 |
Conference papers
Enlargement of the active rift during glaciations
Abstract : During the last glaciation, an ice sheet covered Iceland approximately 1000 m thick. A reconstruction of the ice flow lines shows that the ice sheet was partly drained through fast-flowing streams. The major drainage routes correlate with locations of geothermal anomalies, suggesting that ice stream activity was favoured by water produced in regions of high geothermal heat flux. A widening of active rift zone was also deduced revealing a coupling between deep and surface processes.
Cited literature [7 references]
https://hal.univ-brest.fr/hal-00480686
Contributor : Adminhal Univbrestbu <>
Submitted on : Tuesday, May 4, 2010 - 5:11:42 PM
Last modification on : Thursday, January 14, 2021 - 11:45:21 AM
Long-term archiving on: : Thursday, September 16, 2010 - 1:12:22 PM
Contributor : Adminhal Univbrestbu <>
Submitted on : Tuesday, May 4, 2010 - 5:11:42 PM
Last modification on : Thursday, January 14, 2021 - 11:45:21 AM
Long-term archiving on: : Thursday, September 16, 2010 - 1:12:22 PM
File
DauteuilSummerSchool2010_1_.pd...
Files produced by the author(s)