The Chagnon-Orford Intrusive Complex is characterized by two types of banding: first, a large-scale zoning consisting of ultrabasic rocks at the bottom overlain by belts of successively more acid differentiates at the roof of the laccolith; secondly, a rhythmic banding near the floor of the intrusive, consisting of alternating peridotite and pyroxenite layers. The writer is of the opinion that the zonal arrangement of the Chagnon-Orford laccolith is the result of differentiation in situ under the influence of gravity. © 1963 Ferdinand Enke Verlag Stuttgart.
| Documento: | Artículo |
| Título: | Differentiation im Chagnon-Orford-Intrusiv-Komplex, Südostteil der Provinz Quebec, Kanada |
| Autor: | de Römer, H.S. |
| Filiación: | Dpto. de Geologia, Facultad de Ciencias Exactas y Naturales, Universidad de Buenos Aires, Perú 222, Argentina |
| Año: | 1963 |
| Volumen: | 52 |
| Número: | 2 |
| Página de inicio: | 825 |
| Página de fin: | 835 |
| DOI: | http://dx.doi.org/10.1007/BF01821159 |
| Título revista: | Geologische Rundschau |
| Título revista abreviado: | Geol Rundsch |
| ISSN: | 00167835 |
| Registro: | https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_00167835_v52_n2_p825_deRomer |
