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THERMAL ANISOTROPY - A FACTOR CONTRIBUTING TO THE DISTRIBUTION OF CALEDONIAN METAMORPHIC ZONES IN THE SW SCOTTISH HIGHLANDS.

Author
BORRADAILE GJ
GEOL. INST., UNIV. AMSTERDAM, AMSTERDAM, NETH.
Source
GEOL. EN MIJNBOW; NEDERL.; 1976, VOL. 55, NUM. 0001-0002, P. 41 A 45
Document type
Serial Issue
Language
English
Keyword (fr)
ORIGINE ZONALITE FACIES METAMORPHISME CHLORITE BIOTITE GRENAT ANISOTROPIE CONDUCTIVITE THERMIQUE NAPPE OROGENIE CALEDONIENNE ECOSSE HIGHLANDS ROCHES CRISTALLINES GEOLOGIE SCIENCES DE LA TERRE ROYAUME UNI EUROPE
Keyword (en)
ORIGIN ZONATION METAMORPHIC FACIES CHLORITE BIOTITE GARNET ANISOTROPY THERMAL CONDUCTIVITY NAPPE CALEDONIAN OROGENY SCOTLAND CRYSTALLINE ROCKS GEOLOGY EARTH SCIENCES
Keyword (es)
ROCAS CRISTALINAS GEOLOGIA CIENCIAS DE LA TIERRA
Classification
Pascal
001 Exact sciences and technology / 001E Earth, ocean, space / 001E02 External geophysics / 001E02F Geophysics. Techniques, methods, instrumentation and models

Discipline
External geophysics
Origin
Inist-CNRS ; BRGM
Database
PASCAL
INIST identifier
PASCALGEODEBRGM7620291278

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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