柴达木盆地一里坪地区新近系沉积环境及碳酸盐岩碳氧同位素特征
曾旭1(
),林潼1,周飞2,李洁3,张懿2,沈晓双2,房永生4,王科2
),林潼1,周飞2,李洁3,张懿2,沈晓双2,房永生4,王科2
Carbon and oxygen isotope characteristics of carbonate and Neogene depositional environment in the Yiliping area of Qaidam Basin
Xu ZENG1(),Tong LIN1,Fei ZHOU2,Jie LI3,Yi ZHANG2,Xiao-shuang SHEN2,Yong-sheng FANG4,Ke WANG2
),Tong LIN1,Fei ZHOU2,Jie LI3,Yi ZHANG2,Xiao-shuang SHEN2,Yong-sheng FANG4,Ke WANG2
图5. 不同地层单元湖相碳酸盐岩 δ18O 和 δ13C 平均值在开放型和封闭型湖泊中原生碳酸盐 δ18O 和 δ13C 分布区的投影(据文献[
Fig.5. Plot of average δ18O and δ13C values of lacustrine carbonate rocks in different stratigraphic units in comparison with δ18O and δ13C domains of primary lacustrine carbonates in open and closed lakes (according to the Refs.[23-26])
