A reassessment of spectral T e estimation in continental interiors: the case of North America
Conventional spectral T e studies use the real part of the admittance between gravity anomalies and topography or, alternatively, the square of the magnitude of the coherency (i.e., coherence). Here we show the utility of treating both the admittance and coherency as complex quantities. Inverting t...
| Main Authors: | , |
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| Format: | Journal Article |
| Published: |
American Geophysical Union
2009
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| Online Access: | http://hdl.handle.net/20.500.11937/34771 |
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