4D Antarctica: a new effort aims to help bridge the gap between Antarctic crust and lithosphere structure and geothermal heat flux
Seismology, satellite-magnetic and aeromagnetic data, and sparse MT provide the only available geophysical proxies for large parts of Antarctica’s Geothermal Heat Flux (GHF) due to the sparseness of direct measurements. However, these geophysical methods have yielded significantly different GHF esti...
Main Authors: | , , , , , , , , , , , |
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Other Authors: | , , , , , , , , , , , |
Format: | Conference Object |
Language: | English |
Published: |
2020
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Subjects: | |
Online Access: | http://hdl.handle.net/11567/1025659 |