STATFJORD GP

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• Generell informasjon

  Generell informasjon

  Attributt	Verdi
  Litostrat. enhet Den litostratigrafiske enhetens offisielle navn.	STATFJORD GP
  NPDID for litostrat. enhet Sokkeldirektoratets entydige nøkkel for litostratigrafiske enheter.	157
  Nivå Angir den litostratigrafiske enhetens nivå. Lovlige verdier: GROUP, FORMATION, MEMBER.	GROUP

• Nivå under

  Nivå under

  Litostrat. enhet
  EIRIKSSON FM
  NANSEN FM
  RAUDE FM

• Beskrivelse

  Statfjord Group
  
  Name

  Named by Deegan and Scull (1977).

  Well type section

  Norwegian well 33/12-2 (Mobil), from 2700 m to 2951 m, coord N 61°13'31.18", E 01°51'25.97" (Fig 3.6) .

  Well reference sections

  UK well 211/24-1 (Conoco) from 3112 m to 3434 m, coord N 61°11'46.2'', E 01°46'26.3" (Fig 3.7) . Norwegian wells 30/6-1 (Statoil), from 2712 m to 3003 m, coord N 60°33'15.10'', E 02°46'38.36" (Fig 3.8) . and 25/2-5 (Elf) from 3652 m to 3847 m, coord N 59°48'01.40", E 02°28'18.30" (Fig 3.9) .

  Thickness

  251 m in the type well, 322 m in UK well 211/24-1, 291 m and 195 m in Norwegian wells 30/6-1 and 25/2-5 respectively. The group is thinner on the crest of fault blocks and thicker on the downthrown side. It attains its fullest development in the central part of the Viking Graben. To the west, e.g. in the area of the Cormorant Field, only the upper formation is present and this is reduced to a sandstone only a few meters in thickness. To the east, toward the bounding fault zone of the Fennoscandian Shield, the group is reduced to tens of meters in thickness.

  Lithology

  The group exhibits a transition from continental to shallow marine sediments. In the type well area it is a transitional "coarsening upward" sequence in the basal parts consisting of grey, green and sometimes red shale interbedded with thin siltstones, sandstones and dolomitic limestones. Above are massive white to grey sandstone bodies interbedded with greenish-grey to red-brown shales. The top part of the group consists of thick, white to grey, fossiliferous and glauconitic sandstones. On the Horda Platform, east of the Viking Graben, the group consists of massive, white, fine to coarse grained sandstones inter-bedded with light grey, and sometimes red, silty micaceous, lignitic shales. Towards the east the frequency of black, coaly shales and coal layers increases.

  Boundaries

  The base of the Statfjord Group is very difficult to define, and different operators have established different boundaries. In the type well area the proposed boundary marks the base of the thin transitional unit (coarsening upward sequence), which marks the passage from the more shaly Lunde Formation of the Hegre Group to the massive sandstones of the Statfjord Group. It should be emphasized that this transition can only be clearly recognized in some wells in the area of the Brent and Statfjord fields. Towards the east, e.g. in the Viking Graben and the Horda Platform, the lower boundary is chosen at the base of the lowest massive sandstone unit before passing downwards into dominantly red brown shales. This boundary is often associated with a sonic log break. Lervik (2006) proposed to place the boundary between the Statfjord Group and the Hegre Group at the turning point of a fining upward mega-sequence of the Lunde Formation with the coarsening-upward sequence of the Statfjord Group which very often coincides with a sudden upward decrease of sonic log velocity. The top of the group is at the contact between the uppermost medium to coarse-grained calcareous sandstones and the dark shales and siltstones of the overlying Dunlin Group . It should be noted that the top part of the calcareous sandstones in the UK sector (e.g. in the Brent Field and in UK part of the Statfjord Field , passes laterally into calcareous shales and siltstones in the Norwegian sector. The group boundary, being a lithological one, however, is placed at the top of the sandstones, regardless of age.

  Distribution

  The Statfjord Group can be recognized in the entire area between East Shetland Platform to the west and the bounding fault zone of the Fennoscandian Shield to the east. The group is identified in the Viking Graben as far south as Norwegian blocks 25/8 and 11, e.g. in wells 25/8-1 and 25/8-2 (Esso).

  Age

  The formation ranges in age from Rhaetian to Sinemurian.

  Depositional environment

  The lower transitional unit in the type well area appears to represent an upward passage from the dominantly continental deposits of the Lunde Formation of the Hegre Group to lower alluvial plain and braided stream deposits which make up most of the Statfjord Group (Kirk, 1979, Chauvin and Valachi, 1980). Towards the top of the group coarse sandstones with pebble beds, crossbedding and channel structures appear to have been deposited in a coastal environment. The uppermost sandstones are relatively structureless but the presence of marine fossils and glauconite suggests a shallow marine environment (Deegan and Scull, 1977).

  Subdivision

  The Statfjord Group is divided in the type well area ( Statfjord Field ) into three formations, the Raude Formation (base) the Eiriksson Formation and the Nansen Formation (top) (Deegan and Scull, 1977). It should be emphasized that this subdivision can only be applied west of the Viking Graben. Even within this area application of the subdivision is often difficult. No workable subdivision has been established in the few well penetrations of the Statfjord Group east of the Viking Graben. For definition and detailed description of the formations (former members) of the Statfjord Group, see Deegan and Scull (op. cit). Lervik (2006) proposed to elevate the Statfjord Formation to group level and the members Raude, Eiriksson and Nansen to formation level.

  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.
  • Lervik, K.-S. 2006: Triassic lithostratigraphy of the Northern North Sea Basin. Norwegian Journal of Geology, Vol. 86, pp. 93-116.

• Brønnbaner som penetrerer

  Brønnbaner som penetrerer

  Brønnbane navn	Dato for boreslutt	Topp dyp [m]	Bunn dyp [m]
  15/6-2 R	01.08.1974	3682	4779
  15/6-11 A	13.03.2011	4291	4305
  15/6-11 S	19.12.2010	3970	4042
  16/1-20 A	21.10.2013	3049	3060
  16/1-26 S	14.04.2016	4835	4896
  16/1-33 S	05.08.2020	3006	3068
  16/1-34 S	31.07.2021	2261	2383
  16/1-35 S	28.02.2023	3098	3177
  16/2-7	01.09.2011	1985	1986
  16/2-7 A	29.09.2011	2039	2041
  16/2-8	19.08.2011	1949	1951
  16/2-15	13.01.2013	1945	1969
  16/2-16	12.12.2012	1966	1999
  16/2-16 A	07.02.2013	2356	2385
  16/2-17 S	20.05.2013	1913	2020
  16/2-19	03.04.2014	1945	1952
  16/2-20 S	21.11.2013	2027	2038
  16/2-21	07.06.2013	1948	1965
  16/2-U-18	28.11.2016	1981	2057
  16/4-10	07.03.2016	2583	2668
  24/6-1	25.08.1985	4915	4937
  25/2-4	20.10.1975	4084	4261
  25/2-5	04.08.1976	3652	3847
  25/2-6	15.11.1977	3504	3705
  25/2-12	12.11.1988	3990	4102
  25/2-13	25.01.1990	3696	3887
  25/2-14	30.03.1991	3521	3623
  25/3-1	05.09.1989	3870	3922
  25/4-1	09.12.1972	3292	3513
  25/4-5	26.03.1981	3949	4127
  25/4-6 S	24.08.1991	4129	4170
  25/4-6 SR	14.09.2003	4138	4179
  25/5-1	01.08.1987	3232	3374
  25/5-3	26.03.1990	2613	2752
  25/5-4	07.03.1991	3052	3185
  25/6-1	03.02.1986	2417	2503
  25/6-6 S	22.04.2019	2927	3170
  25/7-8 S	09.01.2020	2976	3120
  25/8-1	04.07.1970	1987	2158
  25/8-2	01.10.1975	2399	2578
  25/8-5 S	22.09.1994	3040	3338
  25/8-5 SR	03.08.1997	3040	3338
  25/8-11	02.12.1997	1891	1994
  25/8-12 A	19.06.1999	1946	2028
  25/8-12 S	09.06.1999	1906	2040
  25/8-13	20.11.2001	2237	2276
  25/8-14 S	22.09.2003	2540	2825
  25/8-15 S	07.08.2004	4698	4804
  25/8-16 S	13.05.2009	2495	2550
  25/8-19 A	19.03.2020	2211	2483
  25/8-19 S	30.12.2019	2245	2434
  25/8-20 B	28.05.2021	2276	2438
  25/8-20 S	10.05.2021	2313	2504
  25/8-21 S	20.06.2021	2310	2391
  25/8-22 S	20.07.2021	2114	2325
  25/9-1	22.04.1995	2301	2415
  25/9-3	20.09.2009	2218	2267
  25/10-1 R	03.08.1970	1963	2091
  25/10-4	18.01.1981	2003	2154
  25/10-4 R	13.06.1981	2003	2154
  25/10-9	27.07.2009	2961	2985
  25/10-10	02.04.2010	2072	2173
  25/10-11	10.08.2011	4146	4351
  25/10-12 S	18.01.2015	2241	2439
  25/10-13 S	19.06.2015	2475	2555
  25/10-14 S	17.01.2016	2341	2410
  25/10-16 A	09.08.2018	3627	3653
  25/10-16 C	26.08.2018	4277	4305
  25/10-17 S	10.02.2023	3944	3978
  25/11-1	09.07.1967	1988	2109
  25/11-5	08.05.1974	1955	2087
  25/11-15	25.12.1991	1983	2035
  25/11-17	22.03.1993	1997	2146
  25/11-19 S	18.05.1995	2200	2250
  25/11-19 SR	06.05.1997	2200	2250
  25/11-23	28.05.1999	1975	2014
  25/11-24	29.03.2007	2029	2117
  25/11-25 A	10.03.2008	2372	2448
  25/11-26	17.02.2013	2184	2235
  25/11-28	25.09.2015	2005	2147
  25/11-29 S	13.05.2019	2050	2147
  26/4-1	17.07.1987	3308	3665
  29/3-1	15.09.1986	4389	4427
  29/6-1	09.05.1982	4729	4786
  29/9-1	24.02.1984	4640	4703
  30/2-1	12.10.1982	4110	4243
  30/2-3	05.10.1992	4288	4325
  30/2-4 S	09.08.2008	4309	4325
  30/3-1 R	26.04.1982	4227	4421
  30/3-2 R	16.02.1981	3228	3567
  30/3-3	30.05.1983	3387	3419
  30/3-4	12.06.1985	3232	3287
  30/3-4 R	18.11.2001	3234	3287
  30/3-5 S	19.06.1992	4538	4724
  30/3-6 S	06.03.1994	6027	6085
  30/3-7 B	04.08.1998	4611	4948
  30/3-7 BR	17.11.2001	4611	4948
  30/3-7 S	12.12.1995	5271	5322
  30/3-10 S	29.04.2009	4034	4168
  30/4-2	16.05.1980	4337	4670
  30/6-1	22.09.1979	2712	3003
  30/6-2	11.12.1979	2568	2808
  30/6-3	07.03.1980	2884	2940
  30/6-5	15.08.1981	3223	3550
  30/6-7	24.08.1982	3152	3236
  30/6-8	06.08.1982	3532	3600
  30/6-9	16.12.1982	3046	3389
  30/6-9 R	12.05.1990	3044	3387
  30/6-11	30.03.1983	3893	4001
  30/6-14	08.02.1984	2784	2900
  30/6-15	05.09.1984	3241	3548
  30/6-16	21.01.1985	2960	3224
  30/6-17 A	18.03.1986	2632	2686
  30/6-17 R	04.02.1986	2563	2650
  30/6-18	23.11.1985	3121	3670
  30/6-19	21.06.1986	3255	3301
  30/6-19 R	25.05.1994	3254	3300
  30/6-20	13.04.1986	2937	3046
  30/6-21	09.04.1987	3052	3100
  30/6-22	13.07.1988	3290	3336
  30/6-22 R	02.06.1994	3289	3335
  30/6-23	01.07.1990	3163	3210
  30/6-24 S	06.12.1991	3682	3940
  30/6-26	07.10.2001	2669	2865
  30/6-27	30.10.2001	3101	3432
  30/6-28 S	29.03.2012	2483	2754
  30/6-29 S	03.03.2015	5735	5765
  30/7-7	01.07.1979	4884	5127
  30/7-8 R	29.01.1982	4482	4687
  30/8-1 SR	01.03.1996	4691	5149
  30/9-3 A	20.05.1984	3679	4249
  30/9-4 S	30.03.1985	4173	4303
  30/9-5 S	19.07.1985	2604	2872
  30/9-6	21.04.1987	2981	3034
  30/9-7	23.12.1988	3535	3565
  30/9-9	06.11.1989	2757	2809
  30/9-10	21.09.1990	3622	3649
  30/9-11 A	29.12.1990	2973	3002
  30/9-13 S	11.10.1991	3976	4027
  30/9-13 SR	17.07.2002	3980	4031
  30/9-15	05.01.1994	2616	2764
  30/9-16	08.08.1994	3457	3550
  30/9-24	17.10.2009	3150	3718
  30/9-28 S	26.02.2016	3645	4083
  30/10-5	01.05.1975	5049	5127
  30/11-3	14.03.1983	4637	4662
  30/11-4	24.07.1984	4640	5255
  30/12-1	07.03.1994	3596	3641
  31/1-1	15.02.2008	2882	2920
  31/2-1	09.11.1979	2293	2381
  31/2-1 R	09.11.1981	2294	2382
  31/2-2 R	06.10.1980	2360	2500
  31/2-3	20.07.1980	2236	2358
  31/2-4 R	06.04.1981	2256	2422
  31/2-4 R2	12.11.1982	2256	2422
  31/2-5	21.12.1980	2404	2471
  31/2-5 R	20.07.1981	2397	2464
  31/2-5 R2	22.04.1984	2397	2464
  31/2-8	18.08.1982	3048	3274
  31/2-19 S	13.07.1996	4059	4114
  31/3-1	13.10.1983	2105	2160
  31/3-3	18.11.1984	2432	2573
  31/4-2	15.11.1979	2632	2786
  31/4-3	11.05.1980	2702	2879
  31/4-4	17.02.1981	3087	3150
  31/4-5	29.07.1981	2645	2849
  31/4-7	11.09.1984	2384	2505
  31/4-8	11.05.1986	2346	2438
  31/4-11	12.09.2000	3178	3271
  31/4-A-13 C	26.07.2022	7704	7799
  31/5-2	11.11.1983	2336	2393
  31/5-2 R	30.08.1984	2336	2393
  31/5-7	06.03.2020	2832	2915
  31/6-1	28.10.1983	2111	2156
  31/6-2 R	08.09.1984	2164	2198
  31/6-3	26.12.1983	2143	2195
  31/6-6	29.07.1984	2225	2277
  31/11-1 S	28.06.2021	3008	3120
  32/2-1	01.07.2008	1228	1247
  32/4-1	04.12.1996	1816	1832
  32/4-3 S	26.10.2019	1823	1847
  33/2-1	26.12.2014	4388	4459
  33/5-2	18.11.1981	4412	4455
  33/6-1	06.07.1979	3792	3862
  33/6-2	02.01.1997	3913	3950
  33/6-3 S	24.07.2012	4267	4377
  33/9-1	04.06.1974	2923	3126
  33/9-3	14.11.1974	2849	2973
  33/9-4	17.09.1975	2889	2974
  33/9-5	01.01.1976	2998	3157
  33/9-6	31.08.1976	3322	3354
  33/9-7	07.11.1976	2958	3127
  33/9-8	18.02.1977	3055	3085
  33/9-9	17.11.1977	2715	3100
  33/9-10	12.06.1978	3500	3715
  33/9-11	28.08.1978	3437	3528
  33/9-12	03.08.1987	2814	2936
  33/9-13 S	24.12.1987	3003	3077
  33/9-19 S	23.07.1996	3122	3197
  33/12-1	18.04.1974	2836	3060
  33/12-2	23.08.1974	2700	2951
  33/12-4	17.07.1975	2776	2896
  33/12-6	21.06.1976	3721	4030
  33/12-7	27.04.1989	3660	3703
  33/12-8 S	26.04.2002	3647	3750
  34/2-2 R	08.05.1981	3840	4074
  34/2-4	11.06.1985	4063	4107
  34/2-5 S	31.03.2018	3451	3568
  34/3-1 S	10.09.2008	4125	4221
  34/3-2 S	30.12.2009	4273	4331
  34/4-2	24.05.1980	2597	2697
  34/4-3	30.03.1982	4353	4410
  34/4-5	06.04.1984	3559	3599
  34/4-8	21.06.1994	2799	2913
  34/4-10 R	18.04.2000	4186	4246
  34/4-11	10.01.2010	4131	4224
  34/4-13 S	02.01.2011	4800	4905
  34/4-14 S	19.05.2015	4640	4754
  34/4-18 S	06.03.2022	2855	3045
  34/5-1 S	13.03.2010	3834	3900
  34/6-1 S	28.08.2002	4199	4313
  34/6-2 S	05.11.2012	4055	4252
  34/6-3 A	01.11.2014	3953	4019
  34/6-3 S	24.09.2014	4360	4462
  34/7-2	10.10.1984	2152	2271
  34/7-3	02.01.1985	2414	2513
  34/7-4	16.01.1985	2536	2628
  34/7-5	16.03.1985	2893	3010
  34/7-6	30.05.1985	2510	2654
  34/7-7	16.12.1985	2560	2678
  34/7-8	11.04.1986	2299	2373
  34/7-10	29.10.1986	2531	2683
  34/7-12	17.12.1987	2606	2763
  34/7-13	13.04.1988	2859	2962
  34/7-16 R	15.10.1990	2821	2945
  34/7-16 R2	05.07.1994	2820	2944
  34/7-17	07.04.1991	2943	3085
  34/7-20	27.08.1992	3046	3128
  34/7-34	10.03.2009	2461	2584
  34/7-34 A	20.03.2009	2639	2972
  34/8-1	08.03.1986	3324	3417
  34/8-2	17.11.1986	3001	3051
  34/8-3	14.09.1988	3278	3328
  34/8-4 A	27.05.1992	3057	3143
  34/8-4 AR	07.03.2003	3065	3151
  34/8-5	01.04.1991	3384	3484
  34/8-7	16.07.1992	5118	5208
  34/8-7 R	10.02.1993	5118	5208
  34/8-8	24.08.1992	3388	3474
  34/8-8 R	09.03.1993	3387	3474
  34/8-9 S	28.12.1992	3150	3245
  34/8-10 S	09.12.1993	3039	3125
  34/8-12 S	09.12.2001	3185	3253
  34/8-13 A	13.05.2009	3735	3852
  34/8-13 S	26.06.2009	4123	4282
  34/8-17 S	14.03.2014	4285	4485
  34/8-18 S	22.02.2019	5769	6001
  34/10-1	08.09.1978	2268	2367
  34/10-2	08.12.1978	3325	3540
  34/10-3	07.06.1979	2495	2715
  34/10-3 R	10.10.1987	2492	2712
  34/10-4	15.10.1979	2340	2481
  34/10-5	02.01.1980	2562	2764
  34/10-7	23.03.1980	2053	2180
  34/10-7 R	14.07.1983	2050	2177
  34/10-9 R	03.07.1980	2375	2421
  34/10-11	05.03.1981	1890	2089
  34/10-12	12.09.1981	2688	2800
  34/10-13	05.01.1982	1924	2052
  34/10-14	19.03.1982	2372	2596
  34/10-15	12.12.1982	2213	2400
  34/10-16	11.04.1983	3798	4010
  34/10-16 R	27.09.1983	3796	4007
  34/10-17	08.07.1983	3422	3466
  34/10-18	30.08.1983	2978	3025
  34/10-19	06.12.1983	2005	2188
  34/10-21	22.10.1984	3906	4005
  34/10-23	13.10.1985	4715	4764
  34/10-30	12.05.1986	3120	3375
  34/10-32	13.07.1987	3353	3538
  34/10-32 R	10.08.1987	3353	3538
  34/10-33	15.12.1988	3799	3870
  34/10-35	01.07.1992	4239	4310
  34/10-38 S	29.05.1995	3451	3844
  34/10-39 S	20.06.1995	3238	3290
  34/10-41 S	28.08.1997	3368	3420
  34/10-43 S	11.04.2001	3878	4370
  34/10-44 S	08.07.2001	3720	4200
  34/10-46 S	30.01.2002	5428	5568
  34/10-47 A	14.11.2002	2964	3020
  34/10-49 B	21.05.2006	3405	3482
  34/10-49 B	21.05.2006	4196	4563
  34/10-49 S	08.05.2006	3278	4563
  34/10-53 S	24.03.2011	4424	4526
  34/10-54 A	18.04.2014	4467	4656
  34/10-55 S	26.03.2017	7274	7390
  34/11-1	25.10.1994	4514	4580
  34/11-2 S	17.05.1996	4696	4743
  34/11-3	16.01.1997	4471	4482
  35/1-1	18.07.2002	4264	4476
  35/1-2 S	19.12.2010	4142	4202
  35/3-2	26.10.1980	4143	4167
  35/4-1	24.05.1997	4704	4918
  35/8-1	24.01.1981	4093	4345
  35/8-2	21.05.1982	4203	4336
  35/9-1	07.05.1989	2312	2314
  35/9-1 R	27.07.1989	2312	2314
  35/9-2	03.04.1991	2754	2856
  35/9-6 S	07.12.2010	3691	3710
  35/9-11 A	21.05.2014	3801	3860
  35/10-1	16.01.1992	3826	3986
  35/10-2	22.08.1996	4601	4677
  35/11-1	06.08.1984	2995	3265
  35/11-2	04.12.1987	3798	4025
  35/11-3 S	09.09.1989	3930	4040
  35/11-4	29.12.1990	3082	3127
  35/11-4 R	27.01.1992	3092	3137
  35/11-5	03.11.1991	3689	3769
  35/11-6	20.04.1992	3943	3995
  35/11-7	29.09.1992	2840	2895
  35/11-18 A	16.12.2015	3968	4020
  35/11-20 B	15.09.2016	5075	5114
  35/11-22 S	02.02.2019	3738	3882
  35/12-4 S	26.06.2011	3534	3585
  36/7-1	07.05.1996	2808	2834
  36/7-2	22.09.1997	1363	1429

• Brønnbaner med kjerner

  Brønnbaner med kjerner

  Brønnbane navn	Dato for boreslutt	Kjernelengde [m]
  16/2-7 A	29.09.2011	2
  16/2-8	19.08.2011	2
  16/2-15	13.01.2013	24
  16/2-16	12.12.2012	20
  16/2-16 A	07.02.2013	28
  16/2-17 S	20.05.2013	106
  16/2-19	03.04.2014	7
  16/2-20 S	21.11.2013	10
  16/2-21	07.06.2013	17
  25/2-6	15.11.1977	9
  25/2-12	12.11.1988	25
  25/2-13	25.01.1990	144
  25/3-1	05.09.1989	4
  25/4-1	09.12.1972	143
  25/4-5	26.03.1981	58
  25/4-6 S	24.08.1991	5
  25/5-1	01.08.1987	55
  25/5-3	26.03.1990	23
  25/5-4	07.03.1991	17
  25/7-8 S	09.01.2020	144
  25/8-5 S	22.09.1994	9
  25/8-12 A	19.06.1999	38
  25/8-12 S	09.06.1999	33
  25/8-19 A	19.03.2020	16
  25/8-19 S	30.12.2019	25
  25/10-11	10.08.2011	72
  25/11-1	09.07.1967	9
  25/11-17	22.03.1993	18
  25/11-28	25.09.2015	42
  26/4-1	17.07.1987	9
  30/3-2 R	16.02.1981	12
  30/6-1	22.09.1979	10
  30/6-2	11.12.1979	6
  30/6-14	08.02.1984	14
  30/6-15	05.09.1984	137
  30/6-16	21.01.1985	8
  30/6-17 A	18.03.1986	37
  30/6-17 R	04.02.1986	43
  30/6-18	23.11.1985	74
  30/6-24 S	06.12.1991	26
  30/6-26	07.10.2001	28
  30/6-27	30.10.2001	27
  30/7-8 R	29.01.1982	26
  30/9-4 S	30.03.1985	8
  30/9-5 S	19.07.1985	18
  30/9-16	08.08.1994	27
  30/9-28 S	26.02.2016	55
  30/11-4	24.07.1984	19
  31/4-2	15.11.1979	4
  31/4-3	11.05.1980	14
  31/4-8	11.05.1986	86
  33/6-1	06.07.1979	5
  33/9-9	17.11.1977	157
  33/12-1	18.04.1974	8
  33/12-2	23.08.1974	13
  33/12-6	21.06.1976	7
  34/4-2	24.05.1980	6
  34/4-3	30.03.1982	8
  34/4-5	06.04.1984	34
  34/4-13 S	02.01.2011	58
  34/7-2	10.10.1984	18
  34/7-3	02.01.1985	90
  34/7-4	16.01.1985	21
  34/7-6	30.05.1985	94
  34/7-7	16.12.1985	92
  34/7-8	11.04.1986	39
  34/7-10	29.10.1986	114
  34/7-13	13.04.1988	17
  34/7-34	10.03.2009	29
  34/8-2	17.11.1986	12
  34/8-4 A	27.05.1992	77
  34/8-5	01.04.1991	14
  34/8-7	16.07.1992	5
  34/8-9 S	28.12.1992	20
  34/8-10 S	09.12.1993	81
  34/10-2	08.12.1978	50
  34/10-4	15.10.1979	6
  34/10-9 R	03.07.1980	4
  34/10-11	05.03.1981	27
  34/10-13	05.01.1982	105
  34/10-15	12.12.1982	19
  34/10-16	11.04.1983	18
  34/10-21	22.10.1984	16
  34/10-30	12.05.1986	200
  34/10-32	13.07.1987	86
  34/10-33	15.12.1988	37
  34/10-35	01.07.1992	37
  34/10-38 S	29.05.1995	160
  34/10-54 A	18.04.2014	47
  34/11-3	16.01.1997	0
  35/4-1	24.05.1997	29
  35/9-1	07.05.1989	2
  35/9-2	03.04.1991	28
  35/9-6 S	07.12.2010	2