Misorientation analysis in garnet coronitic textures

  1. J.M. Benítez-Pérez 1
  2. J. Gómez-Barreiro 1
  3. E. Mariani 2
  4. J.R. Martínez Catalán 1
  1. 1 Universidad de Salamanca
    info

    Universidad de Salamanca

    Salamanca, España

    ROR https://ror.org/02f40zc51

  2. 2 Earth, Ocean And Ecological Sciences School of Environmental Science
Journal:
Geotemas (Madrid)

ISSN: 1576-5172

Year of publication: 2016

Issue Title: IX CONGRESO GEOLÓGICO DE ESPAÑA

Issue: 16

Pages: 475-478

Type: Article

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More publications in: Geotemas (Madrid)

Abstract

The microstructures of garnet grains in coronas from the upper slice of the HP-HT Sobrado Unit (Upper Allochthon, Órdenes Complex, NW Iberia) have been mapped using automated EBSD (Electron backscattering diffraction). Pole figures and inverse pole figures are presented in order to evaluate the crystallographic preferred orientation of two types of garnets in coronas. In both cases their intraphase misorientation maps have been compared. Furthermore the interphase misorientation angle distribution, either correlated or uncorrelated, is used to analyse the type of deformation that produces this microstructure and try to explain the crystallographic preferred orientation in the garnets.

Data source: Dialnet