Early mafic magmatism and crustal anatexis on the Isle of Rum: evidence from the Am Màm intrusion breccia

NICOLL, GRAEME R. and Holness, Marian B. and TROLL, VALENTIN R. and DONALDSON, COLIN H. and HOLOHAN, EOGHAN P. and EMELEUS, C. HENRY and CHEW, DAVID (2009) Early mafic magmatism and crustal anatexis on the Isle of Rum: evidence from the Am Màm intrusion breccia. Geological Magazine, 146 (03). p. 368. ISSN 0016-7568, ESSN: 1469-5081 DOI https://doi.org/10.1017/S0016756808005864

[img] Text
early_mafic_magmatism_and_crustal_anatexis_on_the_isle_of_rum_evidence_from_the_am_mam_intrusion_breccia.pdf - Published Version
Restricted to Registered users only

Download (3MB) | Request a copy
Official URL: http://doi.org/10.1017/S0016756808005864


The Rum Igneous Centre comprises two early marginal felsic complexes (the Northern Marginal Zone and the Southern Mountains Zone), along with the later central ultrabasic–basic layered intrusions. These marginal complexes represent the remnants of near-surface to eruptive felsic magmatism associated with caldera collapse, examples of which are rare in the North Atlantic Igneous Province. Rock units include intra-caldera collapse breccias, rhyolitic ignimbrite deposits and shallow-level felsic intrusions, as well the enigmatic ‘Am Màm intrusion breccia’. The latter comprises a dacitic matrix enclosing lobate basaltic inclusions (~1–15 cm) and a variety of clasts, ranging from millimetres to tens of metres in diameter. These clasts comprise Lewisian gneiss, Torridonian sandstone and coarse gabbro. Detailed re-mapping of the Am Màm intrusion breccia has shown its timing of emplacement as syn-caldera, rather than pre-caldera as previously thought. Textural analysis of entrained clasts and adjacent, uplifted country rocks has revealed their thermal metamorphism by early mafic intrusions at greater depth than their present structural position. These findings provide a window into the evolution of the early mafic magmas responsible for driving felsic magmatism on Rum. Our data help constrain some of the physical parameters of this early magma–crust interaction and place it within the geochemical evolution of the Rum Centre.

Item Type: Article
Uncontrolled Keywords: 2009AREP;
Subjects: 05 - Petrology - Igneous, Metamorphic and Volcanic Studies
Divisions: 05 - Petrology - Igneous, Metamorphic and Volcanic Studies
Journal or Publication Title: Geological Magazine
Volume: 146
Page Range: p. 368
Identification Number: https://doi.org/10.1017/S0016756808005864
Depositing User: Sarah Humbert
Date Deposited: 09 Apr 2017 22:05
Last Modified: 09 Apr 2017 22:05
URI: http://eprints.esc.cam.ac.uk/id/eprint/3900

Actions (login required)

View Item View Item

About cookies