6The Norrbotten county is rich in apatite-Fe ores of the ”Kiruna-type ” and several investigations have been focused on this ore type, although the genetical aspects are still a matter of debate (cf. Nyström & Henríquez, 1994). Another widespread ore type is the Cu-Au mineralizations, which may...

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http://www.ltu.se/cms_fs/1.5007!/f0167b4a.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.461.511 2023-05-15T17:04:12+02:00 The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.461.511 http://www.ltu.se/cms_fs/1.5007!/f0167b4a.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.461.511 http://www.ltu.se/cms_fs/1.5007!/f0167b4a.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.ltu.se/cms_fs/1.5007!/f0167b4a.pdf text ftciteseerx 2016-10-16T00:02:49Z 6The Norrbotten county is rich in apatite-Fe ores of the ”Kiruna-type ” and several investigations have been focused on this ore type, although the genetical aspects are still a matter of debate (cf. Nyström & Henríquez, 1994). Another widespread ore type is the Cu-Au mineralizations, which may be sub-divided into an epige-netic and a syngenetic group (Martinsson, 1997). Although lim-ited research has been devoted to this ore type, both these groups of deposits apparently formed from highly, saline hydrothermal fl uids, but they differ with respect to metal association and altera-tion features. The timing of the Cu-Fe-Au ore-forming event(s) is poorly understood, and the present work is directed at reaching better temporal constraints on ore-forming processes in northern Sweden. The geology of the Norrbotten county forms part of the Fen-noscandian shield and involves both a partly exposed Archaean Text Kiruna Northern Sweden Norrbotten Unknown Kiruna
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description 6The Norrbotten county is rich in apatite-Fe ores of the ”Kiruna-type ” and several investigations have been focused on this ore type, although the genetical aspects are still a matter of debate (cf. Nyström & Henríquez, 1994). Another widespread ore type is the Cu-Au mineralizations, which may be sub-divided into an epige-netic and a syngenetic group (Martinsson, 1997). Although lim-ited research has been devoted to this ore type, both these groups of deposits apparently formed from highly, saline hydrothermal fl uids, but they differ with respect to metal association and altera-tion features. The timing of the Cu-Fe-Au ore-forming event(s) is poorly understood, and the present work is directed at reaching better temporal constraints on ore-forming processes in northern Sweden. The geology of the Norrbotten county forms part of the Fen-noscandian shield and involves both a partly exposed Archaean
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geographic Kiruna
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