Six million years of magnetic grain-size records reveal that temperature and precipitation were decoupled on the Chinese Loess Plateau during ~ 4.5–2.6 Ma
| Image |  |
|---|---|
| Description | scientific article published in May 2013 |
| Author/s |
author: Junsheng Nie |
| Publication date | May 2013 |
| Language | |
| Country of origin | |
| Wikipedia link | |
| Copyright status | |
| Missing/wrong data? | Edit Wikidata item |