Journal
INTERNATIONAL GEOLOGY REVIEW
Volume 64, Issue 7, Pages 953-969Publisher
TAYLOR & FRANCIS INC
DOI: 10.1080/00206814.2021.1894611
Keywords
Offlap; endorheic basins; the Qaidam Basin; the Qilian Mountains; the Eastern Kunlun Mountains
Categories
Funding
- Key Program of the National Natural Science Foundation of China [41930213]
- Jilin University [4190805119L7]
Ask authors/readers for more resources
The offlap process in endorheic basins is controlled by newborn faults or new isostatic flexures inside the previous basin margin. Interpretation of seismic reflection profiles of the Qaidam basin reveals that the rigid Qaidam block was gradually broken during the India-Eurasian collision, and the plateau expanded progressively from pre-existing mountains to basins.
Accumulating sediments is an inherent attribute of endorheic basins. Overall aggradational stratigraphic architecture can be predicted in endorheic basins, whereas the offlap process can be regarded as an important geological indicator in closed basins. This study theoretically proposes the possible offlap process in endorheic basins, and then explores the actual pattern of the offlap process in the Qaidam basin, the largest endorheic basin in the northern Tibetan Plateau. According to the interpretation of drilling well data and seismic reflection profiles, widespread offlap is identified at all the three boundaries of the Qaidam basin since the late Miocene. The offlap process in endorheic basins is controlled by newborn faults or new isostatic flexures inside the previous basin margin. Interpretation of seismic reflection profiles reflects that the rigid Qaidam block was gradually broken during the India-Eurasian collision and the plateau progressively expanded from pre-existing mountains to basins.
Authors
I am an author on this paper
Click your name to claim this paper and add it to your profile.
Reviews
Recommended
No Data Available