In:
Geochemistry, Geophysics, Geosystems, American Geophysical Union (AGU), Vol. 18, No. 11 ( 2017-11), p. 3741-3757
Kurzfassung:
Paleomagnetism and fossil mammals determined the sequence deposited from approximately 12.7 to 4.8 Ma Sedimentation rates with paleocurrents and simultaneously changes of facies indicate uplifts of the eastern Qilian Shan at 8.1 and 6.3 Ma Paleomagnetic results provide an age constraint on the river terraces and eolian dust deposition on the basin
Materialart:
Online-Ressource
ISSN:
1525-2027
,
1525-2027
DOI:
10.1002/2017GC006945
Sprache:
Englisch
Verlag:
American Geophysical Union (AGU)
Publikationsdatum:
2017
ZDB Id:
2027201-7