The protracted development of focused magmatic intrusion during continental rifting
The protracted development of focused magmatic intrusion during continental rifting
The transition from mechanical thinning toward focused magmatic intrusion during continental rifting is poorly constrained; the tectonically active Main Ethiopian Rift (MER) provides an ideal study locale to address this issue. The presence of linear magmatic-tectonic belts in the relatively immature central MER may indicate that the transition from mechanical to magmatic rifting is more spatially distributed and temporally protracted than has previously been assumed. Here we examine lava geochemistry and vent distribution of a Pliocene-Quaternary linear magmatic chain along the western margin of the central MER—the Akaki Magmatic Zone. Our results show limited variability in parental magma that evolve in a complex polybaric fractionation system that has not changed significantly over the past 3 Ma. Our results suggest the following: (1) channeling of plume material and the localization of shear- or topography-induced porosity modulates melt intrusion into the continental lithosphere. (2) Pre-existing lithospheric structures may act as catalysts for intrusion of magmas into the lithospheric mantle. (3) The midcrustal to upper crustal strain regime dictates the surface orientation of volcanic vents. Therefore, although linear magmatic belts like those in the central MER may young progressively toward the rift axis and superficially resemble oceanic style magmatism, they actually represent prebreakup magmatism on continental crust. The oldest linear magmatic belts observed seismically and magnetically at the edge of the ocean basins thus may not, as is often assumed, actually mark the onset of seafloor spreading.
rifting, Main Ethiopian Rift
875-897
Rooney, Tyrone O.
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Bastow, Ian D.
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Keir, Derek
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Mazzarini, Francesco
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Movsesian, Emily
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Grosfils, Eric B.
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Zimbelman, James R.
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Ramsey, Michael S.
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Ayalew, Dereje
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Yirgu, Gezahegn
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June 2014
Rooney, Tyrone O.
c5c64eee-082a-4199-861d-c1d83b50a92c
Bastow, Ian D.
7a2698d0-d535-4462-a9a9-0e3293d2d667
Keir, Derek
5616f81f-bf1b-4678-a167-3160b5647c65
Mazzarini, Francesco
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Movsesian, Emily
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Grosfils, Eric B.
55688edd-8008-4677-af6b-8a16273965a9
Zimbelman, James R.
8425f59f-0ed8-43fe-9e0e-c26bffa81b4c
Ramsey, Michael S.
abd8f35d-e753-406d-a4f6-01859d84052c
Ayalew, Dereje
aeb42f7d-2062-42f1-a1a2-a8c014d0c1fe
Yirgu, Gezahegn
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Rooney, Tyrone O., Bastow, Ian D., Keir, Derek, Mazzarini, Francesco, Movsesian, Emily, Grosfils, Eric B., Zimbelman, James R., Ramsey, Michael S., Ayalew, Dereje and Yirgu, Gezahegn
(2014)
The protracted development of focused magmatic intrusion during continental rifting.
Tectonics, 33 (6), .
(doi:10.1002/2013TC003514).
Abstract
The transition from mechanical thinning toward focused magmatic intrusion during continental rifting is poorly constrained; the tectonically active Main Ethiopian Rift (MER) provides an ideal study locale to address this issue. The presence of linear magmatic-tectonic belts in the relatively immature central MER may indicate that the transition from mechanical to magmatic rifting is more spatially distributed and temporally protracted than has previously been assumed. Here we examine lava geochemistry and vent distribution of a Pliocene-Quaternary linear magmatic chain along the western margin of the central MER—the Akaki Magmatic Zone. Our results show limited variability in parental magma that evolve in a complex polybaric fractionation system that has not changed significantly over the past 3 Ma. Our results suggest the following: (1) channeling of plume material and the localization of shear- or topography-induced porosity modulates melt intrusion into the continental lithosphere. (2) Pre-existing lithospheric structures may act as catalysts for intrusion of magmas into the lithospheric mantle. (3) The midcrustal to upper crustal strain regime dictates the surface orientation of volcanic vents. Therefore, although linear magmatic belts like those in the central MER may young progressively toward the rift axis and superficially resemble oceanic style magmatism, they actually represent prebreakup magmatism on continental crust. The oldest linear magmatic belts observed seismically and magnetically at the edge of the ocean basins thus may not, as is often assumed, actually mark the onset of seafloor spreading.
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e-pub ahead of print date: 3 June 2014
Published date: June 2014
Keywords:
rifting, Main Ethiopian Rift
Organisations:
Geology & Geophysics
Identifiers
Local EPrints ID: 365415
URI: http://eprints.soton.ac.uk/id/eprint/365415
ISSN: 0278-7407
PURE UUID: b0d81233-caa6-463a-a8db-5b4cd5307cb0
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Date deposited: 04 Jun 2014 09:05
Last modified: 15 Mar 2024 03:38
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Contributors
Author:
Tyrone O. Rooney
Author:
Ian D. Bastow
Author:
Francesco Mazzarini
Author:
Emily Movsesian
Author:
Eric B. Grosfils
Author:
James R. Zimbelman
Author:
Michael S. Ramsey
Author:
Dereje Ayalew
Author:
Gezahegn Yirgu
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