The Precambrian basement rocks in the Bengbu and neighboring areas, located at the southeastern margin of the North China Craton, occur as granulite terrains and xenoliths in the Mesozoic dioritic porphyry.
基金financially supported by the Ph.D Foundation of the Ministry of Education of China(grant No.20133402130008)the National Basic Research Program of China(grant No.2015CB856104)the National Natural Science Foundation of China(grant No.41273036)
文摘The Precambrian basement rocks in the Bengbu and neighboring areas, located at the southeastern margin of the North China Craton, occur as granulite terrains and xenoliths in the Mesozoic dioritic porphyry.
