Nironen M. 1997. The Svecofe nnian orogen: A tectonic model[J]. Precambr ian. Res. 86: 21-44.
[2]
Seedorff E, Barton M D, Stavat W J A and Maher D J. 2008. Root zones of porphyry systems: Extending the porphyry model to depth[J]. Econ. Geol., 103: 939-956.
[3]
Wanhainen C, Billstr？m K, Martinsson O and Magnor B. 2012. Modification of a Palaeoproterozoic porphyry-like system: Integration of structural, geochemical, petrographic, andfluid inclusion data from the Aitik Cu-Au-Ag deposit, northern Sweden[J]. Ore Geology Reviews, 48: 306-331.
[4]
Wanhainen C, Broman C and Martinsson O. 2003. The Aitik Cu-Au-Ag deposit in Northern Sweden: A product of high salinity fluids[J]. Mineralium Deposita, 38: 715-726.
[5]
Witschard F. 1984. The geological and tectonic evolution of the Precambrian of northern Sweden a case for basement reactivation[J]. Precamb. Res., 23: 273-315.
[6]
Boliden A B. 2011. Annual report [EB/OL]. www. boliden. com/Documents/Press/Publications 2011.
[7]
Martinsson O. 1997. Paleoproterozoic greenstones at Kiruna in northern Sweden: A product of continental rifting and associ-ated mafic-ultramafic volcanism. Paper I in Tectonic setting and metallogeny of the Kiruna greenstones[D]. PhD Thesis, Lulea University of Technology.
[8]
Martinsson O and Wanhainen C. 2004. Character of Cu-Au mineralization and related hydrothermal alteration along the Nautanen deformation zone, G？llivare area, Northern Sweden[J]. Society of Economic Geologists Guidebook Series 33, 149-160.
