Precambrian geodynamics and ore formation : the Fennoscandian Shield
The complex geodynamic evolution of the Fennoscandian Shield from 2.06 to 1.78 Ga involved rapid accretion of island arcs and several microcontinent-continent collisions in a complex array of orogens. With a few exceptions, all major ore deposits formed in specific tectonic settings between 2.06 and...
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Luleå tekniska universitet, Geovetenskap och miljöteknik
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ftluleatu:oai:DiVA.org:ltu-27631 2023-05-15T16:12:51+02:00 Precambrian geodynamics and ore formation : the Fennoscandian Shield Weihed, Pär Arndt, Nicholas Billström, Kjell Duchesne, Jean-Clair Eilu, Pasi Martinsson, Olof Papunen, Heikki Lahtinene, Raimo 2006 application/pdf http://urn.kb.se/resolve?urn=urn:nbn:se:ltu:diva-27631 eng eng Luleå tekniska universitet, Geovetenskap och miljöteknik Swedish Museum of Natural History Helsinki : Geological Society of Finland Bulletin of the Geological society of Finland, 0367-5211 Special issue 1 The 27th Nordic Geological Winter Meeting, January 9-12, 2006, Oulu, Finland : abstract volume, p. 172- http://urn.kb.se/resolve?urn=urn:nbn:se:ltu:diva-27631 Local 1230e260-ee8b-11db-bb5c-000ea68e967b info:eu-repo/semantics/openAccess Geology Geologi Conference paper info:eu-repo/semantics/conferenceObject text 2006 ftluleatu 2022-10-25T20:53:53Z The complex geodynamic evolution of the Fennoscandian Shield from 2.06 to 1.78 Ga involved rapid accretion of island arcs and several microcontinent-continent collisions in a complex array of orogens. With a few exceptions, all major ore deposits formed in specific tectonic settings between 2.06 and 1.78 Ga and thus a strong geodynamic control on ore deposit formation is suggested.All orogenic gold deposits formed syn- to post-peak metamorphism and their timing reflects the orogenic younging of the shield towards the SW and west.The ca. 2.5 to 2.4 Ga Ni-Cu±PGE deposits formed in basins formed during rifting of the Archaean craton at ca. 2.5 to 2.4 Ga, while Svecokarelian ca. 1.89 to 1.88 Ga Ni-Cu deposits are related to mafic-ultramafic rocks intruded along linear belts at the accretionary margins of microcratons.All major VMS deposits in the Fennoscandian Shield formed between 1.97 and 1.88 Ga, in extensional settings, prior to basin inversion and accretion. This occurred in primitive, bimodal arc complexes during extension, in strongly extensional intra-arc regions that developed on continental or mature arc crust or in intra-continental, or continental margin back-arc, extensional regions developed on older continental crust.Of the iron oxide-copper-gold deposits the oldest deposits formed in continental arcs or magmatic arcs inboard of the active subduction zone. Younger mineralization took place during cratonization distal to the subduction zone.Finally, the large volumes of anorthositic magmas formed a major concentration of Ti under granulite facies conditions, about 40 million years after the last regional deformation of the Sveconorwegian Orogeny. Godkänd; 2006; 20111007 (andbra) Conference Object Fennoscandian Luleå University of Technology Publications (DiVA) |
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Open Polar |
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Luleå University of Technology Publications (DiVA) |
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ftluleatu |
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English |
topic |
Geology Geologi |
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Geology Geologi Weihed, Pär Arndt, Nicholas Billström, Kjell Duchesne, Jean-Clair Eilu, Pasi Martinsson, Olof Papunen, Heikki Lahtinene, Raimo Precambrian geodynamics and ore formation : the Fennoscandian Shield |
topic_facet |
Geology Geologi |
description |
The complex geodynamic evolution of the Fennoscandian Shield from 2.06 to 1.78 Ga involved rapid accretion of island arcs and several microcontinent-continent collisions in a complex array of orogens. With a few exceptions, all major ore deposits formed in specific tectonic settings between 2.06 and 1.78 Ga and thus a strong geodynamic control on ore deposit formation is suggested.All orogenic gold deposits formed syn- to post-peak metamorphism and their timing reflects the orogenic younging of the shield towards the SW and west.The ca. 2.5 to 2.4 Ga Ni-Cu±PGE deposits formed in basins formed during rifting of the Archaean craton at ca. 2.5 to 2.4 Ga, while Svecokarelian ca. 1.89 to 1.88 Ga Ni-Cu deposits are related to mafic-ultramafic rocks intruded along linear belts at the accretionary margins of microcratons.All major VMS deposits in the Fennoscandian Shield formed between 1.97 and 1.88 Ga, in extensional settings, prior to basin inversion and accretion. This occurred in primitive, bimodal arc complexes during extension, in strongly extensional intra-arc regions that developed on continental or mature arc crust or in intra-continental, or continental margin back-arc, extensional regions developed on older continental crust.Of the iron oxide-copper-gold deposits the oldest deposits formed in continental arcs or magmatic arcs inboard of the active subduction zone. Younger mineralization took place during cratonization distal to the subduction zone.Finally, the large volumes of anorthositic magmas formed a major concentration of Ti under granulite facies conditions, about 40 million years after the last regional deformation of the Sveconorwegian Orogeny. Godkänd; 2006; 20111007 (andbra) |
format |
Conference Object |
author |
Weihed, Pär Arndt, Nicholas Billström, Kjell Duchesne, Jean-Clair Eilu, Pasi Martinsson, Olof Papunen, Heikki Lahtinene, Raimo |
author_facet |
Weihed, Pär Arndt, Nicholas Billström, Kjell Duchesne, Jean-Clair Eilu, Pasi Martinsson, Olof Papunen, Heikki Lahtinene, Raimo |
author_sort |
Weihed, Pär |
title |
Precambrian geodynamics and ore formation : the Fennoscandian Shield |
title_short |
Precambrian geodynamics and ore formation : the Fennoscandian Shield |
title_full |
Precambrian geodynamics and ore formation : the Fennoscandian Shield |
title_fullStr |
Precambrian geodynamics and ore formation : the Fennoscandian Shield |
title_full_unstemmed |
Precambrian geodynamics and ore formation : the Fennoscandian Shield |
title_sort |
precambrian geodynamics and ore formation : the fennoscandian shield |
publisher |
Luleå tekniska universitet, Geovetenskap och miljöteknik |
publishDate |
2006 |
url |
http://urn.kb.se/resolve?urn=urn:nbn:se:ltu:diva-27631 |
genre |
Fennoscandian |
genre_facet |
Fennoscandian |
op_relation |
Bulletin of the Geological society of Finland, 0367-5211 Special issue 1 The 27th Nordic Geological Winter Meeting, January 9-12, 2006, Oulu, Finland : abstract volume, p. 172- http://urn.kb.se/resolve?urn=urn:nbn:se:ltu:diva-27631 Local 1230e260-ee8b-11db-bb5c-000ea68e967b |
op_rights |
info:eu-repo/semantics/openAccess |
_version_ |
1765998466030370816 |