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Geology, petrology and alteration geochemistry of the Palaeoproterozoic intrusive hosted Ägträsk Au deposit, Northern Sweden
Boliden Mineral AB.
Luleå University of Technology, Department of Civil, Environmental and Natural Resources Engineering, Geosciences and Environmental Engineering.ORCID iD: 0000-0003-3879-3897
Boliden Mineral AB.
2011 (English)In: Geological Society Special Publication, ISSN 0305-8719, E-ISSN 2041-4927, no 350, p. 105-132Article in journal (Refereed) Published
Abstract [en]

The Ägträsk intrusive hosted Au deposit, Skellefte district, northern Sweden, is situated in the oldest, most heterogeneous part of the c. 1.89-1.86 Ga Jörn granitoid complex, which intruded a complex volcano-sedimentary succession in an island arc or continental margin arc environment. The Tallberg porphyry Cu deposit, situated only 3 km west of Ägträsk, is associated with quartz feldspar porphyritic dykes. These dykes are suggested to be genetically related to similar porphyry dykes in Älgträsk and the tonalitic host rock in Tallberg. The granodiorite hosting the Ägträsk Au-deposit does not appear to be genetically related to the tonalite or the porphyry dykes.

Place, publisher, year, edition, pages
2011. no 350, p. 105-132
National Category
Geology
Research subject
Ore Geology
Identifiers
URN: urn:nbn:se:ltu:diva-9663DOI: 10.1144/SP350.7Scopus ID: 2-s2.0-78651497033Local ID: 8548fb21-6c31-4220-88ce-ad14731d0c9fOAI: oai:DiVA.org:ltu-9663DiVA, id: diva2:982601
Note
Validerad; 2011; 20110131 (ysko)Available from: 2016-09-29 Created: 2016-09-29 Last updated: 2018-07-10Bibliographically approved

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Bejgarn, ThereseWeihed, Pär

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