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词条 Chaitenia
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{{refimprove|date=November 2018}}{{short description|A distinct fragment of Earth's crust in southern Chile}}Chaitenia is a distinct fragment of Earth's crust in southern Chile. Rocks of Chaitenia represents an ancient island arc that existed next to Patagonia which became eventually accreted to it.[1] The accretion of Chaitenia to Patagonia occurred in the Devonian period (c. 400-360 million years ago) as inferred from an event where rocks were put under pressure, deformed and heated dated to that period.[1] After merging into Patagonia, accretionary complexes developed west of it, meaning Chaitenia constituted a backstop.[1] Chaitenia is not thought to extend beyond the Huincul lineament to the north, beyond which lies the Chilenia terrane.[1]

References

1. ^{{cite journal |last1=Hervé |first1=Francisco|author-link1=Francisco Hervé |last2=Calderón |first2=Mauricio |last3=Fanning |first3=Mark |last4=Pankhurst |first4=Robert|author-link4=Robert John Pankhurst |last5=Rapela |first5=Carlos W. |last6=Quezada |first6=Paulo |date=2018 |title=The country rocks of Devonian magmatism in the North Patagonian Massif and Chaitenia |url=http://www.andeangeology.cl/index.php/revista1/article/view/V45n3-3117 |journal=Andean Geology |volume=45 |issue=3 |pages=301–317 |doi=10.5027/andgeoV45n3-3117 |access-date= }}
{{coord missing|Chile}}{{Geology of Chile}}{{chile-geo-stub}}{{regional-geology-stub}}{{palaeo-geo-stub}}

7 : Geology of Aysén Region|Geology of Chubut Province|Geology of Los Lagos Region|Geology of Los Ríos Region|Geology of Neuquén Province|Island arcs|Terranes

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