KMS Nanjing Institute of Geology and Palaeonotology,CAS
Triassic‒Jurassic climate in continental high-latitude Asia was dominated by obliquity-paced variations (Junggar Basin, Ürümuqi, China. | |
Sha J. G.(沙金庚)![]() ![]() ![]() | |
2015 | |
发表期刊 | PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA
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卷号 | 112期号:12页码:3624–3629 |
收录类别 | SCI |
语种 | 英语 |
文献类型 | 期刊论文 |
条目标识符 | http://ir.nigpas.ac.cn/handle/332004/12175 |
专题 | 中国科学院南京地质古生物研究所 其他 |
推荐引用方式 GB/T 7714 | Sha J. G.(沙金庚),Olsen, P. E,Pan Y. H.(泮燕红),等. Triassic‒Jurassic climate in continental high-latitude Asia was dominated by obliquity-paced variations (Junggar Basin, Ürümuqi, China.[J]. PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA,2015,112(12):3624–3629. |
APA | Sha J. G..,Olsen, P. E.,Pan Y. H..,Xu D. Y..,Wang Y. Q..,...&Vajda, V.(2015).Triassic‒Jurassic climate in continental high-latitude Asia was dominated by obliquity-paced variations (Junggar Basin, Ürümuqi, China..PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA,112(12),3624–3629. |
MLA | Sha J. G.,et al."Triassic‒Jurassic climate in continental high-latitude Asia was dominated by obliquity-paced variations (Junggar Basin, Ürümuqi, China.".PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA 112.12(2015):3624–3629. |
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