Luolavirta, K., Hanski, E., Maier, W., & Santaguida, F. (2018). Characterization and origin of dunitic rocks in the Ni-Cu-(PGE) sulfide ore-bearing Kevitsa intrusion, northern Finland: whole-rock and mineral chemical constraints. Bulletin of the Geological Society of Finland, 90(1), 5–32. https://doi.org/10.17741/bgsf/90.1.001
Characterization and origin of dunitic rocks in the Ni-Cu-(PGE) sulfide ore-bearing Kevitsa intrusion, northern Finland : whole-rock and mineral chemical constraints
|Author:||Luolavirta, Kirsi1; Hanski, Eero1; Maier, Wolfgang2;|
1Oulu Mining School, University of Oulu, P.O.BOX 3000, FI-90014, Finland
2School of Earth and Ocean Sciences, Cardiff University, Cardiff CF10 3AT, UK
3First Cobalt Corp. Suite 201, 140 Yonge Street, Toronto, Canada
|Online Access:||PDF Full Text (PDF, 4.4 MB)|
|Persistent link:|| http://urn.fi/urn:nbn:fi-fe2019062021548
The Geological Society of Finland,
|Publish Date:|| 2019-06-20
The ca. 2.06 Ga Kevitsa intrusion is one of the ore-bearing mafic-ultramafic igneous bodies in the Central Lapland greenstone belt. A large disseminated Ni-Cu-(PGE) sulfide ore deposit is hosted by olivine-pyroxene cumulates in the lower ultramafic part of the intrusion, indicating involvement of a multiply saturated magma in the ore formation. There are also various dunitic rocks, which occur as numerous inclusions within the Kevitsa intrusion, most commonly in the economic resource area. On textural basis, two distinct types of inclusions are recognized: i) cumulate-textured (Kevitsa Dunite) and ii) recrystallized ultramafic inclusions. In addition, there also exists a separate dunitic body (Central Dunite) with a suface area of 0.6 x 1.0 km, cropping out in the central part of the intrusion.
The Central Dunite and Kevitsa Dunite are similar olivine-chromite cumulates and with comparable whole-rock and mineral compositions, suggesting that they are cogenetic. A magmatic, rather than replacement origin for the dunitic cumulates is evidenced by their systematic mineral compositional trends consistent with magmatic fractionation. Whole-rock major and trace element and mineral compositional data of the dunitic cumulates and Kevitsa olivine pyroxenites fall on the same linear trends and record similar REE characteristics indicating a genetic link between these two. The parental magmas for the dunitic cumulates were probably picritic and related to the picritic and basaltic volcanic rocks in the area. The high Fo content of olivine (up to ~89 mol.%) is consistent with a high-Mg parental melt.
The recrystallized ultramafic inclusions are fine-grained and show a granoblastic/interlobate textures indicative for thermal textural readjustment. Two subgroups are identified: Group 1 shows a chemical affinity towards the dunitic cumulates and are interpreted as their recrystallized clasts. The Group 2 inclusions are compositionally comparable to the ~2.06 Ga komatiitic volcanic rocks in the area and are considered as dehydrated metavolcanic xenoliths. A decrease in the flow rate of the Kevitsa magmas due to entrapment of a high number of inclusions is proposed as a mechanism to promote settling of sulfides, contributing to the formation of the Ni-Cu-(PGE) ore.
Bulletin of the Geological Society of Finland
|Pages:||5 - 32|
|Type of Publication:||
A1 Journal article – refereed
|Field of Science:||
Financial support for this study was obtained from First Quantum Minerals Ltd (FQM), the Academy of Finland (#281859), and K.H. Renlund Foundation.
|Academy of Finland Grant Number:||
281859 (Academy of Finland Funding decision)
© 2018 The Authors. All published content of BGSF is licensed under a Creative Commons Attribution-NonCommercial 4.0 International License.