\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{Interseismic uplift of anticlines above the Rakhine-Bangladesh
Megathrust from ALOS-2 InSAR}



\author[1]{Jeng-Hann Chong}%
\author[2]{Bar Oryan}%
\author[3]{Michael S. Steckler}%
\author[4]{Eric O. Lindsey}%
\affil[1]{University of New Mexico}%
\affil[2]{Scripps Institution of Oceanography}%
\affil[3]{Columbia University}%
\affil[4]{The University of New Mexico}%


\vspace{-1em}



  
  \date{June 06, 2024}


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





\selectlanguage{english}
\begin{abstract}
The shallow portion of a megathrust represents the zone of first contact
between two colliding plates, and its rheological properties control the
seismic and tsunami hazards generated by the fault. Unfortunately,
underwater geodetic observations are sparse due to the high cost of
obtaining geodetic data, meaning limited information is available on the
interseismic behavior of this part of most megathrusts. The
Rakhine-Bangladesh megathrust offers a unique opportunity to probe the
behavior of the shallow megathrust as it is the only ocean-continent
subduction zone where the near-trench region is fully accessible on
land. Here, we use observations from ALOS-2 wide-swath imagery spanning
2015 to 2022 to conduct an InSAR timeseries analysis of the overriding
plate within Bangladesh and the Indo-Myanmar Ranges. We identify a
narrow pattern of alternating uplift and subsidence associated with
mapped anticlines but show that it cannot be explained by plausible
rates of slip on the megathrust or other fault structures. Instead, we
argue that the deformation is likely caused by active aseismic folding
within the wedge above a shallow decollement. We show that estimates of
the decollement depth derived from a viscous folding model and the
observed anticline spacing are in agreement with previous seismic
observations of the decollement depth across the fold belt. We suggest
that the role of ductile deformation in the overriding plate in
subduction zones may be more important than previously recognized.%
\end{abstract}%



\sloppy


\textbf{Hosted file}

\verb`Interseismic_ALOS2_InSAR_RBM_final.docx`  available at \url{https://authorea.com/users/745467/articles/717487-interseismic-uplift-of-anticlines-above-the-rakhine-bangladesh-megathrust-from-alos-2-insar}

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

