Fact Sheet for <b>Deposit 3907

					Norsk versjon
	THE ORE DATABASE
	Deposit 3907 - 001 Kodal
	(Object Id: 5794) (Last updated: 10.10.2023)

Location

County:

Vestfold

Municipality:

Sandefjord (3907)

Map 1:50000:

Sandefjord (1813-3)

Map 1:250000:

Oslo

Coordinate system:

EU89-UTM Zone 32

East:

559469 m.

North:

6565790 m.

Longitude:

10.0420120

Latitude:

59.2269670

Show on map

Resource

	Resource Type:	Ferrous metals(Fe, Mn, Ti)	Resource Subtype:	Iron-Titanium
			Element(s):	Fe Ti P REE

Importance

Raw material meaning:

Not Assessed (reg. 10.06.2015)

Resources and production

	Activity:	Exploration	Reserves:	48900 thousand tons
	Operating method:		Historical production:

Operations

From - To Activity Comments

Core drilling Company/Institution :Norsk Hydro

Investigated by Norsk Hydro in 1959-62, 1973-75 and 1983-84.

Mineralization

Era: Paleozoic Period: Permian

Dating: 300 million year Method:

Genesis: Orthomagmatic formation Form: Layer

Main texture: Structureless Min. distribution:

Main grain size: Main alteration:

Strike/Dip: Direction:

Plunge:

Ti-deposit type(s)

Main type: Magmatic Ilm/Mt-ratio:

Sub type: Mt +/- Ilm +/- Ap in mafic intrusion %TiO(Ore):

Titanium province: Deposits outside the Ti - provinces %P2O5(Ore):

Host rock: %MgO(Ilm): <1

Main Ti mineral: Ilmenite %V2O3(Mt): < 0.4

ppm U (Rutile):

Stratigraphic classification of host rock

Era: Paleozoic Period: Permian

Province: Oslo Region

Geotec.unit: Vestfold-Ringerike Graben

Tectonic complex:

Igneous complex:

Group: Formation:

Mineralogy

Relationship Mineral Amount

Gangue mineral Pyroxene Major mineral (>10%)

Gangue mineral Olivine Major mineral (>10%)

Gangue mineral Biotite Subordinate mineral (1-10%)

Gangue mineral Amphibole Subordinate mineral (1-10%)

Gangue mineral Feldspar Accessory mineral (<1%)

Gangue mineral Carbonate Accessory mineral (<1%)

Gangue mineral Nepheline Accessory mineral (<1%)

Ore mineral Ilmenomagnetite Major mineral (>10%)

Ore mineral Apatite Major mineral (>10%)

Ore mineral Ilmenite Major mineral (>10%)

Lithology:

Relationship Rock Origin

Host rock Magnetite pyroxenite

Wall rock Larvikite Intrusive

Information(s) in free text format

Free text

The Kodal deposit is situated in the Lågen valley 20 km north of Larvik. Discoveries of iron ores in the area dates back to around 1700, but attempts to utilise the deposits as iron ore failed due to the high titanium content. The first detailed description of the orebody was given by Brøgger (1898). Other contributions to the understanding of the mineralisation have been given by Nielsen (1967), Bergstøl (1972) and Lindberg (1985). The following information is entirely based on Lindberg (1985). The potential of the mineralisation as a phosphate resource was first recognised by V.M. Goldsmidt during World War 1 in an evaluation of Norwegian phosphate resources. Norsk Hydro considered the deposit as a possible source of apatite for its fertilize production at Herøya, and carried out investigations in 1959-62, 1973-75 and 1983-84. The Kodal orebody and associated low grade mineralisation are situated within a larvikite-lardalite ring complex occupying about 60% of the southern part of the Permian Oslo Rift. Regional geological mapping has revealed a close relationship between Fe-Ti-P mineralisation and the larvikite-lardalite massif. The mineralisation appears to be restricted to nepheline bearing larvikite. The concentrations of Fe-Ti oxides and apatite are closely associated with the development of modal layering in larvikite. Oxides and mafic silicates are often concentrated at the base of layers and diminish in amount upwards. In some cases these concentrations form minor orebodies some tens of m long and several dm thick. Concentrations of Fe-Ti oxides and apatite are especially well developed in the Kodal area, the Kjosen area, the Gloppe area and the Råsås area. Norsk Hydro has investigated all of these areas in detail. Although all of these areas contain minor orebodies, only the Kodal area is regarded to have an economic potential. The Kodal orebody is situated in densely wooded terrain approx. 150 m.a.s.l. 5 km E of Kvelde in the Lågen valley. The ore occurs in a topographic depression. Due to the limited number of exposures, the investigation of the orebody is to a large extent based on drill cores. A total of 60 drill cores have been put down in the area. 40 of these holes (totalling 2060 m) are less than 50 m long and 20 holes (totalling 4150) have length varying from 110 to 550 m. The orebody consists of a series of lenses of varying size and shape occurring along a zone with a total strike length of 1900 m. This zone has an overall E-W strike and dips 70-80 degrees to the S. A zone of impregnation in the country rock always borders the high-grade lenses. At the eastern end the ore body terminates in larvikite in a number of short, thin lenses arranged en echelon. The western end terminates against a large normarkite intrusion, which is younger than the ore body. Normarkite pegmatite dykes, rhomb-porphyry dykes and lamprophyre dykes also cut the orebody. The average composition of the massive ore is 17% apatite, 40% ilmenomagnetite, 8% ilmenite, 1% sulphides (mainly pyrite and chalcopyrite), 33.5% mafic silicates (pyroxene, amphibole, olivine, biotite) and 0.5% other minerals (feldspar, nepheline, carbonate). Modal analyses reported by Bergstøl (1972) show the following variations: apatite (15-24%), ilmenomagnetite (25-60%), ilmenite (5-15%), pyroxene + olivine (20-40%), biotite + amphbole (3-10%). A number of features in and around the ore body suggest that it originated by cumulus processes. These features include layering and mineralogical gradation, both in the high grade (massive) lenses and the low-grade impregnation zone, which resemble modal layering. In case of an open pit operation, the reserve including the disseminated ore to a cut off at 1% P (2.3% P2O5), are some 70 million tons. In an underground mine it would not be possible to include the disseminated ore; this reduce the mineable reserves to 35 million tons. As of 2016 a JORC-compliant resource of 49 Mt @ 0.5 % P cut-off has been defined by Kodal Minerals Ltd. JORC compliant resources amount to: 14.6 Mt indicated @ 5.18 % P2O5 and 24.12 % Fe; 34.3 Mt inferred @ 4.59 % P2O5 and 20.38 % Fe. The following products could be produced in both cases: (1) An apatite concentrate with 85 BPL (Bone Phosphate of Lime) with 17% P (40% P2O5), < 0.4% MgO and <0.17% Cl, with a recovery of 90%. (2) An ilmenomagnetite concentrate with 61% Fe and 9% TiO2. (3) An ilmenite concentrate with 44-45% TiO2. The apatite contains about 1% REE which constitutes a possible by-product.

Photo(s) from the Deposit area:

Photo no. 1 showing 2,5x"

Photo no. 2 showing 10x"

Photo no. 3 showing 50x"

Photo no. 4 showing 100x"

Bibliography:

From NGU's Reference Archive:

Dalsegg, Einar , 1974

VLF-målinger Kodalsfeltet. Hedrum/Andebu.

;Norges geologiske undersøkelse;FAGRAPPORT;NGU-rapport; No.1232;5 pages

Kihle, Ola , 1976

CP-målinger Kodal/Andebu, Grøsli Gruve/Flesberg.

;Norges geologiske undersøkelse;FAGRAPPORT;NGU-rapport; No.1344;4 pages

Abstract:

Det foreligger ingen formell rapport over målingene. Resultatene av målingene over Kodalforekomsten ble meddelt oppdragsgiver Norsk Hydro A/S i et brev samt et kart som viser potensialbildet over forekomsten. I tillegg til de ordinære CP-målinger i Kodal ble det foretatt ledningsevnemålinger på bakken og i de borhull som det ble jordet i. Den foreløpige konklusjon ut i fra CP-målingene over Kodalforekomsten: 1. Forekomsten går minst 1000 meter mot dypet, muligens betydelig dypere. 2. Det er ikke funnet grunnlag for å anta at fallet flater ut mot syd i de øverste 1000 meter. Det nevnte brev og kartbilag ligger i NGU's arkiv. Når det gjelder Grøsli gruve så viste det seg at borhullene som det skulle jordes i var tette. Målingene ble derfor ikke utført.

Sindre, Atle , 1983

Tyngdemålinger ved Kodal

;Norges geologiske undersøkelse;FAGRAPPORT;NGU-rapport; No.2095;8 pages

Abstract:

Tyngdemålinger ble utført langs tre profiler like nord for den kjente Jacupi- rangittforekomsten i Kodal. Hvert profil var 2 km langt, og det ble målt for hver 50 m. De to sørligste profilene viser klare positive anomalier. Modellberegninger viser hvilke anomalier en del tyngre kropper vil gi. Disse anomaliene er sammenlignet med de målte anomaliene. Det anbefales å undersøke geologien mer langs profilene og å gjøre flere tetthetsbestemmelser.

Stadheim, J. , 1938

Kodal, Andebu. (Fra J. Stadheims dagbok)

;Norges geologiske undersøkelse;FAGRAPPORT;Bergarkivet; No.BA 2754;2 pages

Abstract:

Rapporten er en renskrivning av dagbok fra en befaring av forekomsten. Det gis en del dimensjoner på forekomsten og historie om drift.

Lindberg, Per Aksel , 1985

Fe-Ti-P mineralizations in the Larvikite - Lardalite complex, Oslo Rift.

;Norges geologiske undersøkelse;TIDSSKRIFTARTIKKEL;NGU Bulletin; No.402;93-98 pages

Abstract:

The larvikite-lardalite complex in the southermost part of the Permian Oslo Rift hosts a number of Fe-Ti-P concentrations. Some of these have been investigated by Norsk Hydro a.s. with regard to their possible potential as phosphate resources. A short review of the relationship of the mineralization to the structure and petrology of the complex is given. The only occurrence with an economic potential, the Kodal orebody, is described in detail. The Kodal orebody represent a resource of 70 Mt. of ore minable in an open pit. The ore contains a total of 11.6 Mt. of phosphate.

Bergstøl, S. , 1972

The jacupirangite at Kodal, Vestfold, Norway - a potential magnetite, ilmenite and apatite ore.

;Springer-Verlag;ARTIKKEL;Mineralium Deposita; No.7 (3);233-246 pages

Starmer, I. , 1974

The terminations of the jacupirangite vein at Kodal, Vestfold

;Norsk Hydro / NGU;RAPPORT;NH-arkivet; No.NH 60;13+kart pages

Abstract:

Finnes også i perm NH 241

, 1961

Kodal. Kart og lengdeprofil 1:2000

;Norsk Hydro;KART;Bergarkivet; No.K 2801;1 kart pages

Abstract:

Med inntegnede malmganger

Kielland, Jacob , 1873

Kodalmalmen - supplerende geofysiske metoder

;Norsk Hydro;RAPPORT;Bergarkivet; No.BA 8202;28 pages

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

Stadheim, J. (1938): Kodal, Andebu (fra J. Stadheims dagbok). NGU Bergarkivrapport nr. 2754.

Goldschmidt, V.M. (1939): Fosfat-raastoffer1939. NGU Bergarkivrapport nr. 5005.

Nielsen, N. A. 1967: Kodal-forekomsten. Et industriobjekt i Vestfold. Tidskr. Kjemi, Bergv., Metallurgi 27, 73-76.

Brøgger, W.C. 1898: Die Eruptivgesteine des oslogebietes III. Das gangefolge des Laurdalits. Skr. Nor. Vid. Akad., I Mat.-Naturv. Kl. No. 6, 1-377.

Binns, R.A. 1967: Barroisite-bearing eclogite from Naustdal, Sogn og Fjordane, Norway. Journal of Petrology. 8; 3, 349-371.

Decree S., Coint, N., Debaille, V., Hagen-Peter, G., Leduc, T., Schiellerup, H., 2023. The potential for REEs in igneous-related apatite deposits in Europe. Geological Society, London, Special Publications, 526, https://doi.org/10.6084/m9.figshare.c.5913009

Fieldsamples

Sample No. Sample type Miscellanrous

Bergstol1 Bedrock

No. of registrated oxide analyses = 1

Bergstol2 Bedrock

No. of registrated oxide analyses = 1

Bergstol3 Bedrock

No. of registrated oxide analyses = 1

Kodal 3 Bedrock

Sampler: Peter Ihlen

Comment: fine-grained apatite magnetite pyroxene-rich rock

No. of registrated element analyses = 1

No. of registrated oxide analyses = 1

Kodal 4 Bedrock

Sampler: Peter Ihlen

Comment: fine-grained apatite magnetite pyroxene-rich rock

No. of registrated element analyses = 1

No. of registrated oxide analyses = 1

KODAL112566 Bedrock

Sampler: Peter Ihlen

Comment: fine-grained apatite magnetite pyroxene-rich rock

No. of registrated element analyses = 1

No. of registrated oxide analyses = 1

KODAL112567 Bedrock

Sampler: Peter Ihlen

Comment: fine-grained apatite magnetite pyroxene-rich rock

No. of registrated element analyses = 1

No. of registrated oxide analyses = 1

KODAL112568 Bedrock

Sampler: Peter Ihlen

Comment: fine-grained apatite magnetite pyroxene-rich rock

No. of registrated element analyses = 1

KODAL195773 Bedrock

Sampler: Peter Ihlen

Comment: fine-grained apatite magnetite pyroxene-rich rock

No. of registrated element analyses = 1

No. of registrated oxide analyses = 1

KODAL195775 Bedrock

Sampler: Peter Ihlen

Comment: fine-grained apatite magnetite pyroxene-rich rock

No. of registrated element analyses = 1

No. of registrated oxide analyses = 1

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

Analyse Results

from

Deposit Area 3907 - 001 Kodal

Element analyses
( *=parts pr. million, #=parts pr.billion, Negative values means below detection limit value.)

Sample No. Sample Type Cu* Zn* Pb* Co* Ni* Ba* Mo*

Kodal 3 Bedrock 235 480 -5 69 34 72 10.80

Kodal 4 Bedrock 216 452 -5 60 17 16 7.60

KODAL112566 Bedrock 84 549 -5 68 19 11 7.20

KODAL112567 Bedrock 32 502 -5 63 26 16 5.20

KODAL112568 Bedrock 79 390 -5 52 25 11 7.20

KODAL195773 Bedrock 156 323 50 28 141 5.20

KODAL195775 Bedrock 494 444 77 19 14 9.30

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

Sample No. Sn* Ga* V* Cr* Th* U* W* Rb* Sr*

Kodal 3 4 21.40 440 13 7.30 2.00 4 22.5 333.0

Kodal 4 4 22.70 609 14 5.40 1.60 4 10.8 179.0

KODAL112566 6 29.00 487 17 8.00 2.20 3 16.0 229.0

KODAL112567 5 22.50 402 16 12.00 3.40 1 124.0 222.0

KODAL112568 6 20.00 259 -5 8.10 2.20 4 9.6 199.0

KODAL195773 21.50 348 7 13.50 2.60 1 28.9 278.0

KODAL195775 25.10 408 -5 6.60 1.50 6 6.8 119.0

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

Sample No. Y* Zr* Nb* Ta* Cs* La* Ce* Pr* Nd*

Kodal 3 177.0 167 86.20 4.80 1.70 376.00 802.00 100.00 432.00

Kodal 4 144.0 225 80.60 4.40 -0.40 273.00 597.00 74.80 321.00

KODAL112566 170.0 237 94.80 5.00 0.50 380.00 820.00 94.30 383.00

KODAL112567 230.0 247 83.80 3.90 2.10 516.00 1120.00 125.00 506.00

KODAL112568 186.0 222 64.60 3.60 0.50 423.00 1000.00 110.00 435.00

KODAL195773 233.0 398 101.00 6.10 1.20 518.00 1070.00 133.00 546.00

KODAL195775 174.0 297 123.00 7.80 -0.40 348.00 710.00 91.90 380.00

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

Sample No. Sm* Eu* Gd* Tb* Dy* Ho* Er* Tm* Yb*

Kodal 3 74.00 12.00 53.90 7.30 36.10 6.70 15.30 1.90 9.70

Kodal 4 56.50 10.70 43.60 6.00 29.90 5.60 12.80 1.60 8.70

KODAL112566 66.10 12.60 49.40 6.80 34.00 6.40 15.10 1.90 10.20

KODAL112567 86.40 15.10 65.70 8.90 45.80 8.60 20.20 2.50 14.40

KODAL112568 73.00 13.40 54.90 7.60 38.80 7.30 17.40 2.20 12.40

KODAL195773 94.80 14.00 67.20 9.40 48.20 8.70 22.00 2.80 15.60

KODAL195775 66.80 10.50 50.80 6.90 36.60 6.70 17.20 2.20 12.00

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

Sample No. Lu* Be* F* Sc* Hf*

Kodal 3 1.40 1 0 32.40 4.40

Kodal 4 1.30 2 0 58.60 5.90

KODAL112566 1.50 -1 1 50.70 6.60

KODAL112567 2.00 2 1 60.00 7.00

KODAL112568 1.80 -1 1 68.90 7.70

KODAL195773 2.20 3 1 60.50 11.80

KODAL195775 1.80 -1 1 69.20 9.60

Oxide analyses
( All values are in % )

Sample No. Sample Type SiO2 Al2O3 TiO2 Fe2O3 FeO MnO MgO

Bergstol1 Bedrock 15.24 2.07 7.66 25.97 17.45 1.03 5.08

Bergstol2 Bedrock 11.57 3.46 8.48 28.48 17.45 1.20 4.99

Bergstol3 Bedrock 20.60 8.26 6.30 24.63 14.30 0.35 6.37

Kodal 3 Bedrock 14.20 3.16 8.62 43.10 0.67 5.82

Kodal 4 Bedrock 15.00 2.02 9.96 46.70 0.72 5.53

KODAL112566 Bedrock 10.30 2.01 10.10 53.50 0.91 4.06

KODAL112567 Bedrock 15.10 1.76 7.89 41.60 0.81 4.88

KODAL195773 Bedrock 24.00 3.98 6.34 34.20 0.71 5.48

KODAL195775 Bedrock 16.50 1.92 9.90 48.20 0.77 6.06

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

Sample No. CaO Na2O K2O P2O5 Co2 H2O Loss Sum

Bergstol1 0.39 0.27 7.78 0.08 0.57 84.00

Bergstol2 0.34 0.49 7.98 1.09 86.00

Bergstol3 0.65 0.31 5.13 0.61 88.00

Kodal 3 13.60 0.48 0.42 7.84 0.09 98.00

Kodal 4 13.10 0.24 0.16 6.11 -0.95 99.00

KODAL112566 12.70 -0.10 0.22 6.94 -1.42 99.00

KODAL112567 17.00 -0.10 0.84 8.91 -1.13 98.00

KODAL195773 16.00 0.94 0.61 6.55 -0.77 98.00

KODAL195775 12.60 -0.10 0.13 4.74 -1.15 100.00

From - To	Activity	Comments
	Core drilling	Company/Institution :Norsk Hydro
		Investigated by Norsk Hydro in 1959-62, 1973-75 and 1983-84.

Era:	Paleozoic	Period:	Permian
Dating:	300 million year	Method:
Genesis:	Orthomagmatic formation	Form:	Layer
Main texture:	Structureless	Min. distribution:

Main type:	Magmatic	Ilm/Mt-ratio:
Sub type:	Mt +/- Ilm +/- Ap in mafic intrusion	%TiO(Ore):
Titanium province:	Deposits outside the Ti - provinces	%P2O5(Ore):
Host rock:		%MgO(Ilm):	<1
Main Ti mineral:	Ilmenite	%V2O3(Mt):	< 0.4
		ppm U (Rutile):

	Province:	Oslo Region
	Geotec.unit:	Vestfold-Ringerike Graben
	Tectonic complex:
	Igneous complex:

Relationship	Mineral	Amount
Gangue mineral	Pyroxene	Major mineral (>10%)
Gangue mineral	Olivine	Major mineral (>10%)
Gangue mineral	Biotite	Subordinate mineral (1-10%)
Gangue mineral	Amphibole	Subordinate mineral (1-10%)
Gangue mineral	Feldspar	Accessory mineral (<1%)
Gangue mineral	Carbonate	Accessory mineral (<1%)
Gangue mineral	Nepheline	Accessory mineral (<1%)
Ore mineral	Ilmenomagnetite	Major mineral (>10%)
Ore mineral	Apatite	Major mineral (>10%)
Ore mineral	Ilmenite	Major mineral (>10%)

Relationship	Rock	Origin
Host rock	Magnetite pyroxenite
Wall rock	Larvikite	Intrusive

	Abstract:
	Rapporten er en renskrivning av dagbok fra en befaring av forekomsten. Det gis en del dimensjoner på forekomsten og historie om drift.

Sample No.	Sample Type	Cu*	Zn*	Pb*	Co*	Ni*	Ba*	Mo*
Kodal 3	Bedrock	235	480	-5	69	34	72	10.80
Kodal 4	Bedrock	216	452	-5	60	17	16	7.60
KODAL112566	Bedrock	84	549	-5	68	19	11	7.20
KODAL112567	Bedrock	32	502	-5	63	26	16	5.20
KODAL112568	Bedrock	79	390	-5	52	25	11	7.20
KODAL195773	Bedrock	156	323		50	28	141	5.20
KODAL195775	Bedrock	494	444		77	19	14	9.30

Sample No.	Sn*	Ga*	V*	Cr*	Th*	U*	W*	Rb*	Sr*
Kodal 3	4	21.40	440	13	7.30	2.00	4	22.5	333.0
Kodal 4	4	22.70	609	14	5.40	1.60	4	10.8	179.0
KODAL112566	6	29.00	487	17	8.00	2.20	3	16.0	229.0
KODAL112567	5	22.50	402	16	12.00	3.40	1	124.0	222.0
KODAL112568	6	20.00	259	-5	8.10	2.20	4	9.6	199.0
KODAL195773		21.50	348	7	13.50	2.60	1	28.9	278.0
KODAL195775		25.10	408	-5	6.60	1.50	6	6.8	119.0

Sample No.	Y*	Zr*	Nb*	Ta*	Cs*	La*	Ce*	Pr*	Nd*
Kodal 3	177.0	167	86.20	4.80	1.70	376.00	802.00	100.00	432.00
Kodal 4	144.0	225	80.60	4.40	-0.40	273.00	597.00	74.80	321.00
KODAL112566	170.0	237	94.80	5.00	0.50	380.00	820.00	94.30	383.00
KODAL112567	230.0	247	83.80	3.90	2.10	516.00	1120.00	125.00	506.00
KODAL112568	186.0	222	64.60	3.60	0.50	423.00	1000.00	110.00	435.00
KODAL195773	233.0	398	101.00	6.10	1.20	518.00	1070.00	133.00	546.00
KODAL195775	174.0	297	123.00	7.80	-0.40	348.00	710.00	91.90	380.00

Sample No.	Sm*	Eu*	Gd*	Tb*	Dy*	Ho*	Er*	Tm*	Yb*
Kodal 3	74.00	12.00	53.90	7.30	36.10	6.70	15.30	1.90	9.70
Kodal 4	56.50	10.70	43.60	6.00	29.90	5.60	12.80	1.60	8.70
KODAL112566	66.10	12.60	49.40	6.80	34.00	6.40	15.10	1.90	10.20
KODAL112567	86.40	15.10	65.70	8.90	45.80	8.60	20.20	2.50	14.40
KODAL112568	73.00	13.40	54.90	7.60	38.80	7.30	17.40	2.20	12.40
KODAL195773	94.80	14.00	67.20	9.40	48.20	8.70	22.00	2.80	15.60
KODAL195775	66.80	10.50	50.80	6.90	36.60	6.70	17.20	2.20	12.00

Sample No.	Lu*	Be*	F*	Sc*	Hf*
Kodal 3	1.40	1	0	32.40	4.40
Kodal 4	1.30	2	0	58.60	5.90
KODAL112566	1.50	-1	1	50.70	6.60
KODAL112567	2.00	2	1	60.00	7.00
KODAL112568	1.80	-1	1	68.90	7.70
KODAL195773	2.20	3	1	60.50	11.80
KODAL195775	1.80	-1	1	69.20	9.60

Sample No.	Sample Type	SiO2	Al2O3	TiO2	Fe2O3	FeO	MnO	MgO
Bergstol1	Bedrock	15.24	2.07	7.66	25.97	17.45	1.03	5.08
Bergstol2	Bedrock	11.57	3.46	8.48	28.48	17.45	1.20	4.99
Bergstol3	Bedrock	20.60	8.26	6.30	24.63	14.30	0.35	6.37
Kodal 3	Bedrock	14.20	3.16	8.62	43.10		0.67	5.82
Kodal 4	Bedrock	15.00	2.02	9.96	46.70		0.72	5.53
KODAL112566	Bedrock	10.30	2.01	10.10	53.50		0.91	4.06
KODAL112567	Bedrock	15.10	1.76	7.89	41.60		0.81	4.88
KODAL195773	Bedrock	24.00	3.98	6.34	34.20		0.71	5.48
KODAL195775	Bedrock	16.50	1.92	9.90	48.20		0.77	6.06

Sample No.	CaO	Na2O	K2O	P2O5	Co2	H2O	Loss	Sum
Bergstol1		0.39	0.27	7.78	0.08	0.57		84.00
Bergstol2		0.34	0.49	7.98		1.09		86.00
Bergstol3		0.65	0.31	5.13		0.61		88.00
Kodal 3	13.60	0.48	0.42	7.84			0.09	98.00
Kodal 4	13.10	0.24	0.16	6.11			-0.95	99.00
KODAL112566	12.70	-0.10	0.22	6.94			-1.42	99.00
KODAL112567	17.00	-0.10	0.84	8.91			-1.13	98.00
KODAL195773	16.00	0.94	0.61	6.55			-0.77	98.00
KODAL195775	12.60	-0.10	0.13	4.74			-1.15	100.00