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TheCentralAsianLateMesozoicriftspstem(CALMRS)hasundergonetwostagesofdevelop-ment.TheearlyonespreadallovertheLateJurassicperiodandwasCharactcrizedwiththeformationofvolcano-teetonicstructuresofasubsidencecalderatypeandembryonicriftsvolcanogeneous-terrigenef