Mechanisms responsible for igneous layering and the concentration of critical minerals within alkaline intrusions remain debated. The Ilímaussaq complex, South Greenland, is a layered alkaline intrusion containing economically important rare earth element (REE) deposits. Based on geochemical and petrological data, the two leading hypotheses for the formation of igneous layering at Ilímaussaq are: (1) repeated magma recharge and in situ nucleation of minerals; or (2) gravitational settling of crystal mats within a closed magmatic system. We provide novel field, rock magnetic, and crystallographic preferred orientation (CPO) data from two representative outcrops of igneous layering at Ilímaussaq to test these hypotheses. Our rock magnetic data show that both arfvedsonite and magnetite contribute to the anisotropy of magnetic susceptibility (AMS) fabrics, with magnetite defining a sub-vertical foliation across igneous layering. Our data show that the AMS fabric is inverse to the silicate fabric (i.e. the magnetic foliation is normal to the silicate foliation), and records consistent sub-horizontal mineral foliations and lineations vertically through the layers. Critically, the silicate fabric is often oblique in both strike and dip to the modal igneous layering. Our measured fabrics best support a closed system crystal mat model and subsequent phases of differential and intrusion-wide compaction.
CORE (COnnecting REpositories)
CORE (COnnecting REpositories)