摘要
The ultramafic massif of Bulqiza, which belongs to the eastern ophiolitic belt of Albania, is the most important area for metallurgical chromitite ores. The massif consists of a thick （〉4 km） rock sequence, with a generalized profile from the bottom to the top as follows. The tectonite sequence composed mainly of harzburgites with subordinate intercalations of dunites,
The ultramafic massif of Bulqiza, which belongs to the eastern ophiolitic belt of Albania, is the most important area for metallurgical chromitite ores. The massif consists of a thick （〉4 km） rock sequence, with a generalized profile from the bottom to the top as follows. The tectonite sequence composed mainly of harzburgites with subordinate intercalations of dunites,
基金
funded by grants from Sinoprobe-05-02 from the Ministry of Science and Technology of China
the NSF China (Nos. 40930313, 40921001, 41202036)
the China Geological Survey (Nos. 1212011121263, 12120114061801, 2014DFR2127C)
project from Institute of Geology, Chinese Academy of Geological Sciences (J1526)
