Seismicity properties of the Chain Transform Fault inferred using data from the PI-LAB experiment

Author:

Leptokaropoulos Konstantinos1ORCID,Rychert Catherine A.1ORCID,Harmon Nicholas1ORCID,Kendall John-Michael2ORCID

Affiliation:

1. University of Southampton

2. University of Oxford

Funder

Natural Environment Research Council

European Research Council

Publisher

Wiley

Reference84 articles.

1. Earthquake slip on oceanic transform faults;Abercrombie R. E.;Nature,2001

2. The 2015 Mw 7.1 earthquake on the Charlie-Gibbs transform fault: Repeating earthquakes and multimodal slip on a slow oceanic transform;Aderhold K.;Geophysical Research Letters,2016

3. Sediment characterization at the equatorial Mid-Atlantic Ridge from P-to-S teleseismic phase conversions recorded on the PI-LAB experiment;Agius M. R.;Geophysical Research Letters,2018

4. Agius M. R. Rychert C. A. Harmon N. Tharimena S. & Kendall J. M. (2021). A thin mantle transition zone beneath the equatorial Mid-Atlantic Ridge. Nature doi: 10.1038/s41586-020-03139-x

5. NLOADF: A program for computing oceantide loading;Agnew D. C.;Journal of Geophysical Research.,1997

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