Diamonds and other ultrahigh-pressure（UHP）minerals exist in ophiolitic mantle peridotites and podiform chromitites from different orogenic belts.Most ophiolitehosted diamonds are small（;00-500μm across）,and
文摘Diamonds and other ultrahigh-pressure（UHP）minerals exist in ophiolitic mantle peridotites and podiform chromitites from different orogenic belts.Most ophiolitehosted diamonds are small（;00-500μm across）,and
