During　the　32nd　Chinese　National　Antarctic　Research　Expedition,　the　Frequency-Modulated　Continuous-Wave　(FMCW)　radar　was　used　for　the　first　time　to　obtain　the　distribution　of　shallow　isochronous　layers　within　the　East　Antarctic　region　extending　from　Zhongshan　Station　to　Kunlun　Station.　Taking　a　typical　area　as　a　case　study,　this　article　describes　the　complete　workflow　used　in　radar　data　processing,　including　signal　processing　and　extraction　of　isochronous　layers.　The　wave　velocity　model　is　established　according　to　an　empirical　formula　to　calculate　the　depth　of　the　layer,　and　the　result　is　compared　and　corrected　with　the　volcanic　record　in　ice　core　DT263;　the　relative　error　of　depth　is　only　approximately　5%.　The　echograms　of　the　isochronous　layers　in　three　regions　are　presented,　including　the　area　around　the　Dome　A,　the　area　100　km　from　the　Dome　A　and　the　area　in　the　Lambert　Glacier.　A　comparison　of　the　echograms　within　the　three　regions　shows　that　the　isochronous　layers　are　relatively　stable　in　the　Dome　A　and　change　more　intensely　in　the　Lambert　Glacier,　while　the　folding　of　the　layer　occurs　in　a　concentrated　area　near　Dome　A.　This　folding　may　be　due　to　the　local　layer　mixing　and　compression　caused　by　the　ice　flow　and　wind-driven　processes.　The　analysis　of　the　distribution　of　the　shallow　isochronous　layers　and　age-depth　information　from　different　regions　provides　important　data　that　support　the　calculation　of　large-scale　accumulation　rates　and　flow　history　in　the　Antarctic.