Oxygen and strontium isotopic evidence regarding the role of continental crust in the origin and evolution of the British Caledonian Granites
- Other title
- Mise en évidence par les isotopes de l'oxygène et du strontium du rôle de la croûte continentale dans l'origine et l'évolution des granites calédonniens anglais (fr)
- Author
- HARMON, R.S1
[1] Southern methodist univ., dep. geol. sci., Dallas TX 75275, United States - Conference title
- High grade metamorphism, migmatites and melting. Meeting of the Geochemical Group of the Mineralogical Society
- Conference name
- High grade metamorphism, migmatites and melting. Meeting of the Geochemical Group of the Mineralogical Society (1982-04)
- Source
High grade metamorphism, migmatites and melting. Meeting of the Geochemical Group of the Mineralogical Society. 1983, pp 62-79 ; Draft , Illustration , Table
- Publisher
- Shiva publ, Nantwich
- Publication country
- United Kingdom
- Document type
- Conference Paper
- Language
- English
- Keyword (fr)
- Datation Ecosse Granite O 18 Orogénie calédonienne Sr 87-Sr 86 Synthèse bibliographique U-Pb Zone subduction Europe Roche ignée Royaume Uni
- Keyword (en)
- Absolute age Scotland Granites O-18 Caledonian Orogeny Sr-87/Sr-86 Review U/Pb Subduction zones Europe Igneous rocks United Kingdom
- Keyword (es)
- Fechado Escocia Granito O 18 Orogenia caledoniana Sr 87-Sr 86 Síntesis bibliográfica U-Pb Zona subducto Europa Reino Unido Roca ignea
- Classification
- Pascal
- 001 Exact sciences and technology / 001E Earth, ocean, space / 001E01 Earth sciences / 001E01C Isotope geochemistry. Geochronology / 001E01C02 Geochronology
- Discipline
- Earth sciences
- Origin
- BRGM
- Database
- PASCAL
- INIST identifier
- 7314189
Sauf mention contraire ci-dessus, le contenu de cette notice bibliographique peut être utilisé dans le cadre d’une licence CC BY 4.0 Inist-CNRS / Unless otherwise stated above, the content of this bibliographic record may be used under a CC BY 4.0 licence by Inist-CNRS / A menos que se haya señalado antes, el contenido de este registro bibliográfico puede ser utilizado al amparo de una licencia CC BY 4.0 Inist-CNRS
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