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- Ivrea_zone abstract "The Ivrea zone is a tectonic terrane in the Italian Alps, that consists of a steeply dipping piece of the Earth’s lower crust of the Apulian plate. The zone is named after the Italian city of Ivrea.Geologically the Ivrea zone is considered a part of the Southern Alps. Most rocks in the zone are sedimentary, for example limestones that have been turned into marble by metamorphism. Most of the zone has been through granulite facies metamorphism and was intruded by mafic plutons. This is the type of rock common in the lower regions of the crust. When the terrane was uplifted during the formation of the Alps, the upper crust was eroded off so that these rocks are now at the surface.Geophysical research shows the mantle is relatively close under the surface at the Ivrea zone. Some geologists think the boundary between pyroxenites and lherzolites, that is also found in outcrops in the Ivrea zone, represents the Mohorovičić discontinuity (the Moho). The Moho is seismologically defined as the boundary between the crust and mantle.".
- Ivrea_zone wikiPageID "5404957".
- Ivrea_zone wikiPageLength "1678".
- Ivrea_zone wikiPageOutDegree "32".
- Ivrea_zone wikiPageRevisionID "544403017".
- Ivrea_zone wikiPageWikiLink Adriatic_Plate.
- Ivrea_zone wikiPageWikiLink Alps.
- Ivrea_zone wikiPageWikiLink Apulian_plate.
- Ivrea_zone wikiPageWikiLink Category:Geology_of_Italy.
- Ivrea_zone wikiPageWikiLink Category:Geology_of_the_Alps.
- Ivrea_zone wikiPageWikiLink Category:Structural_geology.
- Ivrea_zone wikiPageWikiLink Category:Terranes.
- Ivrea_zone wikiPageWikiLink Crust_(geology).
- Ivrea_zone wikiPageWikiLink Earth.
- Ivrea_zone wikiPageWikiLink Geology_of_the_Alps.
- Ivrea_zone wikiPageWikiLink Geophysics.
- Ivrea_zone wikiPageWikiLink Granulite.
- Ivrea_zone wikiPageWikiLink Granulite_facies.
- Ivrea_zone wikiPageWikiLink Intrusion.
- Ivrea_zone wikiPageWikiLink Italy.
- Ivrea_zone wikiPageWikiLink Ivrea.
- Ivrea_zone wikiPageWikiLink Lherzolite.
- Ivrea_zone wikiPageWikiLink Limestone.
- Ivrea_zone wikiPageWikiLink Mafic.
- Ivrea_zone wikiPageWikiLink Mantle_(geology).
- Ivrea_zone wikiPageWikiLink Marble.
- Ivrea_zone wikiPageWikiLink Metamorphism.
- Ivrea_zone wikiPageWikiLink Mohorovičić_discontinuity.
- Ivrea_zone wikiPageWikiLink Outcrop.
- Ivrea_zone wikiPageWikiLink Pyroxenite.
- Ivrea_zone wikiPageWikiLink Sedimentary_rock.
- Ivrea_zone wikiPageWikiLink Seismology.
- Ivrea_zone wikiPageWikiLink Southern_Alps_(Europe).
- Ivrea_zone wikiPageWikiLink Southern_Alps_(geology).
- Ivrea_zone wikiPageWikiLink Strike_and_dip.
- Ivrea_zone wikiPageWikiLink Tectonic_uplift.
- Ivrea_zone wikiPageWikiLink Tectonics.
- Ivrea_zone wikiPageWikiLink Terrane.
- Ivrea_zone wikiPageWikiLinkText "Ivrea zone".
- Ivrea_zone hasPhotoCollection Ivrea_zone.
- Ivrea_zone wikiPageUsesTemplate Template:Dablink.
- Ivrea_zone wikiPageUsesTemplate Template:Geology_of_the_Alps.
- Ivrea_zone wikiPageUsesTemplate Template:Unreferenced.
- Ivrea_zone subject Category:Geology_of_Italy.
- Ivrea_zone subject Category:Geology_of_the_Alps.
- Ivrea_zone subject Category:Structural_geology.
- Ivrea_zone subject Category:Terranes.
- Ivrea_zone hypernym Terrane.
- Ivrea_zone type Article.
- Ivrea_zone type Place.
- Ivrea_zone type Article.
- Ivrea_zone type Fragment.
- Ivrea_zone comment "The Ivrea zone is a tectonic terrane in the Italian Alps, that consists of a steeply dipping piece of the Earth’s lower crust of the Apulian plate. The zone is named after the Italian city of Ivrea.Geologically the Ivrea zone is considered a part of the Southern Alps. Most rocks in the zone are sedimentary, for example limestones that have been turned into marble by metamorphism. Most of the zone has been through granulite facies metamorphism and was intruded by mafic plutons.".
- Ivrea_zone label "Ivrea zone".
- Ivrea_zone sameAs Zona_Ivrea_Verbano.
- Ivrea_zone sameAs Ivrea-zone.
- Ivrea_zone sameAs m.0dkb_l.
- Ivrea_zone sameAs Q4024707.
- Ivrea_zone sameAs Q4024707.
- Ivrea_zone wasDerivedFrom Ivrea_zone?oldid=544403017.
- Ivrea_zone isPrimaryTopicOf Ivrea_zone.