Abstract. An approximately 90 km long Palaeoproterozoic supracrustal
belt in the northwestern Norrbotten ore province (northernmost Sweden) was
investigated to characterize its structural components, assess hydrothermal
alteration–structural geology correlations, and constrain a paired
deformation–fluid flow evolution for the belt. New geological mapping of
five key areas (Eustiljåkk, Ekströmsberg, Tjårrojåkka,
Kaitum West, and Fjällåsen–Allavaara) indicates two major
compressional events (D1 and D2) have affected the belt, with each
associated with hydrothermal alteration types typical for iron oxide–apatite
and iron oxide Cu–Au systems in the region. Early D1 generated a
regionally distributed, penetrative S1 foliation and oblique reverse
shear zones that show a southwest-block-up sense of shear that formed in
response to NE–SW crustal shortening. Peak regional metamorphism at
epidote–amphibolite facies broadly overlaps with this D1 event. Based
on overprinting relationships, D1 is associated with regional scapolite ± albite, magnetite + amphibole, and late calcite alteration of
mafic rock types. These hydrothermal mineral associations linked to D1
structures may form part of a regionally pervasive evolving fluid flow event
but are separated in this study by crosscutting relationships. During D2 deformation, folding of S0–S1 structures
generated F2 folds with steeply plunging fold axes in low-strain areas.
NNW-trending D1 shear zones experienced reverse dip-slip reactivation
and strike-slip-dominated movements along steep, E–W-trending D2 shear
zones, producing brittle-plastic structures. Hydrothermal alteration linked
to D2 structures is a predominantly potassic–ferroan association
comprising K-feldspar ± epidote ± quartz ± biotite ± magnetite ± sericite ± sulfides. Locally, syn- or post-tectonic
calcite is the main alteration mineral in D2 shear zones that intersect
mafic rocks. Our results highlight the importance of combining structural
geology with the study of hydrothermal alterations at regional to
belt scales to understand the temporal–spatial relationship between
mineralized systems. Based on the mapping results and microstructural
investigations as well as a review of earlier tectonic models presented for
adjacent areas, we suggest a new structural model for this part of the
northern Fennoscandian Shield. The new model emphasizes the importance of
reactivation of early structures, and the model harmonizes with tectonic
models presented by earlier workers based mainly on petrology of the
northern Norrbotten area.