Structural interpretation of the Iso-Kuotko area, Lapland, with implications to gold precipitation
Central Lapland Belt (CLB) in Northern Finland hosts multiple orogenic gold deposits from which Iso-Kuotko gold deposit is one. The Iso-Kuotko deposit comprises three mineralizations: Kati, Retu and Tiira. Previous studies have focused on the geochronology and geochemical attributes of the deposit,...
Main Author: | |
---|---|
Other Authors: | , , |
Format: | Other/Unknown Material |
Language: | English |
Published: |
2023
|
Subjects: | |
Online Access: | https://www.utupub.fi/handle/10024/176315 |
id |
ftunivturku:oai:www.utupub.fi:10024/176315 |
---|---|
record_format |
openpolar |
spelling |
ftunivturku:oai:www.utupub.fi:10024/176315 2024-01-21T10:08:59+01:00 Structural interpretation of the Iso-Kuotko area, Lapland, with implications to gold precipitation Silvonen, Olli Matemaattis-luonnontieteellinen tiedekunta, Faculty of Science Kallioperägeologia, Bedrock Geology Maantieteen ja geologian laitos, Department of Geography and Geology 2023-12-22 67 https://www.utupub.fi/handle/10024/176315 eng eng https://www.utupub.fi/handle/10024/176315 URN:NBN:fi-fe20231222157170 Julkaisu on tekijänoikeussäännösten alainen. Teosta voi lukea ja tulostaa henkilökohtaista käyttöä varten. Käyttö kaupallisiin tarkoituksiin on kielletty., This publication is copyrighted. You may download, display and print it for Your own personal use. Commercial use is prohibited. avoin structural geology orogenic gold Central Lapland Greenstone Belt 3D modelling rakennegeologia orogeeninen kulta Keski-Lapin vihreäkivivöyhyke 3D mallinnus Pro gradu -tutkielma, Master's thesis 2023 ftunivturku 2023-12-28T00:05:30Z Central Lapland Belt (CLB) in Northern Finland hosts multiple orogenic gold deposits from which Iso-Kuotko gold deposit is one. The Iso-Kuotko deposit comprises three mineralizations: Kati, Retu and Tiira. Previous studies have focused on the geochronology and geochemical attributes of the deposit, whereas the structural geometry of the deposit, and the linkage between gold-bearing veins and shear features remains partly unknown. The main goal of this study is to describe both the ductile and brittle deformation structures of the study area and to link them together. The secondary objective is to identify and compare the orientations distribution of diverse vein sets occurring within the mineralized areas, and further compare them with the mineralization. The study is based on new field observations and structural measurements from drill core and bore hole videos, which complement the pre-existing datasets available from several parts of the study area. Moreover, a structural interpretation of magnetic anomaly maps was conducted, and previously gathered drill core measurements were used in the study. The data were eventually gathered into digital 3D models and lower hemisphere projections. The Kati area is dominated by gently NE dipping foliation which has been sheared during a thrusting event. The Kati area is also cross-cut by NW trending, likely dextral, sub-vertical shear bands splaying out from the Kiistala Shear Zone (KiSZ). Additionally, in the Kati area there is a E-W trending, sub-vertical, shear band possibly splaying out from the NW trending shear bands. The Retu area is dominated by sub-horizontal foliation which is undulating around gently NE plunging fold axis. According to this study, shear deformation occurred along the sub-horizontal foliation surface, and the foliation was cross-cut by the main branch of the NE trending sub-vertical KiSZ and parallel subsidiary shear bands. In total five mineralogically varying vein types were observed: 1) quartz, 2) quartz + Fe-carbonate, 3) quartz + ... Other/Unknown Material Northern Finland Lapland University of Turku: UTUPub Kati ENVELOPE(15.793,15.793,67.536,67.536) Kiistala ENVELOPE(25.336,25.336,67.871,67.871) |
institution |
Open Polar |
collection |
University of Turku: UTUPub |
op_collection_id |
ftunivturku |
language |
English |
topic |
structural geology orogenic gold Central Lapland Greenstone Belt 3D modelling rakennegeologia orogeeninen kulta Keski-Lapin vihreäkivivöyhyke 3D mallinnus |
spellingShingle |
structural geology orogenic gold Central Lapland Greenstone Belt 3D modelling rakennegeologia orogeeninen kulta Keski-Lapin vihreäkivivöyhyke 3D mallinnus Silvonen, Olli Structural interpretation of the Iso-Kuotko area, Lapland, with implications to gold precipitation |
topic_facet |
structural geology orogenic gold Central Lapland Greenstone Belt 3D modelling rakennegeologia orogeeninen kulta Keski-Lapin vihreäkivivöyhyke 3D mallinnus |
description |
Central Lapland Belt (CLB) in Northern Finland hosts multiple orogenic gold deposits from which Iso-Kuotko gold deposit is one. The Iso-Kuotko deposit comprises three mineralizations: Kati, Retu and Tiira. Previous studies have focused on the geochronology and geochemical attributes of the deposit, whereas the structural geometry of the deposit, and the linkage between gold-bearing veins and shear features remains partly unknown. The main goal of this study is to describe both the ductile and brittle deformation structures of the study area and to link them together. The secondary objective is to identify and compare the orientations distribution of diverse vein sets occurring within the mineralized areas, and further compare them with the mineralization. The study is based on new field observations and structural measurements from drill core and bore hole videos, which complement the pre-existing datasets available from several parts of the study area. Moreover, a structural interpretation of magnetic anomaly maps was conducted, and previously gathered drill core measurements were used in the study. The data were eventually gathered into digital 3D models and lower hemisphere projections. The Kati area is dominated by gently NE dipping foliation which has been sheared during a thrusting event. The Kati area is also cross-cut by NW trending, likely dextral, sub-vertical shear bands splaying out from the Kiistala Shear Zone (KiSZ). Additionally, in the Kati area there is a E-W trending, sub-vertical, shear band possibly splaying out from the NW trending shear bands. The Retu area is dominated by sub-horizontal foliation which is undulating around gently NE plunging fold axis. According to this study, shear deformation occurred along the sub-horizontal foliation surface, and the foliation was cross-cut by the main branch of the NE trending sub-vertical KiSZ and parallel subsidiary shear bands. In total five mineralogically varying vein types were observed: 1) quartz, 2) quartz + Fe-carbonate, 3) quartz + ... |
author2 |
Matemaattis-luonnontieteellinen tiedekunta, Faculty of Science Kallioperägeologia, Bedrock Geology Maantieteen ja geologian laitos, Department of Geography and Geology |
format |
Other/Unknown Material |
author |
Silvonen, Olli |
author_facet |
Silvonen, Olli |
author_sort |
Silvonen, Olli |
title |
Structural interpretation of the Iso-Kuotko area, Lapland, with implications to gold precipitation |
title_short |
Structural interpretation of the Iso-Kuotko area, Lapland, with implications to gold precipitation |
title_full |
Structural interpretation of the Iso-Kuotko area, Lapland, with implications to gold precipitation |
title_fullStr |
Structural interpretation of the Iso-Kuotko area, Lapland, with implications to gold precipitation |
title_full_unstemmed |
Structural interpretation of the Iso-Kuotko area, Lapland, with implications to gold precipitation |
title_sort |
structural interpretation of the iso-kuotko area, lapland, with implications to gold precipitation |
publishDate |
2023 |
url |
https://www.utupub.fi/handle/10024/176315 |
long_lat |
ENVELOPE(15.793,15.793,67.536,67.536) ENVELOPE(25.336,25.336,67.871,67.871) |
geographic |
Kati Kiistala |
geographic_facet |
Kati Kiistala |
genre |
Northern Finland Lapland |
genre_facet |
Northern Finland Lapland |
op_relation |
https://www.utupub.fi/handle/10024/176315 URN:NBN:fi-fe20231222157170 |
op_rights |
Julkaisu on tekijänoikeussäännösten alainen. Teosta voi lukea ja tulostaa henkilökohtaista käyttöä varten. Käyttö kaupallisiin tarkoituksiin on kielletty., This publication is copyrighted. You may download, display and print it for Your own personal use. Commercial use is prohibited. avoin |
_version_ |
1788699868485648384 |