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Statements

Subject Item
dbr:Penninic_thrustfront
rdfs:label
Penninic thrustfront Front pennique Fronte Pennidico
rdfs:comment
The Penninic thrustfront is a major tectonic in the French Alps. The thrustfront moves over a developing decollement horizon, and separates the (internal) high grade metamorphic rocks of the Penninic nappes from the (external) sedimentary rocks and crystalline basement of the Helvetic nappes. The last are in France often called zone Dauphiné or Dauphinois. Thrusting over the decollement horizon continues today, as the Apulian tectonic plate moves westward, converging with the European plate. Dans les Alpes occidentales, le front pennique, également dénommé chevauchement pennique frontal, est le chevauchement qui juxtapose les unités internes, métamorphiques (Mont Rose, Grand Paradis, Dora Maira...) sur les unités externes non métamorphiques (massifs cristallins externes, massifs subalpins). Il fonctionne aujourd'hui localement comme une faille normale et/ou comme un décrochement dextre. Il Fronte Pennidico è un lineamento tettonico che separa il dominio Pennidico dal dominio Elvetico nelle Alpi.Il lineamento separa quindi le rocce ad alto grado metamorfico, che si trovano all'interno della catena (a sud del lineamento), dal basamento cristallino e dalle rocce sedimentarie che si trovano verso l'esterno (a nord del lineamento). A causa del moto di convergenza della placca adriatica verso la placca euroasiatica il lineamento è ancora attivo.
dcterms:subject
dbc:Geology_of_France dbc:Geology_of_Switzerland dbc:Geology_of_the_Alps
dbo:wikiPageID
5489950
dbo:wikiPageRevisionID
1022384595
dbo:wikiPageWikiLink
dbr:Geology_of_the_Alps dbr:Metamorphic_rock dbr:Thrust_fault dbr:Helvetic_nappes dbr:Penninic_nappes dbr:Thrustfront dbc:Geology_of_France dbr:Alps dbr:Apulian_plate dbr:Decollement dbc:Geology_of_Switzerland dbc:Geology_of_the_Alps dbr:Sedimentary_rock dbr:Tectonics dbr:Basement_(geology) dbr:Plate_tectonics dbr:Eurasian_plate dbr:France dbr:Convergent_boundary
owl:sameAs
dbpedia-fr:Front_pennique freebase:m.0dp2kr n15:55dca wikidata:Q946529 dbpedia-it:Fronte_Pennidico
dbp:wikiPageUsesTemplate
dbt:Unreferenced dbt:Dablink dbt:Geology_of_the_Alps
dbo:abstract
The Penninic thrustfront is a major tectonic in the French Alps. The thrustfront moves over a developing decollement horizon, and separates the (internal) high grade metamorphic rocks of the Penninic nappes from the (external) sedimentary rocks and crystalline basement of the Helvetic nappes. The last are in France often called zone Dauphiné or Dauphinois. Thrusting over the decollement horizon continues today, as the Apulian tectonic plate moves westward, converging with the European plate. Dans les Alpes occidentales, le front pennique, également dénommé chevauchement pennique frontal, est le chevauchement qui juxtapose les unités internes, métamorphiques (Mont Rose, Grand Paradis, Dora Maira...) sur les unités externes non métamorphiques (massifs cristallins externes, massifs subalpins). Il fonctionne aujourd'hui localement comme une faille normale et/ou comme un décrochement dextre. Il Fronte Pennidico è un lineamento tettonico che separa il dominio Pennidico dal dominio Elvetico nelle Alpi.Il lineamento separa quindi le rocce ad alto grado metamorfico, che si trovano all'interno della catena (a sud del lineamento), dal basamento cristallino e dalle rocce sedimentarie che si trovano verso l'esterno (a nord del lineamento). A causa del moto di convergenza della placca adriatica verso la placca euroasiatica il lineamento è ancora attivo.
prov:wasDerivedFrom
wikipedia-en:Penninic_thrustfront?oldid=1022384595&ns=0
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1020
foaf:isPrimaryTopicOf
wikipedia-en:Penninic_thrustfront