Clay mineralogy of late Eocene to early Miocene sediments of McMurdo Sound, Antarctica
The clay mineral assemblages of upper Eocene to lower Miocene sediments recovered at the CIROS-1 and MSSTS-1 drill sites on the McMurdo Sound shelf, Antarctica, were analyzed in order to reconstruct the Cenozoic Antarctic paleoclimate and ice dynamics. The assemblages are dominated by smectite and i...
Main Author: | |
---|---|
Format: | Dataset |
Language: | English |
Published: |
PANGAEA
1998
|
Subjects: | |
Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.730374 https://doi.org/10.1594/PANGAEA.730374 |