Emily Jones
Igneous layering and magma dynamics in alkaline intrusions: textural evidence for gravitational settling and compaction within cumulates
Jones, Emily; McCarthy, William; Magee, Craig; Mattsson, Tobias; Piazolo, Sandra; Hutchison, William; Humphreys, Madeleine C.S.
Authors
William McCarthy
Craig Magee
Tobias Mattsson
Sandra Piazolo
William Hutchison
Professor Madeleine Humphreys madeleine.humphreys@durham.ac.uk
Professor
Abstract
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.
Citation
Jones, E., McCarthy, W., Magee, C., Mattsson, T., Piazolo, S., Hutchison, W., & Humphreys, M. C. (online). Igneous layering and magma dynamics in alkaline intrusions: textural evidence for gravitational settling and compaction within cumulates. Journal of the Geological Society, https://doi.org/10.1144/jgs2024-181
Journal Article Type | Article |
---|---|
Acceptance Date | Apr 5, 2025 |
Online Publication Date | Apr 11, 2025 |
Deposit Date | Apr 10, 2025 |
Publicly Available Date | Apr 11, 2025 |
Journal | Journal of the Geological Society |
Print ISSN | 0016-7649 |
Electronic ISSN | 2041-479X |
Publisher | The Geological Society |
Peer Reviewed | Peer Reviewed |
DOI | https://doi.org/10.1144/jgs2024-181 |
Public URL | https://durham-repository.worktribe.com/output/3786236 |
Files
Published Journal Article
(5.2 Mb)
PDF
Publisher Licence URL
http://creativecommons.org/licenses/by/4.0/
You might also like
Deciphering variable mantle sources and hydrous inputs to arc magmas in Kamchatka
(2021)
Journal Article