In:
Geophysical Research Letters, American Geophysical Union (AGU), Vol. 47, No. 3 ( 2020-02-16)
Kurzfassung:
The red clay‐loess sequence since ~3 Ma was first found in the Lanzhou Basin, western Chinese Loess Plateau The pronounced increase in grain‐size and sedimentation rate at 2.8 Ma supported the intensified aridification in the Asian interior This obvious aridification was primarily caused by the uplift of the Tibetan Plateau and global cooling
Materialart:
Online-Ressource
ISSN:
0094-8276
,
1944-8007
DOI:
10.1029/2019GL086556
Sprache:
Englisch
Verlag:
American Geophysical Union (AGU)
Publikationsdatum:
2020
ZDB Id:
2021599-X
ZDB Id:
7403-2
SSG:
16,13