Structural study of the Almklovdalen peridotite massif (southern Norway)

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doi: 10.1016/0040-1951(81)90266-3
Authors:Cordellier, F.; Boudier, F.; Boullier, A. M.
Author Affiliations:Primary:
Univ. Nantes, Lab. Tectonophys., Nantes, France
Other:
Cent. Rech. Petrogr. et Geochem., France
Volume Title:Tectonophysics
Source:Tectonophysics, 77(3-4), p.257-281. Publisher: Elsevier, Amsterdam, Netherlands. ISSN: 0040-1951
Publication Date:1981
Note:In English
Summary:The Almklovdalen ultramafic body included in the basal gneisses of S Norway is composed mainly of hydrated harzburgite and dunite with cores of layered garnet lherzolite. The body can be interpreted as a deformed cone surrounding a gneissic central mass. Based on structural, microstructural and mineral preferred orientation studies, a continuous kinematic and metamorphic history is inferred. The major events of this history starting 1400-1800 m.y. ago are presented. [T.R.]
Subjects:Deformation; Dunite; Folds; Foliation; Garnet group; Gneisses; Harzburgite; Igneous rocks; Interpretation; Kinematics; Lherzolite; Lineation; Metaigneous rocks; Metamorphic rocks; Metamorphism; Nesosilicates; Olivine group; Orthosilicates; Peridotites; Plutonic rocks; Precambrian; Proterozoic; Silicates; Structural analysis; Structural geology; Tectonics; Textures; Ultramafics; Upper Precambrian; Europe; Norway; Scandinavia; Sogn; Southern Norway; Western Europe; Almklovdalen Massif; Evolution; Nordfjord
Coordinates:N615000 N620000 E0070000 E0050000
Abstract Numbers:83M/2023
Record ID:1981066476
Copyright Information:GeoRef, Copyright 2019 American Geosciences Institute. Reference includes data from Mineralogical Abstracts, United Kingdom, Twickenham, United Kingdom
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