“…Evidence of arc activity in southern Mexico (Figs. 2 and 14) may also be preserved in (1) the latest Pennsylvanian to Middle Permian Tecomate Formation type area, which contains mafi c fl ows, tuffs, and rare felsic units (Keppie et al, 2004b;Sánchez-Zavala, 2008), (2) the Middle Permian Los Hornos Formation (Ramírez et al, 2000;Vachard et al, 2004), and (3) the uppermost Devonian to Lower Permian Patlanoaya Group, which contains intercalations of bentonite horizons representing ash-fall deposits Vachard and de Dios, 2002). The un deformed Olinalá Formation of Middle to Upper Permian age (Buitrón et al, 2005) is potentially also partially correlative with the Chichihualtepec Tecomate Formation strata, although volcanic rocks have not been described in this unit.…”