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- Q2051262 subject Q8488049.
- Q2051262 abstract "The Infrahelvetic complex is a tectonic unit in the Swiss Alps. It consists of autochthonous rocks of the former southern continental margin of the European Plate.The Infrahelvetic complex has been overthrusted by the Helvetic nappes, that partly contain similar rocks. It crops out in the northern part of the canton of Graubünden, generally south and below the Helvetic nappes and north of the Penninic nappes.The Infrahelvetic complex consists of Mesozoic cover rocks, most notably massive limestones from the European continental shelf. These limestones have a shallower marine facies than contemporary sediments from the Helvetic nappes since they were originally deposited north of those units. The Triassic and Permian consist of dolostones, marls and conglomerates. In contrast to the completely detached Helvetic nappes, the Infrahelvetic complex is still lying conformably on top of a Hercynian basement which forms the external massifs of the Aar and Gotthard nappes.".
- Q2051262 wikiPageWikiLink Q1134814.
- Q2051262 wikiPageWikiLink Q11925.
- Q2051262 wikiPageWikiLink Q134851.
- Q2051262 wikiPageWikiLink Q1780146.
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- Q2051262 wikiPageWikiLink Q3290577.
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- Q2051262 wikiPageWikiLink Q742139.
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- Q2051262 wikiPageWikiLink Q83222.
- Q2051262 wikiPageWikiLink Q840828.
- Q2051262 wikiPageWikiLink Q8488049.
- Q2051262 comment "The Infrahelvetic complex is a tectonic unit in the Swiss Alps. It consists of autochthonous rocks of the former southern continental margin of the European Plate.The Infrahelvetic complex has been overthrusted by the Helvetic nappes, that partly contain similar rocks.".
- Q2051262 label "Infrahelvetic complex".