In:
Journal of Geophysical Research: Earth Surface, American Geophysical Union (AGU), Vol. 124, No. 3 ( 2019-03), p. 812-829
Kurzfassung:
We present Oligocene–Pliocene reconstructions of the bedrock topography of the Wilkes Subglacial Basin and Transantarctic Mountains Preglacial landscape of the Wilkes Subglacial Basin was situated close to sea level and governed in part by flexure and crustal structure Dynamic and oscillatory Oligocene–Miocene ice sheets drove enhanced bedrock erosion and associated flexural isostatic uplift
Materialart:
Online-Ressource
ISSN:
2169-9003
,
2169-9011
DOI:
10.1029/2018JF004705
Sprache:
Englisch
Verlag:
American Geophysical Union (AGU)
Publikationsdatum:
2019
ZDB Id:
3094104-0
ZDB Id:
2130824-X
ZDB Id:
2138320-0
SSG:
16,13
Permalink