In:
Tectonics, American Geophysical Union (AGU), Vol. 42, No. 7 ( 2023-07)
Abstract:
The Beishan fold‐thrust belt was formed by contractional deformation in the late Middle Jurassic–Early Cretaceous Normal faulting exhumed the footwall rocks at ∼124–115 Ma, indicative of the late Mesozoic contraction–extension transition Intracontinental shortening in central Asia was driven by far‐field plate convergence around the Asian continent
Type of Medium:
Online Resource
ISSN:
0278-7407
,
1944-9194
DOI:
10.1029/2022TC007532
Language:
English
Publisher:
American Geophysical Union (AGU)
Publication Date:
2023
detail.hit.zdb_id:
2013221-9
detail.hit.zdb_id:
780264-X
SSG:
16,13
SSG:
13
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