| dbo: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) 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) |
| dbo:thumbnail |
wiki-commons:Special:FilePath/Fold_and_Thrust_belts_modelled_in_sandbox.png?width=300 |
| dbo:wikiPageExternalLink |
http://www.aapg.org/science/discipline/structure/fold-and-thrust-belts%234068426-new-publications |
| dbo:wikiPageID |
17463956 (xsd:integer) |
| dbo:wikiPageLength |
6851 (xsd:nonNegativeInteger) |
| dbo:wikiPageRevisionID |
1078744833 (xsd:integer) |
| dbo:wikiPageWikiLink |
dbr:Canadian_Rockies dbr:Carboniferous dbr:Precambrian dbr:Quaternary dbr:Rocky_Mountains dbr:Devonian dbr:Richardson_Mountains dbr:Upper_Cretaceous dbc:Orogeny dbr:Thin-skinned_deformation dbr:Cretaceous dbr:Geology_of_Chile dbr:Chugach_Mountains dbr:Cisuralian dbr:Eocene dbr:Miocene dbr:Cordillera_Oriental_(Bolivia) dbr:Lachlan_Fold_Belt dbr:Orogenic_belt dbr:Aravalli_Range dbr:Mackenzie_Mountains dbr:Caledonian_orogeny dbr:California_Coast_Ranges dbr:Sierra_Madre_Occidental dbr:Sierra_Madre_Oriental dbr:Yukon dbr:Marañón_fold_and_thrust_belt dbr:Brooks_Range dbr:Cenozoic dbr:Alaska_Range dbr:Alps dbr:Anadyr_Highlands dbc:Geological_processes dbr:Foreland_basin dbr:Paleocene dbr:Paleozoic dbr:Cape_Fold_Belt dbr:Fold_(geology) dbr:Greenland dbr:Himalayas dbr:Tectonics dbr:Maria_Fold_and_Thrust_Belt dbr:Arctic_Cordillera dbr:Atlas_Mountains dbr:Jurassic dbr:Late_Cretaceous dbr:Tertiary dbr:Thrust_fault dbr:Innuitian_Mountains dbr:Kuskokwim_Mountains dbr:Mesozoic dbr:Ogilvie_Mountains dbr:Oligocene dbr:Ordovician dbr:Carpathians dbr:Middle_Eocene dbr:Zagros_fold_and_thrust_belt dbr:Sevier_Orogeny dbr:Thick-skinned_deformation dbr:Transpressional dbr:Appalachians dbr:Middle_Paleozoic dbr:Ouachitas dbr:Chihuahua_Belt dbr:File:Fold_and_Thrust_belts_modelled_in_sandbox.png dbr:File:Profile_through_the_Pyrenees_EN.svg dbr:File:SunRiver.JPG dbr:Malargüe_fold_and_thrust_belt dbr:Oregon_Accretionary_Prism dbr:Selwyn_Fold_Belt dbr:Wyoming-Utah_Thrustbelt |
| dbp:wikiPageUsesTemplate |
dbt:Tectonics-stub dbt:Reflist dbt:Structural_geology |
| dct:subject |
dbc:Orogeny dbc:Geological_processes |
| gold:hypernym |
dbr:Series |
| rdf:type |
dbo:TelevisionShow |
| 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) |
| 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) |
| owl:sameAs |
freebase:Fold and thrust belt wikidata:Fold and thrust belt dbpedia-eu:Fold and thrust belt dbpedia-fr:Fold and thrust belt dbpedia-zh:Fold and thrust belt https://global.dbpedia.org/id/4jgtj |
| prov:wasDerivedFrom |
wikipedia-en:Fold_and_thrust_belt?oldid=1078744833&ns=0 |
| foaf:depiction |
wiki-commons:Special:FilePath/Fold_and_Thrust_belts_modelled_in_sandbox.png wiki-commons:Special:FilePath/Profile_through_the_Pyrenees_EN.svg wiki-commons:Special:FilePath/SunRiver.jpg |
| foaf:isPrimaryTopicOf |
wikipedia-en:Fold_and_thrust_belt |
| is dbo:type of |
dbr:Zagros_Mountains dbr:Guadalupe_Hill |
| is dbo:wikiPageRedirects of |
dbr:Fold-Thrust_Belt dbr:Fold_Thrust_Belt dbr:Foldbelt |
| is dbo:wikiPageWikiLink of |
dbr:California_River dbr:Campanian_Ignimbrite_eruption dbr:Canton_10 dbr:Carpathian_Mountains dbr:Princess_Elizabeth_Alps dbr:Rub'_al_Khali_Basin dbr:El_Tigre_Fault dbr:2008_Ziarat_earthquakes dbr:2012_Northern_Italy_earthquakes dbr:Brian_K._Horton dbr:Archean_subduction dbr:Pectodens dbr:Décollement dbr:East_Greenland_Orogen dbr:Lewis_Overthrust dbr:Numerical_modeling_(geology) dbr:Thin-skinned_deformation dbr:1348_Friuli_earthquake dbr:1349_Apennine_earthquakes dbr:1456_Central_Italy_earthquakes dbr:1461_L'Aquila_earthquake dbr:1858_Prome_earthquake dbr:1902_Turkestan_earthquake dbr:1906_Manasi_earthquake dbr:1930_Senigallia_earthquake dbr:1570_Ferrara_earthquake dbr:1706_Abruzzo_earthquake dbr:1762_Arakan_earthquake dbr:1805_Molise_earthquake dbr:1825_Blida_earthquake dbr:1977_Bob–Tangol_earthquake dbr:1979_Ghaenat_earthquakes dbr:1990–91_Alto_Mayo_earthquakes dbr:1991_Racha_earthquake dbr:1992_Kohat_earthquake dbr:Croatia_proper dbr:Croatian_Littoral dbr:Andean_orogeny dbr:Sabana_Formation dbr:Geology_of_British_Columbia dbr:Geology_of_Croatia dbr:Geology_of_East_Sussex dbr:Geology_of_Gabon dbr:Geology_of_North_America dbr:Geology_of_Paraguay dbr:Geology_of_Russia dbr:Geology_of_Sicily dbr:Geology_of_Tunisia dbr:Geology_of_the_Baltic_Sea dbr:Geology_of_the_Western_Carpathians dbr:Topography_of_Croatia dbr:Cima_di_e_Follicie dbr:Geography_of_Croatia dbr:Geography_of_Trinidad_and_Tobago dbr:Geology_of_Bolivia dbr:Geology_of_the_Alps dbr:Monte_Renoso dbr:Monte_Stello dbr:Congo_Craton dbr:Cordillera_Oriental_(Bolivia) dbr:1946_Ancash_earthquake dbr:1949_Karlıova_earthquake dbr:1957_Sangchal_earthquake dbr:1968_Belice_earthquake dbr:1969_Sulawesi_earthquake dbr:2018_Papua_New_Guinea_earthquake dbr:2020_Kashgar_earthquake dbr:2021_Balochistan_earthquake dbr:Andes dbr:Apennine_Mountains dbr:Lufilian_Arc dbr:Bohemian_Massif dbr:Snake_River_Canyon_(Wyoming) dbr:Soatá_Formation dbr:Sulaiman_Mountains dbr:Zagros_Mountains dbr:Lesser_Himalayan_Strata dbr:Nastapoka_arc dbr:Mauritanide_Belt dbr:2002_Baltistan_earthquakes dbr:Tierra_del_Fuego dbr:Trinidad dbr:Trinidad_and_Tobago dbr:Sabkha dbr:2021_Mansfield_earthquake dbr:2021_West_Sulawesi_earthquake dbr:Allamoore_Formation dbr:Eastern_Hills_(Bogotá) dbr:Foreland_basin dbr:Papua_New_Guinea dbr:Cape_Fold_Belt dbr:Fold_mountains dbr:Forebulge dbr:Himalayan_salt dbr:Guadalupe_Hill dbr:Hardangervidda dbr:Baikal_Rift_Zone dbr:Soledad_caldera dbr:August_2016_Central_Italy_earthquake dbr:Kibaran_orogeny dbr:Laguna_del_Maule_(volcano) dbr:Lake_Enriquillo dbr:Las_Pavas dbr:Cochabamba_Fault_Zone dbr:Pieniny_Klippen_Belt dbr:Dinocephalosaurus dbr:Phlegra_Montes dbr:Piotruś dbr:Grenville_orogeny dbr:Neuquén_Basin dbr:Carpathian_Flysch_Belt dbr:Shenandoah_National_Park dbr:Yakima_Fold_Belt dbr:Uinta_County,_Wyoming dbr:Superior_Craton dbr:Thrust_tectonics dbr:Exhumation_(geology) dbr:Yilgarn_Craton dbr:Yenisey_Fold_Belt dbr:Molasse_basin dbr:Zagros_fold_and_thrust_belt dbr:Weald_Basin dbr:Paleocontinent dbr:Section_restoration dbr:Serranía_del_Aguaragüe dbr:Pampean_flat-slab dbr:Rhenohercynian_Zone dbr:Strike-slip_tectonics dbr:Zhongwei-Tongxin_fault dbr:Tectonic_evolution_of_Patagonia dbr:Statherian dbr:Fold-Thrust_Belt dbr:Fold_Thrust_Belt dbr:Foldbelt |
| is dbp:formedBy of |
dbr:Cima_di_e_Follicie dbr:Monte_Renoso dbr:Monte_Stello |
| is dbp:geology of |
dbr:Princess_Elizabeth_Alps |
| is dbp:mountainType of |
dbr:Eastern_Hills_(Bogotá) |
| is dbp:type of |
dbr:Zagros_Mountains dbr:Guadalupe_Hill dbr:Yakima_Fold_Belt |
| is foaf:primaryTopic of |
wikipedia-en:Fold_and_thrust_belt |
