Publication details for Professor Christine PeircePeirce, C., Gardiner, A. & Sinha, M.C. (2005). Temporal and spatial cyclicity of accretion at slow-spreading ridges - evidence from the Reykjanes Ridge. Geophysical Journal International 163(1): 56-78.
- Publication type: Journal Article
- ISSN/ISBN: 0956-540X, 1365-246X
- DOI: 10.1111/j.1365-246X.2005.02738.x
- Keywords: crustal accretion; crustal structure; gravity anomalies; mid-ocean ridges; oceanic crust; residual mantle Bouguer anomaly.
- Further publication details on publisher web site
- Durham Research Online (DRO) - may include full text
Author(s) from Durham
A unifying model of oceanic crustal development at slow
spreading rates is presented in which accretion follows a cyclic pattern
of magmatic construction and tectonic destruction, controlled by
along-axis variation in melt supply and coupled to along-axis variation in
spreading rate and across-axis asymmetry in spreading.
This study focuses on the Reykjanes Ridge, Mid-Atlantic Ridge south of
Iceland, which is divided along its entire length into numerous axial
volcanic ridges (AVR). Five adjacent AVRs have been analysed, located
between 57 deg 30N and 58 deg 30N and south of any strong Iceland hotspot
influence. The seabed morphology of each AVR is investigated using
sidescan sonar data to determine relative age and eruptive history.
Along-axis gravity profiles for each AVR are modelled relative to a
seismically derived crustal reference model, to reveal the underlying
crustal thickness and density structure. Correlating these models with
seabed features, crustal structure, ridge segment morphology and relative
ages, a model of cyclic ridge segmentation is developed in which accretion
results in adjacent AVRs with a range of crustal features which, when
viewed collectively, reveal that second-order segments on the Reykjanes
Ridge have an along-axis length of 70 km and comprise several adjacent
AVRs which, in turn, reflect the pattern of third-order segmentation.
Tectono-magmatic accretion is shown to operate on the scale of individual
AVRs, as well as on the scale of the second-order segment as a whole.
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