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\begin{document}

\title{Imaging seismic and aseismic plate coupling with interferometric radar
(InSAR) in the Hikurangi subduction zone}



\author[1]{Louise Maubant}%
\author[1]{William Benjamin Frank}%
\author[2]{Laura Wallace}%
\author[2]{Charles A. Williams}%
\author[2]{Ian James Hamling}%
\affil[1]{Massachusetts Institute of Technology}%
\affil[2]{GNS Science}%


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  \date{May 27, 2024}


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\begin{abstract}
The coupling at the interface between tectonic plates is a key
geophysical parameter to capture the frictional locking across plate
boundaries, and provides a means to estimate where tectonic strain is
accumulating through time. Here, we use both interferometric radar
(InSAR) and GNSS data to investigate the plate coupling of the Hikurangi
subduction zone beneath the North Island of New Zealand, where multiple
slow slip cycles are superimposed on the long-term loading. We estimate
the plate coupling across the subduction zone over different
observational periods (2, 4, and 10 years) targeting different stages of
the slow slip cycles. Our results highlight the importance of the
observational period when interpreting coupling maps, notably
highlighting the temporal dependence of plate coupling. Through our
analysis of multiple geodetic datasets, we demonstrate how InSAR
provides powerful constraints on the spatial resolution of plate
coupling, even in a region where a dense GNSS network exists.%
\end{abstract}%



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