Isotopic and trace-element arguments for the lower-crustal origin of Hercynian granitoids and pre-Hercynian orthogneisses, Massif Central (France)
- 1 May 1988
- journal article
- Published by Elsevier in Chemical Geology
- Vol. 68 (3-4) , 291-308
- https://doi.org/10.1016/0009-2541(88)90027-7
Abstract
No abstract availableKeywords
This publication has 21 references indexed in Scilit:
- Nd isotopic characteristics of S- and I-type granitesPublished by Elsevier ,2002
- A Nd, Sr and O isotopic investigation into the causes of chemical and isotopic zonation in the Bishop Tuff, CaliforniaPublished by Elsevier ,2002
- Recycling processes in granite-granodiorite complex genesis: the Querigut case studied by NdSr isotope systematicsPublished by Elsevier ,2002
- Geochemistry and petrology of meta-igneous granulitic xenoliths in Neogene volcanic rocks of the Massif Central, France — implications for the lower crustPublished by Elsevier ,2002
- Textural, isotopic and REE variations in spinel peridotite xenoliths, Massif Central, FranceEarth and Planetary Science Letters, 1987
- Petrogenesis of Hercynian leucogranites from the southern Armorican Massif: contribution of REE and isotopic (Sr, Nd, Pb and O) geochemical data to the study of source rock characteristics and agesEarth and Planetary Science Letters, 1985
- Palaeozoic granitoids from the French Massif Central: age and origin studied by 87Rb87Sr systemPhysics of the Earth and Planetary Interiors, 1984
- Nd—Sr isotopic composition of granulites and constraints on the evolution of the lower continental crustNature, 1984
- Granulites and related rocks in variscan median Europe: A dualistic interpretationTectonophysics, 1983
- Mantle and crustal granites: Genetic classification of orogenic granites and the nature of their enclavesJournal of Volcanology and Geothermal Research, 1982