In:
Tectonics, American Geophysical Union (AGU), Vol. 42, No. 1 ( 2023-01)
Kurzfassung:
Three end‐member deformation modes for Tibetan lithosphere are produced by varying the width, thickness and strength of the Qaidam crust Strong crust‐mantle coupling of the Qaidam Basin prevents southward lithospheric subduction of the Eastern Kunlun‐Qaidam‐Qilian terrane Our simulations provide a plausible explanation for the two phases of Cenozoic crustal deformation in northeastern Tibet
Materialart:
Online-Ressource
ISSN:
0278-7407
,
1944-9194
DOI:
10.1029/2022TC007261
Sprache:
Englisch
Verlag:
American Geophysical Union (AGU)
Publikationsdatum:
2023
ZDB Id:
2013221-9
ZDB Id:
780264-X
SSG:
16,13
SSG:
13