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扬子地台寒武系碳酸盐岩的碳同位素组成及地质意义
左景勋; 彭善池; 朱学剑
2008
Source Publication地球化学
ISSN0379-1726
Volume37Issue:2Pages:118-128
Keyword碳同位素组成 地层对比与划分 寒武系 长岩沟-岩孔剖面 贵州 扬子地台
Document Type期刊论文
Identifierhttp://ir.nigpas.ac.cn/handle/332004/3859
Collection中国科学院南京地质古生物研究所
其他
Recommended Citation
GB/T 7714
左景勋,彭善池,朱学剑. 扬子地台寒武系碳酸盐岩的碳同位素组成及地质意义[J]. 地球化学,2008,37(2):118-128.
APA 左景勋,彭善池,&朱学剑.(2008).扬子地台寒武系碳酸盐岩的碳同位素组成及地质意义.地球化学,37(2),118-128.
MLA 左景勋,et al."扬子地台寒武系碳酸盐岩的碳同位素组成及地质意义".地球化学 37.2(2008):118-128.
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