%0 Journal Article %T Magma–host interactions during differentiation and emplacement of a shallow-level, zoned granitic pluton (Tarçouate pluton, Morocco): implications for magma emplacement %+ Centre de Recherches Pétrographiques et Géochimiques (CRPG) %+ Département des Sciences de la Terre (DéPARTEMENT DES SCIENCES DE LA TERRE) %+ Institut des Sciences de la Terre d'Orléans (ISTO) %A Barbey, P. %A Nachit, H. %A Pons, José %< avec comité de lecture %@ 0024-4937 %J Lithos %I Elsevier %V 58 %P 125-143 %8 2001 %D 2001 %R 10.1016/S0024-4937(01)00053-6 %K Morocco %K Anti-Atlas %K Pluton %K Granodiorite %K Emplacement %K Assimilation–fractional crystallisation %Z Sciences of the Universe [physics]/Earth Sciences/VolcanologyJournal articles %X The Tarçouate pluton (Anti-Atlas, Morocco) is an inversely zoned laccolith emplaced 583 Ma ago into low-grade metasediments, with the following succession: leucocratic granites, biotite–granodiorites (±monzodiorites), hornblende–granodiorites (±monzodiorites) and monzodiorites syn-plutonic dykes. These rocks form two distinct, chemically coherent, units: (1) A main unit consists of layered (57 %G English %2 https://insu.hal.science/hal-00089706/document %2 https://insu.hal.science/hal-00089706/file/Barbey-Lithos-2001.pdf %L hal-00089706 %U https://insu.hal.science/hal-00089706 %~ INSU %~ CNRS %~ UNIV-ORLEANS %~ ISTO %~ OSUC %~ UNIV-LORRAINE %~ OTELO-UL %~ CRPG-UL %~ TEST3-HALCNRS