Dislocation Creep of Olivine and Amphibole in Amphibole Peridotites from Åheim, Norway

• Published in: Minerals (Basel) Vol. 11; no. 9; p. 1018
• Main Authors: Jung, Sejin, Yamamoto, Takafumi, Ando, Jun-ichi, Jung, Haemyeong
• Format: Journal Article
• Language: English
• Published: Basel MDPI AG 01.09.2021
• Subjects: amphibole; Amphiboles; Boundaries; Deformation; deformation mechanism; Deformation mechanisms; Dislocations; Electron backscatter diffraction; Electron microscopy; Grain boundaries; Grain size; Grain sub boundaries; lattice preferred orientation; Mapping; Metamorphism; Microstructural analysis; Moisture content; Olivine; Orogeny; Peridotite; Research methodology; Shear deformation; shear localization; Slip; Software; Solifluction; Transmission electron microscopy; Tremolite; Water content; Åheim amphibole peridotite; United Kingdom > UK; Norway
• ISSN: 2075-163X; 2075-163X
• DOI: 10.3390/min11091018

Amphibole peridotite samples from Åheim, Norway, were analyzed to understand the deformation mechanism and microstructural evolution of olivine and amphibole through the Scandian Orogeny and subsequent exhumation process. Three Åheim amphibole peridotite samples were selected for detailed microstructural analysis. The Åheim amphibole peridotites exhibit porphyroclastic texture, abundant subgrain boundaries in olivine, and the evidence of localized shear deformation in the tremolite-rich layer. Two different types of olivine lattice preferred orientations (LPOs) were observed: B- and A-type LPOs. Electron backscatter diffraction (EBSD) mapping and transmission electron microscopy (TEM) observations revealed that most subgrain boundaries in olivine consist of dislocations with a (001)[100] slip system. The subgrain boundaries in olivine may have resulted from the deformation of olivine with moderate water content. In addition, TEM observations using a thickness-fringe method showed that the free dislocations of olivine with the (010)[100] slip system were dominant in the peridotites. Our data suggest that the subgrain boundaries and free dislocations in olivine represent a product of later-stage deformation associated with the exhumation process. EBSD mapping of the tremolite-rich layer revealed intracrystalline plasticity in amphibole, which can be interpreted as the activation of the (100)[001] slip system.