Norsk versjon
	THE ORE DATABASE
	Deposit Area 1739 - 039
	(Last updated 13.mar.2024)

Importance

Public:

International Importance (reg. 25.07.2018)

Economical:

Significant , (Confirmed 25.feb.2008 by Jan Sverre Sandstad)

Products

	Element/product	Crude ore grade or quality
	CU	1,0 %
	ZN	1.66 %

Operations

	From - To	Activity	Comments
	1912 - 1916	Core drilling
	1943 - 1945	Geophysics
	1956 - 1956	Test mining
	1963 - 1965	Geology
	1969 - 1972	Test mining	Company/Institution :Grong Gruber A/S
	1972 - 1998	Regular production	Company/Institution :Grong Gruber A/S, Norsulfid A/S

Mineralization

	Era:	Paleozoic	Period:	Ordovician
	Dating:		Method:
	Genesis:	Volcex	Form:	Plate
	Main texture:	Banded	Min. distribution:	Massive (>50 % ore minerals)

Main grain size:

Fine grained (< 1 mm)

Main alteration:

Albitisation

	Strike/Dip:	240 / 12	Direction:
			Plunge:

Stratigraphic classification of host rock

Era:

Paleozoic

Period:

	Province:	Caledonides
	Geotec.unit:	Køli Nappe Complex
	Tectonic complex:	Leipikvatndekket
	Igneous complex:

Group:

Røyrvikgruppen

Formation:

Mineralogy

	Relationship	Mineral	Amount
	Gangue mineral	Calcite	Major mineral (>10%)
	Gangue mineral	Amphibole	Subordinate mineral (1-10%)
	Gangue mineral	Quartz	Subordinate mineral (1-10%)
	Gangue mineral	Chlorite	Subordinate mineral (1-10%)
	Ore mineral	Pyrite	Major mineral (>10%)
	Ore mineral	Chalcopyrite	Subordinate mineral (1-10%)
	Ore mineral	Sphalerite	Subordinate mineral (1-10%)
	Ore mineral	Magnetite	Subordinate mineral (1-10%)
	Ore mineral	Pyrrhotite	Subordinate mineral (1-10%)
	Ore mineral	Silver	Accessory mineral (<1%)
	Ore mineral	Valleriite	Accessory mineral (<1%)
	Ore mineral	Ilmenite	Accessory mineral (<1%)
	Ore mineral	Cobaltite	Accessory mineral (<1%)
	Ore mineral	Arsenopyrite	Accessory mineral (<1%)
	Ore mineral	Galena	Accessory mineral (<1%)
	Ore mineral	Mackinawite	Accessory mineral (<1%)
	Ore mineral	Tetrahedrite	Accessory mineral (<1%)
	Ore mineral	Argentite	Accessory mineral (<1%)
	Ore mineral	Cubanite	Accessory mineral (<1%)

Lithology:

	Relationship	Rock	Origin
	Wall rock	Albitite	Extrusive Original rock :Basalt
			Metamorphic facies :Greenschist
	Wall rock	Greenstone	Extrusive Original rock :Basalt
			Metamorphic facies :Greenschist

Structures

	Location:	Type:	Orientation(360 gr.):	Relation to min.:
	Unknown	Fold axis		Post-mineralisation ;...Effect :Modifies

Information(s) in free text format

Free text

The Joma deposit is located in mafic metavolcanic rocks of the Røyrvik Group. The greenstones are underlain by recrystallised ribbon chert and graphitic phyllites which sit on a thick sequence of quartz- and calcareous phyllites. The greenstones are interpreted as having formed in an ocean island, probably in an off-axis setting. The massive sulphide deposit occurs at the interface between an older volcanic-intrusive complex and a younger volcanic-volcaniclastic sequence, which show WPB and MORB affinities, respectively. The feeder zone to the massive ore comprises extensive albitisation, chloritisation and quartz-sericite alteration associated with sulphide dissemination and stockwork veining. A general sulphide stratigraphy shows compositional changes from a thin Cu-rich (chalcopyrite-pyrrhotite) layer at the base, thinning westwards away from the feeder-zone and intercalated with numerous thin layers of magnetite, chlorite schist and albitite, and overlain by massive pyrite. At the eastern flank of the ore body, the feeder zone mineralisation is overlain by Zn-rich pyritic ore. The most Cu-rich ore is a tectonic breccias, which contains fragments of quartz, carbonate, pyrite and magnetite in a chalcopyrite-pyrrhotite matrix. Primary sulphide-breccia ore types also exist, and a palinspastic reconstruction of the Joma deposit suggests that the massive sulphides were deposited in a submarine environment, on top and adjacent to a major growth fault.

Bibliography:

From NGU's Reference Archive:

Foslie, S. , 1926

	Rapport over: Joma forekomst.

;Norges geologiske undersøkelse;FAGRAPPORT;Bergarkivet; No.BA 4296;5 pages

	Abstract:
	Rapporten opplyser om malmgehalter i feltet, og malmen deles i følgende produksjonstyper: I Kobbermalm II Kobberholdig svovelkis IIIa Kobberholdig sinkfattig svovelkis IIIb Kobberfattig, sinkholdig svovelkis IV Koberholdig oppredningsmalm Rapporten er skrevet før forekomsten er ferdig oppboret, og opererer med 12,15 mill tonn påvist og 4,48 mill tonn sannsynlig malm.

Bjørlykke, H. , 1959

	Rapport over: Undersøkelsesarbeidet i Jomafeltet.

;Norges geologiske undersøkelse;FAGRAPPORT;Bergarkivet; No.BA 4304;16 pages

	Abstract:
	Rapporten summerer alt som er gjort i og rapportert fra feltet fra det ble funnet i 1911 til dato. Følgende avsnitt finnes: 1. Malmberegning 2. Verdifulle bestandeler i malmen 3. Oppredningsmuligheter. 4. Vurdering av de tidligere utførte undersøkelser 5. Nyere undersøkelser 6. Forslag til videre undersøkelser.

Svinndal, S. , 1960

	Rapport over: Geologisk rapport, Joma.

;Norges geologiske undersøkelse;TEKNISK RAPPORT;Bergarkivet; No.BA 4283;6 pages

	Abstract:
	Rapporten gjRapporten gjør opp status for diamantboringer og prøvedrift pr. rapportdato. Vedlagt er borlog for to borhull, nr. 106 og 108.

Singsaas, Per , 1963

	Geofysisk undersøkelse Joma kisfelt.

;Norges geologiske undersøkelse;FAGRAPPORT;NGU-rapport; No.232-359;16 pages

Abstract:

Under 2. verdenskrig foretok Gesellschaft fur praktiche Lagerstattenforschung, Berlin, elektromagnetiske målinger over Joma-forekomsten og dens aller nærmeste omgivelser. (Rapport i Bergarkivet). Feltet er kartlagt geologisk av statsgeolog S. Foslie og professor Chr. Oftedal (kfr. NGU-publikasjon nr.202). Joma-forekomsten er undersøkt ved en rekke borhull fra dagen og er påvist til et vertikalt dyp av ca. 300 meter. En grunnstoll inn til forekomsten ble ferdig i 1961. De geofysiske målinger som nå er gjort dekker et areal på 21 km2, 14 km2 ble målt i 1958 og 7 km2 i 1962. Det ble utført Turammålinger på vanlig måte ut fra 5 konduktive kabelanlegg, tildels med direkte strøm- tilførsel til Joma-forekomsten. Det ble observert sterke indikasjoner på forekomsten som ble relativt nøye kartlagt. Malmsonens utgåender som er fulgt over en lengde av ca. 2 000 meter og for det aller meste er overdekket - danner en markert bue, Jomaombøyningen. Ellers i feltet ble det påvist en lang rekke tildels meget sterkt ledende soner som også tegner et klart bilde av Jomabuen. Disse soner - de aller fleste er sannsynligvis grafittførende - har ikke i vesentlig grad forstyrret målingene over Joma-forekomsten. På basis av stikningsnettet foretok geologene F. Skjerlie og T. H. Tan i 1958 en nøyere kartlegging av bergartsgrenser, strøk og fall etc.

Olsen, Jørn , 1980

	Genesis of the Joma stratiform sulfide deposit, central Norwegian Caledonides.

;E. Schweizerbart'sche Verlagsbuchhandlung, Stuttgart;TIDSSKRIFTARTIKKEL;Proceedings of the Fifth Quadrennial IAGOD Symposium.;745-757 pages

Abstract:

The Joma orebody is a massive, stratiform sulfide deposit interbedded in a rock series consisting of greenstones, phyllites, and quartzites, belonging to a weakly metamorphosed nappe sequence in the central Scandinavian Caledonides. The area has undergone at least two episodes of penetrative deformation. The orebody is situated within a sequence of basaltic greenstones of tholeiitic composition. Trace-element contents of the greenstone suggest formation in a back-arc basin. The deposit consists of two principal ore types: (1) a massive, pyritic layer with interbedded meta-limestone and lenses of chlorite schist and (2) a massive chalcopyrite/pyrrhotite ore containing layers, lenses, and rolled fragments of pyritic ore, chlorite, schist, and quartz. The genesis of the chalcopyrite-pyrrhotite ore is discussed in the light of its stratigraphic position.

Odling, Noelle E. , 1989

	The structural history of the Leipikvattnet Nappe in the Joma area of Nord Trøndelag, central Scandinavian Caldonides, Norway.

;Norsk geologisk forening;TIDSSKRIFTARTIKKEL;Norsk geologisk tidsskrift; No.69 (3);141-161 pages

Abstract:

The Leipikkvattnet Nappe in the Joma area is composed of the stratigraphic sequence, greenstone, quartzitic phyllite, graphitic phyllite, tectonically repeated by thrusting and locally overturned in the area of the Joma sulphide deposit. The greenstones (Røyrvik Group) are composed of massive and pillowed lava flows overlain by volcaniclastic deposits and are thought to represent the remnants of a basaltic sea mount or oceanic island. In the Joma area, D1 and D2 deformations are associated with movements on the major and internal thrust planes, whereas D3 and D4 postdate them. This sequence is correlated with deformation histories from the rest of the central Scandinavian Caledonides, using the major NE-SW trending folds to which the F3 Joma Synform belongs. D3 deformation is suggested, from lineation distributions and finite strain results, to have resulted from late movement of the Børgefjell massif. Subhorizontally oriented F4 folds are suggested to have formed in response to overburden pressure when horizontal stress was reduced over the crest of the rising massif.

References not to be found in NGU's Reference Archive.:

Reinsbakken, A. 1986: The Joma Cu-Zn massive sulphide deposit hosted by mafic metavolcanites. I Stephens, M.B. (red.): Stratabound sulphide deposits in the Central Scandinavian Caledonides. SGU Ca. 60, 45-50.

Haugen, A. 2001: Grong Gruber - en hjørnesteinsbedrift i indre Namdal. I Carstens, H. (red.) ...bygger i berge. Norsk bergindustriforening og Den Norske Bergingeniørforening, 132-133.

Fieldsamples

	Sample No.	Sample type	Miscellanrous
	Bh207, 10.00-15.00	Core	Sampler :T. Bjerkgård/J.S. Sandstad Comment :Fine grained pyrite ore No. of registrated element analyses = 1
	Bh207, 15.00-19.60	Core	Sampler :T. Bjerkgård/J.S. Sandstad Comment :Fine grained pyrite ore No. of registrated element analyses = 1

NB! All analyse values are shown at the end of the printout.:

Name of Locality : Elvegangen

(Object Id : 1739,039,01,00)

---

Location

County :

Nord-Trøndelag (17)

Municipality :

Røyrvik (1739)

Map 1:50000:

Jomafjellet (1924-1)

Map 1:250000:

Grong

Marking point:

Longitude:

13.8870460

Latitude:

64.8535650

EU89-UTM Zone 33

(Coordinates IS confirmed)

X-coord:

447231 m.

Y-coord:

7192598 m.

Commodity

	Main Type:	Base metals (Cu,Zn,Pb,Fe sulphides, As,Sb,Bi,Sn)	Sub Type:	Copper
			Element(s):	Cu Zn Kis

Production

	Activity:	Pitting	Reserves:
	Prod. method:		Production:
	Prod. status:		Volume of dump:

Name of Locality : Lindseth

(Object Id : 1739,039,02,00)

---

Location

County :

Nord-Trøndelag (17)

Municipality :

Røyrvik (1739)

Map 1:50000:

Jomafjellet (1924-1)

Map 1:250000:

Grong

Marking point:

Longitude:

13.8648980

Latitude:

64.8535780

EU89-UTM Zone 33

(Coordinates IS confirmed)

X-coord:

446181 m.

Y-coord:

7192618 m.

Commodity

	Main Type:	Base metals (Cu,Zn,Pb,Fe sulphides, As,Sb,Bi,Sn)	Sub Type:	Copper
			Element(s):	Cu Zn Kis

Production

	Activity:	Pitting	Reserves:
	Prod. method:		Production:
	Prod. status:		Volume of dump:

Fieldsamples

	Sample No.	Sample type	Miscellanrous
	1031	Bedrock	Comment :Lindseth skjerp. No. of registrated element analyses = 1
	1032	Bedrock	Comment :Lindseth skjerp. No. of registrated element analyses = 1
	1033	Bedrock	Comment :Lindseth skjerp. No. of registrated element analyses = 1
	1034	Bedrock	Comment :Lindseth skjerp. No. of registrated element analyses = 1
	1035	Bedrock	Comment :Lindseth skjerp. No. of registrated element analyses = 1
	1036	Bedrock	Comment :Lindseth skjerp. No. of registrated element analyses = 1

NB! All analyse values are shown at the end of the printout.:

Name of Locality : Sjapmelia (Joma syd)

(Object Id : 1739,039,03,00)

---

Location

County :

Nord-Trøndelag (17)

Municipality :

Røyrvik (1739)

Map 1:50000:

Jomafjellet (1924-1)

Map 1:250000:

Grong

Marking point:

Longitude:

13.8755950

Latitude:

64.8373260

EU89-UTM Zone 33

(Coordinates IS confirmed)

X-coord:

446656 m.

Y-coord:

7190798 m.

Commodity

	Main Type:	Base metals (Cu,Zn,Pb,Fe sulphides, As,Sb,Bi,Sn)	Sub Type:	Copper
			Element(s):	Cu Zn Kis

Production

	Activity:	Pitting	Reserves:
	Prod. method:		Production:
	Prod. status:		Volume of dump:

Name of Sample point : Bh 3135/3133

(Object Id : 1739,039,03,01)

---

Location

County :

Nord-Trøndelag (17)

Municipality :

Røyrvik (1739)

Map 1:50000:

Jomafjellet (1924-1)

Map 1:250000:

Grong

Marking point:

Longitude:

13.8703590

Latitude:

64.8527230

EU89-UTM Zone 33

(Coordinates IS confirmed)

X-coord:

446439 m.

Y-coord:

7192518 m.

Commodity

	Main Type:	Base metals (Cu,Zn,Pb,Fe sulphides, As,Sb,Bi,Sn)	Sub Type:	Copper
			Element(s):	Cu Zn Kis Co

Fieldsamples

	Sample No.	Sample type	Miscellanrous
	Bh3133, 11.00-12.00	Core	Sampler :T. Bjerkgård/J.S. Sandstad Comment :Lenses of pyrrhotite-chalcopyrite ore No. of registrated element analyses = 1
	Bh3135, 10.00-11.00	Core	Sampler :T. Bjerkgård/J.S. Sandstad Comment :Fine grained, massive pyrite-chalcopyrite ore No. of registrated element analyses = 1
	Bh3135, 13.40-14.40	Core	Sampler :T. Bjerkgård/J.S. Sandstad Comment :Lenses of pyrite-chalcopyrite ore No. of registrated element analyses = 1
	Bh3135, 4.00-5.00	Core	Sampler :T. Bjerkgård/J.S. Sandstad Comment :Massive pyrrhotite-chalcopyrite ore No. of registrated element analyses = 1
	Bh3135, 6.40-7.40	Core	Sampler :T. Bjerkgård/J.S. Sandstad Comment :Disseminated chalcopyrite-sphalerite No. of registrated element analyses = 1

NB! All analyse values are shown at the end of the printout.:

Name of Sample point : Bh 3118

(Object Id : 1739,039,03,02)

---

Location

County :

Nord-Trøndelag (17)

Municipality :

Røyrvik (1739)

Map 1:50000:

Jomafjellet (1924-1)

Map 1:250000:

Grong

Marking point:

Longitude:

13.8709380

Latitude:

64.8530060

EU89-UTM Zone 33

(Coordinates IS confirmed)

X-coord:

446467 m.

Y-coord:

7192550 m.

Commodity

	Main Type:	Base metals (Cu,Zn,Pb,Fe sulphides, As,Sb,Bi,Sn)	Sub Type:	Copper
			Element(s):	Cu Zn Kis Co

Fieldsamples

	Sample No.	Sample type	Miscellanrous
	Bh3118, 37.00-38.00	Core	Sampler :T. Bjerkgård/J.S. Sandstad Comment :Lenses of sphalerite-pyrite ore No. of registrated element analyses = 1
	Bh3118, 38.00-38.80	Core	Sampler :T. Bjerkgård/J.S. Sandstad Comment :Lenses of pyrite-chalcopyrite-sphalerite ore No. of registrated element analyses = 1

NB! All analyse values are shown at the end of the printout.:

Name of Sample point : Bh 3107

(Object Id : 1739,039,03,03)

---

Location

County :

Nord-Trøndelag (17)

Municipality :

Røyrvik (1739)

Map 1:50000:

Jomafjellet (1924-1)

Map 1:250000:

Grong

Marking point:

Longitude:

13.8812650

Latitude:

64.8511630

EU89-UTM Zone 33

(Coordinates IS confirmed)

X-coord:

446952 m.

Y-coord:

7192335 m.

Commodity

	Main Type:	Base metals (Cu,Zn,Pb,Fe sulphides, As,Sb,Bi,Sn)	Sub Type:	Copper
			Element(s):	Cu Zn Kis Co

Fieldsamples

	Sample No.	Sample type	Miscellanrous
	Bh3107, 1.00-2.00	Core	Sampler :T. Bjerkgård/J.S. Sandstad Comment :Fine grained pyrite-sphalerite ore No. of registrated element analyses = 1
	Bh3107, 3.00-4.00	Core	Sampler :T. Bjerkgård/J.S. Sandstad Comment :Fine grained pyrite ore No. of registrated element analyses = 1

NB! All analyse values are shown at the end of the printout.:

---

Analyse Results

from

Deposit Area 1739 - 039 Joma

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#
Bh207, 10.00-15.00	Core	8460	21700	1085	2	14	30.9	172.0
Bh207, 15.00-19.60	Core	2890	14050	669	4	8	15.2	165.0
Bh3107, 1.00-2.00	Core	6550	17500	509	50	14	22.0	180.0
Bh3107, 3.00-4.00	Core	6650	25000	339	6	2	28.0	214.0
Bh3118, 37.00-38.00	Core	6840	12600	282	142	14	6.6	77.0
Bh3118, 38.00-38.80	Core	40900	6580	162	583	19	29.9	165.0
Bh3133, 11.00-12.00	Core	77200	2420	22	200	20	32.8	131.0
Bh3135, 10.00-11.00	Core	13600	7940	124	198	3	8.5	99.0
Bh3135, 13.40-14.40	Core	14450	2500	203	198	12	8.1	73.0
Bh3135, 4.00-5.00	Core	14150	546	20	231	14	7.2	32.0
Bh3135, 6.40-7.40	Core	18800	1025	21	131	5	8.1	39.0
1031	Bedrock	3509	13830	380	6	10	7.8	284.0
1032	Bedrock	57693	2175	45	94	4	60.9	376.0
1033	Bedrock	16658	898	42	244	25	18.2	108.0
1034	Bedrock	4572	382	16	241	23	5.5	102.0
1035	Bedrock	4096	21817	916	8	14	11.0	296.0
1036	Bedrock	42977	3712	102	267	5	52.0	405.0

------------------

Sample No.	Pt#	Pd#	As*	Cd*	Ba*	Mo*	Sn*	Sb*	Bi*
Bh207, 10.00-15.00	2.5	.5	619	123.5	10	21.50	2	7	8
Bh207, 15.00-19.60	2.5	.5	544	75.4	10	18.75	2	8	8
Bh3107, 1.00-2.00	2.5	.5	946	91.6	5	17.25	1	7	8
Bh3107, 3.00-4.00	2.5	1.0	1055	106.5	5	31.70	1	8	3
Bh3118, 37.00-38.00	5.0	.5	249	63.4	20	13.30	2	5	5
Bh3118, 38.00-38.80	2.5	.5	358	37.4	10	13.40	1	9	5
Bh3133, 11.00-12.00	2.5	.5	16	19.1	40	5.65	0	1	2
Bh3135, 10.00-11.00	2.5	.5	258	46.8	5	14.40	1	11	7
Bh3135, 13.40-14.40	2.5	.5	223	11.0	40	5.81	1	8	4
Bh3135, 4.00-5.00	2.5	.5	20	3.5	40	5.75	0	1	6
Bh3135, 6.40-7.40	2.5	.5	62	5.8	5	5.07	0	2	4
1031	1.0	3.0	144	82.3	2	3.00		4	5
1032	1.0	3.0	79	18.5	5	1.00		3	18
1033	1.0	4.0	46	7.8	2	3.00		5	6
1034	2.0	2.0	35	2.3	2	4.00		2	2
1035	1.0	2.0	246	121.1	2	4.00		5	16
1036	1.0	3.0	48	24.9	2	3.00		2	64

------------------

Sample No.	Se*	Ga*	Ge*	In*	S%	V*	Cr*	Mn*	Fe%
Bh207, 10.00-15.00	32.00	5.96	0.28	0.60	10.00	22	5	340	42.90
Bh207, 15.00-19.60	19.00	8.24	0.29	0.32	10.00	19	5	251	39.10
Bh3107, 1.00-2.00	31.00	5.38	0.26	0.53	10.00	16	7	389	38.90
Bh3107, 3.00-4.00	13.00	2.17	0.26	0.14	10.00	7	2	455	40.80
Bh3118, 37.00-38.00	38.00	4.26	0.24	0.36	10.00	21	10	667	32.20
Bh3118, 38.00-38.80	113.00	3.20	0.46	0.90	10.00	13	8	296	38.60
Bh3133, 11.00-12.00	120.00	0.95	0.46	0.68	10.00	11	5	163	39.00
Bh3135, 10.00-11.00	62.00	1.49	0.31	0.48	10.00	6	2	139	42.10
Bh3135, 13.40-14.40	70.00	2.53	0.34	0.23	10.00	27	20	657	33.10
Bh3135, 4.00-5.00	122.00	1.65	0.49	0.53	10.00	6	5	355	46.90
Bh3135, 6.40-7.40	63.00	0.79	0.24	0.34	10.00	1	6	32	24.30
1031					40.80	1	3	95	25.50
1032					35.33	1	4	28	26.96
1033					38.73	1	1	28	29.38
1034					33.81	2	1	108	25.79
1035					37.52	1	3	101	20.70
1036					40.30	1	4	17	22.12

------------------

Sample No.	Th*	U*	W*	Rb*	Sr*	Y*	Zr*	Nb*	Ta*
Bh207, 10.00-15.00	0.01	1.30	0	0.4	41.8	1.4	1	0.05	0.03
Bh207, 15.00-19.60	0.02	1.50	0	0.4	47.0	1.0	4	0.10	0.03
Bh3107, 1.00-2.00	0.01	0.20	0	0.1	57.6	1.0	2	0.05	0.03
Bh3107, 3.00-4.00	0.01	0.50	0	0.1	37.0	0.1	-1	0.05	0.03
Bh3118, 37.00-38.00	0.02	0.90	0	2.8	232.0	2.4	4	0.10	0.03
Bh3118, 38.00-38.80	0.01	0.50	0	0.6	69.9	1.3	2	0.10	0.03
Bh3133, 11.00-12.00	0.01	0.10	0	1.8	31.6	1.0	1	0.05	0.07
Bh3135, 10.00-11.00	0.01	0.60	0	0.1	44.3	0.8	-1	0.05	0.03
Bh3135, 13.40-14.40	0.03	0.60	0	4.0	124.0	3.0	6	0.20	0.05
Bh3135, 4.00-5.00	0.01	0.10	0	4.4	43.8	1.0	2	0.10	0.03
Bh3135, 6.40-7.40	0.01	0.05	0	0.1	5.9	0.1	-1	0.05	0.03
1031	2.00	5.00	1		1.0
1032	3.00	5.00	3		2.0
1033	3.00	5.00	1		2.0
1034	2.00	5.00	1		2.0
1035	2.00	5.00	3		1.0
1036	2.00	5.00	6		2.0

------------------

Sample No.	Cs*	La*	Ce*	B*	Li*	Be*	P*	Sc*	Ti*
Bh207, 10.00-15.00	0.93	0.25	0.30		0	0	120	0.20	25
Bh207, 15.00-19.60	0.43	0.25	0.52		1	0	20	0.80	310
Bh3107, 1.00-2.00	0.09	0.25	0.35		2	0	20	2.10	210
Bh3107, 3.00-4.00	0.32	0.25	0.09		1	0	5	0.05	25
Bh3118, 37.00-38.00	5.15	0.25	0.80		2	0	100	1.60	380
Bh3118, 38.00-38.80	1.34	0.25	0.50		1	0	20	1.10	200
Bh3133, 11.00-12.00	2.98	0.25	0.23		0	0	10	2.10	120
Bh3135, 10.00-11.00	0.03	0.25	0.06		1	0	5	0.05	25
Bh3135, 13.40-14.40	0.29	0.25	1.12		6	0	80	3.20	770
Bh3135, 4.00-5.00	26.30	0.25	0.26		0	0	10	0.90	220
Bh3135, 6.40-7.40	0.03	0.25	0.05		0	0	5	0.05	25
1031		2.00		3
1032		2.00		2
1033		2.00		2
1034		2.00		2
1035		2.00		2
1036		2.00		2

------------------

Sample No.	Te*	Hf*	Re*	Tl*
Bh207, 10.00-15.00	2.95	0.10	0	3
Bh207, 15.00-19.60	3.98	0.10	0	3
Bh3107, 1.00-2.00	2.10	0.10	0	4
Bh3107, 3.00-4.00	1.04	0.05	0	9
Bh3118, 37.00-38.00	1.03	0.10	0	2
Bh3118, 38.00-38.80	2.57	0.10	0	1
Bh3133, 11.00-12.00	1.06	0.05	0	0
Bh3135, 10.00-11.00	3.49	0.05	0	1
Bh3135, 13.40-14.40	1.17	0.20	0	1
Bh3135, 4.00-5.00	1.55	0.10	0	0
Bh3135, 6.40-7.40	2.56	0.05	0	0
1031
1032
1033
1034
1035
1036

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The fact sheet was created on 28.04.2024

Questions or comments regarding the fact sheet can be emailed to: ressursdatabaser@ngu.no

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