In:
Geochemistry, Geophysics, Geosystems, American Geophysical Union (AGU), Vol. 21, No. 3 ( 2020-03)
Abstract:
A major transition in the sediment source and transport dynamic of eolian sediments on the NE TP occurred between the red clay and the overlying loess deposits From the Pliocene onward, the paleo‐EAWM and EASM were intensified and exerted an increasing influence on the XSZ planation surface The contribution of the CAO to the XSZ red clay showed an increasing trend from the Late Miocene to the Middle Pliocene
Type of Medium:
Online Resource
ISSN:
1525-2027
,
1525-2027
DOI:
10.1029/2019GC008682
Language:
English
Publisher:
American Geophysical Union (AGU)
Publication Date:
2020
detail.hit.zdb_id:
2027201-7