| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 6441202 | Lithos | 2011 | 18 Pages |
Abstract
⺠The SJIC and NGIC are mafic-silicic layered intrusions in the Armorican Massif. ⺠At some stages, both were mafic reservoirs invaded by intermediate magmas. ⺠Layering can result from spreading of dioritic magma within a crystallizing gabbro. ⺠Extraction of late diapirs results in cumulative textures in dioritic layers. ⺠Associated pegmatoids correspond to liquids issued from a mafic intercumulus melt.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geochemistry and Petrology
Authors
Martial Caroff, Nolwenn Coint, Erwan Hallot, Cédric Hamelin, Jean-Jacques Peucat, Gilles Charreteur,