. . . "58"^^ . . . . . . . "zaobloukov\u00E1 p\u00E1nev"@cs . . . . "5688"^^ . "zaobloukov\u00E9"@cs . . . . . . . . . "1271939"^^ . . . . . "zaobloukov\u00E9 oblasti"@cs . . . . . . . . . "zaobloukov\u00E9ho"@cs . . "zaobloukov\u00E9 p\u00E1nve"@cs . "Zaobloukov\u00E1 p\u00E1nev"@cs . "zaobloukov\u00FDch"@cs . . . . . . "16261279"^^ . . . . . . "Zaobloukov\u00E1 p\u00E1nev (anglicky back-arc basin nebo retro-arc basin) je mo\u0159sk\u00E9 sedimenta\u010Dn\u00ED prost\u0159ed\u00ED souvisej\u00EDc\u00ED s ostrovn\u00EDmi oblouky a subduk\u010Dn\u00EDmi z\u00F3nami.Zaobloukov\u00E9 p\u00E1nve vznikaj\u00ED na konvergentn\u00EDch okraj\u00EDch tektonick\u00FDch desek. V sou\u010Dasnosti se nach\u00E1z\u00ED v\u011Bt\u0161ina takov\u00FDch p\u00E1nv\u00ED v z\u00E1padn\u00ED \u010D\u00E1sti Tich\u00E9ho oce\u00E1nu. V\u011Bt\u0161ina z nich vznikla v d\u016Fsledku tenzn\u00EDch sil p\u0159i subdukci oce\u00E1nsk\u00E9 k\u016Fry."@cs . . . . . . "zaobloukov\u00FDch p\u00E1nv\u00ED"@cs . . . . . . . . . . . . "Zaobloukov\u00E1 p\u00E1nev (anglicky back-arc basin nebo retro-arc basin) je mo\u0159sk\u00E9 sedimenta\u010Dn\u00ED prost\u0159ed\u00ED souvisej\u00EDc\u00ED s ostrovn\u00EDmi oblouky a subduk\u010Dn\u00EDmi z\u00F3nami.Zaobloukov\u00E9 p\u00E1nve vznikaj\u00ED na konvergentn\u00EDch okraj\u00EDch tektonick\u00FDch desek. V sou\u010Dasnosti se nach\u00E1z\u00ED v\u011Bt\u0161ina takov\u00FDch p\u00E1nv\u00ED v z\u00E1padn\u00ED \u010D\u00E1sti Tich\u00E9ho oce\u00E1nu. V\u011Bt\u0161ina z nich vznikla v d\u016Fsledku tenzn\u00EDch sil p\u0159i subdukci oce\u00E1nsk\u00E9 k\u016Fry. Zaobloukov\u00E9 p\u00E1nve sice p\u016Fvodn\u011B nebyly koncepc\u00ED deskov\u00E9 tektoniky p\u0159\u00EDmo p\u0159edpokl\u00E1d\u00E1ny, ale pln\u011B zapadaj\u00ED do modern\u00EDch koncepc\u00ED vysv\u011Btluj\u00EDc\u00EDch chladnut\u00ED Zem\u011B."@cs . .