| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 4690064 | Sedimentary Geology | 2010 | 9 Pages |
Abstract
⺠The Rogen moraine ridges are fluted on their surfaces and exhibit down-ice horn-features linked to active transverse-to-ice and subglacial genesis. ⺠The maximum Ïa-anisotropy of sediments in the cores of the Rogen ridges is parallel to the orientation of the ridge trends. ⺠The core is mantled with sediments exhibiting Ïa-anisotropy parallel-to-iceflow. ⺠Rogen moraine is polygenetic in origin and exhibits both transverse-to-ice (older) and parallel-to-ice (younger) electrical-sedimentary stratigraphy.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Earth-Surface Processes
Authors
Raimo Sutinen, Mari Jakonen, Matti Piekkari, Paula Haavikko, Paavo Närhi, Maarit Middleton,