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THE ORE DATABASE | |||||
Occurence 5532 - 019 Sagelvvatnet | |||||
(Object Id: 1421) (Last updated: 18.02.2005) |
Drill Cores: Sagelvvatnet |
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Location |
County: | Troms | Municipality: | Balsfjord (5532) |
Map 1:50000: | Takvatnet (1533-3) | Map 1:250000: | Tromsø |
Coordinate system: | EU89-UTM Zone 34 |
East: | 422875 m. | North: | 7675821 m. |
Longitude: | 19.0552880 | Latitude: | 69.1814800 |
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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 |
Importance |
Raw material meaning: | Not Assessed (reg. 18.02.2015) |
Resources and production |
Activity: | Pitting | Reserves: | ||
Operating method: | Historical production: |
Mineralization |
Era: | Paleozoic | Period: | ||
Genesis: | Form: | |||
Main texture: | Min. distribution: |
Main grain size: | Main alteration: |
Strike/Dip: | 260 / 60 | Direction: | ||
Plunge: |
Stratigraphic classification of host rock |
Era: | Paleozoic | Period: | Silurian |
Province: | ||
Geotec.unit: | ||
Tectonic complex: | Lyngendekket | |
Igneous complex: |
Group: | Sagelvvatngruppen | Formation: | Mosbergformasjonen |
Lithology: |
Relationship | Rock | Origin | |
Host rock | kalkstein | Sedimentary Original rock :Limestone |
Structures |
Location: | Type: | Orientation(360 gr.): | Relation to min.: | |
Wall rock | Foliation | Strike/Dip :260 / 60 |
Information(s) in free text format |
Free text |
Skjerpet er avmerket på foreløpig berggrunnskart Takvatnet. Røskegropa er imidlertid gjenfylt med søppel, og tippen er helt overgrodd. Det er heller ikke funnet mineraliserte blotninger i nærheten. |
Bibliography: |
From NGU's Reference Archive: |
Bjørlykke, Arne; Olaussen, Snorre , 1981 |
Silurian sediments, volcanics and mineral deposits in the Sagelvvatn area, Troms, North Norway. |
;Norges geologiske undersøkelse;TIDSSKRIFTARTIKKEL;NGU; No.365;1-38 pages |
Abstract: | |
Low-grade metamorphic rocks of the Sagelvvatn area in Troms reflect a regressive and transgressive cycle within the Lower Silurian. The carbonates, which contain halysitid corals indicating an Upper Llandovery age, are interpreted as shallow marine deposits. In the area a carboante-evaporite tidal sequence interdigitates with tholeitic greenstones of within-plate geochemical affinity. The final regional transgression is represented by the Hansvoll Formation which is thought to have been deposited as a hemipelagic/pelagic hypersaline limestone. The full sequence, the Sagelvvatn Group recors sedimentation and volcanism in an arid climate on a Lower Silurian continental shelf. Zinc deposits occur in the carbonate-evaporite sequence (a reservoir rock); volcanic rocks with a high zinc content are interpreted as the main source of the metals. |
The fact sheet was created on 02.05.2024 |
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