Evidence of extensional metamorphism associated to Cretaceous rifting of the North-Maghrebian passive margin: The Tanger- Ketama Unit (External Rif, northern Morocco)

The distribution pattern of diagenetic conditions to very low-grade metamorphism in the eastern Rif has been determined based on a study of clay-mineral assemblages and illite crystallinity of Mesozoic metapelites. Lowgrade conditions were reached in marb

Bibliographic Details
Authors: Vázquez, M., Asebriy, L., Azdimousa, A., Jabaloy, A., Booth-Rea, G., Barbero, L., Mellini, M., González-Lodeiro, F.
Format: article
Status:Published version
Publication Date:2013
Country:Chile
Language:English
OAI Identifier:oai:repositorio.anid.cl:10533/238086
Online Access:https://hdl.handle.net/10533/238086
Access Level:Open access
Description
Summary:The distribution pattern of diagenetic conditions to very low-grade metamorphism in the eastern Rif has been determined based on a study of clay-mineral assemblages and illite crystallinity of Mesozoic metapelites. Lowgrade conditions were reached in marb