cbBergvesenetPostboks 3021, 7002 Trondheim Rapportarkivet

Internt arkiv nr

Oversendt fra

Rapport lokalisering Gradering

Fortrolig

Fortrolig pga Fortrolig fra dato:

Bergvesenet rapport nr Intern Journal nr

BV 2238

Kommer fra ..arkiv Ekstern rapport nr"522300006"Sulitjelma Bergverk A/S

1972 !

Dato Forfatter

LAUX S.J. Sulitjelma Gruber A/S

Bedritt

Tittel

Report of mapping done in the Kvenangen window near Badderen, N.Troms.

Fylke 1:50 000 kartblad 1: 250 000 kartbladBergdistriktKommune

Dokument type ' ForekomsterFagområde

Emneord

Sammendrag

Genere11 geologisk undersokelse av Alta - Kvenangen -vinduet i Nord-Troms. Dette er et omrade avprekambriske grimnfjell som er omgitt av overskjovne kaledonske bergarter. Grunnljellsvinduet bestarav Raipas-formasjonen, med lavaer, doleritter, vulkanoklastitter og dolomittiske konglomerater, ogskiferlag. Petrog;rafi, metamorfose og strukturer kort omtalt. Ingen mineraliseringer av betydningobservert.

t

REPORT OF MAPPING DONE IN THEKVAENANGEN WINDOW, NEAR

r BADDEREN. N. TROMS

10th July -16th August 1972

ø by

S. J. Laux, B. A. (Oxon)

11thSeptember1972

REPORTOF MAPPINGDONEIN THEKVAENANGENWINEOW,NEARBADDEREN,N. TROMS

10thJuly 16thAugust1972

by

S. J. Laux,B.A.(Oxon)

CONTENTS PAGE

Introduction 1

Locationandworkingarea 1

Physicalfeatures 2

Generalgeology 2

Previunswork 3Generaldetails 3

Stratigraphy 3

Petrographyandmetamorphism 4

Structure 5

Raipasformation 5Boasekopformation 6

Economicgeology 6

Summaryand geologicalhistory 7

Comments 8

References 8

Listof samples 8

Geologicalmap

INTRODUCTICK

ThoAlto-KvaenangenvindarontoodatromFinnmarkintoN. Tromo.Thoaroainvoatigatodwas amoot approxleatoly35 oq.loaoltuatodoantot Baddoron,N. Troion,

Nep to ahm location ot thoaroa.

Revidert utgave av

Revised edition of„Berggrunnskart over Norge•'Nr. 164, 1953

Oslo 1960

Målestokk1 : ItIO0 1100

Seale

bt) ta m

Prnabrian (Indpaa)windowsin calodontdooomplex.

. /cte,k »; '!'er 1/21,r ‘),

' )

1/32

,rt

RAI

Julo

2

ThedominantteatureIn theareaia thevalleyof theriverBadderelvarunningapproximatelyeast-westbeforeturningnorthto reachthecoastat Badderen.Mostof theotherriversdrainIn a nort-aouthdirectionintotheBadderolva.On bothsidesofthemainrivervalleythegroundrisessteeply,especiallyonthenorthside,toglvathemountainsnedreHoankaandøvreHoanka.Mostof therivershavetheirsourcein oneof theusnymountaInlakes.

Oeologyls oftenrelatedto topography,thegeneraltrendbeingin a northsouthdirection,andmanyof theriversondlakesmark geologicalboundarlesforaomewayalongthoirlength.

TheAlta- Kvaenangentoctonicwindowls an arecof Pzbac3mbrianrockssurroundedby overthrustCaledonides.Thearetwoformationsoutcroppingin thiswindow.TheRalpasBormationis a seriesof lavas,pillowlavas,dolerites,volcaniclastica,enddolomiticconglomeratesuhichhovobeextmeta-morphosedonlyup to greenachistgrade.Minerallsationoccursintheaerocksbutismuchmorepronouncedin thcoldmlningareas,totheeastaroundtheBergmastanti-cline.

TheBossekopFormationlieswithmarkedunconfolaltyon theRalpasFormation,andla thoughtto be Eocambrianin age. It consista

11. of interbeddedquartziteandshalebedsup to 30 u, andbearsa markedresemblenceto aomeof theFormationsof theTanatjordOrompInEastFinnmark,butthisis onlyspeculative.

Theexistenceot a tillitein theareais queationable.Verylocalpatchesof conglomerateoccurnearthebaseof theLossekopForma-tion4butareunlikelytobe ot glacialorigha.Howevera poorlysortedangularconglomerateof possibleglacialoriginwasfoundin theextremesouthof thearea,althoughitsstrucuralpositionwasinvestigated.

Thesetwoformationahavebeenoverthustby a Calodonideachistwhichoutcropsto thenorthendsouthof thearoa.

3

The areawas originallymappedby Zenzånin 1915an a scaleof1:100000,and much laterby theN.G.U.in 1965,on a scaleof1:50000. Howeverthe lattermap was foundto be of verylittleuse.An Indiangeologisthas mappedthe Bergmarkareafor A/S Blelk-

vassliGrUberin 1970,and futhereastin theKåfjord-Alta-areaa Swissgeologist,Mr. AndråGautier,has made a geologicalmapfor ChristianiaSpigerverk.

ls111

Lodgingwas in an old housein Badderenand in a tentto map themore remoteareas. Threefieldassistantsworkedwith the But-hor as streamsedimentsamplersfor a periodof throoweeka.Theytooksamplesfromall of themajorstreamsin theareaandalsofromthosefurtherto the west.

STRATIGRAPHY

The Raipas Formationis Precambrianin age,andaceordingtoReitan,of Karelianage. Somestromatoliticdolomitevas foundand handspecimennumber50 may containa prinitivecoralorspongealthoughthlsis by no meanscertain.

The listof rock-typesdescribedon the map arenot in stratigrap-hicalorderand can occurin differenthorizons.Howeverthe grey-blackgraphiticsiltstoneseemsto representonsstratigraphicalhorizon,althoughotherthinblacksiltstonebandsoccurthroughoutthe formation,but not on a mapnablescale.Withinthe RalpasFormationfurtherto the east,twm serieshavebeenrecognisedby Zenz6n(1915); a lowergreenstoneseriesover-lainby a greyquartzite.HoweverLn the areamapped,onlytheformerwas foundto be present.

The BossekopFormationis of presumedEocambrianage (Reitan1960)althoughno fossilshaveeverbeenfoundto giveatreciseage.

4

PETROGBAPHYANDMETAMORPHISM

Rocksot theRaipasFormationareof lowmetamorphicgrade(green-ach1atto albite-epidotefacies)whichoftenenablesoriginaldeposi-tionalfeaturessuchas cross-bedding,gradedbedding,ripplemarkaandpillowatructuresto be seen.

TheBossekopFormationhaasufferedverylittlemetamorphism.In theRelpasFormatlontendifferentrocktypeswerefoundto occur.

11Theseare:

1, Bas c lavaaWh1chveryfromfine-grainedtilltheygradeintodolerites.

2. P 11w la of basalticcomposition.

Maas doleritesof darklahgreencolour,weatheringbrownegreen.A black ticsiltstoneoutcroppingin thecentralpart

of theareaandof about20 - 30m, thickneas.Thisformstheonlygoodmarkerhorlzonwhichcanbe followedforanyUstance,faintlaminationswereseenoccasionally,andthisrocktypeprobablyrepre-sentsa relativelylongperiodof volcanicquiescenceduringwhichonlypelagicmaterialwasdepositedin thesea. Thepercentageofgraphiteis probablyonlyamall.

Masalvetuffsof sh en colourandcon smallf -1222. Therearenumeroustuffbedsoccuringin betweenlavaflowsbutmostaretoosmallto be markedon themap, Theboundarlesbetweentuff,lavaanddoleriteproveda majorproblemin thefteld,andfor

11 greateraccuracythinsectlonswouldhaveto be made.

Greenlah- horzon laminatedmudstones.Thesearetuffites in thattheyareof thesamecompoaltionas mostof thebasalticlavas.In mostcaseatheyarejusthorizontallylamlnatedln bedsof about1 cm,butoccasionalrlpplesarefound.Eachbedprobablyrepreaentsthefall-outfroma volcaniceruption.

G • h- or -blacktuffbreccias.Theyareunbeddedand cartalnangalarclasto,setin a veryflne-gralnedmatrix.Mcstof theclastaaresmall,<5 cm,butthetuffbrecclaoutcropping1n theBadderelvacontainsclastsup to 75 cm ofmalnlydolomitesill-stoneandigneouscomposition.Theseclastsprobablyrepresentsacciden-talvolcanicejectaandselsadcactivitybringingmaterialInt°a quietwaterenvironment.

5

S, G eniehvolcanic outcroppingin extremeeastof the area. TheBoumasequencecanbe observedin a fewraseswith a sequenceof

pelagicunithorizontallylaminatedunitripplecross-laminationherizontallylpmingtedunitgradedunit

Northof the Badderelvaintra-formationalconglomeratesoccuratthe baseof the gradedunit,auggestingtearingup of the bedbeneathby the turbiditycurrent. The factthata completeBoumasequenceis seenindicatesa distalturbidite.

C omeraticand dolomiticsandstones,medium-grninedand of a ught greenishcolour. Theseare sometimescross-beddedwithshallowchannels.Clastsaremeinlyof dolomite(stromatolitic)and greensiltstone,the alltstoneclastsoftenbeingelongated.The conglomeratescanbe verypoerlysortedwithclastof up tometrwoccurringwithmuch smallerclasts< 2 cm in a sandymatrix.Completebedsof dolomiteup to 3 m thiCkoccasiorn11,are seen,but seemto be verylenticular.Thisunitwas probablydepositedin a veryshallowmarineenvirons• mentwith fluvialinfluence,

Dolomiticlimestone,buffweatheringand outcroppingonly inthe extramewestof the area.

The rocksof the BossekopFormationconsistof crossbeddedquart-zitesand shalesindicatinga ahallowmarineenvironment,

STRUCTURE

F rma s

The dominantstructureis one of north-southtrendingfolds. Theareasouthof the BadderelvaaroundLausfjelletis of greatcon-plexityconsistingof isoclinalfoldsleaningto thewastwhichhavebeenbentand refolded.Thrustinghas alsooccuredin thisregion.Howeverin the north-eastof the areathe foldpattealseemsto bedifferent.Apartfromthenorth-southtrendthereis alsoadominanteast-westor northiewestsouth-easttrend,suggestingthatthereare twomain interfering phasesin the region.

6

Herethemaintrendis N.W.-S.E.changingtoEast-Westin theextremesouthas oneapproachestheoverthrustCaledonides.Asecondphaseof foldinghasalsoaffectedtheformation,makingthequartziteandshalebodsdieoutandreappearmainidbentollowedalongstrike.

It is notknownhowthefoldsin theBossekopFormationrelatetothosein theunderlyingRaipasFormation.

ECONOMICGEOLOGY

411 Minsralisationhasaffectedtherocksof tbeRaipaaFormationbutnottheBossekopFormation,indicatingthatthemineralisationisof Precambrianage.Themainareasof mineralisationarein theBergmarkant3c1inejuatto theeastandsout-eastof theareainvestigated,andalsoatMiddavarreto thenortheast. Themainpurposeof themappingwas to seeif thismineralisationcontinuedintotheauthor'sarea.Smallareasof mineralisationwerefound,butareunlitelyto beof anyeconomicinterests

a. Intheconglomeraticanddolomiticsandstonean areaofdissemination-typeminenlisationwasfound,butthisconsistedmainlyof smallsoatteredpyritecryatals.

b. Thegrey•blackgraphiticsiltstoneoutcroppingin theBadder-elvais intemselydeformedandhasveinsof calcitecontainingaverylittlepyriteandchalcopyrite.Thevoinshoweverarelessthan20 cm thickandnotof economicimportance.

Theareaof greatestdeformationaroundLausfjelletandcontt-nuingsouthhasmanyquartzveinsup to 2 metresthickrunningthroughtherocks,butno accompanyingmetallicdepositawerefound.

Southof theBadderelvaa talcveinwaafoundin a dolerite,sandwichedbetweentwographiticsillatonebeds. Theveinwasupto a metrethickandranin a northeaouthdirectionalongstrikeforabout1 km beforsdyingout. It alsocarrieda littlemala-chite.

7

e. Otheramallareasof disseminationtypeminnalisationareshownon themap,butareconsideredto be of no economicinterest.

It is of theauthor'sopinionthattheminaralisationis associatrednotwithareasofmaximumdeformationbutwithareasof updaningcausedby theinterterenceot thetwomajorfoldaxes(aN- S axisandan E-Wto S.E.-N.W.axis)of thearea. ThiscouldaccauntfOrthamineralisationin theBergmarkanticlineandatNiddavarre.TheNorthsSouthtrand dominantin thewestandtheEast-Weat

11 trendin theeast.In themiddleiterebothhaveapproximatelyequalinfluencethemineralisationseamsto haveoccurred.Updomingfavourathefor-mationof manytensioncracksthroughwhichtheminenaisationvelnacanrun.

GeophysicalworkusingOeigercountersfalledto detectanyradio-aktivedepositsin theares.

Thereaultsof analysieof thestreamsedimentsamplesuerenotknownat thetimeof writingthisreport.

SUNNARYANDOEOLOGICALHISTORY

A verybrieigeologicalhistoryla an follows.

111 1. Depositionof a serlosof basaltIclavas,pillowlavas,doleri-tesandvolcaniclasticrocksin a probableoceanicenvironment.Conglomeratesandstrematoliticdolomitesformedin a veryshallowmarineenviromentsurroundingvolcaniclalands.Probableminorunconformitieswithintheaeries.

Foldingandlowksgraderegionalmetamorphismwithassociatedmineralisation.Probablythreephasesof tolding.

Erosionanddepositionof shallowmarinesandsof BessekopFor-mation.

CaledonideFoldingof bothformationsandoverthrustingofCaledosideschist.

Archingof theCaledonideato formthepresenttectonicwindow.To summarizestheRalpasFormationia a typicalgreenstonesucces-sionof volcanica& volcaniclasticsthathaveundergonea certaindegreeofmineralleationin PreCambriantimes. Themineralisationin theareamappedis notconsideredto be of economicimportance.

Flhep1'oviQioncL moDed in the t3o1,. ut..yJilhancedthe

officionci-j2 ..appin-,and it :_htthe co:npany

Laishtinst in 02 the:s3 tj Hc:11.inj

into =Jas 32 acc-,ss.

11

-31tedan1,:

Uoitan•. . 1_1-J : , ,

Goologyof 1-ctonicvindow of

J.J.L.172/ la ;.-Hanlomeratican:

/ •L• :vrite•,diueralisuAlub.

111

17:/ H4tvi crystals,

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9? tuffite. litt7cT7r12 0"2.(\1copyrite.

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/20a dolomitic

Tnt-rbeekedbasaltic1=.

line-yrainedlava Lis=1::Ition-type rainerali-

9

Smallmagnetitecrystalsand a littlemalachiteand chalcopyrite.

/37 Volcanicturbiditewithpyritemineralisation(dissemination-type).

/39 Poorlysortedgrwy siltstonewithpyriteminerali-sation(dissemination).Probablya tuff.

/45a Doleritewith someamphibolisation.

b Talcvein (2 specimens).

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