Norsk versjon | |||||
THE ORE DATABASE | |||||
Occurence 5035 - 005 Høgberga | |||||
(Object Id: 35) (Last updated: 16.02.2005) |
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Location |
County: | Trøndelag | Municipality: | Stjørdal (5035) |
Map 1:50000: | Stjørdal (1621-1) | Map 1:250000: | Trondheim |
Coordinate system: | EU89-UTM Zone 32 |
East: | 594279 m. | North: | 7026392 m. |
Longitude: | 10.8843330 | Latitude: | 63.3537760 |
Show on map |
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Resource |
Resource Type: | Ferrous metals(Fe, Mn, Ti) | Resource Subtype: | Iron | |
Element(s): | Fe |
Importance |
Raw material meaning: | Little Importance (reg. 18.02.2015) |
Resources and production |
Activity: | Pitting | Reserves: | ||
Operating method: | Historical production: |
Operations |
From - To | Activity | Comments | |
1996 - 1996 | Sampling | Company/Institution :NGU |
Mineralization |
Era: | Paleozoic | Period: | ||
Genesis: | Volcex | Form: | Layer | |
Main texture: | Banded | Min. distribution: | Semi-massive (20-50 % ore minerals) |
Main grain size: | Fine grained (< 1 mm) | Main alteration: |
Strike/Dip: | Direction: | |||
Plunge: |
Stratigraphic classification of host rock |
Era: | Paleozoic | Period: |
Province: | Caledonides | |
Geotec.unit: | Trondheim Nappe Complex | |
Tectonic complex: | Støren Nappe | |
Igneous complex: |
Group: | Støren | Formation: |
Mineralogy |
Relationship | Mineral | Amount | |
Gangue mineral | Quartz | Major mineral (>10%) | |
Gangue mineral | Amphibole | Subordinate mineral (1-10%) | |
Ore mineral | Magnetite | Major mineral (>10%) | |
Ore mineral | Hematite | Subordinate mineral (1-10%) |
Lithology: |
Relationship | Rock | Origin | |
Host rock | Jasper | Sedimentary Original rock :Exhalite |
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Metamorphic facies :Greenschist | |||
Wall rock | Greenschist | Extrusive Original rock :Tuff |
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Metamorphic facies :Greenschist |
Information(s) in free text format |
Free text |
Forekomsten Høgberga ligger 200 m SV for ei bru over Nævra. Skjerpet er en 15 m lang vannfylt, grunn grøft langs underkant av 3 - 4 m høy skrent. I veggen er blottet jaspis med euhedral magnetitt og noe hematitt som disseminasjon og i årer og bånd (prøve 01). I nordveggen av grøfta (hengen?) er det finkornet grønnskifer med mm-cm-mektige kvarts-feltspatbånd/-linser med tilknyttet litt svovelkis. Det er to små skjerp henholdsvis 20 og 40 m mot øst i samme magnetitt-hematitt-mineraliserte jaspis. Mektigheten er vanskelig å anslå - minst 1 m. |
Bibliography: |
From NGU's Reference Archive: |
Vogt, J.H.L. , 1910 |
Norges jernmalmforekomster |
;Norges geologiske undersøkelse;TIDSSKRIFTARTIKKEL;NGU; No.51;225 pages |
Abstract: | |
Magmatische Ausscheidungen (I-VI). |
Torske, Tore , 1965 |
Geology of the Mostadmarka and Selbustrand area, Trøndelag. |
;Norges geologiske undersøkelse;TIDSSKRIFTARTIKKEL;NGU; No.232;1-83 + ka pages |
Abstract: | |
The bedrock of the area consists of metamorphic epiclastic, volcanic, and intrusive rocks of assumed Lower Ordovician age, assigned to, and lithologically matching the rocks of, the Røros, Støren and Lower Hovin Groups of the Trondheim Region. A detailed petrographic description of the rock varieties is given. The metamorphic grade of all rocks corresponds to the Greenschist Facies. - Small ore deposits occur in connection with the volcanic rocks. They comprise pyrite-pyrrhotite ores of the Leksdal Type, mixed pyrite-magnetite ores, and iron oxide ores. - Lithological variations of the sedimentary rocks is tentatively correlated with events during the early periods of the Caledonian Orogeny. - The volcanism within the area seems to have started with a phase of explosive activity, followed by extrusion (mostly submarine) of copious amounts of spilitic lavas; towards the end of the main period of volcanism a new episode of explosive activity has produced what is called the upper pyroclastic horizon, comprising rocks ranging from coarse volcanic breccia to finegrained tuffs. - The intrusive rocks consist mainly of saussurite gabbros and quartz keratophyres. The latter are thought to be intrusive rather than effusive, and evidence is offered to support this. In some places the character of pyroclastic material points to a quartz keratophyre parentage. Thus, quartz keratophyres may have occurred both as intrusive and volcanic rocks. |
Fieldsamples |
Sample No. | Sample type | Miscellanrous | ||||
NT0035.01 | Bedrock |
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NB! All analyse values are shown at the end of the printout.: |
Analyse Results |
from |
Deposit Area 5035 - 005 Høgberga |
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# |
NT0035.01 | Bedrock | 7 | 41 | 105 | 2 | 9 | -.3 | 3.0 |
------------------ |
Sample No. | Pt# | Pd# | Rh# | As* | Cd* | Ba* | Mo* | Sb* | Bi* |
NT0035.01 | 3.0 | 1.0 | -1.0 | -2 | -.2 | -1 | -1.00 | 4 | -2 |
------------------ |
Sample No. | S% | V* | Cr* | Mn* | Fe% | Th* | U* | W* | Sr* |
NT0035.01 | .19 | 55 | 1 | 316 | 12.88 | 2.00 | -5.00 | -2 | 13.0 |
------------------ |
Sample No. | La* | B* | |||||||
NT0035.01 | -1.00 | -3 |
The fact sheet was created on 25.04.2024 |
Questions or comments regarding the fact sheet can be emailed to: ressursdatabaser@ngu.no |
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