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
Main Authors: | , , , , |
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Other Authors: | |
Format: | Text |
Language: | English |
Subjects: | |
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 |
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 |
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