In:
Journal of Geophysical Research: Planets, American Geophysical Union (AGU), Vol. 122, No. 11 ( 2017-11), p. 2344-2361
Kurzfassung:
Gobabeb is dominated by basaltic minerals (~60%) and X‐ray amorphous phases (~40%) and likely derives from more than one parent material CheMin‐derived crystal chemistry provides insights into the origin(s) and geologic history of the dune material CheMin analyses of Gobabeb confirm inferences of mafic‐enriched sands and allow for an evaluation of orbital‐based mineralogy estimates
Materialart:
Online-Ressource
ISSN:
2169-9097
,
2169-9100
DOI:
10.1002/jgre.v122.11
DOI:
10.1002/2017JE005262
Sprache:
Englisch
Verlag:
American Geophysical Union (AGU)
Publikationsdatum:
2017
ZDB Id:
1086497-0
ZDB Id:
3094268-8
ZDB Id:
2016810-X
SSG:
16,13