Seismic imaging of 'broken bridges': linking seismic to outcrop-scale investigations of intrusive magma lobes

Three-dimensional seismic datasets have provided unrivalled insights into magma flow within sub-volcanic systems. One of the key revelations is that sills appear to be constructed of a series of discrete magma lobes that form during the emplacement of magma into host-rock. We focus on a large sill,...

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Published in:Journal of the Geological Society
Main Authors: Schofield, N., Heaton, L., Holford, S., Archer, S., Jackson, C., Jolley, D.
Format: Article in Journal/Newspaper
Language:English
Published: Geological Soc Publ House 2012
Subjects:
Online Access:http://hdl.handle.net/2440/72704
https://doi.org/10.1144/0016-76492011-150
id ftunivadelaidedl:oai:digital.library.adelaide.edu.au:2440/72704
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spelling ftunivadelaidedl:oai:digital.library.adelaide.edu.au:2440/72704 2023-12-24T10:23:09+01:00 Seismic imaging of 'broken bridges': linking seismic to outcrop-scale investigations of intrusive magma lobes Schofield, N. Heaton, L. Holford, S. Archer, S. Jackson, C. Jolley, D. 2012 http://hdl.handle.net/2440/72704 https://doi.org/10.1144/0016-76492011-150 en eng Geological Soc Publ House Journal of the Geological Society, 2012; 169(4):421-426 0016-7649 2041-479X http://hdl.handle.net/2440/72704 doi:10.1144/0016-76492011-150 Holford, S. [0000-0002-4524-8822] © The Geological Society of London http://dx.doi.org/10.1144/0016-76492011-150 Journal article 2012 ftunivadelaidedl https://doi.org/10.1144/0016-76492011-150 2023-11-27T23:22:01Z Three-dimensional seismic datasets have provided unrivalled insights into magma flow within sub-volcanic systems. One of the key revelations is that sills appear to be constructed of a series of discrete magma lobes that form during the emplacement of magma into host-rock. We focus on a large sill, within the Faroe–Shetland Basin, North Atlantic, that is well imaged on seismic data, and identify the presence of ‘broken bridges’ within the sill, developed between elongate magma lobes, and reveal for the first time in three dimensions the development of broken bridges. Critically, by relating the imaged structures to key outcrop-scale examples we confirm that bridge and broken-bridge structures are oriented perpendicular to the magma flow direction. This work thus demonstrates a key link that can be made between seismic-scale investigation of intrusions and sub-seismic (outcrop-scale) processes, highlighting the seemingly scale-invariant nature of the magmatic emplacement process. Nick Schofield, Lucy Heaton, Simon P. Holford, Stuart G. Archer, Christopher A.-L. Jackson and David W. Jolley Article in Journal/Newspaper North Atlantic The University of Adelaide: Digital Library Archer ENVELOPE(162.867,162.867,-76.850,-76.850) Journal of the Geological Society 169 4 421 426
institution Open Polar
collection The University of Adelaide: Digital Library
op_collection_id ftunivadelaidedl
language English
description Three-dimensional seismic datasets have provided unrivalled insights into magma flow within sub-volcanic systems. One of the key revelations is that sills appear to be constructed of a series of discrete magma lobes that form during the emplacement of magma into host-rock. We focus on a large sill, within the Faroe–Shetland Basin, North Atlantic, that is well imaged on seismic data, and identify the presence of ‘broken bridges’ within the sill, developed between elongate magma lobes, and reveal for the first time in three dimensions the development of broken bridges. Critically, by relating the imaged structures to key outcrop-scale examples we confirm that bridge and broken-bridge structures are oriented perpendicular to the magma flow direction. This work thus demonstrates a key link that can be made between seismic-scale investigation of intrusions and sub-seismic (outcrop-scale) processes, highlighting the seemingly scale-invariant nature of the magmatic emplacement process. Nick Schofield, Lucy Heaton, Simon P. Holford, Stuart G. Archer, Christopher A.-L. Jackson and David W. Jolley
format Article in Journal/Newspaper
author Schofield, N.
Heaton, L.
Holford, S.
Archer, S.
Jackson, C.
Jolley, D.
spellingShingle Schofield, N.
Heaton, L.
Holford, S.
Archer, S.
Jackson, C.
Jolley, D.
Seismic imaging of 'broken bridges': linking seismic to outcrop-scale investigations of intrusive magma lobes
author_facet Schofield, N.
Heaton, L.
Holford, S.
Archer, S.
Jackson, C.
Jolley, D.
author_sort Schofield, N.
title Seismic imaging of 'broken bridges': linking seismic to outcrop-scale investigations of intrusive magma lobes
title_short Seismic imaging of 'broken bridges': linking seismic to outcrop-scale investigations of intrusive magma lobes
title_full Seismic imaging of 'broken bridges': linking seismic to outcrop-scale investigations of intrusive magma lobes
title_fullStr Seismic imaging of 'broken bridges': linking seismic to outcrop-scale investigations of intrusive magma lobes
title_full_unstemmed Seismic imaging of 'broken bridges': linking seismic to outcrop-scale investigations of intrusive magma lobes
title_sort seismic imaging of 'broken bridges': linking seismic to outcrop-scale investigations of intrusive magma lobes
publisher Geological Soc Publ House
publishDate 2012
url http://hdl.handle.net/2440/72704
https://doi.org/10.1144/0016-76492011-150
long_lat ENVELOPE(162.867,162.867,-76.850,-76.850)
geographic Archer
geographic_facet Archer
genre North Atlantic
genre_facet North Atlantic
op_source http://dx.doi.org/10.1144/0016-76492011-150
op_relation Journal of the Geological Society, 2012; 169(4):421-426
0016-7649
2041-479X
http://hdl.handle.net/2440/72704
doi:10.1144/0016-76492011-150
Holford, S. [0000-0002-4524-8822]
op_rights © The Geological Society of London
op_doi https://doi.org/10.1144/0016-76492011-150
container_title Journal of the Geological Society
container_volume 169
container_issue 4
container_start_page 421
op_container_end_page 426
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