Diamond from the Dabie Shan metamorphic rocks and its implication for tectonic setting

Diamonds occurs in ultrahigh pressure metamorphic rocks from Dabie Shan, Anhui Province, eastern China. Diamond-bearing rocks include eclogite, garnet-pyroxenite, and jadeitite. Diamonds occurs in a mineral assemblage with coesite and jadeite. The diamonds and diamondiferous rocks of Dabie Shan are interpreted to be the products of ultrahigh pressure metamorphism in the underthrust basement of the Yangtze continental plate during the early Mesozoic, at greater than 4.0 gigapascals and 900 ° C. This interpretation is based on the distribution of rock units, the stability field of diamond, the isotopic data indicating a crustal origin for he rocks. Most diamonds occur as euhedral inclusions in garnets and are 10 to 60 micrometers across, although some are up to 700 micrometers across.
Formation of diamond requires high pressures and temperatures; thus, its presence in crustal metamorphic rocks has important implications of tectonic models of metamorphism in that burial of crustal rocks to [...]