A method of isotopic age determination. CHIME (chemical Th-U-total Pb isochron method) for dating radioactive minerals, is introduced briefly in this paper. The monazite. xenotime and zircon from the gneissic granitoi...A method of isotopic age determination. CHIME (chemical Th-U-total Pb isochron method) for dating radioactive minerals, is introduced briefly in this paper. The monazite. xenotime and zircon from the gneissic granitoids in the Pingtan-Dengshan belt, Fujian. yield CHIME ages of 92. 7 Ma. 94. 4 Ma. 107. 1 Ma and 108. 2 Ma. reconfirming the Yanshanian granitism in southeast coast area of China.展开更多
文摘A method of isotopic age determination. CHIME (chemical Th-U-total Pb isochron method) for dating radioactive minerals, is introduced briefly in this paper. The monazite. xenotime and zircon from the gneissic granitoids in the Pingtan-Dengshan belt, Fujian. yield CHIME ages of 92. 7 Ma. 94. 4 Ma. 107. 1 Ma and 108. 2 Ma. reconfirming the Yanshanian granitism in southeast coast area of China.
