The cretaceous Ladakh arc of NW himalaya—slab melting and melt–mantle interaction during fast northward drift of Indian Plate - CNRS - Centre national de la recherche scientifique Accéder directement au contenu
Article Dans Une Revue Chemical Geology Année : 2002

The cretaceous Ladakh arc of NW himalaya—slab melting and melt–mantle interaction during fast northward drift of Indian Plate

Résumé

The Kohistan–Ladakh Terrane in the NW Himalaya is a remnant of a Cretaceous arc sequence obducted onto the Indian margin. This paper presents a geochemical study major and trace elements and Sr, Nd, Pb isotopes of the Mid-Cretaceous lavas of the Ladakh side of the arc sequence, which were erupted in response to northward subduction of Neo-Tethys oceanic crust.

Domaines

Géochimie
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Dates et versions

hal-03882895 , version 1 (02-12-2022)

Identifiants

Citer

Yann Rolland, Christian Picard, Arnaud Pecher, Henriette Lapierre, Delphine Bosch, et al.. The cretaceous Ladakh arc of NW himalaya—slab melting and melt–mantle interaction during fast northward drift of Indian Plate. Chemical Geology, 2002, 182 (2-4), pp.139-178. ⟨10.1016/S0009-2541(01)00286-8⟩. ⟨hal-03882895⟩
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