Three-dimensional P-wave velocity structure of oceanic core complexes at 13°N on the Mid-Atlantic Ridge

Research output: Contribution to journalAbstractpeer-review

Authors

  • Nuno Simao
  • Christine Peirce
  • Matthew Funnell
  • AH Robinson
  • Roger Searle
  • Christopher MacLeod

Colleges, School and Institutes

External organisations

  • Durham University
  • University of Durham, Department of Geological Sciences
  • Cardiff University

Abstract

The Mid-Atlantic Ridge at 13°N is regarded as a type locality for oceanic core complexes (OCCs), as it
contains, within ~70 km along the spreading axis, four that are at different stages of their life cycle. The
wealth of existing seabed observations and sampling makes this an ideal target to resolve contradictions
between the existing models of OCC development. Here we describe the results of P-wave seismic
tomographic modelling within a 60 x 60 km footprint, containing several OCCs, the ridge axis and both
flanks, which determines OCC crustal structure, detachment geometry and OCC interconnectivity along axis.
A grid of wide-angle seismic refraction data was acquired along a series of 17 transects within which a
network of 46 ocean-bottom seismographs was deployed. Approximately 130,000 first arrival travel times,
together with sparse Moho reflections, have been modelled, constraining the crust and uppermost mantle to a
depth of ~10 km below sea level. Depth slices through this 3-D model reveal several independent structures
each with a higher P-wave velocity (Vp) than its surrounds. At the seafloor, these features correspond to the
OCCs adjacent to the axial valley walls at 1320‟N and 1330‟N, and off axis at 1325‟N. These high-Vp
features display dipping trends into the deeper crust, consistent with the surface expression of each OCC‟s
detachment, implying that rocks of the mid-to-lower crust and uppermost mantle within the footwall are
juxtaposed against lower Vp material in the hanging-wall. The neovolcanic zone of the ridge axis has
systematically lower Vp than the surrounding crust at all depths, and is wider between OCCs. On average,
throughout the 13N region, the crust is ~6 km-thick. However, beneath a deep lava-floored basin between
axial OCCs the crust is thinner and is more characteristically oceanic in layering and velocity-depth
structure. Thicker crust at the ridge axis suggests a more magmatic phase of current crustal formation, while
modelling of the sparse Moho reflections suggests the crust-mantle boundary is a transition zone throughout
most of the 13N segment. Our results support a model in which OCCs are bounded by independent
detachment faults whose dip increases with depth and is variable with azimuth around each OCC, suggesting
a geometry and mechanism of faulting that is more complicated than previously thought. The steepness of
the northern flank of the 1320‟N detachment suggests that it represents a transfer zone between different
faulting regimes to the south and north. We propose that individual detachments may not be linked alongaxis,
and that OCCs act as transfer zones linking areas of normal spreading and detachment faulting. Along
ridge variation in magma supply influences the nature of this detachment faulting. Consequently, not only
does magma supply control how detachments rotate and migrate off axis before finally becoming inactive,
but also how, when and where new OCCs are created.

Details

Original languageEnglish
JournalGeophysical Journal International
Publication statusAccepted/In press - 20 Feb 2020