COMPOSITIONAL AND THERMAL DIFFERENCES BETWEEN LITHOSPHERIC AND ASTHENOSPHERIC MANTLE AND THEIR INFLUENCE ON CONTINENTAL DELAMINATION

The lower part of lithosphere in collisional orogens may delaminate due to density inversion between the asthenosphere and the cold thickened lithospheric mantle. Generally, standard delamination models have neglected density changes within the crust and the lithospheric mantle, which occur due to p...

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Detalhes bibliográficos
Main Authors: A. I. Kiselev, A. V. Ivanov, B. S. Danilov
Formato: Artigo
Idioma:Inglês
Publicado em: Institute of the Earth's crust, Siberian Branch of RAS 2015-09-01
Colecção:Geodinamika i Tektonofizika
Assuntos:
delamination
lithosphere
asthenosphere
collisional orogeny
craton
eclogites
Acesso em linha:https://www.gt-crust.ru/jour/article/view/42
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