IGSNRR OpenIR
青藏高原腹地湖泊沉积序列与古气候变化
胡东生1; 张华京1; 温景春2; 李炳元3
2000
Source Publication地质学报
ISSN0001-5717
Volume074Issue:004Pages:363
Abstract在青藏高原综合科学考察中,选择其腹地系列剖面的沉积物记录进行地层气候学和同位素气候学的研究。沉积物记录的气候变化与同位素丰度变化的响应关系十分吻合,其时间尺度和分辨率也能够互为补偿,在较大范围内覆盖了32kaBP以来的古气候环境变化。更为有意义的是,清晰准确地检出新仙女木期气候冷干颤动事件,用同位素丰度变化拟合的降温幅度可达11C;并且识别出“仙女木期”(包括老-中-新仙女木事件)高分辩率气候变化
Language英语
Document Type期刊论文
Identifierhttp://ir.igsnrr.ac.cn/handle/311030/110330
Collection中国科学院地理科学与资源研究所
Affiliation1.湖南师范大学
2.中国科学探险协会
3.中国科学院地理科学与资源研究所
Recommended Citation
GB/T 7714
胡东生,张华京,温景春,等. 青藏高原腹地湖泊沉积序列与古气候变化[J]. 地质学报,2000,074(004):363.
APA 胡东生,张华京,温景春,&李炳元.(2000).青藏高原腹地湖泊沉积序列与古气候变化.地质学报,074(004),363.
MLA 胡东生,et al."青藏高原腹地湖泊沉积序列与古气候变化".地质学报 074.004(2000):363.
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