Consists of a variety of metaigneous rocks of presumed Devonian age in central Alaska. Main part of unit lies north of the Denali Fault System and consists of a mixture of massive greenstone that locally contains thin septa of phyllite (Richter, 1976), and fine-grained, mylonitic, metavolcanic rocks interlayered with lesser metasedimentary rocks (Nokleberg and others, 1992a; Csejtey and others, 1992). Metavolcanic rocks are interpreted to consist chiefly of metamorphosed quartz keratophyre, dacite, andesite, and lesser metarhyodacite and metabasalt derived from fine-grained tuffs and flows (Nokleberg and others, 1992a) or metabasalt (Csejtey and others, 1992). Regionally metamorphosed to greenschist facies. Unit most certainly extends through the Tanacross quadrangle, but mapping is insufficient to allow us to distinguish this unit there. Unit includes the Spruce Creek sequence of Bundtzen (1981) and the Muskox sequence of Newberry and others (1996). Two samples of metarhyolite schist from the Spruce Creek sequence in the Mount McKinley quadrangle yielded TIMS U/Pb zircon ages of 370±5 and 369±4 Ma (Dusel-Bacon and others, 2006). South of the Denali Fault System, unit is sheared serpentinite tectonically intermixed with chert and pillow basalt, which form lenticular and podiform tectonic blocks (Csejtey and others, 1992). Radiolaria from the chert are Late Devonian (Famennian). South of the Denali Fault System, in the Healy and Mount McKinley quadrangles, this unit is part of the Chulitna sequence, and it was originally interpreted by Jones and others (1981) to be part of a dismembered ophiolite sequence, and it was reinterpreted by Clautice and others (2001) as feeders for the volcanic rocks included in unit TrPzvs