{"title":"Texture Analysis of Quartz in a Granite Mylonite byEBSP-Orientation Imaging Microscopy","authors":"A. Pearson, F. Heidelbach, H. Wenk","doi":"10.1155/TSM.29.185","DOIUrl":null,"url":null,"abstract":"The crystallographic preferred orientation (texture) of the quartz phase in a mylonitic \nleucogranite from the Santa Rosa mylonite zone was investigated using automated \nanalysis of electron backscattering patterns (EBSP) in the scanning electron microscope \n(SEM). The separation of the quartz diffraction patterns from patterns of other constituents \n(feldspar, mica, etc.) in this polymineralic rock was achieved using an image \nquality parameter. The quartz phase displays a texture typical for high temperature \nmylonites (c-axis maximum in the intermediate strain direction). The misorientation \ndistribution between next neighbors is dominated by Dauphine twins.","PeriodicalId":129427,"journal":{"name":"Textures and Microstructures","volume":"32 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"2","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Textures and Microstructures","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.1155/TSM.29.185","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 2
Abstract
The crystallographic preferred orientation (texture) of the quartz phase in a mylonitic
leucogranite from the Santa Rosa mylonite zone was investigated using automated
analysis of electron backscattering patterns (EBSP) in the scanning electron microscope
(SEM). The separation of the quartz diffraction patterns from patterns of other constituents
(feldspar, mica, etc.) in this polymineralic rock was achieved using an image
quality parameter. The quartz phase displays a texture typical for high temperature
mylonites (c-axis maximum in the intermediate strain direction). The misorientation
distribution between next neighbors is dominated by Dauphine twins.