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\begin{document}

\title{Forearc evolution in complex subduction settings -- Mesozoic and
Cenozoic examples from SE Asia}



\author[1,1]{Max Webb}%
\author[1,1]{Amy Gough}%
\affil[1]{SE Asia Research Group - Royal Holloway University of London}%


\vspace{-1em}



  
  \date{May 22, 2024}


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\begin{abstract}
SE Asia is renowned as a region of complex plate tectonic interactions,
both in the present day and throughout its Mesozoic and Cenozoic
history. The study of subduction processes in SE Asia has been
instrumental in our understanding of how complex subduction systems
develop and evolve, including understanding double subduction zones,
areas of subduction polarity reversal, and the interaction of subduction
and strike-slip systems. This complexity in subduction style makes SE
Asia an ideal natural laboratory for studying forearc development in a
range of subduction styles across a relatively small area still exposed
in the rock record. Here we present a recently studied example of
forearc development in a Mesozoic double subduction zone exposed on
Natuna Island in the South China Sea, as well as highlighting two other
examples of forearc development in SE Asia. These include a Cenozoic
subduction polarity reversal event and transform plate boundary in
western New Guinea and forearc sedimentation along the Sunda Trench. All
three scenarios chronicle histories of forearc accretion, either of
deep-water cherts or continental-derived turbidites, whilst also
recording the impacts of case-specific tectonic processes (such as
ophiolite obduction, arc-continent collision, or strike-slip movement)
that have fundamentally impacted their respective forearcs. Comparing
these contrasting examples shows that studying forearc development of
these complex subduction systems (including their structural styles,
geochemistry and timing of associated magmatism, and sedimentation) in
SE Asia can be a powerful tool for improving understanding of forearc
evolution in other ancient and complex subduction systems.%
\end{abstract}%



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