About: Fold and thrust belt

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A fold and thrust belt (FTB) is a series of mountainous foothills adjacent to an orogenic belt, which forms due to contractional tectonics. Fold and thrust belts commonly form in the forelands adjacent to major orogens as deformation propagates outwards. Fold and thrust belts usually comprise both folds and thrust faults, commonly interrelated. They are commonly also known as thrust-and-fold belts, or simply thrust-fold belts.

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rdf:type	television show
rdfs:label	Toles eta zamalkadura gerriko (eu) Ceinture de plissement-chevauchement (fr) Fold and thrust belt (en) 褶皺與逆衝斷層帶 (zh)
rdfs:comment	A fold and thrust belt (FTB) is a series of mountainous foothills adjacent to an orogenic belt, which forms due to contractional tectonics. Fold and thrust belts commonly form in the forelands adjacent to major orogens as deformation propagates outwards. Fold and thrust belts usually comprise both folds and thrust faults, commonly interrelated. They are commonly also known as thrust-and-fold belts, or simply thrust-fold belts. (en) Toles eta zamalkadura gerrikoa tolestuak eta zamalkatuak diren eta metamorfismorik jasan ez duten arroka sedimentarioen egitura bat da. Luzera eta lodiera aldakorreko lurraldeak dira; lodiera, orokorrean, urrundu ahala txikitu egiten da. (eu) Une ceinture de plissement et de chevauchement (traduction littérale de l'anglais fold-and-thrust belt) est une série de contreforts montagneux, adjacents à une ceinture orogénique et se formant dans les domaines soumis à une (en). Les ceintures de plissement-chevauchement se forment dans les avant-pays des chaînes de montagnes. Au niveau des zones de collisions, la déformation se propage vers l'extérieur de la chaîne de montagnes en générant des zones de plis et des chevauchements, généralement interdépendants. (fr) 褶皺與逆衝斷層帶（英語：fold and thrust belt）（FTB）是坐落在造山帶前緣的一系列山地丘陵，主要是由造山帶相鄰的[前陸盆地]]構成。盆地地層因受受縮構造力影響，被變形成一系列相聯的褶皺和逆衝斷層。 (zh)
foaf:depiction
dcterms:subject	Orogeny Geological processes
Wikipage page ID	17463956 (xsd:integer)
Wikipage revision ID	1078744833 (xsd:integer)
Link from a Wikipage to another Wikipage	Canadian Rockies Carboniferous Precambrian Quaternary Rocky Mountains Devonian Richardson Mountains Upper Cretaceous Orogeny Thin-skinned deformation Cretaceous Geology of Chile Chugach Mountains Cisuralian Eocene Miocene Cordillera Oriental (Bolivia) Lachlan Fold Belt Orogenic belt Aravalli Range Mackenzie Mountains Caledonian orogeny California Coast Ranges Sierra Madre Occidental Sierra Madre Oriental Yukon Marañón fold and thrust belt Brooks Range Cenozoic Alaska Range Alps Anadyr Highlands Geological processes Foreland basin Paleocene Paleozoic Cape Fold Belt Fold (geology) Greenland Birds of the Himalayas Tectonics Maria Fold and Thrust Belt Arctic Cordillera Atlas Mountains Jurassic Late Cretaceous Tertiary Thrust fault Innuitian Mountains Kuskokwim Mountains Mesozoic Ogilvie Mountains Oligocene Ordovician Carpathians Middle Eocene Zagros fold and thrust belt Sevier Orogeny Thick-skinned deformation Transpressional Appalachians Middle Paleozoic Ouachitas dbr:Chihuahua_Belt dbr:Malargüe_fold_and_thrust_belt dbr:Oregon_Accretionary_Prism dbr:Selwyn_Fold_Belt dbr:Wyoming-Utah_Thrustbelt
Link from a Wikipage to an external page	http://www.aapg.org/science/discipline/structure/fold-and-thrust-belts%234068426-new-publications
sameAs	Fold and thrust belt Fold and thrust belt Fold and thrust belt Fold and thrust belt Fold and thrust belt Fold and thrust belt
dbp:wikiPageUsesTemplate	dbt:Tectonics-stub dbt:Reflist dbt:Structural_geology
thumbnail	wiki-commons:Special:FilePath/Fold_and_Thrust_belts_modelled_in_sandbox.png?width=300
has abstract	A fold and thrust belt (FTB) is a series of mountainous foothills adjacent to an orogenic belt, which forms due to contractional tectonics. Fold and thrust belts commonly form in the forelands adjacent to major orogens as deformation propagates outwards. Fold and thrust belts usually comprise both folds and thrust faults, commonly interrelated. They are commonly also known as thrust-and-fold belts, or simply thrust-fold belts. (en) Toles eta zamalkadura gerrikoa tolestuak eta zamalkatuak diren eta metamorfismorik jasan ez duten arroka sedimentarioen egitura bat da. Luzera eta lodiera aldakorreko lurraldeak dira; lodiera, orokorrean, urrundu ahala txikitu egiten da. (eu)

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