Norsk versjon | |||||
THE INDUSTRIAL MINERAL DATABASE | |||||
Deposit Area 1718 - 303 | |||||
(Last updated 22.jul.2004) |
Name of Deposit Area : Storlia |
(Object Id : 1718,303,00,00) |
Location |
County : | Nord-Trøndelag (17) | Municipality : | Leksvik (1718) |
Map 1:50000: | Leksvik (1622-3) | Map 1:250000: | Trondheim |
Marking point: | Longitude: | 10.5271520 | Latitude: | 63.6892830 |
EU89-UTM Zone 32 | (Coordinates IS confirmed) |
X-coord: | 575519 m. | Y-coord: | 7063293 m. |
|
Commodity |
Main Type: | Carbonates | Sub Type: | Limestone |
Production |
Activity: | Mining | Reserves: | 200 thousand tons | |
Prod. method: | Open pit mining | Production: | 0 thousand tons | |
Prod. status: | Disused, closed | Volume of dump: | 20 m3 |
Importance |
Public: | Little Importance (reg. 18.02.2015) |
Economical: | Minor interest , (Confirmed 20.feb.2001 by Havard Gautneb) |
Products |
Element/product | Crude ore grade or quality | |
SOIADD | 100 % |
Mineralization |
Era: | Paleozoic | Period: | ||
Dating: | Method: | |||
Genesis: | Sedimentary deposit | Form: | Irregular | |
Main texture: | Banded | Min. distribution: | Massive (>50 % ore minerals) |
Main grain size: | Medium grained (1-3 mm) |
Strike/Dip: | 114 / 60 | Direction: | ||
Plunge: |
Stratigraphic classification of host rock |
Era: | Paleozoic | Period: | Ordovician |
Province: | ||
Geotec.unit: | ||
Tectonic complex: | ||
Igneous complex: |
Group: | Formation: |
Mineralogy |
Relationship | Mineral | Amount | |
Not defined | Calcite | Major mineral (>10%) | |
Not defined | Opaque | Subordinate mineral (1-10%) | |
Not defined | Plagioclase | Subordinate mineral (1-10%) | |
Not defined | Pyroxene | Subordinate mineral (1-10%) | |
Not defined | Quartz | Subordinate mineral (1-10%) | |
Not defined | Muscovite | Accessory mineral (<1%) |
Structures |
Location: | Type: | Orientation(360 gr.): | Relation to min.: | |
Host rock | Foliation | Strike/Dip :114 / 60 | Pre-mineralisation ;...Effect :Modifies |
Information(s) in free text format |
Free text |
Forekomsten ligger ved gården Storlia. Det finnes flere små brudd ved denne forekomsten. Kalken ble knust i et lokalt knuseri som fremdeles er synlig (2004). Kalksonen har en mektighet på 8-10 m. Bergarten er grå og forurenset av silikater. |
Fieldsamples |
Sample No. | Sample type | Miscellanrous | |||
NT0035 | Bedrock |
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The fact sheet was created on 19.05.2024 |
Questions or comments regarding the fact sheet can be emailed to: ressursdatabaser@ngu.no |
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