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The Liquine-Ofquifault zone (LOFZ) cuts the Patagonian batholith and the modern volcanic arc of southern Chile for ca 1000km. The rock fabric along three transects of the LOFZ combined with new and published geochronological data suggest marked differences in the nature and timing of deformation along strike. In the Liquine transect (39 o S), a 1km wide, northeast-striking subvertical mylonitic...
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