SKAGERRAK FM
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Generell informasjon
Generell informasjon Attributt Verdi Litostrat. enhet Den litostratigrafiske enhetens offisielle navn.SKAGERRAK FMNPDID for litostrat. enhet Sokkeldirektoratets entydige nøkkel for litostratigrafiske enheter.146Nivå Angir den litostratigrafiske enhetens nivå. Lovlige verdier: GROUP, FORMATION, MEMBER.FORMATIONLitostrat. 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
Skagerrak Formation
NameFrom the channel separating Norway from Denmark.Well type sectionWell reference sectionThicknessThe formation is 1182 m thick in the type well and thicker further east where seismic data indicate that it may reach a maximum thickness of over 3000 m. Westward from the type well the formation interdigitates with and progrades over the associated claystone sequence ( Smith Bank Formation ). The maximum thickness at the north-west limit of well control is 660 m and at the south-west limit 250 m.LithologyThe formation consists of interbedded conglomerates, sandstones, siltstones and shales. Various shades of reds and browns are the dominant colours but light to dark grey beds are also present. Sandstones may be orthoquartzitic arkosic or highly lithic. Anhydrite, dolomite and limestone are subordinate lithologies.BoundariesThe formation has gradational to sharp contacts with the claystone sequence of the Smith Bank Formation . Dip meter surveys suggest that in places this contact is an unconformity. Over some structures the formation rests on pre-Triassic rocks. The formation is normally overlain unconformably by Jurassic or younger sediments but in a few wells it passes up into the Gassum Formation (of Rhaetian age).DistributionThe formation is present throughout the eastern part of the Central North Sea and the western Skagerrak. It may be missing over certain structures because of erosion or halokinesis.AgeMiddle to Late Triassic. It may possibly extend down to the Early Triassic in the areas of maximum development.Depositional environmentThe bulk of the Skagerrak Formation was probably deposited in a coalescing and prograding system of alluvial fans along the the eastern and southern flanks of a structurally controlled basin. The limited areal extent and poorly preserved faunal components suggest that some of the dark shale, carbonate and anhydrite beds were deposited in lakes. Better preserved microfossils and other indicators such as glauconite show that some beds were deposited when minor marine incursions occurred between floods of continental clastics.Source-
Deegan, C. E. and Scull, B. J. (compilers) 1977: A standard lithostratigraphic nomenclature for the Central and Northern North Sea. UK Institute of Geological Sciences, Report 77/25. The Norwegian Petroleum Directorate, NPD-Bulletin No. 1, 36 pp.
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Brønnbaner som penetrerer
Brønnbaner som penetrerer 22.07.20105818593129.03.19804101416303.08.19824346447012.08.19844587458823.11.19854081415114.01.19924435452507.03.20094362443503.07.19823820394703.04.19692580283220.11.19712875293005.09.20155310554816.08.19784087413224.02.19844387453126.08.19934587470125.09.19934673471521.01.20094576467518.01.20193521354527.04.19895225530020.06.19812945299827.05.20193611370601.02.19852978356010.03.19863165329305.08.19712661280813.03.20083400342103.06.20064021416829.05.19712609281125.12.19834566485608.10.19844566485631.12.20115587567216.07.20115213542003.11.20123697380006.09.19773929409507.06.19813917414524.07.19813521370023.12.19883814390014.05.19903760382029.08.19913642366706.11.19913800386807.02.19722704272710.10.19662113220504.12.19822417265725.07.19772513258201.07.19692833286617.03.19802752279506.10.20103158322118.12.20113602363927.10.20113004305824.05.20142470261804.03.20142760279116.07.20142110219629.06.19752871318223.07.19712813287521.11.20112484253328.04.19873685375621.09.19873498355004.09.19861955197109.12.20053118315419.05.19682329259029.08.19702633302519.08.19722613268220.08.19772845290201.08.20062836463819.08.19712121219606.05.19692107241726.06.19761539156117.01.19711567274928.02.197614564419.08.19691900243009.08.19795033511530.03.19824044425907.09.20084008403719.12.19743579379516.08.19763268350529.11.19773723382409.06.19823655376008.06.19933411347605.04.19973174322513.06.20073666369027.05.20073872394006.04.20093613370009.02.20113876393015.05.20153499357703.06.20153860392529.06.20153670377302.06.20193645379528.06.20194130420330.05.19773701373417.06.19783699376403.04.19793703379614.06.19793629371611.04.19803769394607.09.19803828394625.05.19813625367614.07.19812642277607.11.19813183324127.06.19823360354301.08.19822821320030.03.19832741284702.03.19843420359309.11.19973966409729.04.19934340464125.07.19974343464420.03.19943259350313.03.20063756392303.01.20103169322506.09.19753204326904.05.19863077315004.11.19902979305007.01.19913036347714.07.19912854305429.07.19912856294008.10.19923688384804.11.19963429355019.05.19973544359709.02.20012977308511.06.20033092315131.03.20062914296123.03.20073550362004.02.20073331334520.05.20082973321201.07.20083874419221.05.20093122331021.06.20093493370216.05.20102985303529.05.20103192348520.05.20153097318107.08.19762424262028.05.20043083318622.04.20082456254426.04.20102401262509.05.20102501259530.11.20102496255007.12.20122429264201.01.20132729289714.05.20141894198521.10.20133060310620.04.20153194331303.03.20152491263004.06.20152769289614.06.20153066321527.05.20152506264025.08.20151953209414.04.20164896533011.04.20171968224005.08.20203068315828.02.20233177325720.09.20101955207501.09.20111986213429.09.20112041210019.08.20111951214024.09.20111949198628.10.20111968209029.03.20121946212604.05.20122239236529.09.20122626265830.08.20121949195517.11.20121887198213.01.20131969200612.12.20121999206507.02.20132385250320.05.20132020205203.04.20141952198903.05.20142283231016.02.20142125216721.11.20132038209507.06.20131965207028.11.20162057214303.05.20131955219821.08.20132529260026.08.20141934270016.08.20151984235801.04.20181950206928.01.20121967204220.03.20131912199028.09.20131936210010.07.20162241235006.12.19822521278103.08.19842594277524.07.19972565272529.12.19972770299419.01.20032856290003.01.20112515255304.09.20152546265012.07.19682464307414.07.19863053311601.08.19912923315001.12.19962532262610.08.19982547255026.08.19682352253207.02.20112988306523.10.20212466254411.06.19742992316124.03.19692825339830.06.19682211231517.05.19762521260821.06.19722446396503.02.19802638273010.07.20092439247001.01.19802506280026.03.19814127420703.02.19862503265109.01.20203120325019.03.20202483280630.12.20192434271628.05.20212438269810.05.20212504273320.06.20212391263320.07.20212325258902.04.20102173236818.01.20152439254002.08.20162564262809.08.20183653368009.08.20183686370418.08.20184832489326.08.20184305440530.07.20182655270130.07.20182706271210.02.20234052415009.07.19672109239113.05.201921472230 -
Brønnbaner med kjerner
Brønnbaner med kjerner 22.07.2010826.08.1993327.04.19891701.02.198513710.03.19863213.03.20082025.12.19834624.07.198112629.08.19911306.11.1991927.10.20112404.03.20141016.07.2014019.12.19745916.08.19763708.06.19931605.04.1997714.07.198110701.08.19825730.03.19835309.11.19975029.04.19934204.11.1990807.01.19911829.07.19914604.11.19961809.02.20011920.05.200815601.07.20082421.05.20094529.05.201010426.04.201012107.12.20121314.05.20148320.04.20153003.03.20159627.05.20154425.08.201511711.04.20175220.09.2010329.09.20111219.08.20115624.09.20113329.03.2012704.05.2012429.09.20123230.08.2012617.11.20121813.01.20132207.02.20133520.05.20132103.04.20143703.05.20142216.02.20141421.11.20131607.06.20131103.05.20136926.08.20147416.08.20158001.04.20185228.01.2012720.03.20131128.09.20132706.12.19829403.08.1984924.07.19976129.12.199711611.06.1974517.05.1976826.03.19813209.01.20201419.03.2020830.12.20198810.05.20215220.06.202111009.07.196725