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English version | ||||
| MALMDATABASEN | |||||
| Forekomstområde 1813 - 024 | |||||
| (Sist oppdatert 01.mar.2000) | |||||
Navn på deposit area : Vandalsvik |
| (Objekt Id : 1813,024,00,00) |
| Lokalisering |
| Fylke : | Nordland (18) | Kommune : | Brønnøy (1813) |
| Kart 1:50000: | Velfjord (1825-4) | Kart 1:250000: | Mosjøen |
| Markeringspunkt: | Lengdegrad: | 12.4482600 | Breddegrad: | 65.4634200 |
| EU89-UTM Zone 33 | (Coordinates IS confirmed) |
| X-koord: | 381782 m. | Y-koord: | 7262498 m. |
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| Materialtype |
| Hovedtype: | Basemetaller (Cu,Zn,Pb,Fe sulfider,As,Sb,Bi,Sn) | Subtype: | Sink | |
| Element(s): | Zn Pb As |
| Production |
| Activity: | Prospektering | Reserves: | ||
| Prod. method: | Production: | |||
| Prod. status: | Volume of dump: |
| Betydning |
| Offentlig: | Not Assessed (reg. 18.02.2015) |
| Economical: | Ikke vurdert |
Operations |
| From - To | Activity | Comments | |
| 1982 - 1983 | Geochemistry | Company/Institution :BP Norge A/S Minerals | |
| 1989 - 1989 | Sampling | Company/Institution :NGU-Malmreg. |
Mineralization |
| Era: | Paleozoic | Period: | Devonian | |
| Dating: | Method: | |||
| Genesis: | Hydrotermal gang | Form: | Plate | |
| Main texture: | Sprekkefylling | Min. distribution: | Uregelmessig |
| Main grain size: | Middelskornet (1-3 mm) | Main alteration: |
| Strike/Dip: | 117 / 40 | Direction: | ||
| Plunge: |
| Stratigraphic classification of host rock |
| Era: | Paleozoic | Period: | Silurian |
| Province: | Caledonides | |
| Geotec.unit: | Helgeland Nappe Complex | |
| Tectonic complex: | ||
| Igneous complex: | Bindal Batholith |
| Group: | Formation: |
Mineralogy |
| Relationship | Mineral | Amount | |
| Gangue mineral | Quartz | Major mineral (>10%) | |
| Ore mineral | Pyrrhotite | Major mineral (>10%) | |
| Ore mineral | Galena | Major mineral (>10%) | |
| Ore mineral | Sphalerite | Major mineral (>10%) | |
| Ore mineral | Arsenopyrite | Subordinate mineral (1-10%) | |
| Ore mineral | Molybdenite | Accessory mineral (<1%) |
Lithology: |
| Relationship | Rock | Origin | |
| Host rock | Turmalingranitt | Intrusive Original rock :Granite |
Structures |
| Location: | Type: | Orientation(360 gr.): | Relation to min.: | |
| Host rock | Joints/Fractures | Strike/Dip :124 / 76 | Pre-mineralisation ;...Effect :Controls |
Opplysning(er) i fritekstformat |
| Fri tekst |
| Mineraliseringen ble påvist av BP Norge A/S Minerals i forbindelse med oppfølging av geokjemiske gullanomalier under regional prospektering i Helgeland. Langs veien mellom Vandalsvik og Skomovik på vestsiden av Velfjord opptrer et massiv av lys grå turmalinførende toglimmergranitt som fører tidlige turmalin-kvartsganger lokalt med litt molybdenglans. Disse gjennomsettes av glassaktige kvartsganger som ofte viser mylonittisk tekstur og/eller duktil skjærdeformasjon av granitten langs ganggrensen og langs skjærplan inne i gangen. Magnetkisen ledsages av varierende mengde sinkblende, blyglans og lokalt noe arsenkis. Gangene er sjelden mer enn 10 cm brede og 5 cm lange. Helt lokalt finnes det stokkverk av 1-5 mm sulfidårer. |
Bibliography: |
| From NGU's Reference Archive: |
| Nordgulen, Øystein; Sundvoll, Bjørn , 1992 |
| Strontium isotope composition of the Bindal Batholith, Central Norwegian Caledonides |
| ;Norges geologiske undersøkelse;TIDSSKRIFTARTIKKEL;NGU Bulletin; No.423;19-39 pages |
| Abstract: | |
| Forkortet: A strontium isotope study of the Bindal Batholith has been carried out. The data generally do not permit precise and accurate age calculations; however, good estimates for initial Sr ratios are commonly obtained. Low initial ratios (c. 0.704-0.705) with little internal variation are present in granitoids in the southeastern part of the batholith. Rocks with intermediate initial ratios (0.705-0.710) predominate and are present throughout most of the batholith, whereas very high ratios (>0.715) are found in tourmaline granites and anatec- tic granitoids in the west. Considering a subduction related setting for the plutonism, the geographical distribution of Sr initial ratios would be consis- tent with a westward-dipping subduction zone. |
| Myrland, Rolf , 1972 |
| Velfjord. Beskrivelse til det berggrunnsgeologiske gradteigskart I 18 - 1:100 000. |
| ;Norges geologiske undersøkelse;KARTBESKRIVELSE; TIDSSKRIFTARTIKKEL;NGU; Skrifter; No.274; 1;1-30 + ka pages |
| Abstract: | |
| The various lithologies are described. These comprise granitic basements rocks of supposed Pre-Cambrian age and Cambro-Silurian supracrustals and intrusives. The intrusives are mostly found within the Bindal and Velfjord massifs. These massifs are younger than the supracrustals, but their mutual age relationship is uncertain. Tectonically the rocks are sitated in "the high metamorphic nappe-complex" of central and western Helgeland. The supracrustal rocks have undergone at least three phases of Caledonian folding, the F2 phase producing the main regional structures. The rocks have mineral assemblages which place them in the almandine-amphibolite metamorphic facies. |
Navn på sample point : Prøvepunkt 1 |
| (Objekt Id : 1813,024,00,01) |
| Lokalisering |
| Fylke : | Nordland (18) | Kommune : | Brønnøy (1813) |
| Kart 1:50000: | Velfjord (1825-4) | Kart 1:250000: | Mosjøen |
| Markeringspunkt: | Lengdegrad: | 12.4501360 | Breddegrad: | 65.4663240 |
| EU89-UTM Zone 33 | (Coordinates IS confirmed) |
| X-koord: | 381882 m. | Y-koord: | 7262818 m. |
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| Materialtype |
| Hovedtype: | Basemetaller (Cu,Zn,Pb,Fe sulfider,As,Sb,Bi,Sn) | Subtype: | Sink | |
| Element(s): | Zn Pb As |
Fieldsamples |
| Sample No. | Sample type | Miscellanrous | ||||
| B25-1 | Bedrock |
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| NO0838.04 | Bedrock |
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| NO0838.05 | Bedrock |
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| NO0838.06 | Bedrock |
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| 39/9089659 | Bedrock |
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| 39/9089660 | Bedrock |
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| NB! All analyse values are shown at the end of the printout.: |
Navn på locality : Steinbruddet |
| (Objekt Id : 1813,024,01,00) |
| Lokalisering |
| Fylke : | Nordland (18) | Kommune : | Brønnøy (1813) |
| Kart 1:50000: | Velfjord (1825-4) | Kart 1:250000: | Mosjøen |
| Markeringspunkt: | Lengdegrad: | 12.4505680 | Breddegrad: | 65.4663310 |
| EU89-UTM Zone 33 | (Coordinates IS confirmed) |
| X-koord: | 381902 m. | Y-koord: | 7262818 m. |
|
|
| Materialtype |
| Hovedtype: | Basemetaller (Cu,Zn,Pb,Fe sulfider,As,Sb,Bi,Sn) | Subtype: | Sink | |
| Element(s): | Zn Pb As |
| Production |
| Activity: | Prospektering | Reserves: | ||
| Prod. method: | Production: | |||
| Prod. status: | Volume of dump: |
Analyse Results |
| from |
| Forekomstområde 1813 - 024 Vandalsvik |
Element analyses |
( *=parts pr. million, #=parts pr.billion, Negative values means below detection limit value.) |
| Sample No. | Sample Type | Cu* | Zn* | Pb* | Co* | Ni* | Ag* | Au# |
| NO0838.04 | Bedrock | 363 | 11511 | 14633 | 24 | 19 | 57.7 | 53.0 |
| NO0838.05 | Bedrock | 18 | 36 | 22 | 2 | 2 | -.3 | 16.0 |
| NO0838.06 | Bedrock | 59 | 273 | 228 | 22 | 1 | 1.0 | 35.0 |
| ------------------ |
| Sample No. | Pt# | Pd# | Rh# | As* | Cd* | Ba* | Mo* | Sb* | Bi* |
| NO0838.04 | -3.0 | -3.0 | -5.0 | 4 | 287.4 | 3 | 1.00 | 4 | 210 |
| NO0838.05 | -3.0 | -3.0 | -5.0 | -2 | .4 | 13 | -1.00 | -2 | 3 |
| NO0838.06 | -3.0 | -3.0 | -5.0 | 3946 | 1.9 | 8 | 1.00 | -2 | 5 |
| ------------------ |
| Sample No. | S% | V* | Cr* | Mn* | Fe% | Th* | U* | W* | Sr* |
| NO0838.04 | 5.25 | 1 | 8 | 158 | 6.79 | 2.00 | -5.00 | -2 | 4.0 |
| NO0838.05 | .32 | 6 | 3 | 156 | 2.11 | 20.00 | 9.00 | -2 | 7.0 |
| NO0838.06 | .35 | -1 | 2 | 36 | 1.02 | 10.00 | 11.00 | -2 | 6.0 |
| ------------------ |
| Sample No. | La* | B* | |||||||
| NO0838.04 | 3.00 | 4 | |||||||
| NO0838.05 | 49.00 | 3 | |||||||
| NO0838.06 | 22.00 | 3 |
| Faktaarket ble generert 13.06.2026 |
| Spørsmål eller kommentarer vedrørende faktaarket kan mailes til: ressursdatabaser@ngu.no |
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