| http://dbpedia.org/ontology/abstract
|
Lanalhue Fault is a northwest-striking fau … Lanalhue Fault is a northwest-striking fault that marks the contact between two distinct units of continental basement, the Eastern and Western Series in south-central Chile, separating the Nahuelbuta Range Cordillera de Nahuelbuta to the east and the Arauco Peninsula and Basin to the west. The fault takes its name from Lanalhue Lake, which is located in part of the fault trace – the lake's elongated shape shows the NW-SE trend. The Lanalhue Fault is a major lithological boundary in the Chilean Coast Range to which Cordillera de Nahuelbuta belongs. The Nahuelbuta Range is composed by Carboniferous granitic core bounded by high-temperature metasedimentary rocks referred as the Eastern Series. The Arauco Basin contains over 3 km of Late Cretaceous to Holocene continental and marine sediments, being a major center of coal mining and hydrocarbon exploration for over a century. From Valparaíso Region to Lanalhue Fault, Carboniferous-Permian granitoids make up a large part of the bedrock of the Chilean Coast Range. These igneous rocks were once part of a proto-Andean magmatic belt. South of Lanalhue Fault, most of the Chilean Coast Range is an accretionary wedge formed since the Paleozoic along the subduction zone at South America's western coast. From a tentative correlation of the fault zone with the similarly NW-SE striking dextral Jurassic Gastre Fault System (cf. Rapela & Pankhurst, 1992) in Central Patagonia, Argentina, it was termed ‘Gastre Fault Zone’ or ‘Gastre-Purén Fault Zone’. However, in later works it is shown that this correlation is incorrect. It was speculated that the inferred Gastre Fault Zone aligned Villarrica, Quetrupillán and Lanín volcanoes, until the Mocha-Villarrica Fault Zone was discovered.ocha-Villarrica Fault Zone was discovered.
, La falla de Lanalhue es un sistema de fall … La falla de Lanalhue es un sistema de fallas geológicas que corre de noroeste a sureste. Este sistema de fallas contiene una falla principal y varias secundarias del tipo "splay". Comienza cerca del mar, sigue por la planicie litoral hasta dividirse cerca del lago Lanalhue. Luego, la falla pasa por el cerro Lanalhue mientras que la falla secundaria pasa por el lago Lanalhue, de donde fue nombrado este sistema de fallas. La falla continúa por la cordillera de Nahuelbuta de las regiones del Bío-Bío y de la Araucanía. Continúa por los cerros Ñielol-Humpil y Conun Huenu. Después continúa por la depresión intermedia hasta terminar cerca de Villarrica (una de las ciudades turísticas más importantes del sur de Chile). Además, esta falla poco conocida atraviesa grandes urbes como Temuco, la quinta ciudad más grande de Chile. Esta falla delimita por el norte casi toda la placa de Chiloé.por el norte casi toda la placa de Chiloé.
, Plus que d'une faille, il serait plus corr … Plus que d'une faille, il serait plus correct de parler d'un système de failles. Ce système de failles contient une faille principale et plusieurs failles secondaires du genre "splay". La faille du Lanalhue est la faille principale avec une orientation du nord-ouest au sud-est. Elle démarre près de la côte et elle suit par la plaine littorale. Elle se divise en deux près du . La faille principale passe à travers la colline Cerro Lanalhue en tant que la faille secondaire passe à travers le lac Lanalhue, d’où ce système de failles tient son nom. La faille principale après continue par la cordillère de Nahuelbuta des régions du Biobío et de l'Araucanie. Ensuite, elle passe à travers les collines cerro Ñielol et cerro Conun Huenu. Ensuite, cette faille continue par la Vallée centrale avant de terminer près de Villarrica, une des plus importantes villes touristiques du sud du Chili. Cette faille délimite presque tout le bloc de Chiloé par le nord.resque tout le bloc de Chiloé par le nord.
|
| http://dbpedia.org/ontology/wikiPageID
|
26659131
|
| http://dbpedia.org/ontology/wikiPageLength
|
2567
|
| http://dbpedia.org/ontology/wikiPageRevisionID
|
1006902223
|
| http://dbpedia.org/ontology/wikiPageWikiLink
|
http://dbpedia.org/resource/Quetrupill%C3%A1n +
, http://dbpedia.org/resource/Strike_and_dip +
, http://dbpedia.org/resource/Late_Cretaceous +
, http://dbpedia.org/resource/Patagonia +
, http://dbpedia.org/resource/Chilean_Coast_Range +
, http://dbpedia.org/resource/Category:Seismic_faults_of_Chile +
, http://dbpedia.org/resource/Permian +
, http://dbpedia.org/resource/Category:Geology_of_the_Chilean_Coast_Range +
, http://dbpedia.org/resource/Gastre_Fault_Zone +
, http://dbpedia.org/resource/Bedrock +
, http://dbpedia.org/resource/Granitoid +
, http://dbpedia.org/resource/Subduction_zone +
, http://dbpedia.org/resource/Mocha-Villarrica_Fault_Zone +
, http://dbpedia.org/resource/Category:Geology_of_Biob%C3%ADo_Region +
, http://dbpedia.org/resource/Valpara%C3%ADso_Region +
, http://dbpedia.org/resource/Carboniferous +
, http://dbpedia.org/resource/Holocene +
, http://dbpedia.org/resource/Metasedimentary_rock +
, http://dbpedia.org/resource/Magmatic +
, http://dbpedia.org/resource/Lan%C3%ADn +
, http://dbpedia.org/resource/Basement_%28geology%29 +
, http://dbpedia.org/resource/Accretionary_wedge +
, http://dbpedia.org/resource/Cordillera_de_Nahuelbuta +
, http://dbpedia.org/resource/Paleozoic +
, http://dbpedia.org/resource/Jurassic +
, http://dbpedia.org/resource/Igneous_rocks +
, http://dbpedia.org/resource/Lanalhue_Lake +
, http://dbpedia.org/resource/Lithology +
, http://dbpedia.org/resource/Category:Geology_of_Araucan%C3%ADa_Region +
, http://dbpedia.org/resource/Villarrica_%28volcano%29 +
|
| http://dbpedia.org/property/wikiPageUsesTemplate
|
http://dbpedia.org/resource/Template:Geology-stub +
, http://dbpedia.org/resource/Template:Reflist +
|
| http://purl.org/dc/terms/subject
|
http://dbpedia.org/resource/Category:Geology_of_Araucan%C3%ADa_Region +
, http://dbpedia.org/resource/Category:Geology_of_Biob%C3%ADo_Region +
, http://dbpedia.org/resource/Category:Geology_of_the_Chilean_Coast_Range +
, http://dbpedia.org/resource/Category:Seismic_faults_of_Chile +
|
| http://purl.org/linguistics/gold/hypernym
|
http://dbpedia.org/resource/Fault +
|
| http://www.w3.org/ns/prov#wasDerivedFrom
|
http://en.wikipedia.org/wiki/Lanalhue_Fault?oldid=1006902223&ns=0 +
|
| http://xmlns.com/foaf/0.1/isPrimaryTopicOf
|
http://en.wikipedia.org/wiki/Lanalhue_Fault +
|
| owl:sameAs |
http://rdf.freebase.com/ns/m.0bh79kt +
, http://es.dbpedia.org/resource/Falla_de_Lanalhue +
, http://www.wikidata.org/entity/Q6482880 +
, https://global.dbpedia.org/id/4qCq9 +
, http://yago-knowledge.org/resource/Lanalhue_Fault +
, http://fr.dbpedia.org/resource/Faille_du_Lanalhue +
, http://dbpedia.org/resource/Lanalhue_Fault +
|
| rdf:type |
http://dbpedia.org/class/yago/Crack109258715 +
, http://dbpedia.org/class/yago/PhysicalEntity100001930 +
, http://dbpedia.org/class/yago/AmorphousShape113867492 +
, http://dbpedia.org/class/yago/Opening109379111 +
, http://dbpedia.org/class/yago/Abstraction100002137 +
, http://dbpedia.org/class/yago/Space113910384 +
, http://dbpedia.org/class/yago/YagoLegalActorGeo +
, http://dbpedia.org/class/yago/YagoPermanentlyLocatedEntity +
, http://dbpedia.org/class/yago/Fault109278537 +
, http://dbpedia.org/class/yago/Object100002684 +
, http://dbpedia.org/class/yago/YagoGeoEntity +
, http://dbpedia.org/class/yago/Shape100027807 +
, http://dbpedia.org/ontology/WorldHeritageSite +
, http://dbpedia.org/class/yago/Attribute100024264 +
, http://dbpedia.org/class/yago/Location100027167 +
, http://dbpedia.org/class/yago/WikicatGeologicalFaultsOfChile +
|
| rdfs:comment |
Lanalhue Fault is a northwest-striking fau … Lanalhue Fault is a northwest-striking fault that marks the contact between two distinct units of continental basement, the Eastern and Western Series in south-central Chile, separating the Nahuelbuta Range Cordillera de Nahuelbuta to the east and the Arauco Peninsula and Basin to the west. The fault takes its name from Lanalhue Lake, which is located in part of the fault trace – the lake's elongated shape shows the NW-SE trend. The Lanalhue Fault is a major lithological boundary in the Chilean Coast Range to which Cordillera de Nahuelbuta belongs. The Nahuelbuta Range is composed by Carboniferous granitic core bounded by high-temperature metasedimentary rocks referred as the Eastern Series. The Arauco Basin contains over 3 km of Late Cretaceous to Holocene continental and marine sediments Holocene continental and marine sediments
, La falla de Lanalhue es un sistema de fall … La falla de Lanalhue es un sistema de fallas geológicas que corre de noroeste a sureste. Este sistema de fallas contiene una falla principal y varias secundarias del tipo "splay". Comienza cerca del mar, sigue por la planicie litoral hasta dividirse cerca del lago Lanalhue. Luego, la falla pasa por el cerro Lanalhue mientras que la falla secundaria pasa por el lago Lanalhue, de donde fue nombrado este sistema de fallas. La falla continúa por la cordillera de Nahuelbuta de las regiones del Bío-Bío y de la Araucanía. Continúa por los cerros Ñielol-Humpil y Conun Huenu. Después continúa por la depresión intermedia hasta terminar cerca de Villarrica (una de las ciudades turísticas más importantes del sur de Chile). Además, esta falla poco conocida atraviesa grandes urbes como Temuco, la quinraviesa grandes urbes como Temuco, la quin
, Plus que d'une faille, il serait plus corr … Plus que d'une faille, il serait plus correct de parler d'un système de failles. Ce système de failles contient une faille principale et plusieurs failles secondaires du genre "splay". La faille du Lanalhue est la faille principale avec une orientation du nord-ouest au sud-est. Elle démarre près de la côte et elle suit par la plaine littorale. Elle se divise en deux près du . La faille principale passe à travers la colline Cerro Lanalhue en tant que la faille secondaire passe à travers le lac Lanalhue, d’où ce système de failles tient son nom. La faille principale après continue par la cordillère de Nahuelbuta des régions du Biobío et de l'Araucanie. Ensuite, elle passe à travers les collines cerro Ñielol et cerro Conun Huenu. Ensuite, cette faille continue par la Vallée centrale avant de continue par la Vallée centrale avant de
|
| rdfs:label |
Falla de Lanalhue
, Lanalhue Fault
, Faille du Lanalhue
|
