Ardnamurchan 3D cone-sheet architecture explained by a single elongate magma chamber View Full Text


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Article Info

DATE

2013-12

AUTHORS

Steffi Burchardt, Valentin R. Troll, Lucie Mathieu, Henry C. Emeleus, Colin H. Donaldson

ABSTRACT

The Palaeogene Ardnamurchan central igneous complex, NW Scotland, was a defining place for the development of the classic concepts of cone-sheet and ring-dyke emplacement and has thus fundamentally influenced our thinking on subvolcanic structures. We have used the available structural information on Ardnamurchan to project the underlying three-dimensional (3D) cone-sheet structure. Here we show that a single elongate magma chamber likely acted as the source of the cone-sheet swarm(s) instead of the traditionally accepted model of three successive centres. This proposal is supported by the ridge-like morphology of the Ardnamurchan volcano and is consistent with the depth and elongation of the gravity anomaly underlying the peninsula. Our model challenges the traditional model of cone-sheet emplacement at Ardnamurchan that involves successive but independent centres in favour of a more dynamical one that involves a single, but elongate and progressively evolving magma chamber system. More... »

PAGES

2891

Identifiers

URI

http://scigraph.springernature.com/pub.10.1038/srep02891

DOI

http://dx.doi.org/10.1038/srep02891

DIMENSIONS

https://app.dimensions.ai/details/publication/pub.1021909664

PUBMED

https://www.ncbi.nlm.nih.gov/pubmed/24100542


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