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7. 柴西—一里坪地区N22沉积相剖面（位置见图1中C—C’）
Fig.7. Sedimentary facies of Upper Youshashan Formation of connecting wells from the western Qaidam Basin to Yiliping Sag(the C-C’location is shown in Fig.1)
