TILJE FM

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Generell informasjon

Generell informasjon
Attributt	Verdi
Litostrat. enhet Den litostratigrafiske enhetens offisielle navn.	TILJE FM
NPDID for litostrat. enhet Sokkeldirektoratets entydige nøkkel for litostratigrafiske enheter.	169
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.	BÅT GP

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Litostrat. enhet
Beskrivelse
Tilje Formation

Name

The Norwegian word for a boat's decking. This unit corresponds to the upper part of the informal Aldra Formation (H1-2).

Well type section

6507/11-1 (Saga Petroleum), coordinates 65°04'43.82"N, 07°29'23.33"E, from 2596 m to 2498 m, (Fig 4.9) . Five cores (33 m recovery) were taken through the upper part of the formation.

Well reference section

6609/10-1 (Saga Petroleum), coordinates 66°14' 42.27"N, 09°14'59.50"E, from 1733 m to 1642 m (Fig 4.10) . One core (11.5 m recovery) was taken uppermost in the unit.

Thickness

98 m in the type well, 91 m in the reference well.

Lithology

Very fine to coarse-grained sandstones are interbedded with shales and siltstones. The sandstones are commonly moderately sorted with a high clay content and most beds are bioturbated. Shale clasts and coaly plant remains are common. Pure shale beds are rare; most of the finer grained interbeds are silty or sandy.

Basal Stratotype

The base of the Tilje Formation is defined at the top of a mudstone interval recognized in most wells on Haltenbanken. The overlying sequence shows a markedly higher sand content and a greater average thickness of individual sandstone bodies. The gamma ray log shows a shift to generally lower values and a slightly more blocky pattern over the boundary.
The mudstone interval is most pronounced on the Halten Terrace, but is often difficult to pick further east on the Trøndelag Platform. Coal beds are here developed at higher stratigraphic levels than on Halten Terrace, and the top of the highest coal bed is recommended as the formational boundary.
In the reference well from Trænabanken the formational base is taken at an upward shift in the gamma ray log from relatively irregular, high amplitude variations to more uniform, low amplitude and generally lower readings. Limestone interbeds are common below the boundary and much less frequent above in this area.

Lateral extent and variation

The formation is present both on Haltenbanken and Trænabanken, although it is locally absent on the Nordland Ridge due to erosion. The formation is uniformly developed throughout the Halten Terrace where it is from 100 m to 150 m thick, but it thins northeastwards to less than 100 m on the Trøndelag Platform. Shallow drilling close to the coast (Bugge et al. 1984) indicates time equivalent deposits dominated by coarse-grained clastics.

Age

Sinemurian to Pliensbachian.

Depositional environment

Nearshore marine to intertidal environments are typical of the formation. Subcrops near the coast (Bugge et al. 1984) indicate a gradual transition to continental environments eastwards.

Correlation

The Tilje Formation is comparable in age and lithology to the Neill Klinter Formation of East Greenland and to the lower part of the Stø Formation in the Hammerfest Basin.

Source

Dalland, A., Worsley, D. and Ofstad, K. (eds.) 1988: A lithostratigraphic scheme for the Mesozoic and Cenozoic succession offshore mid- and northern Norway. NPD-Bulletin No. 4, 65 pp.

Brønnbaner som penetrerer

Brønnbaner som penetrerer
Brønnbane navn	Dato for boreslutt	Topp dyp [m]	Bunn dyp [m]
6307/1-1 S	28.12.2018	2325	2433
6406/1-1	10.06.2001	4806	4996
6406/2-1	09.04.1995	4910	5188
6406/2-1 R	07.01.1996	4908	5186
6406/2-2	27.03.1996	4978	5291
6406/2-2 R	03.03.2006	4972	5285
6406/2-3	15.04.1997	5028	5210
6406/2-4 SR	15.02.1999	4755	4950
6406/2-5	29.09.1997	5210	5396
6406/2-6	07.11.1998	4965	5204
6406/2-6 R	23.05.2000	4966	5205
6406/2-7	26.12.1999	4916	4981
6406/2-8	05.05.2015	4308	4331
6406/2-9 S	15.01.2019	4880	4983
6406/3-1	14.08.1984	4177	4380
6406/3-2	22.11.1986	4285	4496
6406/3-3	26.10.1986	4202	4404
6406/3-4	29.12.1987	4372	4414
6406/3-5	01.06.1988	4139	4283
6406/3-6	15.11.2002	4041	4175
6406/3-7	19.09.2006	4333	4473
6406/3-8	10.08.2010	4166	4216
6406/3-10	05.04.2020	4386	4533
6406/3-10 A	31.08.2021	4715	4862
6406/5-1	30.04.2002	4628	4692
6406/6-1	30.12.1985	4592	4715
6406/6-2	31.01.2007	4561	4670
6406/6-3	09.07.2013	4188	4373
6406/6-4 S	30.10.2015	4430	4484
6406/8-1	11.04.1988	4667	4895
6406/8-2	08.04.2007	4593	4700
6406/9-1	02.06.2005	4826	5024
6406/9-2	01.07.2007	5042	5241
6406/9-3	29.09.2013	4954	5138
6406/11-1 S	18.02.1991	3871	3985
6407/1-2	15.05.1983	4050	4220
6407/1-3	16.01.1984	3950	4150
6407/1-5 S	21.05.2012	4119	4177
6407/2-1	06.08.1982	3176	3345
6407/2-2	31.07.1983	2709	2892
6407/2-3	23.01.1987	2739	2910
6407/2-5 S	02.09.2009	3096	3311
6407/2-6 S	13.05.2010	2993	3148
6407/3-1 S	08.05.2011	2875	2928
6407/3-2 S	05.09.2019	2314	2430
6407/4-1	15.11.1985	4272	4500
6407/5-2 S	04.09.2011	3498	3545
6407/6-1	26.10.1984	2244	2457
6407/6-3	16.02.1987	2727	2902
6407/6-4	13.12.1990	2933	3027
6407/6-5	27.12.1999	2709	2759
6407/6-6	05.02.2008	2422	2508
6407/6-7 S	27.05.2009	3046	3179
6407/7-1 S	07.04.1986	2839	3017
6407/7-2	21.01.1987	2771	2878
6407/7-2 R	30.04.1990	2773	2880
6407/7-3	18.05.1988	2937	3014
6407/7-4	28.03.1989	2973	3139
6407/7-5	15.02.1991	3355	3496
6407/7-6	16.12.2000	3684	3882
6407/7-7 S	20.09.2007	3576	3712
6407/7-8	14.09.2008	4752	4981
6407/7-8 A	05.11.2008	4896	5145
6407/7-9 A	16.10.2016	4483	4717
6407/7-9 S	20.09.2016	3860	4068
6407/8-3	27.05.1997	1842	1935
6407/8-4 A	16.06.2008	2217	2424
6407/8-4 S	21.05.2008	2550	2724
6407/8-5 A	13.06.2009	2566	3004
6407/8-5 S	26.05.2009	2549	2731
6407/8-6	20.10.2013	2902	3035
6407/8-6 A	09.12.2013	3224	3351
6407/8-7	12.05.2015	2629	2830
6407/8-7 A	23.05.2015	2786	2927
6407/8-8 S	10.12.2022	3392	3537
6407/9-1	07.09.1984	1968	2073
6407/9-2	02.02.1985	1829	1865
6407/9-3	28.07.1985	1821	1868
6407/9-4	10.09.1985	1794	1820
6407/9-7	25.05.1988	2043	2139
6407/9-8	22.09.1992	2053	2126
6407/9-9	06.07.1999	1883	1920
6407/10-1	19.06.1987	2974	3155
6407/10-2	23.06.1990	3679	3825
6407/11-1	07.12.2018	1937	2042
6408/4-1	18.10.1988	2157	2323
6506/6-1	07.12.2000	5165	5302
6506/9-1	15.09.2009	5435	5572
6506/9-2 S	28.04.2010	4578	4699
6506/9-3	27.08.2013	4492	4656
6506/11-1	31.03.1988	4485	4662
6506/11-2	26.10.1991	4553	4705
6506/11-4 S	06.06.1996	4852	5022
6506/11-5 S	10.11.1996	4528	4692
6506/11-6	22.08.1998	5080	5260
6506/11-7	27.07.2001	4821	4927
6506/11-8	16.07.2006	4928	4990
6506/11-9 S	03.09.2012	5104	5282
6506/12-1	06.02.1985	4229	4437
6506/12-3	17.07.1985	4147	4360
6506/12-4	13.08.1985	4252	4414
6506/12-5	27.03.1986	4274	4510
6506/12-6	02.08.1986	4515	4735
6506/12-7	12.08.1987	4693	4840
6506/12-8	30.08.1988	4186	4335
6506/12-9 S	10.09.1993	4672	4837
6506/12-10	26.06.1995	4858	5024
6506/12-10 A	11.12.1995	5552	5711
6506/12-11 S	07.09.1996	5042	5211
6506/12-11 SR	01.02.1997	5042	5211
6506/12-12 A	01.09.2009	5181	5430
6506/12-12 S	06.08.2009	5218	5496
6507/2-1	29.09.1986	3947	4135
6507/2-2	16.03.1992	3770	3810
6507/2-5 S	14.09.2019	4170	4230
6507/2-6	14.07.2022	4812	4929
6507/3-1	26.10.1990	3776	3976
6507/3-2	27.04.1997	1225	1274
6507/3-3	25.03.1999	3538	3680
6507/3-3 B	16.06.1999	4216	4275
6507/3-4	30.04.2004	3919	4047
6507/3-5 S	08.05.2008	4113	4216
6507/3-6	23.06.2009	1360	1422
6507/3-7	22.07.2009	3687	3785
6507/3-8	15.12.2009	2844	2990
6507/3-10	16.08.2013	3357	3406
6507/3-11 S	15.08.2015	2312	2435
6507/3-15	11.08.2022	2028	2126
6507/3-16	21.08.2022	1666	1672
6507/5-1	03.05.1998	3579	3688
6507/5-2	23.09.1999	3772	3855
6507/5-4	15.04.2001	3687	3774
6507/5-5	14.02.2002	3831	3925
6507/5-7	24.06.2014	1400	1447
6507/5-9 A	15.10.2019	2156	2169
6507/5-9 S	27.09.2019	2073	2086
6507/6-2	16.07.1991	3904	4014
6507/6-3	24.11.2008	1490	1590
6507/7-1	01.12.1984	4586	4825
6507/7-2	10.06.1985	2285	2482
6507/7-3	18.09.1985	2499	2720
6507/7-4	13.01.1986	2604	2850
6507/7-5	06.03.1986	2474	2660
6507/7-5 A	05.04.1986	2598	2673
6507/7-6	06.09.1986	2190	2369
6507/7-8	02.08.1987	2558	2787
6507/7-10	29.10.1993	2604	2759
6507/7-11 S	14.08.1997	3615	3749
6507/7-14 S	26.09.2010	4478	4534
6507/7-15 S	02.05.2012	4499	4567
6507/7-16 S	18.12.2019	3187	3238
6507/8-1	09.12.1986	2387	2559
6507/8-2	09.09.1987	1945	2123
6507/8-3	20.09.1988	1446	1542
6507/8-5	16.03.1991	1943	2000
6507/8-6	09.10.1993	2165	2275
6507/8-7	31.01.2004	2957	2975
6507/8-8	20.04.2011	2151	2327
6507/8-10 S	23.04.2020	2053	2203
6507/10-1	31.10.1982	3081	3226
6507/10-2 S	10.02.2014	2823	2950
6507/11-1	10.12.1981	2498	2596
6507/11-2	30.05.1982	2117	2290
6507/11-3	15.08.1985	2630	2825
6507/11-4	22.06.1987	2992	3045
6507/11-6	08.07.2001	3261	3387
6507/11-8	03.07.2007	2594	2701
6507/11-9	18.04.2008	2812	2910
6507/11-10	16.02.2010	2285	2319
6507/12-1	26.10.1980	2303	2412
6507/12-2	24.11.1981	2076	2193
6507/12-3	13.09.1985	2186	2351
6508/1-1 S	29.08.1999	2530	2714
6508/1-2	12.09.2011	1752	1810
6508/5-1	24.05.1987	1824	1981
6510/2-1	10.10.1997	1823	1945
6510/2-1 R	21.12.1997	1823	1945
6607/12-2 S	25.10.2011	3815	3935
6607/12-3	26.12.2012	4172	4271
6607/12-4	13.10.2020	3811	3863
6608/10-2	29.01.1992	2720	2819
6608/10-3	11.03.1993	2712	2791
6608/10-3 R	17.08.1995	2712	2791
6608/10-4	06.03.1994	2657	2697
6608/10-8	12.04.2002	2391	2403
6608/10-8 A	26.04.2002	2615	2660
6608/10-9	18.02.2003	2222	2228
6608/10-10	07.08.2003	2529	2567
6608/10-11 S	15.08.2006	3695	3725
6608/10-16	13.06.2014	3817	3993
6608/11-3	15.12.2002	1517	1530
6608/11-4	23.05.2004	1656	1668
6608/11-6	06.08.2008	1601	1630
6609/10-1	29.08.1983	1642	1733
6609/10-2	03.10.2009	2054	2142
6609/11-1	07.07.1983	2546	2735
6610/2-1 S	28.09.1996	2067	2278
6610/3-1 R	11.12.1993	3772	3935
6610/3-1 R2	07.10.1996	3774	3937
6610/7-1	19.06.1983	2746	2855
6610/7-2	14.03.1984	1487	1533
6610/10-1	03.02.2013	2539	2657
6611/1-1	24.11.2019	1258	1387

Brønnbaner med kjerner

Brønnbaner med kjerner
Brønnbane navn	Dato for boreslutt	Kjernelengde [m]
6406/2-1	09.04.1995	249
6406/2-2	27.03.1996	150
6406/2-3	15.04.1997	27
6406/2-4 SR	15.02.1999	184
6406/3-2	22.11.1986	80
6406/3-10 A	31.08.2021	147
6406/9-2	01.07.2007	63
6407/2-3	23.01.1987	28
6407/2-6 S	13.05.2010	110
6407/4-1	15.11.1985	56
6407/7-1 S	07.04.1986	154
6407/7-2	21.01.1987	88
6407/7-3	18.05.1988	77
6407/7-4	28.03.1989	172
6407/7-5	15.02.1991	51
6407/7-6	16.12.2000	126
6407/7-7 S	20.09.2007	133
6407/7-8	14.09.2008	118
6407/7-9 S	20.09.2016	109
6407/8-6	20.10.2013	115
6407/10-1	19.06.1987	28
6407/10-2	23.06.1990	12
6506/6-1	07.12.2000	63
6506/9-1	15.09.2009	125
6506/11-1	31.03.1988	20
6506/11-2	26.10.1991	144
6506/11-4 S	06.06.1996	169
6506/11-5 S	10.11.1996	152
6506/11-6	22.08.1998	27
6506/11-7	27.07.2001	19
6506/11-9 S	03.09.2012	28
6506/12-1	06.02.1985	55
6506/12-3	17.07.1985	121
6506/12-5	27.03.1986	80
6506/12-6	02.08.1986	104
6506/12-7	12.08.1987	8
6506/12-8	30.08.1988	58
6506/12-9 S	10.09.1993	158
6506/12-10	26.06.1995	163
6506/12-10 A	11.12.1995	37
6506/12-11 S	07.09.1996	161
6506/12-12 A	01.09.2009	19
6507/2-2	16.03.1992	9
6507/3-1	26.10.1990	82
6507/3-2	27.04.1997	3
6507/3-3	25.03.1999	109
6507/3-5 S	08.05.2008	37
6507/3-8	15.12.2009	0
6507/3-15	11.08.2022	31
6507/5-1	03.05.1998	107
6507/5-2	23.09.1999	41
6507/5-4	15.04.2001	36
6507/5-9 S	27.09.2019	13
6507/7-1	01.12.1984	7
6507/7-2	10.06.1985	134
6507/7-3	18.09.1985	158
6507/7-4	13.01.1986	164
6507/7-5	06.03.1986	147
6507/7-5 A	05.04.1986	30
6507/7-6	06.09.1986	52
6507/8-1	09.12.1986	87
6507/8-2	09.09.1987	6
6507/10-1	31.10.1982	1
6507/11-1	10.12.1981	30
6507/11-2	30.05.1982	7
6507/11-3	15.08.1985	27
6507/12-1	26.10.1980	2
6508/1-2	12.09.2011	12
6510/2-1	10.10.1997	10
6607/12-3	26.12.2012	53
6608/10-2	29.01.1992	22
6608/10-3	11.03.1993	52
6608/10-4	06.03.1994	39
6608/10-8	12.04.2002	11
6608/11-4	23.05.2004	6
6609/10-1	29.08.1983	12
6609/11-1	07.07.1983	37
6610/2-1 S	28.09.1996	13
6610/7-2	14.03.1984	9

TILJE FM

Generell informasjon

Nivå under

Beskrivelse

Brønnbaner som penetrerer

Brønnbaner med kjerner