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Mierostylolites are here reported in both quartzite and in welded tuff. Descriptions of these unusual occurrences and accompanying photomicrographs suggest difficulties in applying the widely held theory of presstire--solution for the origin of these features.doi:10.1306/d42697ec-2b26-11d7-8648000102c1865d fatcat:ykubboulrzbdlgq4zx6drpol5y