Английская Википедия:Coastal Batholith of central Chile
Шаблон:Short description Шаблон:Infobox rockunit The Coastal Batholith of central Chile is a group of plutons in the Chilean Coast Range of Central Chile appearing contiguously from 33° S to 38° S.[1][2] At a latitude of 40° S an outlying group of plutons of the batholith appear in a more eastward position in the Andes.[1]
Together with the Elqui-Limarí Batholith and the Colangüil Batholith, the Coastal Batholith of central Chile is a remnant of the volcanic arcs that erupted the volcanic material of the Choiyoi Group. During the Permian the zone of arc magmatism moved from the Coastal Batholith 350 km inland reaching San Rafael about 280 million years ago.[2] The batholith is emplaced amidst metamorphic rocks belonging to a Paleozoic accretionary complex. The northern parts are of the batholith are themselves intruded by Jurassic gabbros.[1]
Rocks of the batholith belong to the calc-alkaline magma series.[3]
References
Шаблон:Geology of Chile
Шаблон:Chile-geo-stub
Шаблон:Geology-stub
- Английская Википедия
- Batholiths of South America
- Lithodemic units of Chile
- Carboniferous South America
- Carboniferous Chile
- Carboniferous magmatism
- Geology of the Chilean Coast Range
- Geology of Araucanía Region
- Geology of Biobío Region
- Geology of Los Ríos Region
- Geology of Maule Region
- Geology of O'Higgins Region
- Geology of Santiago Metropolitan Region
- Geology of Valparaíso Region
- Coasts of Valparaíso Region
- Coasts of O'Higgins Region
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- Страницы с телепортом
- Википедия
- Статья из Википедии
- Статья из Английской Википедии
