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Propagation of back-arc extension into the arc lithosphere in the southern New Hebrides volcanic arc

Citation

Patriat, M and Collot, J and Danyushevsky, LV and Fabre, M and Meffre, S and Falloon, T and Rouillard, P and Pelletier, B and Roach, M and Fournier, M, Propagation of back-arc extension into the arc lithosphere in the southern New Hebrides volcanic arc, Geochemistry, Geophysics, Geosystems, 16, (9) pp. 3142-3159. ISSN 1525-2027 (2015) [Refereed Article]


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Copyright Statement

Copyright 2015 American Geophysical Union

DOI: doi:10.1002/2015GC005717

Abstract

New geophysical data acquired during three expeditions of the R/V Southern Surveyor in the southern part of the North Fiji Basin allow us to characterize the deformation of the upper plate at the southern termination of the New Hebrides subduction zone, where it bends eastward along the Hunter Ridge. Unlike the northern end of the Tonga subduction zone, on the other side of the North Fiji Basin, the 90 bend does not correspond to the transition from a subduction zone to a transform fault, but it is due to the progressive retreat of the New Hebrides trench. The subduction trench retreat is accommodated in the upper plate by the migration toward the southwest of the New Hebrides arc and toward the south of the Hunter Ridge, so that the direction of convergence remains everywhere orthogonal to the trench. In the back-arc domain, the active deformation is characterized by propagation of the back-arc spreading ridge into the Hunter volcanic arc. The N-S spreading axis propagates southward and penetrates in the arc, where it connects to a sinistral strike-slip zone via an oblique rift. The collision of the Loyalty Ridge with the New Hebrides arc, less than two million years ago, likely initiated this deformation pattern and the fragmentation of the upper plate. In this particular geodynamic setting, with an oceanic lithosphere subducting beneath a highly sheared volcanic arc, a wide range of primitive subduction-related magmas has been produced including adakites, island arc tholeiites, back-arc basin basalts, and medium-K subduction-related lavas.

Item Details

Item Type:Refereed Article
Keywords:Vanuatu, sea floor spreading, subduction zone
Research Division:Earth Sciences
Research Group:Geology
Research Field:Tectonics
Objective Division:Expanding Knowledge
Objective Group:Expanding Knowledge
Objective Field:Expanding Knowledge in the Earth Sciences
Author:Danyushevsky, LV (Professor Leonid Danyushevsky)
Author:Meffre, S (Dr Sebastien Meffre)
Author:Falloon, T (Dr Trevor Falloon)
Author:Roach, M (Dr Michael Roach)
ID Code:105857
Year Published:2015
Web of Science® Times Cited:1
Deposited By:Centre for Ore Deposit Research - CODES CoE
Deposited On:2016-01-18
Last Modified:2016-08-24
Downloads:27 View Download Statistics

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