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冈底斯山的隆升过程与青藏高原古高度研究 被引量:5

Paleoelevation research on Gangdise Mountains and Qinghai Tibet Plateau
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摘要 青藏高原古高度不仅是其深部变形的结果,也是地表风化剥蚀作用的产物。古高度是约束青藏高原隆升模式最重要的独立变量。传统观点认为,印度板块与欧亚大陆碰撞之后,青藏高原一直处于低海拔的状态,于新近纪时期约3 Ma才开始整体逐渐隆升形成的。但越来越多的证据表明青藏高原不同的块体之间存在着显著的差异隆升,甚至同一块体不同区域也存在着明显的高差,并且其主体隆升时间比传统认识要早得多。
作者 许强 丁林
出处 《中国科学基金》 CSSCI CSCD 北大核心 2015年第1期54-59,共6页 Bulletin of National Natural Science Foundation of China
基金 国家自然科学基金项目(批准号:41490615) 中国科学院先导专项(批准号:XDB03010401)的资助
关键词 氧同位素 古高度 冈底斯 青藏高原 oxygen isotope paleoelevation reconstruction Gangdise Mountains Qinghai Tibet Plateau
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参考文献20

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