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http://dbpedia.org/ontology/abstract L'Old Red Sandstone (Antiga Pedra Sorrenca … L'Old Red Sandstone (Antiga Pedra Sorrenca Vermella) és una unitat de la litoestratigrafia a Gran Bretanya (una seqüència d'estrats de roques) que té l'estatus de supergrup geològic que ocupa uns 700 km de longitud i que és de considerable importància en els inicis de la paleontologia. Per conveniència aquest terme s'abreuja com ORS. Aquest terme va ser encunyat per distingir-lo del més recent el qual també es presenta a Gran Bretanya.el qual també es presenta a Gran Bretanya. , Old Red Sandstone är en faciesbildning av … Old Red Sandstone är en faciesbildning av devonsystemet som består av grova, röda sandstenar, konglomerat och skiffrar, innehållande en fauna av pansarhajar och stora kräftdjur, merostomata, skapade för ungefär 360-400 miljoner år sedan. Floran består av kärlkryptogamer och i nedre delen av Old Red Sandstone har man påträffat växter tillhöriga släktet Psilotophyta. Avlagringarna är bildade i floder och sjöar då grus, sand, sten och lera från den nybildade bergskedjan Kaledonierna erroderade. Avlagringarna kring Kaledonierna kom att bilda den så kallade Old Red-kontinenten, även kallad . Avlagringarna förekommer i stora delar av Nordamerika, på Brittiska öarna, i Nordsjöbäckenet, Spetsbergen, Grönland och i Norge.ckenet, Spetsbergen, Grönland och i Norge. , L'Old Red Sandstone (in inglese: arenaria … L'Old Red Sandstone (in inglese: arenaria rossa antica o vecchia) è un'unità litostratigrafica presente nella sequenza stratigrafica paleozoica dell'Inghilterra, a cui gli stratigrafi assegnano lo status di supergruppo e che riveste anche una notevole importanza per gli studi paleontologici. Il nome viene normalmente abbreviato in ORS nella letteratura specializzata. La terminologia è stata coniata per distinguere questa sequenza dalla più recente New Red Sandstone, anch'essa piuttosto diffusa nel territorio inglese. piuttosto diffusa nel territorio inglese. , Old Red Sandstone (en español, literalment … Old Red Sandstone (en español, literalmente, arenisca roja antigua, también traducida como arenisca roja vieja) es una unidad litoestratigráfica (una secuencia de estratos de roca) británica la cual de acuerdo con los estratígrafos tiene estatus de supergrupo​ y la que es de una considerable importancia para los comienzos de la Paleontología. Para mayor comodidad se abrevia a menudo en la literatura sobre el tema como ORS, por sus siglas inglesas. El término fue acuñado para distinguir la secuencia de la más joven , que también está muy extendida en toda Gran Bretaña.n está muy extendida en toda Gran Bretaña. , 旧赤色砂岩（きゅうせきしょくさがん、旧赤砂岩層、英: Old Red Sandstone）はイギリスのシェトランドからウェールズにかけて広く分布するデボン紀の地層名でペルム紀の新赤色砂岩と区別される。厳密な年代は後期シルル紀から初期石炭紀まで含む。 砂岩を主とし、礫岩、泥岩、シルト岩、薄い石灰岩が見られる。で砂丘、湖沼、河川での堆積による。赤色は酸化鉄を含むためだが、灰色、緑色、紫色を示すこともある。カレドニア造山運動によりできた旧赤色砂岩大陸が浸食された堆積物と考えられる。 , De Old Red Sandstone (Engels voor oude rod … De Old Red Sandstone (Engels voor oude rode zandsteen) is zijn kenmerkende gesteentelagen uit het Devoon in Wales, Schotland, gebieden in Engeland die daaraan grenzen, en in Omagh in Noord-Ierland. De naam wordt ook gebruikt voor gesteentelagen in het noordwesten van Europa en oosten van Noord-Amerika die een vergelijkbaar uiterlijk, ouderdom, en ontstaanswijze hebben. De Old Red Sandstone bestaat voornamelijk uit mariene bruine en rode zandsteen uit het Devoon. Het was een van de eerste sedimentaire gesteentes die geologen en paleontologen nauwkeurig bestudeerden, aan het begin van de 19e eeuw. De Old Red Sandstone is afgezet van 408 tot 370 Ma. Het zand was het product van erosie van Silurische gesteenten, opgeheven door de zich in dat tijdperk voltrekkende Caledonische orogenese. Omdat de Caledoniden een lange gebergteketen vormden, zijn langs de Noord-Amerikaanse oostkust en de Europese westkust veel rode siliclastische gesteentes uit deze tijd te vinden. Het paleocontinent dat tijdens de Caledonische orogenese gevormd werd uit Baltica en Laurentia wordt daarom wel het Old Red Sandstone Continent genoemd. De Old Red Sandstone kan extreem dik zijn (11 km op sommige plekken) en bestaat grotendeels uit rivierdelta-afzettingen. Er wordt een onderverdeling gemaakt in een onder-, midden- en boven-gedeelte. De Old Red Sandstone bevat veel mariene fossielen, waaronder agnatha- en vissen en uitgestorven soorten planten. De naam Old Red Sandstone werd ingevoerd door William Daniel Conybeare en William Phillips in 1822, ter onderscheid met de uit het Perm en Trias. In de eerste helft van de 19e eeuw werd de Old Red Sandstone bestudeerd door geologen en paleontologen als , Henry de la Beche, Roderick Murchison en Adam Sedgwick. Sedgwick plaatste de rode lagen in het Devoon, waarvan hij de naam zelf invoerde. De Old Red Sandstone wordt op plaatsen waar hij dagzoomt gebruikt als bouwmateriaal. Voorbeelden zijn te vinden in de omgeving van Stirling, Perth, Caithness en .geving van Stirling, Perth, Caithness en . , Les vieux grès rouges (VGR, Old Red Sandst … Les vieux grès rouges (VGR, Old Red Sandstone) forment une unité lithostratigraphique du Royaume-Uni ayant le statut de supergroupe. Elle date principalement du Dévonien. Elle est nommée ainsi pour la distinguer de la formation géologique plus récente des nouveaux grès rouges.que plus récente des nouveaux grès rouges. , The Old Red Sandstone is an assemblage of … The Old Red Sandstone is an assemblage of rocks in the North Atlantic region largely of Devonian age. It extends in the east across Great Britain, Ireland and Norway, and in the west along the northeastern seaboard of North America. It also extends northwards into Greenland and Svalbard. These areas were a part of the ancient continent of Euramerica/Laurussia. In Britain it is a lithostratigraphic unit (a sequence of rock strata) to which stratigraphers accord supergroup status and which is of considerable importance to early paleontology. For convenience the short version of the term, ORS is often used in literature on the subject. The term was coined to distinguish the sequence from the younger New Red Sandstone which also occurs widely throughout Britain.ich also occurs widely throughout Britain. , Древний красный песчаник (англ. Old Red Sa … Древний красный песчаник (англ. Old Red Sandstone, ORS) — надгруппа (стратиграфическое подразделение) девонского периода, распространённая в основном на Британских островах. Состоит из континентальных и лагунных отложений в виде слюдистых красных и серых песчаников и сланцев, в которых наблюдаются остатки панцирных, двоякодышащих (Dipterus) и кистепёрых (Holoptychius) рыб, ракоскорпионов (Eurypterus) и двустворчатых. Образование древнего красного песчаника стало возможным благодаря разрушению гор, образовавшихся в ходе каледонского горообразования.шихся в ходе каледонского горообразования. , Der Old-Red-Sandstein (engl.: Old Red Sand … Der Old-Red-Sandstein (engl.: Old Red Sandstone), kurz auch Old Red oder ORS, ist eine Gesteinsformation von beträchtlicher Bedeutung für die Paläontologie und die historische Geologie. Von diesen in England und Schottland weit verbreiteten Gesteinen leiten sich die Bezeichnungen Old-Red-Fazies und Old-Red-Kontinent ab, die in der regionalen Geologie Europas eine weit über Großbritannien hinausreichende Bedeutung besitzen. Er stammt überwiegend aus dem Devon.tzen. Er stammt überwiegend aus dem Devon. , Дре́вній черво́ний піскови́к (англ. Old Re … Дре́вній черво́ний піскови́к (англ. Old Red Sandstone, рос. древний красный песчаник, нім. Altrotsandstein m) — потужна, — понад 3 000 м, — товща континентальних, переважно червоноколірних порід. Складена головним чином пісковиками, конґломератами та сланцями. Локалізована у Шотландії та Ірландії. Охоплює весь девон, верхній силур.ландії. Охоплює весь девон, верхній силур. , 老红砂岩（Old Red Sandstone）主要指分布于欧洲西北部的泥盆纪陆相沉积物。在陆地上，苏格兰东北部沿海区域，奥克尼群岛（Orkney Island），设得兰群岛（Shetland Island），米德兰山谷（Midland Valley），英格兰西南部，爱尔兰以及斯堪的纳维亚半岛西岸均有分布；在北海区域，老红砂岩主要分布于北海中部和北部，而北海南部迄今为止没有关于钻遇该地层的报告。
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http://dbpedia.org/property/age Late Silurian-earliest Carboniferous
http://dbpedia.org/property/caption Folded Old Red Sandstone rock formation at St Annes Head in Pembrokeshire, Wales
http://dbpedia.org/property/country Canada, Greenland, Ireland, Norway, United Kingdom
http://dbpedia.org/property/name Old Red Sandstone
http://dbpedia.org/property/otherlithology http://dbpedia.org/resource/Siltstone + , http://dbpedia.org/resource/Mudstone + , http://dbpedia.org/resource/Limestone + , http://dbpedia.org/resource/Shale + , http://dbpedia.org/resource/Conglomerate_%28geology%29 +
http://dbpedia.org/property/period Devonian
http://dbpedia.org/property/prilithology http://dbpedia.org/resource/Sandstone +
http://dbpedia.org/property/region North Atlantic
http://dbpedia.org/property/subunits See text
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rdfs:comment 老红砂岩（Old Red Sandstone）主要指分布于欧洲西北部的泥盆纪陆相沉积物。在陆地上，苏格兰东北部沿海区域，奥克尼群岛（Orkney Island），设得兰群岛（Shetland Island），米德兰山谷（Midland Valley），英格兰西南部，爱尔兰以及斯堪的纳维亚半岛西岸均有分布；在北海区域，老红砂岩主要分布于北海中部和北部，而北海南部迄今为止没有关于钻遇该地层的报告。 , Old Red Sandstone är en faciesbildning av … Old Red Sandstone är en faciesbildning av devonsystemet som består av grova, röda sandstenar, konglomerat och skiffrar, innehållande en fauna av pansarhajar och stora kräftdjur, merostomata, skapade för ungefär 360-400 miljoner år sedan. Floran består av kärlkryptogamer och i nedre delen av Old Red Sandstone har man påträffat växter tillhöriga släktet Psilotophyta. Avlagringarna är bildade i floder och sjöar då grus, sand, sten och lera från den nybildade bergskedjan Kaledonierna erroderade. Avlagringarna kring Kaledonierna kom att bilda den så kallade Old Red-kontinenten, även kallad .kallade Old Red-kontinenten, även kallad . , Old Red Sandstone (en español, literalment … Old Red Sandstone (en español, literalmente, arenisca roja antigua, también traducida como arenisca roja vieja) es una unidad litoestratigráfica (una secuencia de estratos de roca) británica la cual de acuerdo con los estratígrafos tiene estatus de supergrupo​ y la que es de una considerable importancia para los comienzos de la Paleontología. Para mayor comodidad se abrevia a menudo en la literatura sobre el tema como ORS, por sus siglas inglesas. El término fue acuñado para distinguir la secuencia de la más joven , que también está muy extendida en toda Gran Bretaña.n está muy extendida en toda Gran Bretaña. , L'Old Red Sandstone (Antiga Pedra Sorrenca … L'Old Red Sandstone (Antiga Pedra Sorrenca Vermella) és una unitat de la litoestratigrafia a Gran Bretanya (una seqüència d'estrats de roques) que té l'estatus de supergrup geològic que ocupa uns 700 km de longitud i que és de considerable importància en els inicis de la paleontologia. Per conveniència aquest terme s'abreuja com ORS. Aquest terme va ser encunyat per distingir-lo del més recent el qual també es presenta a Gran Bretanya.el qual també es presenta a Gran Bretanya. , De Old Red Sandstone (Engels voor oude rod … De Old Red Sandstone (Engels voor oude rode zandsteen) is zijn kenmerkende gesteentelagen uit het Devoon in Wales, Schotland, gebieden in Engeland die daaraan grenzen, en in Omagh in Noord-Ierland. De naam wordt ook gebruikt voor gesteentelagen in het noordwesten van Europa en oosten van Noord-Amerika die een vergelijkbaar uiterlijk, ouderdom, en ontstaanswijze hebben. De Old Red Sandstone bestaat voornamelijk uit mariene bruine en rode zandsteen uit het Devoon. Het was een van de eerste sedimentaire gesteentes die geologen en paleontologen nauwkeurig bestudeerden, aan het begin van de 19e eeuw.studeerden, aan het begin van de 19e eeuw. , 旧赤色砂岩（きゅうせきしょくさがん、旧赤砂岩層、英: Old Red Sandstone）はイギリスのシェトランドからウェールズにかけて広く分布するデボン紀の地層名でペルム紀の新赤色砂岩と区別される。厳密な年代は後期シルル紀から初期石炭紀まで含む。 砂岩を主とし、礫岩、泥岩、シルト岩、薄い石灰岩が見られる。で砂丘、湖沼、河川での堆積による。赤色は酸化鉄を含むためだが、灰色、緑色、紫色を示すこともある。カレドニア造山運動によりできた旧赤色砂岩大陸が浸食された堆積物と考えられる。 , Древний красный песчаник (англ. Old Red Sa … Древний красный песчаник (англ. Old Red Sandstone, ORS) — надгруппа (стратиграфическое подразделение) девонского периода, распространённая в основном на Британских островах. Состоит из континентальных и лагунных отложений в виде слюдистых красных и серых песчаников и сланцев, в которых наблюдаются остатки панцирных, двоякодышащих (Dipterus) и кистепёрых (Holoptychius) рыб, ракоскорпионов (Eurypterus) и двустворчатых. Образование древнего красного песчаника стало возможным благодаря разрушению гор, образовавшихся в ходе каледонского горообразования.шихся в ходе каледонского горообразования. , The Old Red Sandstone is an assemblage of … The Old Red Sandstone is an assemblage of rocks in the North Atlantic region largely of Devonian age. It extends in the east across Great Britain, Ireland and Norway, and in the west along the northeastern seaboard of North America. It also extends northwards into Greenland and Svalbard. These areas were a part of the ancient continent of Euramerica/Laurussia. In Britain it is a lithostratigraphic unit (a sequence of rock strata) to which stratigraphers accord supergroup status and which is of considerable importance to early paleontology. For convenience the short version of the term, ORS is often used in literature on the subject. The term was coined to distinguish the sequence from the younger New Red Sandstone which also occurs widely throughout Britain.ich also occurs widely throughout Britain. , L'Old Red Sandstone (in inglese: arenaria … L'Old Red Sandstone (in inglese: arenaria rossa antica o vecchia) è un'unità litostratigrafica presente nella sequenza stratigrafica paleozoica dell'Inghilterra, a cui gli stratigrafi assegnano lo status di supergruppo e che riveste anche una notevole importanza per gli studi paleontologici. Il nome viene normalmente abbreviato in ORS nella letteratura specializzata. La terminologia è stata coniata per distinguere questa sequenza dalla più recente New Red Sandstone, anch'essa piuttosto diffusa nel territorio inglese. piuttosto diffusa nel territorio inglese. , Les vieux grès rouges (VGR, Old Red Sandst … Les vieux grès rouges (VGR, Old Red Sandstone) forment une unité lithostratigraphique du Royaume-Uni ayant le statut de supergroupe. Elle date principalement du Dévonien. Elle est nommée ainsi pour la distinguer de la formation géologique plus récente des nouveaux grès rouges.que plus récente des nouveaux grès rouges. , Der Old-Red-Sandstein (engl.: Old Red Sand … Der Old-Red-Sandstein (engl.: Old Red Sandstone), kurz auch Old Red oder ORS, ist eine Gesteinsformation von beträchtlicher Bedeutung für die Paläontologie und die historische Geologie. Von diesen in England und Schottland weit verbreiteten Gesteinen leiten sich die Bezeichnungen Old-Red-Fazies und Old-Red-Kontinent ab, die in der regionalen Geologie Europas eine weit über Großbritannien hinausreichende Bedeutung besitzen. Er stammt überwiegend aus dem Devon.tzen. Er stammt überwiegend aus dem Devon. , Дре́вній черво́ний піскови́к (англ. Old Re … Дре́вній черво́ний піскови́к (англ. Old Red Sandstone, рос. древний красный песчаник, нім. Altrotsandstein m) — потужна, — понад 3 000 м, — товща континентальних, переважно червоноколірних порід. Складена головним чином пісковиками, конґломератами та сланцями. Локалізована у Шотландії та Ірландії. Охоплює весь девон, верхній силур.ландії. Охоплює весь девон, верхній силур.
rdfs:label 旧赤色砂岩 , Древний красный песчаник , Old Red Sandstone , Vieux grès rouges , Древній червоний пісковик , Old-Red-Sandstein , 老红砂岩
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