Low-grade, multiply-deformed, locally mylonitic assemblage of gritty semischist that contains clear to bluish-gray quartz “eyes,” chloritic quartzo-feldspathic schist and augen gneiss, phyllitic schist and semischist, phyllite, metavolcanic rocks, quartzite, marble, and greenstone. Porphyritic volcanic and sedimentary textures preserved in places; metavolcanic compositions range from mafic to felsic. Fossil age is poorly defined; conodonts collected from one marble interbed were Middle Devonian to Early Mississippian, and crinoids, corals, and gastropods were less precisely dated (Wahrhaftig, 1968). Meta-andesite from the northeastern Big Delta quadrangle yields an upper intercept U/Pb zircon age of 375 Ma that is interpreted as an extrusive age of the protolith (Dusel-Bacon and others, 1993; revised to 374±3 Ma, Cynthia Dusel-Bacon, written commun., 2014). Dusel-Bacon and others (2006) report U/Pb (SHRIMP) zircon ages between 372±3 and 360±5 Ma for meta-igneous rocks included in the Totatlanika Schist. Unit consists of the Totatlanika Schist of the Fairbanks and Healy quadrangles (Péwé and others, 1966; Csejtey and others, 1992), various units of the Totatlanika Schist in the Chena River area (Smith and others, 1994), unit Pzsg of Weber and others (1978) in the Big Delta quadrangle, and the blastomylonite subunit of unit PzpCs of Foster (1992)