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Statements

Subject Item
dbr:Winton_Formation
rdf:type
yago:WikicatCretaceousPaleontologicalSitesOfAustralia yago:Site108651247 yago:Region108630985 yago:YagoLegalActorGeo yago:Location100027167 yago:YagoPermanentlyLocatedEntity yago:YagoGeoEntity yago:PhysicalEntity100001930 yago:GeographicalArea108574314 yago:Object100002684 geo:SpatialThing yago:Tract108673395 dbo:MilitaryUnit
rdfs:label
Winton-Formation Formació de Winton Formación Winton Winton Formation 윈턴 층 Formation de Winton
rdfs:comment
La Formació de Winton és una formació del Cretaci situada en el centre-oest de Queensland, Austràlia. El dinosaure sauròpode Austrosaurus fou trobar en la formació de Winton del Cretaci inferior. Aquesta formació és una unitat rocosa que cobreix àrees extenses del centre-oest de Queensland. Està constituïda per roques sedimentàries com el gres i l'argila. Els sediments que van formar aquestes roques deriven de restes de les planes fluvials que van omplir una conca a l'esquerra del - un mar interior que cobria extenses zones de Queensland i de l'Austràlia central almenys quatre vegades durant el Cretaci inferior. La formation de Winton est une formation géologique du début du Crétacé supérieur (Cénomanien et Turonien inférieur), située au Queensland en Australie. Elle est constituée de grès, de siltstones et d'argilites, âgés entre 103 et 93,9 millions d'années environ. La formation a livré une faune importante en vertébrés terrestres, tels les dinosaures Australovenator, Diamantinasaurus et Savannasaurus. Die Winton-Formation ist eine Formation im Great Artesian Basin in Australien. Diese Abfolge kreidezeitlicher Sedimentgesteine ist vom nördlichen bis ins westliche zentrale Queensland und weiter südlich in New South Wales und South Australia aufgeschlossen. Die Sedimentgesteine der Formation rühren größtenteils von recycelten vulkanischem Material her. So waren an der Nordostküste Queenslands in der Kreide Vulkane aktiv. 윈턴 층(Winton Formation)은 오스트레일리아의 퀸즐랜드에 위치한 지층으로, 지질연대는 백악기 전기이다. 위로는 매쿤다 층이 퇴적되어있다. La formación Winton es una formación geológica del Cretácico en el centro-oeste de Queensland, Australia. Tiene una edad entre el albiense tardío y el turoniense,​ por lo que se extiende a ambos lados del límite entre Turoniano y Cenomaniano. The Winton Formation is a Cretaceous geological formation in central-western Queensland, Australia. It is late Albian to early Turonian in age. The formation blankets large areas of central-western Queensland. It consists of sedimentary rocks such as sandstone, siltstone and claystone. The sediments that make up these rocks represent the remnants of the river plains that filled the basin left by the - an inland sea that covered large parts of Queensland and central Australia at least four times during the Early Cretaceous. Great meandering rivers, forest pools and swamps, creeks, lakes and coastal estuaries all left behind different types of sediment.
dbp:name
Winton Formation
geo:lat
-22.29999923706055
geo:long
143.1000061035156
foaf:depiction
n8:Tempskya_sp._-_MUSE.jpg n8:Diamantinasaurus_AODF_836.jpg n8:Banjo_Australovenator.jpg n8:Isisfordia.jpg n8:Australotitan_holotype.png n8:Savannasaurus_skeleton.jpg n8:Winton_formation.svg n8:Wintonotitan_arm.png n8:Ferrodraco.jpg
dcterms:subject
dbc:Early_Cretaceous_Australia dbc:Coal_in_Australia dbc:Albian_Stage dbc:Cenomanian_Stage dbc:Fluvial_deposits dbc:Cretaceous_System_of_Australia dbc:Siltstone_formations dbc:Shale_formations dbc:Geologic_formations_of_Australia dbc:Turonian_Stage dbc:Ichnofossiliferous_formations dbc:Fossiliferous_stratigraphic_units_of_Oceania dbc:South_West_Queensland dbc:Paleontology_in_Queensland dbc:Sandstone_formations dbc:Central_West_Queensland
dbo:wikiPageID
14996464
dbo:wikiPageRevisionID
1105575574
dbo:wikiPageWikiLink
dbc:Early_Cretaceous_Australia dbr:Mississippi_River n14:Australotitan_holotype.png n14:Tempskya_sp._-_MUSE.jpg dbr:Wintonotitan dbr:Coal dbr:Anhangueria dbr:Tempskya n14:Banjo_Australovenator.jpg dbc:Coal_in_Australia dbr:Rolling_Downs_Group dbr:Unconformity dbr:Fossil dbr:Amazon_River dbr:Ginkgoales dbr:Elasmaria dbc:Cenomanian_Stage dbc:Albian_Stage dbr:Albian dbr:Confractosuchus dbc:Fluvial_deposits dbr:Theropod n14:Isisfordia.jpg dbr:Australotitan dbr:Australovenator dbc:Cretaceous_System_of_Australia dbc:Siltstone_formations dbr:Neornithischia dbr:Crocodyliformes dbr:Cycad dbr:Eromanga_Sea dbr:Savannasaurus n14:Ferrodraco.jpg dbr:Geological_formation dbr:Actinopterygii dbr:Winton,_Queensland dbr:Liverwort dbr:Oodndatta_Formation dbc:Shale_formations dbr:Dinosaur dbr:Ornithopoda dbr:Araucaria dbr:Osmundaceae dbr:Cupressaceae dbr:Sandstone dbr:Claystone dbr:Araucariaceae dbr:Metaceratodus_wollastoni n14:Savannasaurus_skeleton.jpg dbr:Ankylosauria dbc:Geologic_formations_of_Australia dbr:Equisetites dbr:Lygodium dbr:Equisetum dbr:Microphyllopteris dbc:Turonian_Stage dbr:Sauropoda dbr:Dicotyledons dbr:Quaternary dbr:Sedimentary_rock dbr:Australia dbr:Laurales dbr:Siltstone dbr:Cretaceous dbr:Ginkgo dbr:Monocotyledon dbr:Lark_Quarry dbr:Lark_Quarry_Conservation_Park dbr:South_Polar_region_of_the_Cretaceous dbr:Titanosauria dbr:Cladocyclus dbr:Pentoxylales dbc:Ichnofossiliferous_formations n14:Wintonotitan_arm.png n14:Diamantinasaurus_AODF_836.jpg dbr:Megaraptora dbr:Gleicheniaceae dbr:Turonian dbc:Fossiliferous_stratigraphic_units_of_Oceania dbr:Pterostoma_(plant) dbr:Sediment dbr:Agathis dbc:South_West_Queensland dbr:Dipnoi dbr:Wollemia dbc:Paleontology_in_Queensland dbr:Ptilophyllum dbr:Ichnite dbr:Diamantinasauria dbr:Diamantinasaurus dbr:Metaceratodus_bonei dbc:Central_West_Queensland dbr:Metaceratodus_ellioti dbr:Angiospermae dbr:Austrosequoia dbr:Taeniopteris dbr:Titanosauriformes dbr:Formation_(geology) dbr:Lovellea dbr:Ferrodraco dbr:Lake_Eyre_Basin dbc:Sandstone_formations dbr:Cheirolepidiaceae dbr:Eromanga_Basin dbr:Queensland dbr:Phyllopteroides dbr:Conglomerate_(geology) dbr:Marchantites dbr:Mackunda_Formation dbr:List_of_dinosaur-bearing_rock_formations dbr:Bennettitales dbr:Emwadea dbr:Otozamites dbr:Tree_fern dbr:Isisfordia
owl:sameAs
dbpedia-fr:Formation_de_Winton dbpedia-fi:Wintonin_muodostuma dbpedia-ca:Formació_de_Winton dbpedia-de:Winton-Formation dbpedia-ko:윈턴_층 wikidata:Q2543891 freebase:m.03h44tp dbpedia-es:Formación_Winton yago-res:Winton_Formation n28:2PnVJ
dbp:underlies
Unconformity with Quaternary Lake Eyre Basin sediments
dbp:unitof
dbr:Rolling_Downs_Group
dbp:yearTs
1955
dbp:wikiPageUsesTemplate
dbt:Flag dbt:Convert dbt:Reflist dbt:Coord dbt:Infobox_rockunit dbt:Use_Australian_English dbt:Use_dmy_dates dbt:Fossilrange
dbo:thumbnail
n8:Winton_formation.svg?width=300
dbp:age
dbr:Turonian dbr:Albian ~
dbp:mapCaption
Formation distribution within Australia
dbp:period
Turonian
dbp:thickness
in the centre < at the margin
dbp:type
dbr:Geological_formation
georss:point
-22.3 143.1
dbo:abstract
La Formació de Winton és una formació del Cretaci situada en el centre-oest de Queensland, Austràlia. El dinosaure sauròpode Austrosaurus fou trobar en la formació de Winton del Cretaci inferior. Aquesta formació és una unitat rocosa que cobreix àrees extenses del centre-oest de Queensland. Està constituïda per roques sedimentàries com el gres i l'argila. Els sediments que van formar aquestes roques deriven de restes de les planes fluvials que van omplir una conca a l'esquerra del - un mar interior que cobria extenses zones de Queensland i de l'Austràlia central almenys quatre vegades durant el Cretaci inferior. En algunes àrees la formació Winton fa més de 400 metres de gruix. The Winton Formation is a Cretaceous geological formation in central-western Queensland, Australia. It is late Albian to early Turonian in age. The formation blankets large areas of central-western Queensland. It consists of sedimentary rocks such as sandstone, siltstone and claystone. The sediments that make up these rocks represent the remnants of the river plains that filled the basin left by the - an inland sea that covered large parts of Queensland and central Australia at least four times during the Early Cretaceous. Great meandering rivers, forest pools and swamps, creeks, lakes and coastal estuaries all left behind different types of sediment. In some areas, the Winton Formation is over 400 metres thick. To bring with them such a huge amount of sediment, the rivers that flowed across these plains must have been comparable in size to the present-day Amazon or Mississippi rivers. As more and more sediment was brought in, the margins of the inland sea slowly contracted. By around 95 million years ago, the deposition was complete and the inland sea would never be seen again. By virtue of its age and the environmental conditions under which the rocks it consists of were deposited, the Winton Formation represents one of the richest sources of dinosaur fossils anywhere in Australia. 윈턴 층(Winton Formation)은 오스트레일리아의 퀸즐랜드에 위치한 지층으로, 지질연대는 백악기 전기이다. 위로는 매쿤다 층이 퇴적되어있다. La formation de Winton est une formation géologique du début du Crétacé supérieur (Cénomanien et Turonien inférieur), située au Queensland en Australie. Elle est constituée de grès, de siltstones et d'argilites, âgés entre 103 et 93,9 millions d'années environ. La formation a livré une faune importante en vertébrés terrestres, tels les dinosaures Australovenator, Diamantinasaurus et Savannasaurus. La formación Winton es una formación geológica del Cretácico en el centro-oeste de Queensland, Australia. Tiene una edad entre el albiense tardío y el turoniense,​ por lo que se extiende a ambos lados del límite entre Turoniano y Cenomaniano. Die Winton-Formation ist eine Formation im Great Artesian Basin in Australien. Diese Abfolge kreidezeitlicher Sedimentgesteine ist vom nördlichen bis ins westliche zentrale Queensland und weiter südlich in New South Wales und South Australia aufgeschlossen. Die Winton-Formation ist eine der größten Formationen Australiens. Am Diamantina-Nationalpark ist die Formation mit etwa 400 Metern eher geringmächtig, während die Mächtigkeit bei nahezu 1200 Meter beträgt. Durch Bohrungen wurde festgestellt, dass auch dünne Lagen von Kohle in den Schichten eingelagert sind. Die Formation ist größtenteils tief verwittert, was zur Bildung von Laterit und Silcreten führte. In den Gebieten, die starker Erosion unterlagen, befinden sich die Opalfelder im Westen von Queensland. Fossilien finden sich in Gebieten, die weniger stark erodiert sind. Die Sedimentgesteine der Formation rühren größtenteils von recycelten vulkanischem Material her. So waren an der Nordostküste Queenslands in der Kreide Vulkane aktiv. Aus der Winton-Formation stammen zahlreiche Überreste von Dinosauriern wie Sauropoden und Theropoden; Funde schließen Australovenator, Diamantinasaurus und Wintonotitan mit ein. Westlich der Stadt Eromanga wurden die Überreste von Krokodilen, Fischen, Lungenfischen, Schildkröten, Insekten und Frischwassermuscheln gefunden.
dbp:extent
dbr:Eromanga_Basin
dbp:locationTs
Bores in and around Winton
dbp:namedby
Whitehouse
dbp:namedfor
dbr:Winton,_Queensland
dbp:otherlithology
dbr:Coal dbr:Conglomerate_(geology)
dbp:overlies
dbr:Oodndatta_Formation dbr:Mackunda_Formation
dbp:prilithology
dbr:Siltstone dbr:Sandstone dbr:Claystone
gold:hypernym
dbr:Formation
prov:wasDerivedFrom
wikipedia-en:Winton_Formation?oldid=1105575574&ns=0
dbo:wikiPageLength
19061
foaf:isPrimaryTopicOf
wikipedia-en:Winton_Formation
geo:geometry
POINT(143.10000610352 -22.299999237061)