摘要
Rare earth element concentrations were determined in 15 Middle Jurassic carbonate source rocks from Buqu Formation in Nadigangri area, Qiangtang basin of Qinghai-Tibet Plateau. The results show that analyses of the REEs,especially ΣREE,Ce/Ce* values and Eu/Eu* values change regularly, which are closely related to it’s sedimentary environment. Being the continuous of expansion of transgression and the water column’s stratification effects, some water column in the bottom become into reducing environment for lacking of oxygen.