Wiens (2012), Motion of an Antarctic glacier by repeated tidally modulated earthquakes, Nat

Between debris-laden glacial ice and bedrock, basal seismicity can develop that yields information about bed properties 1,2 , stress distribution 3 , outburst flooding 4 , and crevassing and calving

Bibliographic Details
Main Authors:	Lucas K Zoet, Sridhar Anandakrishnan, Richard B Alley, Andrew A Nyblade, Douglas A Wiens
Other Authors:	The Pennsylvania State University CiteSeerX Archives
Format:	Text
Language:	English
Subjects:	Antarctic Antarc*
Online Access:	http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1074.7390 http://epsc.wustl.edu/seismology/doug/wp-content/uploads/2013/08/zoet_etal_natgeosc_2012.pdf

Description
Summary:	Between debris-laden glacial ice and bedrock, basal seismicity can develop that yields information about bed properties 1,2 , stress distribution 3 , outburst flooding 4 , and crevassing and calving