摘要
Rodingite, coexisting with serpentinized harzburgite,was found in the Shaliuhe ophiolite sequence, North Qaidam UHPM belt. It is mainly composed of grossular, dioposide, chlorite, carbonate and minor prehnite, zoisite. Rodingite is a typical product of ocean-floor metamorphism. The Shaliuhe rodingite is the second evidence for the oceanic subduction in North Qaidam UHPM belt.