In:
Tectonics, American Geophysical Union (AGU), Vol. 42, No. 7 ( 2023-07)
Kurzfassung:
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
Materialart:
Online-Ressource
ISSN:
0278-7407
,
1944-9194
DOI:
10.1029/2022TC007532
Sprache:
Englisch
Verlag:
American Geophysical Union (AGU)
Publikationsdatum:
2023
ZDB Id:
2013221-9
ZDB Id:
780264-X
SSG:
16,13
SSG:
13
Permalink