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
Sampler :T. Bjerkgård
Comment :Massive pyrite-sphalerite in chlorite-quartz, some calcite
No. of registrated element analyses = 1
BH11/2: 21.70-22.50 Core
Sampler :T. Bjerkgård
Comment :Massive pyrite-sphalerite in chlorite-quartz, some calcite
No. of registrated element analyses = 1
BH13/2: 13.75-14.20 Core
Sampler :T. Bjerkgård
Comment :Massive pyrite in quartz, some chalcopyrite and sphalerite
No. of registrated element analyses = 1
BH13/2: 9.50-9.60 Core
Sampler :T. Bjerkgård
Comment :Massive pyrite with quartz matrix
No. of registrated element analyses = 1
BH16: 1.25-1.80 Core
Sampler :T. Bjerkgård
Comment :Massive pyrite-sphalerite-pyrrhotite, matrix of quartz with some calcite
No. of registrated element analyses = 1
BH16: 1.80-2.55 Core
Sampler :T. Bjerkgård
Comment :Massive pyrite-sphalerite-pyrrhotite, matrix of quartz with some calcite
No. of registrated element analyses = 1
BH16: 2.55-3.35 Core
Sampler :T. Bjerkgård
Comment :Quartz-sericite schist with mainly iron sulfides
No. of registrated element analyses = 1
BH16: 3.35-3.42 Core
Sampler :T. Bjerkgård
Comment :Massive pyrite-sphalerite, some chalcopyrite. Quartz-calcite matrix.
No. of registrated element analyses = 1
BH16: 3.55-3.64 Core
Sampler :T. Bjerkgård
Comment :Massive pyrite-sphalerite, some chalcopyrite. Quartz-calcite matrix.
No. of registrated element analyses = 1
BH2/1: 11.35-11.60 Core
Sampler :T. Bjerkgård
Comment :Quartz-sericite impregnation with pyrrhotite-sphalerite impregnation
No. of registrated element analyses = 1
BH2/1: 13.20-14.35 Core
Sampler :T. Bjerkgård
Comment :rich impregnation of pyrite, sphalerite and pyrrhotite in quartz-calcite matrix
No. of registrated element analyses = 1
BH2/1: 20.80-21.05 Core
Sampler :T. Bjerkgård
Comment :Quartz-sericite schist with sphalerite-chalcopyrite impregnation
No. of registrated element analyses = 1
BH2/1: 21.65-22.50 Core
Sampler :T. Bjerkgård
Comment :Massive pyrrhotite-pyrite with lesser sphalerite and chalcopyrite. Quartz-calcite matrix
No. of registrated element analyses = 1
BH2/1: 48.60-49.00 Core
Sampler :T. Bjerkgård
Comment :Rich pyrite-chalcopyrite-sphalerite impregnation in quartz-sericite-chlorite schist
No. of registrated element analyses = 1
BH2/1: 49.00-49.32 Core
Sampler :T. Bjerkgård
Comment :Rich pyrite-chalcopyrite-sphalerite impregnation in quartz-sericite-chlorite schist
No. of registrated element analyses = 1
BH3/2: 14.30-15.00 Core
Sampler :T. Bjerkgård
Comment :Semimassive chalcopyrite-pyrrhotite, some pyrite and sphalerite. Quartz-dominated matrix
No. of registrated element analyses = 1
BH3/2: 22.10-22.70 Core
Sampler :T. Bjerkgård
Comment :Massive pyrite-sphalerite in quartz-calcite matrix
No. of registrated element analyses = 1
BH3/2: 27.65-28.30 Core
Sampler :T. Bjerkgård
Comment :Rich pyrrhotite-chalcopyrite-sphalerite impr. in quartz-calcite with chlorite bands.
No. of registrated element analyses = 1
BH3/2: 33.75-34.30 Core
Sampler :T. Bjerkgård
Comment :Rich impr. of pyrite, sphalerite, chalcopyrite and pyrrhotite in quartz-chlorite
No. of registrated element analyses = 1
BH3/2: 7.80-8.40 Core
Sampler :T. Bjerkgård
Comment :massive sphalerite-pyrite. Quartz matrix.
No. of registrated element analyses = 1
BH5/3: 49.50-49.90 Core
Sampler :T. Bjerkgård
Comment :very rich impr. of pyrite, sphalerite and chalcopyrite in quartz-calcite-chlorite matrix.
No. of registrated element analyses = 1
BH8/2: 15.80-16.10 Core
Sampler :T. Bjerkgård
Comment :Massive chalcopyrite-sphalerite-pyrrhotite in quartz-calcite matrix
No. of registrated element analyses = 1
BH8/2: 23.35-23.75 Core
Sampler :T. Bjerkgård
Comment :Massive pyrite-sphalerite. Quartz-calcite matrix.
No. of registrated element analyses = 1
BH8/2: 25.15-25.40 Core
Sampler :T. Bjerkgård
Comment :Chlorite-quartz rock with rich pyrrhotite-chalcopyrite impregnation
No. of registrated element analyses = 1
BH8/2: 25.40-25.75 Core
Sampler :T. Bjerkgård
Comment :Massive pyrite-sphalerite-chalcopyrite in quartz-calcite
No. of registrated element analyses = 1
BH9/2: 11.15-11.36 Core
Sampler :T. Bjerkgård
Comment :Massive sphalerite with lesser pyrite and chalcopyrite. Quartz-calcite matrix.
No. of registrated element analyses = 1
BH9/2: 15.00-15.20 Core
Sampler :T. Bjerkgård
Comment :massive pyrrhotite-sphalerite-chalcopyrite with quartz-calcite matrix
No. of registrated element analyses = 1
BH9/2: 15.20-15.50 Core
Sampler :T. Bjerkgård
Comment :Pyrrhotite lenses with sphalerite and chalcopyrite in chlorite
No. of registrated element analyses = 1
BH9/2: 9.45-10.25 Core
Sampler :T. Bjerkgård
Comment :Chloritic quartz-sericite schist. Pyrrhotite with som sphalerite and chalcopyrite in zones of impregnation
No. of registrated element analyses = 1
HE0058.01 Dump
Sampler :T. Bjerkgård/...Stored :Løkken/...Size(kg) :3
Comment :Chlorite-quartz schist containing 2-4 cm massive pyrite-sphalerite bands.
No. of registrated element analyses = 1
HE0058.02 Dump
Sampler :T. Bjerkgård/...Stored :Løkken/...Size(kg) :3
Comment :Massive homogeneous pyrite-sphalerite ore. mm-sized sulfide grains.
No. of registrated element analyses = 1
HE0058.03 Dump
Sampler :T. Bjerkgård/...Stored :Løkken/...Size(kg) :3
Comment :Massive pyrite-sphalerite ore, 1-1.5 mm sulfide grains.
No. of registrated element analyses = 1
HE0058.04 Dump
Sampler :T. Bjerkgård/...Stored :Løkken/...Size(kg) :3
Comment :Semimassive pyrrhotite-chalcopyrite-pyrite ore with subordinate sphalerite in quartz.
No. of registrated element analyses = 1
HE0058.05 Dump
Sampler :T. Bjerkgård/...Stored :Løkken/...Size(kg) :3
Comment :Semimassive to rich impregnation of pyrite in chloritic sericite schist.
No. of registrated element analyses = 1
HE0058.06 Dump
Sampler :T. Bjerkgård/...Stored :Løkken/...Size(kg) :3
Comment :Quartz-chlorite schist with scattered 2-3 mm pyrite cubes.
No. of registrated element analyses = 1
HE0058.07 Dump
Sampler :T. Bjerkgård/...Stored :Løkken/...Size(kg) :3
Comment :Semimassive pyrite-chalcopyrite mineralization in matrix of quartz and carbonate.
No. of registrated element analyses = 1
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
Sampler :T. Bjerkgård/...Stored :Løkken/...Size(kg) :3
Comment :Weak impregnation of finegrained pyrrhotite and minor chalcopyrite in strongly silicified schist
No. of registrated element analyses = 1
HE0058.09 Dump
Sampler :T. Bjerkgård/...Stored :Løkken/...Size(kg) :3
Comment :Weak, finegrained pyrrhotite impregnation in strongly silicified schist with needles of amphibole. Minor chalcopyrite.
No. of registrated element analyses = 1
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
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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
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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
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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 04.05.2024
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