A three-dimensional study of a crustal low velocity region beneath the 9,3'N overlapping spreading center


Bazin, S. and Sinha, M.C. (2003) A three-dimensional study of a crustal low velocity region beneath the 9,3'N overlapping spreading center. Geophysical Research Letters, 30, (2), 1039-[4pp]. (doi:10.1029/2002GL015137).

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Original Publication URL: http://dx.doi.org/10.1029/2002GL015137

Description/Abstract

Overlapping spreading centers (OSCs) play a key role in models of magma distribution at fast spreading ridges. To investigate the relationship between ridge-axis discontinuities and magma supply, we conducted a three-dimensional seismic reflection and tomography experiment at the 9°03′N OSC along the East Pacific Rise. Tomographic analysis imaged a broad mid-crustal low velocity zone (LVZ) beneath parts of the overlapper and the associated overlap basin, demonstrating that it is magmatically robust. The complementary datasets reveal a complex storage and tapping of melt: the LVZ and melt sill at either end of the overlap basin are not simply centered beneath the rise crest but are skewed inwards. The subsequent focussing of the LVZ and sill beneath the axis of the eastern limb appears to be due to melt migration toward the tip. The OSC western limb is less magmatically robust and may be in the process of dying.

Item Type: Article
Related URLs:
Keywords: SPREADING CENTRES, SEISMIC REFLECTION, EAST PACIFIC RISE, TOMOGRAPHY, GEOLOGY
Subjects: Q Science > QE Geology
G Geography. Anthropology. Recreation > GC Oceanography
Divisions: University Structure - Pre August 2011 > School of Ocean & Earth Science (SOC/SOES)
ePrint ID: 2227
Date Deposited: 20 May 2004
Last Modified: 27 Mar 2014 18:00
URI: http://eprints.soton.ac.uk/id/eprint/2227

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