.png){kind=icon}
.png){kind=icon}
Return
Source-to-sink evolution of the western margin of the Yangtze Block and its implications for the paleogeography of South China during Gondwana assembly
.png){kind=icon}
PRE
AI
Y
DOI：10.1016/j.gr.2026.07.003.png)
.png){kind=icon}
Original request for help.png){kind=icon}
Share.png){kind=icon}
Save
Abstract
En 中文
• Ediacaran-Ordovician source-to-sink (S2S) evolution of the western Yangtze Block. • Integrated detrital zircons and paleotopographic data to identify S2S regimes. • Recognized spatiotemporal S2S changes among exogenous, endogenous, and composite. • South China was a marginal component of East Gondwana.
Journal
IF:
8.6
Papers:
4.3K
Citations:
2.1W
Organization
Cited Papers