Strelna Metamorphics is defined as metamorphosed part of (now abandoned) Strelna Formation of Moffit [1938]. Exposed mainly in southern Wrangellia terrane margin between Chitina and Border Ranges faults east of Taral fault and in thin fault-bounded sheets between Taral fault and Richardson HWY. Reference section designated in headwaters of Canyon Creek (SW/4 sec.12 T6S R6E, Valdez B-1 quad); this locality yielded age-diagnostic fossils. Metamorphic assemblage includes greenschist, marble, schistose marble, quartzo-feldspathic-mica schist, and micaceous quartz schist. Is considered to be in part as old as Early Pennsylvanian by correlation along strike with strata containing age-diagnostic conodonts in marble about 10 km east of Copper River.
Source: GNU records (USGS DDS-6; Menlo GNULEX).
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