\documentclass[10pt]{article}

\usepackage{fullpage}
\usepackage{CJKutf8} 
\usepackage[utf8]{inputenc}
\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[ngerman,english]{babel}



\usepackage{float}






% Edit this header.tex file to include frontmatter definitions and global macros

% Add here any LaTeX packages you would like to load in all document blocks
% \usepackage{xspace}

% Add here any LaTeX macros you would like to load in all document blocks
% \def\example{This is an example macro.}

% -----

\iflatexml
% Add here any LaTeXML-specific commands

% -----

\else
% Add here any export style-specific LaTeX commands. These will only be loaded upon document export.
% \paperfield{Subject domain of my document}
% \keywords{keyword1, keyword2}
% \corraddress{Author One PhD, Department, Institution, City, State or Province, Postal Code, Country}
% \fundinginfo{Funder One, Funder One Department, Grant/Award Number: 123456.}
\fi


\begin{document}
\begin{CJK}{UTF8}{gbsn}

\title{Shallow bulk yielding above buried sections of the 2021 Mw7.4 Maduo,
Tibet, rupture}



\author[1]{Solene L Antoine}%
\author[2]{Zhen Liu}%
\author[3]{Rishav Mallick}%
\author[4]{Arthur Delorme}%
\author[5]{Yann Klinger}%
\affil[1]{Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA, USA}%
\affil[2]{California Institute of Technology}%
\affil[3]{Affiliation not available}%
\affil[4]{Institut De Physique Du Globe De Paris}%
\affil[5]{Université de Paris Cité, Institut de physique du globe de Paris, CNRS}%


\vspace{-1em}



  
  \date{May 06, 2026}


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





\selectlanguage{english}
\begin{abstract}
Surface deformation associated with continental earthquake ruptures
includes localized deformation on the faults, as well as deformation in
the surrounding medium through distributed and/or diffuse processes.
However, the role of the diffuse part of the surface deformation to the
overall rupture process, as well as its underlying physical mechanisms
are not yet well understood. In this study, we compute high-resolution
near-fault displacement maps from optical image correlations for the
2021/05/21 M\textsubscript{w}7.4 Maduo, Tibet, strike-slip earthquake,
and measure the contributions of the different deformation components to
the surface deformations for that event. Results show that surface slip
along primary faults accommodates, on average, only
\textasciitilde{}25\% of the total surface deformation. Majority of the
surface coseismic deformation is in fact accommodated by diffuse
deformation,especially in the epicentral area where no surface slip was
observed. In fact, the contribution of the diffuse deformation increases
as localized deformation on the fault decreases. Localized deformation
also decreases with decreasing total surface displacement. These
observations highlight a gradual localization of the surface coseismic
deformation, from regions of diffuse low (0.1-0.3\%) strain, to regions
of highly localized (\textgreater{}1 \%) strain, with increasing
coseismic displacement. Using simple two-dimensional mechanical models
we show that diffuse deformation may correspond to elastoplastic bulk
yielding, accounting for the deficit in shallow fault slip in the
regions of surface rupture gap.%
\end{abstract}%



\sloppy




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

