\documentclass[10pt]{article}

\usepackage{fullpage}
\usepackage{setspace}
\usepackage{parskip}
\usepackage{titlesec}
\usepackage[section]{placeins}
\usepackage{xcolor}
\usepackage{breakcites}
\usepackage{lineno}
\usepackage{hyphenat}





\PassOptionsToPackage{hyphens}{url}
\usepackage[colorlinks = true,
            linkcolor = blue,
            urlcolor  = blue,
            citecolor = blue,
            anchorcolor = blue]{hyperref}
\usepackage{etoolbox}
\makeatletter
\patchcmd\@combinedblfloats{\box\@outputbox}{\unvbox\@outputbox}{}{%
  \errmessage{\noexpand\@combinedblfloats could not be patched}%
}%
\makeatother


\usepackage{natbib}




\renewenvironment{abstract}
  {{\bfseries\noindent{\abstractname}\par\nobreak}\footnotesize}
  {\bigskip}

\titlespacing{\section}{0pt}{*3}{*1}
\titlespacing{\subsection}{0pt}{*2}{*0.5}
\titlespacing{\subsubsection}{0pt}{*1.5}{0pt}


\usepackage{authblk}


\usepackage{graphicx}
\usepackage[space]{grffile}
\usepackage{latexsym}
\usepackage{textcomp}
\usepackage{longtable}
\usepackage{tabulary}
\usepackage{booktabs,array,multirow}
\usepackage{amsfonts,amsmath,amssymb}
\providecommand\citet{\cite}
\providecommand\citep{\cite}
\providecommand\citealt{\cite}
% You can conditionalize code for latexml or normal latex using this.
\newif\iflatexml\latexmlfalse
\providecommand{\tightlist}{\setlength{\itemsep}{0pt}\setlength{\parskip}{0pt}}%

\AtBeginDocument{\DeclareGraphicsExtensions{.pdf,.PDF,.eps,.EPS,.png,.PNG,.tif,.TIF,.jpg,.JPG,.jpeg,.JPEG}}

\usepackage[utf8]{inputenc}
\usepackage[english]{babel}



\usepackage{float}








\begin{document}

\title{Seismic signature of subduction termination from teleseismic P- and
S-wave arrival-time tomography: the case of northern Borneo}



\author[1]{Simone Pilia}%
\affil[1]{University of  Milan-Bicocca}%


\vspace{-1em}



  
  \date{May 08, 2024}


\begingroup
\let\center\flushleft
\let\endcenter\endflushleft
\maketitle
\endgroup





\selectlanguage{english}
\begin{abstract}
Studies attempting to gain new insights into the last stage of the
subduction cycle are typically challenged by limited direct observations
owing to a lack of recent post-subduction settings around the world.
Central to unravelling how the subduction cycle ends is an understanding
of crust and mantle processes that take place after subduction
termination. Northern Borneo (Malaysia) represents a unique natural
laboratory because it has been the site of two sequential subduction
episodes of opposite polarity since the mid-Paleogene. The region
exhibits several enigmatic post-subduction (after \textasciitilde{}10
Ma) features, including: subsidence followed by rapid uplift, localised
intraplate volcanism, possible orogen collapse, and a pluton that
emerged to become the third highest peak in southeast Asia, Mt Kinabalu
(4095 m). Arrival-time residuals from distant earthquake data recorded
by the nBOSS seismic network have been used to investigate P- and
S-wavespeed variations in the crust and underlying upper mantle beneath
northern Borneo. Our 3-D tomographic images consistently show a
high-velocity perturbation in western Sabah that we associate with an
upper-mantle remnant of the Proto South-China Sea slab, thus providing
important constraints for tectonic reconstructions of SE Asia. The
tomographic models, combined with other seismological and geological
information, reveal evidence for lithospheric removal in eastern Sabah
via a drip instability. Our results suggest that lithospheric drips can
be smaller than previously thought, yet their effects on the
post-subduction evolution of continental lithosphere can be significant.%
\end{abstract}%



\sloppy




\selectlanguage{english}
\FloatBarrier
\end{document}

