Greenland ice sheet retreat history in the northeast Baffin Bay based on high-resolution bathymetry
详细信息    查看全文
文摘
Ice streams reached the continental shelf edge through the cross-shelf troughs, presumably during the LGM. Discontinuous ice stream retreat of the Northwest Greenland ice sheet. Grounding zone wedge complexes formed in mid-shelf position. Final ice stream retreat within the cross-shelf troughs occurred before 8.41 ka BP. Small ice streams occur on inter-trough banks.
NGLC 2004-2010.National Geological Library of China All Rights Reserved.
Add:29 Xueyuan Rd,Haidian District,Beijing,PRC. Mail Add: 8324 mailbox 100083
For exchange or info please contact us via email.