Structure, setting, and petrography of the Raudvatnet sulphide deposit, Hattfjelldal, Northern Norway
The Raudvatnet massive sulphide deposit is located in Hattfjelldal in Nordland, Northern Norway. Deposit investigations have been made by mining companies Boliden AB and Aspro AS in the 1960’s and 1980’s respectively. The Deposit lies in the Bjørkvatnet Nappe belonging to the Lower Køli Nappes of th...
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ftoslouniv:oai:www.duo.uio.no:10852/53262 2023-05-15T16:33:47+02:00 Structure, setting, and petrography of the Raudvatnet sulphide deposit, Hattfjelldal, Northern Norway Svennungsen, Robin Orre 2016 http://hdl.handle.net/10852/53262 http://urn.nb.no/URN:NBN:no-56528 eng eng http://urn.nb.no/URN:NBN:no-56528 Svennungsen, Robin Orre. Structure, setting, and petrography of the Raudvatnet sulphide deposit, Hattfjelldal, Northern Norway. Master thesis, University of Oslo, 2016 http://hdl.handle.net/10852/53262 URN:NBN:no-56528 Fulltext https://www.duo.uio.no/bitstream/handle/10852/53262/5/Thesis-Robin-Orre-Svennungsen-2016.pdf Master thesis Masteroppgave 2016 ftoslouniv 2020-06-21T08:49:58Z The Raudvatnet massive sulphide deposit is located in Hattfjelldal in Nordland, Northern Norway. Deposit investigations have been made by mining companies Boliden AB and Aspro AS in the 1960’s and 1980’s respectively. The Deposit lies in the Bjørkvatnet Nappe belonging to the Lower Køli Nappes of the Upper Allochthon in the North Central Caledonides. Brief structural investigations in the area along with petrographic, geochemical studies were conducted on a selection of samples collected in the field, both from mineralized ore horizons and adjacent lithologies. Geological mapping was conducted to produce an updated geological map of the area along with creation of 4 cross section profile sketches produced from the combined impressions of surface mapping and 4 of the logged drill cores. Geochemical analysis of the host rock of the mineralisation yields a sericite altered quartz keratophyre, which in turn is an altered felsic metavolcanite. The associated metabasites in which the felsic sequence is situated yields anN-MORB type geochemistry. The deposit contains abundant Zn andCu and is classified as a Zn-Cu compositional type. In addition, there are substantial amounts of Pb, Ag and Au as found in various phases associated with the massive mineralisations present. The deposit is characterized as a Kuroko type VMS deposit and is recognized as being a Bimodal mafic type in terms of lithostratigraphic classification. Master Thesis Hattfjelldal Nordland Nordland Northern Norway Nordland Universitet i Oslo: Digitale utgivelser ved UiO (DUO) Bjørkvatnet ENVELOPE(13.317,13.317,64.853,64.853) Hattfjelldal ENVELOPE(13.988,13.988,65.597,65.597) Norway |
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Open Polar |
collection |
Universitet i Oslo: Digitale utgivelser ved UiO (DUO) |
op_collection_id |
ftoslouniv |
language |
English |
description |
The Raudvatnet massive sulphide deposit is located in Hattfjelldal in Nordland, Northern Norway. Deposit investigations have been made by mining companies Boliden AB and Aspro AS in the 1960’s and 1980’s respectively. The Deposit lies in the Bjørkvatnet Nappe belonging to the Lower Køli Nappes of the Upper Allochthon in the North Central Caledonides. Brief structural investigations in the area along with petrographic, geochemical studies were conducted on a selection of samples collected in the field, both from mineralized ore horizons and adjacent lithologies. Geological mapping was conducted to produce an updated geological map of the area along with creation of 4 cross section profile sketches produced from the combined impressions of surface mapping and 4 of the logged drill cores. Geochemical analysis of the host rock of the mineralisation yields a sericite altered quartz keratophyre, which in turn is an altered felsic metavolcanite. The associated metabasites in which the felsic sequence is situated yields anN-MORB type geochemistry. The deposit contains abundant Zn andCu and is classified as a Zn-Cu compositional type. In addition, there are substantial amounts of Pb, Ag and Au as found in various phases associated with the massive mineralisations present. The deposit is characterized as a Kuroko type VMS deposit and is recognized as being a Bimodal mafic type in terms of lithostratigraphic classification. |
format |
Master Thesis |
author |
Svennungsen, Robin Orre |
spellingShingle |
Svennungsen, Robin Orre Structure, setting, and petrography of the Raudvatnet sulphide deposit, Hattfjelldal, Northern Norway |
author_facet |
Svennungsen, Robin Orre |
author_sort |
Svennungsen, Robin Orre |
title |
Structure, setting, and petrography of the Raudvatnet sulphide deposit, Hattfjelldal, Northern Norway |
title_short |
Structure, setting, and petrography of the Raudvatnet sulphide deposit, Hattfjelldal, Northern Norway |
title_full |
Structure, setting, and petrography of the Raudvatnet sulphide deposit, Hattfjelldal, Northern Norway |
title_fullStr |
Structure, setting, and petrography of the Raudvatnet sulphide deposit, Hattfjelldal, Northern Norway |
title_full_unstemmed |
Structure, setting, and petrography of the Raudvatnet sulphide deposit, Hattfjelldal, Northern Norway |
title_sort |
structure, setting, and petrography of the raudvatnet sulphide deposit, hattfjelldal, northern norway |
publishDate |
2016 |
url |
http://hdl.handle.net/10852/53262 http://urn.nb.no/URN:NBN:no-56528 |
long_lat |
ENVELOPE(13.317,13.317,64.853,64.853) ENVELOPE(13.988,13.988,65.597,65.597) |
geographic |
Bjørkvatnet Hattfjelldal Norway |
geographic_facet |
Bjørkvatnet Hattfjelldal Norway |
genre |
Hattfjelldal Nordland Nordland Northern Norway Nordland |
genre_facet |
Hattfjelldal Nordland Nordland Northern Norway Nordland |
op_relation |
http://urn.nb.no/URN:NBN:no-56528 Svennungsen, Robin Orre. Structure, setting, and petrography of the Raudvatnet sulphide deposit, Hattfjelldal, Northern Norway. Master thesis, University of Oslo, 2016 http://hdl.handle.net/10852/53262 URN:NBN:no-56528 Fulltext https://www.duo.uio.no/bitstream/handle/10852/53262/5/Thesis-Robin-Orre-Svennungsen-2016.pdf |
_version_ |
1766023497100820480 |