Norsk versjon | |||||
THE ORE DATABASE | |||||
Occurence 5056 - 014 Andavatnet | |||||
(Object Id: 4509) (Last updated: 14.12.2021) |
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Location |
County: | Trøndelag | Municipality: | Hitra (5056) |
Map 1:50000: | Hitra (1422-2) | Map 1:250000: | Kristiansund |
Coordinate system: | EU89-UTM Zone 32 |
East: | 488904 m. | North: | 7054893 m. |
Longitude: | 8.7761840 | Latitude: | 63.6218200 |
Show on map |
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Resource |
Resource Type: | Base metals (Cu,Zn,Pb,Fe sulphides, As,Sb,Bi,Sn) | Resource Subtype: | Lead | |
Element(s): | Pb Zn Ag |
Importance |
Raw material meaning: | Little Importance (reg. 18.02.2015) |
Resources and production |
Activity: | Pitting | Reserves: | ||
Operating method: | Historical production: |
Mineralization |
Era: | Paleozoic | Period: | Ordovician | |
Genesis: | Replacement/Metasomatism | Form: | Irregular | |
Main texture: | Fracture filling | Min. distribution: | Disseminated (<20 % 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: | Helgeland Nappe Complex | |
Tectonic complex: | ||
Igneous complex: |
Group: | Formation: |
Mineralogy |
Relationship | Mineral | Amount | |
Gangue mineral | Calcite | Major mineral (>10%) | |
Gangue mineral | Amphibole | Subordinate mineral (1-10%) | |
Gangue mineral | Pyroxene | Subordinate mineral (1-10%) | |
Ore mineral | Sphalerite | Major mineral (>10%) | |
Ore mineral | Chalcopyrite | Subordinate mineral (1-10%) | |
Ore mineral | Pyrite | Subordinate mineral (1-10%) |
Lithology: |
Relationship | Rock | Origin | |
Host rock | Calcite marble | Sedimentary Original rock :Limestone |
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Metamorphic facies :Amphibolite | |||
Wall rock | Granodiorite | Intrusive Original rock :Granodiorite |
Information(s) in free text format |
Free text |
Forekomsten består av en liten, vannfylt synk med åpning på 2x2 m på vestsida av Andavatnet. Det skjerpet i flattliggende marmor under foliert granodioritt. Marmoren er dels svakt grønnlig skarnomvandlet. Svært svak sulfidmineralisering er påvist og består av svak disseminasjon av sinkblende i marmor og tynne stikk med svovelkis og kobberkis. Relativt stor tipp med volum på ca. 100 m3. |
Bibliography: |
References not to be found in NGU's Reference Archive.: |
Husmo, T. 1984: Geologi og bly-sink-mineralisering på Nord-Hitra. I Sivertsen, R. m.fl. Geologi og bly-sink-mineralisering på Nord-Hitra. BV Rapport 1370, 148s. |
Fieldsamples |
Sample No. | Sample type | Miscellanrous | ||||
ST0309.01 | Dump |
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NB! All analyse values are shown at the end of the printout.: |
Analyse Results |
from |
Deposit Area 5056 - 014 Andavatnet |
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# |
ST0309.01 | Dump | 35 | 269 | 154 | 27 | 75 | 1.0 | 179.0 |
------------------ |
Sample No. | Pt# | Pd# | As* | Cd* | Ba* | Mo* | Sn* | Sb* | Bi* |
ST0309.01 | -5.0 | -1.0 | 62 | 1.2 | 49 | 3.00 | -20 | 21 | 9 |
------------------ |
Sample No. | V* | Cr* | Mn* | Fe% | W* | Sr* | La* | Na* | Mg* |
ST0309.01 | 36 | 170 | 2654 | 4.77 | -20 | 323.0 | 6.00 | 0 | 2 |
------------------ |
Sample No. | Al* | K * | Ca* | Te* | |||||
ST0309.01 | 1 | 0 | 8 | -10.00 |
The fact sheet was created on 01.05.2024 |
Questions or comments regarding the fact sheet can be emailed to: ressursdatabaser@ngu.no |
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