4-7	21.08.2013	2453	2489
  16/5-4	28.09.2013	1930	1931
  16/5-6	10.07.2016	2235	2241
  16/6-1	19.01.1968	2019	2051
  16/7-2	30.03.1982	2579	2668
  16/7-3	27.07.1982	2332	2333
  16/7-4	06.12.1982	2520	2521
  16/7-5	03.08.1984	2593	2594
  16/7-6	24.07.1997	2555	2556
  16/7-8 S	19.01.2003	2818	2821
  16/7-9	03.01.2011	2467	2500
  16/8-1	29.10.1976	2041	2073
  16/8-2	13.08.1980	2187	2238
  16/8-3 S	01.05.2013	2570	2656
  16/9-1	12.07.1968	2295	2360
  16/10-1	14.07.1986	2794	2853
  16/10-2	01.08.1991	2818	2853
  16/10-3	01.12.1996	2501	2521
  16/10-4	10.08.1998	2449	2474
  17/4-1	26.08.1968	2122	2217
  24/6-1	25.08.1985	4196	4205
  24/9-1	03.07.1976	4330	4800
  24/12-1 R	14.08.1978	4055	4140
  24/12-2	21.01.1982	4261	4640
  24/12-6 S	20.12.2010	4417	4788
  25/1-1	22.07.1971	4203	4280
  25/1-10	14.09.1988	4259	4312
  25/2-4	20.10.1975	3632	3640
  25/2-5	04.08.1976	3302	3316
  25/2-6	15.11.1977	3083	3137
  25/2-7	12.07.1982	3263	3275
  25/2-12	12.11.1988	3614	3634
  25/2-12 A	06.04.1989	3708	3710
  25/2-13	25.01.1990	3318	3329
  25/2-14	30.03.1991	3029	3060
  25/2-15	13.01.1993	3465	3471
  25/2-15 R	01.03.1993	3469	3475
  25/2-15 R2	11.04.1993	3469	3475
  25/2-16 S	13.09.2001	3711	3755
  25/2-18 A	19.10.2016	3585	3669
  25/2-18 B	30.10.2016	3828	3906
  25/2-18 C	17.11.2016	3663	3772
  25/2-18 S	11.09.2016	3298	3379
  25/2-19 A	08.10.2017	3589	3656
  25/2-23 S	01.04.2022	4320	4353
  25/3-1	05.09.1989	3016	3043
  25/4-1	09.12.1972	3171	3185
  25/4-5	26.03.1981	3592	3619
  25/4-6 S	24.08.1991	3571	3619
  25/4-6 SR	14.09.2003	3580	3628
  25/5-1	01.08.1987	2905	2955
  25/5-1 A	16.09.1987	3150	3225
  25/5-2	04.07.1989	3008	3131
  25/5-4	07.03.1991	2783	2860
  25/5-7	23.10.2010	2647	2677
  25/6-1	03.02.1986	2234	2256
  25/6-2	29.05.1992	2278	2301
  25/6-4 S	15.02.2012	2760	2798
  25/6-5 S	10.04.2015	2414	2426
  25/6-6 S	22.04.2019	2529	2570
  25/7-2	18.07.1990	4056	4119
  25/7-7	09.11.2019	4293	4385
  25/7-7	09.11.2019	4513	4559
  25/7-8 S	09.01.2020	2757	2770
  25/7-10	06.09.2022	4090	4161
  25/8-1	04.07.1970	1981	1987
  25/8-5 S	22.09.1994	2795	2822
  25/8-5 SR	03.08.1997	2795	2822
  25/8-7	12.08.1995	2293	2299
  25/8-8 S	24.09.1995	2563	2592
  25/8-9	28.01.1997	2383	2392
  25/9-1	22.04.1995	2167	2175
  25/9-2 S	03.08.2003	2163	2173
  25/9-3	20.09.2009	2093	2099
  25/9-4	27.02.2014	2308	2345
  25/10-4	18.01.1981	1961	1963
  25/10-4	18.01.1981	1982	1985
  25/10-4 R	13.06.1981	1961	1963
  25/10-4 R	13.06.1981	1982	1985
  25/10-6 S	22.03.1996	4240	4314
  25/10-8	07.04.1997	2354	2372
  25/10-8	07.04.1997	2450	2511
  25/10-8 A	27.04.1997	3090	3245
  25/10-8 A	27.04.1997	3420	3460
  25/10-9	27.07.2009	2886	2918
  25/10-11	10.08.2011	3991	4024
  25/10-12 S	18.01.2015	2114	2126
  25/10-15 S	02.08.2016	2416	2447
  25/10-15 S	02.08.2016	2483	2532
  25/10-16 A	09.08.2018	3464	3610
  25/10-16 B	18.08.2018	4485	4819
  25/10-16 C	26.08.2018	4002	4249
  25/10-16 S	30.07.2018	2456	2478
  25/10-16 S	30.07.2018	2580	2638
  25/10-17 S	10.02.2023	3565	3610
  25/11-1	09.07.1967	1980	1988
  25/11-5	08.05.1974	1950	1955
  25/11-15	25.12.1991	1978	1983
  25/11-17	22.03.1993	1985	1997
  25/11-19 S	18.05.1995	2168	2200
  25/11-19 SR	06.05.1997	2168	2200
  25/11-24	29.03.2007	2023	2029
  25/11-25 A	10.03.2008	2362	2372
  25/11-26	17.02.2013	2131	2164
  25/11-28	25.09.2015	1984	2005
  25/11-29 S	13.05.2019	2038	2050
  25/12-1	23.12.1973	2187	2244
  26/4-1	17.07.1987	2637	2725
  29/6-1	09.05.1982	3807	3915
  29/9-1	24.02.1984	3980	4049
  30/2-1	12.10.1982	3636	3657
  30/2-2	04.05.1985	3776	3824
  30/2-3	05.10.1992	3672	3709
  30/3-1 R	26.04.1982	3729	3748
  30/3-2 R	16.02.1981	2714	2731
  30/3-3	30.05.1983	2663	2763
  30/3-7 A	29.01.1998	6024	6052
  30/3-8 A	23.05.2000	4053	4054
  30/3-8 S	04.05.2000	4053	4054
  30/3-9	01.07.2000	3718	3735
  30/3-10 S	29.04.2009	3708	3725
  30/3-11 S	09.09.2022	4004	4125
  30/4-1	14.05.1979	4387	4485
  30/4-2	16.05.1980	3705	3726
  30/4-3 S	09.10.2016	4079	4131
  30/5-3 A	30.05.2009	4650	4704
  30/6-4	11.05.1981	2415	2430
  30/6-5	15.08.1981	2452	2593
  30/6-6	24.03.1982	2587	2700
  30/6-8	06.08.1982	2380	2446
  30/6-11	30.03.1983	3260	3264
  30/6-13	14.05.1983	2401	2424
  30/6-13 R	11.09.1986	2401	2424
  30/6-14	08.02.1984	2275	2334
  30/6-19	21.06.1986	2572	2677
  30/6-19 R	25.05.1994	2571	2676
  30/6-22	13.07.1988	2497	2628
  30/6-22 R	02.06.1994	2496	2627
  30/6-23	01.07.1990	2534	2607
  30/6-31 S	25.04.2020	2514	2536
  30/6-31 S	25.04.2020	2536	2582
  30/7-6 R	03.06.1978	3725	3738
  30/7-7	01.07.1979	3878	3924
  30/7-8	04.04.1981	3807	4066
  30/7-8 R	29.01.1982	3807	3841
  30/8-3	05.01.1998	3192	3197
  30/8-4 S	04.02.2009	3489	3520
  30/9-1	29.01.1983	2425	2470
  30/9-7	23.12.1988	2791	2805
  30/9-8 R	25.09.1989	2763	2771
  30/9-10	21.09.1990	2717	2756
  30/9-12	09.05.1991	2563	2609
  30/9-12 A	04.06.1991	2692	2734
  30/9-12 AR	11.07.2002	2696	2738
  30/9-14	14.05.1993	2968	2974
  30/9-16	08.08.1994	2652	2670
  30/9-18	11.04.1995	2595	2597
  30/9-19	22.10.1998	3087	3093
  30/9-19 A	21.12.1998	3180	3188
  30/9-20 S	11.02.2002	2750	2751
  30/9-21 A	15.06.2008	3582	3636
  30/9-21 S	30.04.2008	3597	3656
  30/9-22	10.03.2009	2790	2830
  30/9-23	21.08.2009	2214	2283
  30/9-25	20.09.2013	2823	2835
  30/9-26 S	22.11.2014	4076	4126
  30/9-27 S	25.08.2015	3460	3558
  30/9-28 S	26.02.2016	2883	2910
  30/9-B-18	25.09.1992	3258	3309
  30/9-B-18 A	23.10.1992	3258	3309
  30/10-5	01.05.1975	4162	4187
  30/10-6	09.11.1992	4344	4368
  30/11-3	14.03.1983	3285	3317
  30/11-4	24.07.1984	3262	3283
  30/11-5	09.01.1997	3082	3115
  30/11-6 S	02.07.2004	2961	2993
  30/11-7	03.02.2009	3722	3734
  30/11-9 A	08.01.2014	3424	3474
  30/11-9 S	13.11.2013	3126	3149
  30/11-11 A	07.04.2016	3647	3650
  30/11-11 S	19.03.2016	3095	3140
  30/11-12 A	20.05.2016	3698	3760
  30/11-12 S	04.05.2016	3148	3192
  30/12-1	07.03.1994	2795	2852
  30/12-2	27.08.2019	2918	3040
  31/1-1	15.02.2008	2051	2055
  31/1-2 A	29.01.2021	3140	3262
  31/1-2 S	12.01.2021	2862	2949
  31/2-1	09.11.1979	1414	1440
  31/2-1 R	09.11.1981	1415	1441
  31/2-2	23.04.1980	1470	1545
  31/2-2 R	06.10.1980	1470	1545
  31/2-6	17.10.1981	1481	1492
  31/2-7	14.06.1982	1535	1546
  31/2-8	18.08.1982	1821	1837
  31/2-9	01.10.1982	1544	1549
  31/2-10	31.10.1982	1565	1600
  31/2-14	21.06.1984	1532	1533
  31/2-17 A	31.01.1992	1682	1689
  31/2-17 B	14.02.1992	1686	1691
  31/2-17 BR	24.02.1993	1691	1696
  31/2-17 S	20.01.1992	1870	1872
  31/2-19 S	13.07.1996	2577	2738
  31/2-21 S	04.06.2014	2059	2180
  31/2-22 A	16.03.2021	2010	2051
  31/2-22 S	03.03.2021	1881	1907
  31/3-1	13.10.1983	1320	1352
  31/3-2	30.04.1984	1541	1567
  31/3-3	18.11.1984	1633	1747
  31/3-4	05.01.2014	1635	1658
  31/4-2	15.11.1979	2146	2171
  31/4-3	11.05.1980	2010	2018
  31/4-4	17.02.1981	2300	2365
  31/4-5	29.07.1981	2060	2070
  31/4-6	20.04.1982	2123	2136
  31/4-8	11.05.1986	2085	2088
  31/4-9	07.03.1987	2102	2118
  31/4-10	13.12.1995	2005	2025
  31/4-11	12.09.2000	2130	2201
  31/4-12	14.03.2005	2043	2089
  31/4-A-13 C	26.07.2022	5053	5115
  31/5-2	11.11.1983	1475	1516
  31/5-2 R	30.08.1984	1475	1516
  31/5-3	09.06.1984	1547	1555
  31/5-4 A	13.12.1990	1515	1621
  31/5-4 AR	18.07.1991	1515	1621
  31/5-4 AR2	05.09.2003	1522	1628
  31/5-4 S	10.10.1990	1515	1619
  31/5-6	25.07.2000	1795	1798
  31/5-7	06.03.2020	1892	1946
  31/6-1	28.10.1983	1313	1335
  31/6-2	11.12.1983	1322	1435
  31/6-2 R	08.09.1984	1322	1435
  31/6-3	26.12.1983	1370	1495
  31/6-5	21.05.1984	1388	1480
  31/6-6	29.07.1984	1392	1515
  31/6-8	25.05.1985	1412	1485
  31/6-8 R	22.09.1985	1412	1485
  31/7-1	22.06.2016	2143	2154
  31/7-1 A	14.07.2016	2355	2371
  31/7-2 A	27.07.2017	2568	2579
  31/7-2 S	08.07.2017	2177	2190
  31/7-3 A	18.01.2019	2712	2726
  31/7-3 S	16.12.2018	2559	2573
  31/8-1	24.07.2011	1999	2109
  31/11-1 S	28.06.2021	2191	2313
  32/2-1	01.07.2008	823	884
  32/4-1	04.12.1996	1109	1216
  32/4-2	21.09.2019	1083	1184
  32/4-3 S	26.10.2019	1101	1237
  33/5-2	18.11.1981	3900	3997
  33/6-1	06.07.1979	3537	3567
  33/6-2	02.01.1997	3466	3488
  33/6-2	02.01.1997	3551	3585
  33/6-3 S	24.07.2012	4084	4114
  33/6-5 S	16.10.2021	3294	3320
  33/9-1	04.06.1974	2448	2452
  33/9-3	14.11.1974	2405	2411
  33/9-5	01.01.1976	2556	2558
  33/9-6	31.08.1976	2939	2982
  33/9-8	18.02.1977	2664	2716
  33/9-10	12.06.1978	3260	3329
  33/9-11	28.08.1978	3096	3099
  33/9-12	03.08.1987	2452	2461
  33/9-14	09.04.1988	2674	2760
  33/9-15	08.06.1992	2742	2743
  33/9-15	08.06.1992	2841	2851
  33/9-16	20.01.1993	2683	2684
  33/9-16	20.01.1993	2748	2753
  33/9-17	04.05.1994	3038	3050
  33/9-17	04.05.1994	3131	3158
  33/9-18	20.12.1994	2846	2946
  33/9-18 A	24.01.1995	3200	3595
  33/9-20 S	09.09.2006	5211	5319
  33/9-21 A	30.04.2009	5662	5819
  33/9-21 B	11.06.2009	5662	5819
  33/9-21 S	19.03.2009	5728	5813
  33/9-22 S	17.09.2017	2669	2672
  33/9-22 S	17.09.2017	2721	2730
  33/12-2	23.08.1974	2480	2483
  33/12-4	17.07.1975	2671	2673
  33/12-7	27.04.1989	2927	2976
  33/12-8 S	26.04.2002	2636	2640
  33/12-9 S	08.01.2012	2984	3006
  33/12-10 S	23.10.2014	2944	3064
  34/4-3	30.03.1982	3526	3784
  34/4-10 R	18.04.2000	3790	3885
  34/4-11	10.01.2010	3840	3903
  34/4-13 S	02.01.2011	4422	4472
  34/4-14 S	19.05.2015	4265	4310
  34/4-15 A	12.08.2020	3532	3563
  34/4-16 S	31.03.2021	3398	3405
  34/6-1 S	28.08.2002	3412	3419
  34/7-15 S	03.09.1990	3440	3550
  34/7-15 S	03.09.1990	3555	3581
  34/7-15 S	03.09.1990	3590	3597
  34/7-15 S	03.09.1990	3601	3656
  34/7-15 S	03.09.1990	3667	3675
  34/7-15 S	03.09.1990	3677	3802
  34/7-15 S	03.09.1990	3805	3846
  34/7-15 S	03.09.1990	3848	3855
  34/7-21	11.12.1992	2545	2565
  34/7-21	11.12.1992	2569	2588
  34/7-21 A	12.02.1993	2905	2960
  34/7-21 A	12.02.1993	2962	3030
  34/7-23 A	20.05.1994	3246	3360
  34/7-23 S	03.04.1994	3102	3182
  34/7-24 S	24.03.1995	2928	3091
  34/7-26 A	26.02.1998	4195	4219
  34/7-26 SR	02.02.1998	4537	4610
  34/7-27	07.10.1998	2740	2757
  34/7-29 S	14.04.1998	2723	2774
  34/7-29 SR	17.03.1999	2722	2773
  34/7-31	13.04.2001	2506	2520
  34/7-31 A	25.04.2001	3090	3105
  34/7-35 S	22.07.2012	3152	3861
  34/7-36 S	17.09.2014	3396	3480
  34/7-37 S	02.12.2020	2655	2735
  34/8-1	08.03.1986	2764	2765
  34/8-2	17.11.1986	2897	2913
  34/8-3	14.09.1988	2827	2837
  34/8-3 A	31.10.1988	3003	3012
  34/8-4 S	09.06.1991	2902	2903
  34/8-5	01.04.1991	2830	2833
  34/8-6	03.11.1991	3477	3581
  34/8-7	16.07.1992	4584	4595
  34/8-7 R	10.02.1993	4584	4595
  34/8-8	24.08.1992	2901	2902
  34/8-8 R	09.03.1993	2900	2902
  34/8-9 S	28.12.1992	2908	2914
  34/8-11	08.02.1994	2853	2854
  34/8-12 S	09.12.2001	3048	3050
  34/8-13 A	13.05.2009	3349	3381
  34/8-13 S	26.06.2009	3865	3884
  34/8-14 A	01.12.2008	3471	3474
  34/8-14 B	25.01.2009	3477	3480
  34/8-14 C	08.12.2008	3506	3514
  34/8-14 D	10.02.2009	3545	3548
  34/8-14 S	21.10.2008	3182	3184
  34/8-15 S	19.02.2013	3439	3465
  34/8-17 S	14.03.2014	3857	3874
  34/8-18 S	22.02.2019	5692	5695
  34/8-19 S	20.06.2018	3108	3112
  34/10-2	08.12.1978	2882	2889
  34/10-5	02.01.1980	1857	1858
  34/10-6	22.01.1980	1995	1997
  34/10-16	11.04.1983	3017	3030
  34/10-16 R	27.09.1983	3014	3027
  34/10-18	30.08.1983	2351	2355
  34/10-21	22.10.1984	2920	3047
  34/10-23	13.10.1985	3862	3923
  34/10-32	13.07.1987	3092	3102
  34/10-32 R	10.08.1987	3092	3102
  34/10-33	15.12.1988	3028	3057
  34/10-33 A	03.02.1989	3034	3077
  34/10-33 B	10.07.1989	3012	3045
  34/10-33 C	01.08.1989	3012	3045
  34/10-33 CR	27.04.1990	3012	3045
  34/10-35	01.07.1992	3791	3877
  34/10-36	13.07.1992	3026	3125
  34/10-37 A	03.04.1995	2587	2593
  34/10-39 S	20.06.1995	2482	2505
  34/10-42 S	19.09.1999	3960	4008
  34/10-43 S	11.04.2001	5360	5675
  34/10-45 S	08.01.2002	7486	7496
  34/10-47 A	14.11.2002	2414	2431
  34/10-47 S	02.11.2002	2458	2489
  34/10-47 S	02.11.2002	3923	3964
  34/10-52 A	06.08.2011	3228	3230
  34/10-53 A	01.06.2011	4129	4184
  34/11-1	25.10.1994	3917	3996
  34/11-2 S	17.05.1996	3697	3699
  34/11-3	16.01.1997	3960	4010
  34/11-4	14.04.1999	3904	4018
  34/11-5 S	03.07.2006	6587	6796
  34/11-6 S	26.01.2017	6538	6599
  34/12-1	30.04.2008	4172	4218
  35/3-6	02.04.2002	3155	3335
  35/4-3	17.05.2022	4100	4116
  35/7-1 S	15.08.2011	3924	3974
  35/8-1	24.01.1981	3186	3200
  35/8-2	21.05.1982	3079	3204
  35/8-3	15.10.1988	3318	3395
  35/8-4	10.08.1999	3465	3591
  35/8-5 S	20.07.2003	3239	3334
  35/8-6 A	14.05.2016	3440	3481
  35/8-6 S	22.04.2016	3610	3687
  35/9-2	03.04.1991	2058	2095
  35/9-5	07.02.2010	3254	3376
  35/9-7	14.04.2012	2594	2610
  35/9-8	11.04.2013	2714	2730
  35/9-10 A	16.01.2014	2725	2728
  35/9-10 S	26.11.2013	3040	3054
  35/9-12 S	26.12.2014	2921	2943
  35/9-14	02.03.2018	3387	3406
  35/9-14 A	29.03.2018	3650	3702
  35/10-1	16.01.1992	3098	3146
  35/10-2	22.08.1996	3921	4018
  35/10-4 A	12.11.2018	3526	3757
  35/10-4 S	10.10.2018	3221	3353
  35/10-7 A	27.12.2021	2982	2983
  35/10-7 S	11.12.2021	2877	3014
  35/11-2	04.12.1987	2927	3011
  35/11-3 S	09.09.1989	2821	3081
  35/11-4	29.12.1990	1966	1984
  35/11-4 R	27.01.1992	1976	1994
  35/11-5	03.11.1991	2658	2875
  35/11-6	20.04.1992	2902	3061
  35/11-7	29.09.1992	1793	1796
  35/11-8 S	11.05.1996	2686	2789
  35/11-9	01.05.1997	2389	2539
  35/11-10	23.06.1997	1965	1971
  35/11-10 A	14.07.1997	2203	2293
  35/11-11	22.05.1998	2469	2540
  35/11-12	14.05.2000	2891	3130
  35/11-13	28.05.2005	2902	3013
  35/11-14 S	07.12.2006	2898	3031
  35/11-15 S	28.06.2007	2697	2829
  35/11-16 S	18.03.2014	3165	3329
  35/11-18	27.09.2015	3037	3098
  35/11-18 A	16.12.2015	3088	3160
  35/11-20 A	07.08.2016	3474	3568
  35/11-20 B	15.09.2016	3812	3871
  35/11-20 S	19.06.2016	3032	3087
  35/11-22 S	02.02.2019	2783	3030
  35/11-23 A	21.11.2019	2216	2255
  35/11-23 A	21.11.2019	2417	2499
  35/11-24 A	28.08.2020	3016	3331
  35/11-24 B	16.09.2020	3044	3331
  35/11-24 S	09.08.2020	2789	3003
  35/11-25 A	04.06.2021	2633	2917
  35/11-25 S	14.05.2021	2556	2795
  35/12-1	24.04.1992	2361	2398
  35/12-3 S	16.02.2011	2019	2033
  35/12-4 A	17.07.2011	2836	2967
  35/12-5 S	19.06.2015	2853	2868
  35/12-6 A	30.06.2018	3027	3058
  35/12-6 S	14.06.2018	2903	2918
  35/12-7	25.07.2018	2019	2020
  36/1-2	27.10.1975	2875	2900
  36/1-4 S	30.01.2022	2766	2786
  36/7-2	22.09.1997	880	917
  36/7-3	06.01.2002	2854	2907
  6201/11-2	11.03.1991	3339	3544

• Wellbores with cores

  Wellbores with cores

  Wellbore name	Wellbore completion date	Core length [m]
  15/3-1 S	06.07.1975	20
  15/3-9	13.08.2010	23
  15/9-5	11.04.1980	1
  15/9-15	01.08.1982	1
  15/9-17	30.03.1983	1
  16/1-12	08.09.2009	1
  16/1-14	30.11.2010	19
  16/1-21 S	03.03.2015	13
  16/2-6	20.09.2010	4
  16/2-7	01.09.2011	4
  16/2-7 A	29.09.2011	2
  16/2-11 A	04.05.2012	4
  16/2-13 A	29.09.2012	10
  16/2-13 S	30.08.2012	7
  16/2-16	12.12.2012	5
  16/2-16 A	07.02.2013	3
  16/2-19	03.04.2014	14
  16/2-19 A	03.05.2014	18
  16/2-20 A	16.02.2014	18
  16/2-20 S	21.11.2013	21
  16/2-21	07.06.2013	3
  16/2-22 S	28.01.2017	13
  16/3-4	28.06.2011	12
  16/3-4 A	18.07.2011	10
  16/3-5	07.03.2013	6
  16/3-6	16.07.2013	14
  16/3-7	08.11.2013	13
  16/5-4	28.09.2013	0
  16/7-5	03.08.1984	1
  24/9-1	03.07.1976	18
  25/10-8 A	27.04.1997	92
  25/10-12 S	18.01.2015	12
  25/10-16 S	30.07.2018	18
  25/11-28	25.09.2015	13
  30/7-8	04.04.1981	10
  30/9-10	21.09.1990	14
  30/9-14	14.05.1993	5
  31/2-2	23.04.1980	18
  31/2-10	31.10.1982	13
  31/3-1	13.10.1983	1
  31/3-2	30.04.1984	2
  31/4-5	29.07.1981	7
  31/4-6	20.04.1982	4
  31/4-9	07.03.1987	11
  31/4-10	13.12.1995	20
  31/4-11	12.09.2000	39
  31/5-2	11.11.1983	10
  31/5-3	09.06.1984	5
  31/6-2	11.12.1983	0
  31/6-3	26.12.1983	0
  31/6-5	21.05.1984	10
  31/7-1 A	14.07.2016	9
  31/7-2 A	27.07.2017	5
  31/7-2 S	08.07.2017	13
  31/7-3 S	16.12.2018	8
  33/6-2	02.01.1997	1
  33/9-8	18.02.1977	28
  33/9-14	09.04.1988	64
  33/9-15	08.06.1992	1
  33/9-16	20.01.1993	2
  33/9-17	04.05.1994	11
  33/9-18 A	24.01.1995	6
  33/12-10 S	23.10.2014	26
  34/4-3	30.03.1982	18
  34/7-21	11.12.1992	39
  34/7-21 A	12.02.1993	16
  34/7-23 A	20.05.1994	44
  34/7-23 S	03.04.1994	30
  34/7-26 A	26.02.1998	21
  34/7-26 SR	02.02.1998	62
  34/7-27	07.10.1998	14
  34/7-29 S	14.04.1998	2
  34/8-6	03.11.1991	9
  34/8-8	24.08.1992	2
  34/10-18	30.08.1983	4
  34/10-36	13.07.1992	24
  35/11-4	29.12.1990	6
  35/11-12	14.05.2000	10
  35/11-22 S	02.02.2019	4