| 刘安娜.黄土磁化率及其古环境意义述评[J].,2006,6(4):80-81 |
| 黄土磁化率及其古环境意义述评 |
| The Review of Paleoenvironmental Influence of Magnetic Susceptibility in the Loess |
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| DOI： |
| 中文关键词: 黄土 磁化率 环境意义 |
| 英文关键词: The loess Magnetic susceptibility The paleoenvironmental influence |
| 基金项目: |
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| 中文摘要: |
| 黄土是第四纪时期的重要堆积物, 其对于古环境的恢复具有极重大的意义。黄土磁化率对古降水量的推算, 以及建立
古气候复元的定量模型等都已成为可行。同时, 对现代土壤环境与降尘等环境因素的研究是磁化率应用性研究的新领域。 |
| 英文摘要: |
| The Chinese loess is important Quaternary sediment. The information from the loess is important to understand Quaternary
paleoenvironment. It is possible to use the magnetic susceptibility of the loess to propose quantitative models for restoring paleoenvironment on the
basis of paleoprecipitation. At the same time, the research of the modern soil and aeolian dust is the new field about the applied study of magnetic
susceptibility. |
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