KnowraBack-arc basinLinked fromLinked fromThe 16 pages that link to Back-arc basin, each with the reason it gives.All 16Broader topic 4Related 4Narrower topic 3Compared with 5Volcanic arcCompared with: Its extension-related volcanism lies behind, rather than along, the arc's volcanic front.Wilson cycleCompared with: A short-lived basin born from closing rather than continental breakup.Island arcRelated: Its position behind an island arc reveals how the overriding plate can stretch as subduction proceeds.Japanese archipelagoRelated: Back-arc extension helped create the sea separating Japan from the mainland.Foreland basinCompared with: It forms behind an arc through tectonic extension, rather than beside an orogen through flexural loading.Izu–Bonin–Mariana arcRelated: Extension behind this arc opened the Shikoku and Parece Vela basins.Pannonian BasinNarrower topic: The Pannonian region developed through extension behind the Carpathian arc.Slab rollbackBroader topic: Extension behind the arc can open a basin as rollback pulls the overriding plate apart.Tectonic subsidenceBroader topic: Extension behind arcs can thin lithosphere and drive tectonic subsidence.Continental riftCompared with: It can form by extension, but its setting depends on nearby subduction.Deception IslandNarrower topic: The Bransfield Basin is commonly described as a developing back-arc basin.Forearc basinCompared with: Its position behind the arc distinguishes it from a trench-side forearc basin.Central Asian Orogenic BeltBroader topic: Back-arc spreading created oceanic crust that could later be consumed or accreted.Japanese island arcRelated: Extension behind Japan’s volcanic front helped open the Sea of Japan.Taupō Volcanic ZoneNarrower topic: The zone lies within the extensional back-arc setting that helps magma rise through the crust.Oceanic basinBroader topic: It is a specific tectonic setting where a smaller oceanic basin can develop.
KnowraBack-arc basinLinked fromLinked fromThe 16 pages that link to Back-arc basin, each with the reason it gives.All 16Broader topic 4Related 4Narrower topic 3Compared with 5Volcanic arcCompared with: Its extension-related volcanism lies behind, rather than along, the arc's volcanic front.Wilson cycleCompared with: A short-lived basin born from closing rather than continental breakup.Island arcRelated: Its position behind an island arc reveals how the overriding plate can stretch as subduction proceeds.Japanese archipelagoRelated: Back-arc extension helped create the sea separating Japan from the mainland.Foreland basinCompared with: It forms behind an arc through tectonic extension, rather than beside an orogen through flexural loading.Izu–Bonin–Mariana arcRelated: Extension behind this arc opened the Shikoku and Parece Vela basins.Pannonian BasinNarrower topic: The Pannonian region developed through extension behind the Carpathian arc.Slab rollbackBroader topic: Extension behind the arc can open a basin as rollback pulls the overriding plate apart.Tectonic subsidenceBroader topic: Extension behind arcs can thin lithosphere and drive tectonic subsidence.Continental riftCompared with: It can form by extension, but its setting depends on nearby subduction.Deception IslandNarrower topic: The Bransfield Basin is commonly described as a developing back-arc basin.Forearc basinCompared with: Its position behind the arc distinguishes it from a trench-side forearc basin.Central Asian Orogenic BeltBroader topic: Back-arc spreading created oceanic crust that could later be consumed or accreted.Japanese island arcRelated: Extension behind Japan’s volcanic front helped open the Sea of Japan.Taupō Volcanic ZoneNarrower topic: The zone lies within the extensional back-arc setting that helps magma rise through the crust.Oceanic basinBroader topic: It is a specific tectonic setting where a smaller oceanic basin can develop.