Imperial College London

Prof Jenny Collier

Faculty of EngineeringDepartment of Earth Science & Engineering

Professor of Marine Geophysics
 
 
 
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Contact

 

+44 (0)20 7594 6443jenny.collier CV

 
 
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Location

 

4.46Royal School of MinesSouth Kensington Campus

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Summary

 

Publications

Citation

BibTex format

@article{Schlaphorst:2016:gji/ggv509,
author = {Schlaphorst, D and Kendall, JM and Collier, JS and Verdon, JP and Blundy, J and Baptie, B and Latchman, JL and Massin, F and Bouin, MP},
doi = {gji/ggv509},
journal = {Geophysical Journal International},
pages = {1405--1420},
title = {Water, oceanic fracture zones and the lubrication of subducting plate boundaries-insights from seismicity},
url = {http://dx.doi.org/10.1093/gji/ggv509},
volume = {204},
year = {2016}
}

RIS format (EndNote, RefMan)

TY  - JOUR
AB - We investigate the relationship between subduction processes and related seismicity for the Lesser Antilles Arc using the Gutenberg-Richter law. This power lawdescribes the earthquakemagnitude distribution, with the gradient of the cumulative magnitude distribution being commonly known as the b-value. The Lesser Antilles Arc was chosen because of its alongstrike variability in sediment subduction and the transition from subduction to strike-slip movement towards its northern and southern ends. The data are derived from the seismicity catalogues from the Seismic Research Centre of The University of the West Indies and the Observatoires Volcanologiques et Sismologiques of the Institut de Physique du Globe de Paris and consist of subcrustal events primarily from the slab interface. The b-value is found using a Kolmogorov-Smirnov test for a maximum-likelihood straight line-fitting routine. We investigate spatial variations in b-values using a grid-search with circular cells as well as an along-arc projection. Tests with different algorithms and the two independent earthquake cataloges provide confidence in the robustness of our results. We observe a strong spatial variability of the b-value that cannot be explained by the uncertainties. Rather than obtaining a simple north-south b-value distribution suggestive of the dominant control on earthquake triggering being water released from the sedimentary cover on the incoming American Plates, or a b-value distribution that correlates with on the obliquity of subduction, we obtain a series of discrete, high b-value 'bull's-eyes' along strike. These bull's-eyes, which indicate stress release through a higher fraction of small earthquakes, coincide with the locations of known incoming oceanic fracture zones on the American Plates. We interpret the results in terms of water being delivered to the Lesser Antilles subduction zone in the vicinity of fracture zones providing lubrication and thus changing the character of the related
AU - Schlaphorst,D
AU - Kendall,JM
AU - Collier,JS
AU - Verdon,JP
AU - Blundy,J
AU - Baptie,B
AU - Latchman,JL
AU - Massin,F
AU - Bouin,MP
DO - gji/ggv509
EP - 1420
PY - 2016///
SN - 1365-246X
SP - 1405
TI - Water, oceanic fracture zones and the lubrication of subducting plate boundaries-insights from seismicity
T2 - Geophysical Journal International
UR - http://dx.doi.org/10.1093/gji/ggv509
UR - http://hdl.handle.net/10044/1/32283
VL - 204
ER -