“…Xenoliths from Late Cenozoic volcanic flows from the central Sierra (CS suite), the High Sierra, Owens Valley, and Inyo Mountains (HS suite) show variations in texture, composition, and thermal history consistent with the MT and seismic anomalies. The CS suite includes feldspathic granulites, garnet-pyroxenites, eclogites, cumulate gabbros and amphibolites, garnet and spinel peridotites, and garnet websterites (18)(19)(20). The HS suite includes spinel lhetzolites, hatzburgites, spinel dunites, spinel webterites, clinopyroxenites, gabbros, and mafic granulites, but lacks garnet.…”