Diopside and magnetite exsolutions occur as oriented intergrowths within olivine of the lower Cr# dunite in the Dongbo ophiolite, Tibet. The fresh lower Cr# dunite has a mineral assemblage of olivine, spinel and diops...Diopside and magnetite exsolutions occur as oriented intergrowths within olivine of the lower Cr# dunite in the Dongbo ophiolite, Tibet. The fresh lower Cr# dunite has a mineral assemblage of olivine, spinel and diopside.展开更多
基金funded by grants from Sinoprobe-05-02 from the Ministry of Science and Technology of Chinathe NSF China (Nos. 40930313, 40921001, 41202036)+1 种基金the China Geological Survey (Nos. 1212011121263, 12120114061801, 2014DFR2127C)project from Institute of Geology, Chinese Academy of Geological Sciences (J1526)
文摘Diopside and magnetite exsolutions occur as oriented intergrowths within olivine of the lower Cr# dunite in the Dongbo ophiolite, Tibet. The fresh lower Cr# dunite has a mineral assemblage of olivine, spinel and diopside.
