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Norsk versjon | ||||
THE ORE DATABASE | |||||
Deposit Area 439 - 006 | |||||
(Last updated 18.mar.2024) |
Name of Deposit Area : Nygruva |
(Object Id : 0439,006,00,00) |
Location |
County : | Hedmark (04) | Municipality : | Folldal (0439) |
Map 1:50000: | Folldal (1519-2) | Map 1:250000: | Røros |
Marking point: | Longitude: | 9.9044210 | Latitude: | 62.1092010 |
EU89-UTM Zone 32 | (Coordinates IS confirmed) |
X-coord: | 547200 m. | Y-coord: | 6886674 m. |
|
Commodity |
Main Type: | Base metals (Cu,Zn,Pb,Fe sulphides, As,Sb,Bi,Sn) | Sub Type: | Zinc | |
Element(s): | Kis Zn Cu |
Production |
Activity: | Mining | Reserves: | ||
Prod. method: | Underground mining | Production: | 300 thousand tons | |
Prod. status: | Disused, closed | Volume of dump: |
Importance |
Public: | Little Importance (reg. 18.02.2015) |
Economical: | Minor interest |
Products |
Element/product | Crude ore grade or quality | |
CU | 0.85 % | |
ZN | 3.5 % |
Operations |
From - To | Activity | Comments | |
1783 - 1787 | Regular production | Company/Institution :Fredriks Gave Verk | |
1842 - 1845 | Regular production | Company/Institution :Røros Kobberverk | |
1906 - 1940 | Test mining | Company/Institution :The Foldal Copper and Sulphur ltd. | |
1941 - 1952 | Regular production | Company/Institution :Folldal Verk A/S | |
1991 - 1994 | Detail mapping | Company/Institution :T. Bjerkgård, University of Oslo | |
1999 - 1999 | Sampling | Company/Institution :NGU mineralressurser |
Mineralization |
Era: | Paleozoic | Period: | Ordovician | |
Dating: | Method: | |||
Genesis: | Volcex | Form: | Layer | |
Main texture: | Banded | Min. distribution: | Massive (>50 % ore minerals) |
Main grain size: | Medium grained (1-3 mm) | Main alteration: | Chloritisation |
Strike/Dip: | 293 / 70 | Direction: | 270 | |
Plunge: | 15 |
Stratigraphic classification of host rock |
Era: | Paleozoic | Period: | Ordovician |
Province: | Caledonides | |
Geotec.unit: | Trondheim Nappe Complex | |
Tectonic complex: | Meråker Nappe | |
Igneous complex: |
Group: | Fundsjø | Formation: |
Mineralogy |
Relationship | Mineral | Amount | |
Gangue mineral | Calcite | Major mineral (>10%) | |
Gangue mineral | Quartz | Major mineral (>10%) | |
Gangue mineral | Chlorite | Subordinate mineral (1-10%) | |
Gangue mineral | Sericite | Subordinate mineral (1-10%) | |
Gangue mineral | Titanite | Accessory mineral (<1%) | |
Gangue mineral | Clinozoisite | Accessory mineral (<1%) | |
Gangue mineral | Biotite | Accessory mineral (<1%) | |
Gangue mineral | Dolomite | Accessory mineral (<1%) | |
Gangue mineral | Clinoamphibole | Accessory mineral (<1%) | |
Gangue mineral | Ankerite | Accessory mineral (<1%) | |
Ore mineral | Sphalerite | Major mineral (>10%) | |
Ore mineral | Chalcopyrite | Major mineral (>10%) | |
Ore mineral | Pyrite | Major mineral (>10%) | |
Ore mineral | Pyrrhotite | Major mineral (>10%) | |
Ore mineral | Galena | Subordinate mineral (1-10%) | |
Ore mineral | Magnetite | Accessory mineral (<1%) | |
Ore mineral | Altaite | Accessory mineral (<1%) | |
Ore mineral | Hessite | Accessory mineral (<1%) | |
Ore mineral | Pentlandite | Accessory mineral (<1%) | |
Ore mineral | Molybdenite | Accessory mineral (<1%) | |
Ore mineral | Arsenopyrite | Accessory mineral (<1%) | |
Ore mineral | Bismuth | Accessory mineral (<1%) | |
Ore mineral | Gold | Accessory mineral (<1%) |
Lithology: |
Relationship | Rock | Origin | |
Wall rock | Tuffite/chlorite schist | Sedimentary Original rock :Tuffite |
|
Metamorphic facies :Greenschist | |||
Wall rock | Quartz keratophyre | Extrusive Original rock :Rhyodacite |
|
Metamorphic facies :Greenschist |
Information(s) in free text format |
Free text |
Nygruva mine was in production in three periods from 1783 to 1952. In total 0.3 Mt ore was produced with 0.85 % Cu and 3.5 % Zn. The ruler-shaped deposit has a length of 680 m, width of 60-70 m and an average thickness of 3 m. Two normal-faults cut across the deposit of which the westernmost one marks the end of the known deposit. Investigations (as late as in 1990) to find the continuation have not been successful. The massive part of the ore is a banded pyrite-sphalerite ore with lesser chalcopyrite and pyrrhotite in a quartz-calcite matrix. In the stratigraphic footwall of the massive ore are irregular lenses of zinc- or copper-rich ore, which locally are enriched in gold (up to 7.1 ppm). |
Bibliography: |
From NGU's Reference Archive: |
Marlow, Wolmer , 1935 |
Foldal. Beskrivelse til geologiske rektangelkart. D. Grubebeskrivelser. 1. Beskrivelse av Foldals kisfelt: 1. Foldals verks gruber. 2. Statens kisanvisninger. 3. Grimsboskjerpene. 4. Rødalens grube. 5. Tronfjellets grube. 6. Verkjensdalens kisfelt. |
;Norges geologiske undersøkelse;KARTBESKRIVELSE; TIDSSKRIFTARTIKKEL;NGU; No.145;69-96 pages |
Riiber, Carl C. , 1923 |
Rapporter over kis -og kobbergruber og skjerp i Foldal, Dovre og Alvdal herreder. |
;Norges geologiske undersøkelse;FAGRAPPORT;Bergarkivet; No.BA 3194;25 pages |
Abstract: | |
Rapporten omfatter følgende gruver og skjerp: I. Foldals verks gruber: a. Hovedgruben. b. Nordre Gjeitryggen grube. c. Søndre jetryggen grube, d. Grev Moltke grube. e. Grimsdalen grube. f. Storthaab grube. g. Boksberg grube. II. Statens kisanvisninger: a. Skjerp øst for Foldals verks hovedgrube. b. Stretlien skjerp. c. Grimsdalen skjerp. III. Grimsbo kisskjerp. IV. Rødalens kobbergrube. V. Tronfjeldets kobbergruber. VI. Verkjendalens kisfelt. Rapporten beskriver forekomstenes beliggenhet, geologiske forhold, malmen, resultater av undersøkelser (boringer, analyser osv.), salgspriser, historiske forhold, juridiske forhold og kraftsituasjonen. Forekomstnr.: 1. 10963, 2. 10973 og 3. 10991. Forekomstens navn og koordinater: 1. Folldal 32 5521 68908, 2. Verkensdalen 32 5281 68816, 3. Gamle Tron 32 5862 68910. |
Aasgaard, Gunnar , 1935 |
Foldal. Beskrivelse til det geologiske rektangelkart. D. grubebeskrivelser. 1. Beskrivelse av Foldals kisfelt : geologisk oversikt |
;Norges geologiske undersøkelse;KARTBESKRIVELSE; TIDSSKRIFTARTIKKEL;NGU; No.145;65-68 pages |
Abstract: | |
In the territory covered by the map there are several mines and also useful rocks. The pyrites are of the greatest economical value. The most important among these are the Foldal mines. In the last three years 1932-1934 the yearly production has been about 40 000 to 50 000 tonn of pyrites containing 1.85-1.90% Cu and 45% S. Other pyrite mines not working at the present, however, are Røstvangen mines, Auma, Rødals- and St. Knuts mines and several smaller places. Of useful rocks there are soapstone occurrences in the Brekkebekkdal, at Strømsås, on the Strålsjøås, and on the Reinsliås. Limestone is found near the Randmelsøyr beside the Foldal road, at the north end of Savalen and in the neighbourhood of Røstvangen. The trondhjemite, which is a bright and pretty rock has been used as buildingstone. It is, however, not worked out at present in this district on account of the transport difficulties, but at Støren there is a quarry of it. There is also a slate quarry in the neighbourhood of Arleite beside the Foldal road. |
Riiber, C.C.; Aasgaard, Gunnar , 1935 |
Foldal. Beskrivelse til det geologiske rektangelkart. D. grubebeskrivelser. Beskrivelse av kis- og kobbergruber og skjerp i Foldal, Dovre og Alvdal herreder |
;Norges geologiske undersøkelse;KARTBESKRIVELSE; TIDSSKRIFTARTIKKEL;NGU; No.145;68-69 pages |
Bjerkgård, Terje , 1995 |
The stratabound massive sulfide deposits in the Folldal area, southern Trondheim region Caledonides, Norway. |
;UiO Geologisk fellesråd;AVHANDLING |
Bjerkgård, Terje; Bjørlykke, Arne , 1994 |
The stratabound sulphide deposits in the Folldal area, Southern Trondheim Region, Norway |
;Norsk geologisk forening;TIDSSKRIFTARTIKKEL;Norsk geologisk tidsskrift; No.74 (4);213-237 pages |
Abstract: | |
Frie emneord: Lagdelt, Malmgenese Five strata-bound massive sulphide deposits are situated at three different stratigraphic levels in the volcanogenic Fundsjø group in the Folldal area. The deposits are hosted in metabasalts, metarhyodacites and volcanoclastic rocks and belong to the Cu-Zn class of volcanic-associated massive sulphide deposits. The metal content of the deposits indicates that the sources of metals are underlying strata, possibly with a contribution from intrusives. Wall rock alteration varies according to differences in host rocks, and is probably a result of chemical variations of the host rocks, temperature differences and proximity to the hydrothermal vent. The clustering of deposits in the Folldal area is considered to be due to the occurrence of a large sub- volcanic trondhjemitic intrusion which acted as the major heat engine for convection. The small size of the deposits might be related to the shallow level of the intrusion. |
Sakshaug, G.F.; Brækken, H. , 1942 |
Elektromagnetisk undersøkelse Moltke Grube Vest |
;Norges geologiske undersøkelse;FAGRAPPORT;NGU-rapport; No.31;9 pages |
Sakshaug, G. F.; Brækken, H. , 1940 |
Elektromagnetisk undersøkelse Moltke Grube og Gjetryggen Søndre Grube. |
;Norges geologiske undersøkelse;FAGRAPPORT;NGU-rapport; No.21;23 pages |
Bugge, Arne , 1948 |
Rapport fra befaring ved Folldal gruver. |
;Norges geologiske undersøkelse;FAGRAPPORT;Bergarkivet; No.BA 784;5 pages |
Abstract: | |
Befaringsrapport for gruvene Nordre og Søndre Gjeiteryggen og Grev Moltke Gruve. Det fremgår av ovenstående utredning at gruvene er drevet på kislinjaler og linser. De enkelte kislinjalene er i forhold til andre kislinjaler i Tronheimsdistriktet av relativt liten utstrekning; men ved vellykkete skjerpningsarbeider i dagen og i gruvene har man stadig funnet nye linser og linjaler når de gamle er utdrevet. Gruvedriften blir på denne måten kostbar, da de nye forekomster stadig drar seg bort fra de gamle sjakter. |
References not to be found in NGU's Reference Archive.: |
Carstens, C.W. & Engzelius, J.G. 1946: Hvorledes den forkastede Moltkegang ble funnet. Tidsskr. for kjemi, bergvesen og metallurgi, 9, p.108-110. |
Heim, J.G. 1972: Zur geologie des Südlichen Trondheim-gebietes. Unpubl. Ph.D. thesis, Univ. Mainz, 156 pp. |
Bjerkgård, T. & Bjørlykke A.,1996: Sulfide deposits in Folldal, Southern Trondheim Region Caledonides, Norway: Source of metals and wall-rock alterations related to host rocks. Economic Geology vol.91, p.676-696. |
Per B. Støen 1948: Folldal Verk gjennom 200 år. Historiske trekk: 1748-1948. festskrift Folldal Verk A/S, 70 sider. |
Bjerkgård, T. & Bjørlykke, A. 1995: Geology of the Folldal area, southern Trondheim Region Caledonides, Norway. NGU bull. 426, p.53-75. |
Fieldsamples |
Sample No. | Sample type | Miscellanrous | ||||
BH11/2: 21.18-21.70 | Core |
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BH11/2: 21.70-22.50 | Core |
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BH13/2: 13.75-14.20 | Core |
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BH13/2: 9.50-9.60 | Core |
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BH16: 1.25-1.80 | Core |
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BH16: 1.80-2.55 | Core |
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BH16: 2.55-3.35 | Core |
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BH16: 3.35-3.42 | Core |
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BH16: 3.55-3.64 | Core |
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BH2/1: 11.35-11.60 | Core |
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BH2/1: 13.20-14.35 | Core |
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BH2/1: 20.80-21.05 | Core |
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BH2/1: 21.65-22.50 | Core |
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BH2/1: 48.60-49.00 | Core |
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BH2/1: 49.00-49.32 | Core |
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BH3/2: 14.30-15.00 | Core |
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BH3/2: 22.10-22.70 | Core |
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BH3/2: 27.65-28.30 | Core |
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BH3/2: 33.75-34.30 | Core |
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BH3/2: 7.80-8.40 | Core |
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BH5/3: 49.50-49.90 | Core |
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BH8/2: 15.80-16.10 | Core |
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BH8/2: 23.35-23.75 | Core |
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BH8/2: 25.15-25.40 | Core |
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BH8/2: 25.40-25.75 | Core |
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BH9/2: 11.15-11.36 | Core |
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BH9/2: 15.00-15.20 | Core |
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BH9/2: 15.20-15.50 | Core |
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BH9/2: 9.45-10.25 | Core |
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HE0058.01 | Dump |
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HE0058.02 | Dump |
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HE0058.03 | Dump |
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HE0058.04 | Dump |
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HE0058.05 | Dump |
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HE0058.06 | Dump |
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HE0058.07 | Dump |
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NB! All analyse values are shown at the end of the printout.: |
Name of Locality : Nygruvtjønna skjerp |
(Object Id : 0439,006,01,00) |
Location |
County : | Hedmark (04) | Municipality : | Folldal (0439) |
Map 1:50000: | Folldal (1519-2) | Map 1:250000: | Røros |
Marking point: | Longitude: | 9.9221220 | Latitude: | 62.1128350 |
EU89-UTM Zone 32 | (Coordinates IS confirmed) |
X-coord: | 548118 m. | Y-coord: | 6887092 m. |
|
Commodity |
Main Type: | Base metals (Cu,Zn,Pb,Fe sulphides, As,Sb,Bi,Sn) | Sub Type: | Zinc | |
Element(s): | Kis Zn Cu |
Production |
Activity: | Pitting | Reserves: | ||
Prod. method: | Production: | |||
Prod. status: | Volume of dump: |
Operations |
From - To | Activity | Comments | |
Pitting | Company/Institution :Folldal verk A/S | ||
1991 - 1994 | Detail mapping | Company/Institution :T. Bjerkgård, University of Oslo | |
1999 - 1999 | Sampling | Company/Institution :NGU mineralressurser |
Mineralogy |
Relationship | Mineral | Amount | |
Gangue mineral | Quartz | Major mineral (>10%) | |
Gangue mineral | Amphibole | Subordinate mineral (1-10%) | |
Ore mineral | Pyrrhotite | Major mineral (>10%) | |
Ore mineral | Chalcopyrite | Subordinate mineral (1-10%) |
Lithology: |
Relationship | Rock | Origin | |
Wall rock | Chlorite schist | Sedimentary Original rock :Tuffite |
|
Metamorphic facies :Greenschist | |||
Wall rock | Quartz keratophyre | Extrusive Original rock :Rhyodacite |
|
Metamorphic facies :Greenschist |
Information(s) in free text format |
Free text |
Skjerpet ligger like øst for Nygruvtjønna og består av en grøft ca. 30 m lang på tvers av strøket til bergartene, dvs. i NNV retning. 10 meter av grøfta i nord er inntil 3 meter dyp og 4 m bred mens resten av grøfta mot sør er gjengrodd og antakelig kun røsket ned på fast fjell. Mineralisering består vesentlig av meget finkornet magnetkis med underordnet kobberkis i sterkt silisifisert skifer (prøve HE0058.08). Stedvis opptrer opptil 1-2 cm lange uorienterte nåler av amfibol (prøve HE0058.09). |
Fieldsamples |
Sample No. | Sample type | Miscellanrous | ||||
HE0058.08 | Dump |
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HE0058.09 | Dump |
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NB! All analyse values are shown at the end of the printout.: |
Name of Locality : Nygruvhøgda skjerp |
(Object Id : 0439,006,02,00) |
Location |
County : | Hedmark (04) | Municipality : | Folldal (0439) |
Map 1:50000: | Folldal (1519-2) | Map 1:250000: | Røros |
Marking point: | Longitude: | 9.8983640 | Latitude: | 62.1065270 |
EU89-UTM Zone 32 | (Coordinates IS confirmed) |
X-coord: | 546888 m. | Y-coord: | 6886372 m. |
|
Commodity |
Main Type: | Base metals (Cu,Zn,Pb,Fe sulphides, As,Sb,Bi,Sn) | Sub Type: | Zinc | |
Element(s): | Kis Zn Cu |
Production |
Activity: | Pitting | Reserves: | ||
Prod. method: | Production: | |||
Prod. status: | Volume of dump: |
Operations |
From - To | Activity | Comments | |
Pitting | Company/Institution :Folldal Verk A/S | ||
1991 - 1994 | Detail mapping | Company/Institution :T. Bjerkgård, University of Oslo |
Mineralogy |
Relationship | Mineral | Amount | |
Gangue mineral | Chlorite | Major mineral (>10%) |
Lithology: |
Relationship | Rock | Origin | |
Wall rock | Chlorite schist | Sedimentary Original rock :Tuffite |
|
Metamorphic facies :Greenschist |
Information(s) in free text format |
Free text |
Skjerpet består av en 12 m lang og inntil 0.75 m dyp røskegrøft, dels gjengrodd. Grøfta er drevet på tvers av strøket, dvs. i VNV-ØNØ retning. Det er ikke funnet synlige sulfider her og bergarten i skjerpet er en noe rusten klorittskifer, sannsynligvis en noe omvandlet mafisk tuffitt. Skjerpet ligger i sørskråningen av Nygruvhøgda, ned mot Streitmyrene. |
Analyse Results |
from |
Deposit Area 439 - 006 Nygruva |
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# |
BH11/2: 21.18-21.70 | Core | 9620 | 56800 | 2140 | 86 | 50 | 25.0 | 320.0 |
BH11/2: 21.70-22.50 | Core | 5540 | 99700 | 3930 | 55 | 50 | 22.0 | 260.0 |
BH13/2: 13.75-14.20 | Core | 12000 | 11900 | 5890 | 100 | 50 | 58.0 | 770.0 |
BH13/2: 9.50-9.60 | Core | 3140 | 7760 | 3200 | 48 | 300 | 16.0 | 120.0 |
BH16: 1.25-1.80 | Core | 11200 | 74400 | 7230 | 46 | 50 | 72.0 | 400.0 |
BH16: 1.80-2.55 | Core | 6970 | 95500 | 11300 | 46 | 50 | 92.0 | 460.0 |
BH16: 2.55-3.35 | Core | 4360 | 5640 | 545 | 9 | 50 | 9.0 | 76.0 |
BH16: 3.35-3.42 | Core | 11700 | 73800 | 118 | 87 | 50 | 24.0 | 270.0 |
BH16: 3.55-3.64 | Core | 1520 | 81400 | 4500 | 75 | 50 | 28.0 | 170.0 |
BH2/1: 11.35-11.60 | Core | 4430 | 7930 | 2340 | 62 | 50 | 26.0 | 42.0 |
BH2/1: 13.20-14.35 | Core | 3410 | 43700 | 3800 | 92 | 50 | 37.0 | 72.0 |
BH2/1: 20.80-21.05 | Core | 16200 | 33500 | 1620 | 25 | 50 | 41.0 | 57.0 |
BH2/1: 21.65-22.50 | Core | 3070 | 11600 | 663 | 310 | 100 | 18.0 | 34.0 |
BH2/1: 48.60-49.00 | Core | 18700 | 23500 | 6920 | 140 | 50 | 71.0 | 2200.0 |
BH2/1: 49.00-49.32 | Core | 14000 | 15000 | 3140 | 160 | 50 | 62.0 | 2600.0 |
BH3/2: 14.30-15.00 | Core | 68000 | 21000 | 1600 | 440 | 50 | 120.0 | 670.0 |
BH3/2: 22.10-22.70 | Core | 4560 | 92100 | 4080 | 100 | 50 | 41.0 | 190.0 |
BH3/2: 27.65-28.30 | Core | 7990 | 14800 | 70 | 220 | 400 | 25.0 | 510.0 |
BH3/2: 33.75-34.30 | Core | 35200 | 21700 | 4050 | 110 | 100 | 96.0 | 7100.0 |
BH3/2: 7.80-8.40 | Core | 7390 | 46700 | 3180 | 110 | 50 | 36.0 | 230.0 |
BH5/3: 49.50-49.90 | Core | 7120 | 41900 | 9240 | 140 | 50 | 54.0 | 460.0 |
BH8/2: 15.80-16.10 | Core | 21500 | 40000 | 4040 | 49 | 50 | 35.0 | 48.0 |
BH8/2: 23.35-23.75 | Core | 3010 | 63400 | 4140 | 160 | 50 | 24.0 | 130.0 |
BH8/2: 25.15-25.40 | Core | 17300 | 2660 | 73 | 45 | 50 | 30.0 | 190.0 |
BH8/2: 25.40-25.75 | Core | 52400 | 33800 | 2620 | 150 | 50 | 69.0 | 490.0 |
BH9/2: 11.15-11.36 | Core | 797 | 130400 | 7950 | 53 | 50 | 11.0 | 57.0 |
BH9/2: 15.00-15.20 | Core | 8540 | 35400 | 3390 | 95 | 100 | 14.0 | 33.0 |
BH9/2: 15.20-15.50 | Core | 3970 | 3840 | 22 | 31 | 50 | 2.5 | 8.0 |
BH9/2: 9.45-10.25 | Core | 1350 | 9850 | 571 | 41 | 50 | 10.0 | 7.0 |
HE0058.01 | Dump | 1752 | 47728 | 4128 | 111 | 21 | 27.9 | 366.0 |
HE0058.02 | Dump | 8612 | 43175 | 5108 | 93 | 11 | 40.6 | 166.0 |
HE0058.03 | Dump | 707 | 54494 | 1101 | 145 | 16 | 13.3 | 111.0 |
HE0058.04 | Dump | 20425 | 3507 | 122 | 375 | 7 | 47.4 | 820.0 |
HE0058.05 | Dump | 6531 | 11573 | 2036 | 117 | 24 | 20.4 | 401.0 |
HE0058.06 | Dump | 144 | 438 | 27 | 16 | 30 | .2 | 11.0 |
HE0058.07 | Dump | 19703 | 14183 | 140 | 105 | 4 | 39.5 | 1541.0 |
HE0058.08 | Dump | 148 | 102 | 13 | 15 | 5 | .2 | 23.0 |
HE0058.09 | Dump | 82 | 76 | 5 | 20 | 5 | -.1 | 7.0 |
------------------ |
Sample No. | As* | Cd* | Ba* | Mo* | Sn* | Sb* | Bi* | Se* | Ga* |
BH11/2: 21.18-21.70 | 89 | 21.00 | 0 | 26 | 79.00 | ||||
BH11/2: 21.70-22.50 | 190 | 24.00 | 1 | 37 | 48.00 | ||||
BH13/2: 13.75-14.20 | 240 | 41.00 | 2 | 28 | 96.00 | ||||
BH13/2: 9.50-9.60 | 120 | 34.00 | 2 | 14 | 57.00 | ||||
BH16: 1.25-1.80 | 1100 | 27.00 | 28 | 50.00 | |||||
BH16: 1.80-2.55 | 1600 | 53.00 | 25 | 56.00 | |||||
BH16: 2.55-3.35 | 87 | 10.00 | 2 | 2 | 5.00 | ||||
BH16: 3.35-3.42 | 250 | 20.00 | 1 | 2 | 55.00 | ||||
BH16: 3.55-3.64 | 370 | 25.00 | 9 | 4 | 62.00 | ||||
BH2/1: 11.35-11.60 | 160 | 19.00 | 8 | 7 | 23.00 | ||||
BH2/1: 13.20-14.35 | 210 | 23.00 | 10 | 12 | 40.00 | ||||
BH2/1: 20.80-21.05 | 3 | 53.00 | 1 | 15 | 28.00 | ||||
BH2/1: 21.65-22.50 | 160 | 18.00 | 2 | 37 | 43.00 | ||||
BH2/1: 48.60-49.00 | 210 | 50.00 | 3 | 40 | 140.00 | ||||
BH2/1: 49.00-49.32 | 60 | 18.00 | 1 | 30 | 72.00 | ||||
BH3/2: 14.30-15.00 | 140 | 23.00 | 1 | 34 | 240.00 | ||||
BH3/2: 22.10-22.70 | 280 | 43.00 | 6 | 17 | 97.00 | ||||
BH3/2: 27.65-28.30 | 12 | 14.00 | 0 | 5 | 40.00 | ||||
BH3/2: 33.75-34.30 | 110 | 39.00 | 1 | 23 | 84.00 | ||||
BH3/2: 7.80-8.40 | 620 | 46.00 | 5 | 22 | 60.00 | ||||
BH5/3: 49.50-49.90 | 100 | 39.00 | 2 | 37 | 120.00 | ||||
BH8/2: 15.80-16.10 | 1 | 24.00 | 1 | 18 | 66.00 | ||||
BH8/2: 23.35-23.75 | 410 | 27.00 | 3 | 30 | 100.00 | ||||
BH8/2: 25.15-25.40 | 30 | 37.00 | 0 | 2 | 55.00 | ||||
BH8/2: 25.40-25.75 | 430 | 25.00 | 2 | 38 | 89.00 | ||||
BH9/2: 11.15-11.36 | 8 | 31.00 | 1 | 40 | 92.00 | ||||
BH9/2: 15.00-15.20 | 140 | 37.00 | 2 | 14 | 62.00 | ||||
BH9/2: 15.20-15.50 | 1 | 6.00 | 0 | 2 | 5.00 | ||||
BH9/2: 9.45-10.25 | 21 | 17.00 | 0 | 2 | 5.00 | ||||
HE0058.01 | 806 | 180.1 | 4 | 24.00 | 2 | 7 | 23 | 64.00 | 3.00 |
HE0058.02 | 555 | 164.9 | 3 | 4.00 | 1 | 10 | 24 | 39.00 | 2.00 |
HE0058.03 | 129 | 188.3 | 3 | 13.00 | 2 | -1 | 13 | 88.00 | 3.00 |
HE0058.04 | 70 | 16.5 | 2 | 5.00 | 3 | 1 | 11 | 72.00 | -1.00 |
HE0058.05 | 424 | 75.3 | 7 | 22.00 | 3 | 5 | 15 | 58.00 | 8.00 |
HE0058.06 | 15 | .2 | 13 | 6.00 | -1 | 1 | -1 | 1.00 | 8.00 |
HE0058.07 | 89 | 81.9 | 2 | 11.00 | 1 | 2 | 8 | 95.00 | 2.00 |
HE0058.08 | -1 | .2 | 9 | 1.00 | -1 | -1 | -1 | 1.00 | 7.00 |
HE0058.09 | -1 | .3 | 4 | 2.00 | -1 | -1 | -1 | -1.00 | 5.00 |
------------------ |
Sample No. | In* | S% | V* | Cr* | Mn* | Fe% | Th* | U* | W* |
BH11/2: 21.18-21.70 | 34.99 | 100 | 2.60 | ||||||
BH11/2: 21.70-22.50 | 39.62 | 30 | 3.30 | ||||||
BH13/2: 13.75-14.20 | 30.38 | 190 | 3.40 | ||||||
BH13/2: 9.50-9.60 | 21.46 | 190 | 4.10 | ||||||
BH16: 1.25-1.80 | 46.73 | 90 | 5.00 | ||||||
BH16: 1.80-2.55 | 49.06 | 80 | 1.50 | ||||||
BH16: 2.55-3.35 | 3.71 | 90 | 1.80 | ||||||
BH16: 3.35-3.42 | 26.08 | 150 | 3.30 | ||||||
BH16: 3.55-3.64 | 42.26 | 100 | 3.30 | ||||||
BH2/1: 11.35-11.60 | 14.80 | 110 | 11.80 | ||||||
BH2/1: 13.20-14.35 | 31.30 | 70 | 1.80 | ||||||
BH2/1: 20.80-21.05 | 16.28 | 90 | 5.60 | ||||||
BH2/1: 21.65-22.50 | 27.98 | 80 | 1.80 | ||||||
BH2/1: 48.60-49.00 | 27.65 | 200 | 5.30 | ||||||
BH2/1: 49.00-49.32 | 13.28 | 80 | 1.10 | ||||||
BH3/2: 14.30-15.00 | 35.02 | 120 | 2.70 | ||||||
BH3/2: 22.10-22.70 | 39.27 | 90 | 2.60 | ||||||
BH3/2: 27.65-28.30 | 11.81 | 690 | 1.00 | ||||||
BH3/2: 33.75-34.30 | 19.71 | 150 | 2.80 | ||||||
BH3/2: 7.80-8.40 | 48.99 | 110 | 2.70 | ||||||
BH5/3: 49.50-49.90 | 22.52 | 220 | 3.80 | ||||||
BH8/2: 15.80-16.10 | 34.95 | 40 | 0.80 | ||||||
BH8/2: 23.35-23.75 | 50.39 | 150 | 2.50 | ||||||
BH8/2: 25.15-25.40 | 9.00 | 120 | 4.40 | ||||||
BH8/2: 25.40-25.75 | 43.77 | 90 | 1.70 | ||||||
BH9/2: 11.15-11.36 | 30.70 | 60 | 2.60 | ||||||
BH9/2: 15.00-15.20 | 34.82 | 120 | 0.60 | ||||||
BH9/2: 15.20-15.50 | 1.49 | 270 | 0.25 | ||||||
BH9/2: 9.45-10.25 | 5.66 | 140 | 0.70 | ||||||
HE0058.01 | -1.00 | 21.06 | 12 | 12 | 938 | 28.46 | -1.00 | 4.00 | 6 |
HE0058.02 | -1.00 | 20.25 | 6 | 23 | 258 | 37.32 | -1.00 | 2.00 | 5 |
HE0058.03 | 1.00 | 24.53 | 3 | 13 | 725 | 33.43 | -1.00 | 3.00 | 6 |
HE0058.04 | -1.00 | 9.91 | -2 | 19 | 809 | 20.55 | -1.00 | -1.00 | 7 |
HE0058.05 | -1.00 | 27.06 | 7 | 16 | 260 | 28.37 | 1.00 | 3.00 | 6 |
HE0058.06 | -1.00 | .70 | 11 | 45 | 431 | 3.21 | 2.00 | 4.00 | 3 |
HE0058.07 | -1.00 | 19.93 | -2 | 15 | 562 | 27.67 | -1.00 | 1.00 | 7 |
HE0058.08 | -1.00 | 1.77 | 102 | 9 | 928 | 5.19 | -1.00 | -1.00 | 5 |
HE0058.09 | -1.00 | 1.55 | 64 | 11 | 501 | 4.05 | -1.00 | -1.00 | 6 |
------------------ |
Sample No. | Sr* | La* | B* | Te* | Hg* | Tl* | |||
BH11/2: 21.18-21.70 | |||||||||
BH11/2: 21.70-22.50 | |||||||||
BH13/2: 13.75-14.20 | |||||||||
BH13/2: 9.50-9.60 | |||||||||
BH16: 1.25-1.80 | |||||||||
BH16: 1.80-2.55 | |||||||||
BH16: 2.55-3.35 | |||||||||
BH16: 3.35-3.42 | |||||||||
BH16: 3.55-3.64 | |||||||||
BH2/1: 11.35-11.60 | |||||||||
BH2/1: 13.20-14.35 | |||||||||
BH2/1: 20.80-21.05 | |||||||||
BH2/1: 21.65-22.50 | |||||||||
BH2/1: 48.60-49.00 | |||||||||
BH2/1: 49.00-49.32 | |||||||||
BH3/2: 14.30-15.00 | |||||||||
BH3/2: 22.10-22.70 | |||||||||
BH3/2: 27.65-28.30 | |||||||||
BH3/2: 33.75-34.30 | |||||||||
BH3/2: 7.80-8.40 | |||||||||
BH5/3: 49.50-49.90 | |||||||||
BH8/2: 15.80-16.10 | |||||||||
BH8/2: 23.35-23.75 | |||||||||
BH8/2: 25.15-25.40 | |||||||||
BH8/2: 25.40-25.75 | |||||||||
BH9/2: 11.15-11.36 | |||||||||
BH9/2: 15.00-15.20 | |||||||||
BH9/2: 15.20-15.50 | |||||||||
BH9/2: 9.45-10.25 | |||||||||
HE0058.01 | 17.0 | 2.00 | -1 | 19.00 | 7 | 1 | |||
HE0058.02 | 10.0 | -1.00 | -1 | 18.00 | 4 | -1 | |||
HE0058.03 | 51.0 | 2.00 | -1 | 12.00 | 3 | -1 | |||
HE0058.04 | 68.0 | -1.00 | -1 | 21.00 | -1 | -1 | |||
HE0058.05 | 14.0 | 4.00 | -1 | 11.00 | 1 | 7 | |||
HE0058.06 | 37.0 | 8.00 | 1 | -1.00 | -1 | 7 | |||
HE0058.07 | 78.0 | -1.00 | -1 | 14.00 | -1 | -1 | |||
HE0058.08 | 11.0 | 2.00 | -1 | -1.00 | -1 | -1 | |||
HE0058.09 | 9.0 | -1.00 | -1 | -1.00 | -1 | -1 |
The fact sheet was created on 18.02.2025 |
Questions or comments regarding the fact sheet can be emailed to: ressursdatabaser@ngu.no |
Copyright © 2025 Geological Survey of Norway |