摘要
ry name="EnDivSummary">Continuous laser microprobe 40Ar/39Ar technique has been used to analyze the ore-bearing vein quartz, in the Bangpu porphyry-type Mo-Cu polymetallic deposits. A 40Ar/39Ar isochron gives out an age of (13.9 ±0.9) Ma (MSWD=29), representing the age of mineralization which is somewhat lower than the crystallization age (13.9±0.9) Ma, MSWD=3.05) of monzonite granite-porphyry, and indicating that the rock-forming and ore-forming process is a continuous magmatic process. Meanwhile, a statistic study of rock-forming and ore-forming ages of Gangdese porphyry copper belt shows that its peak progress age is 15 Ma with the linear equation of Yrock=1.291Xore+7.785(R2=0.291), suggesting that the formation of Bangpu deposit is the same as the Gangdese belt, characterized by explosive ore-forming progress with uniform and intensive ore-forming events.