Mineral inclusions in chrome-spinels from the cumulate sequence of the Dongcaohe ophiolite of north Qilian Mountains, NW China: Their genesis and petrological significance Chien-Yuan Tseng and Houng-Yi Yang Department of Earth Sciences, National Cheng Kung University, Tainan, Taiwan Chrome-spinels occurring in the cumulate sequence of the Dongcaohe ophiolite of north Qilian Mountains, NW China, frequently carry mineral inclusions of anhydrous silicate minerals (clinopyroxene and orthopyroxene), hydrous high-temperature silicate minerals (sodium phlogopite and pargasitic hornblende), hydrous low-temperature silicate minerals (chlorite, serpentine, hydrogarnet, and analcime), Fe-Ti oxide minerals and base-metal sulfides. Clinopyroxene, orthopyroxene, sodium phlogopite, pargasitic hornblende and Fe-Ti oxide minerals are considered as primary by their being texturally-isolated grains within host chrome-spinels and by their diagnostic characteristic mineral composition. Other inclusions are clearly secondary because they are connected with the serpentinized matrix by cracks and they were formed in the pressure-temperature range of their stability field. The secondary hydrothermal products including chlorite, serpentine, hydrogarnet, and analcime mainly reflect a low-temperature seafloor alteration under 200oC. The origin of these primary inclusions reflected a closed system evolution after entrapment of a H2O-bearing primary basaltic melt. By the fractional crystallization in the closed system, as temperature down it gave rise to volatile-enriched differentiated melts to crystallize the hydroxyl-sodic phases (sodium phlogopite and/or pargasitic hornblende). The H2O-bearing primary basaltic melt was probably resulted from the melt-mantle interaction in uppermost mantle beneath an active spreading ridge. 47