Modes of Gravity Anomaly Distributions in Relation to the Crustal Structure of the Antarctic Continent
An analytical method is introduced in applying the gravity data to the study of crustal structure by using a reduced gravity anomaly when the thickness of ice sheet is unknown. The reduced gravity anomaly designated as Δg_h(mgal) is defined by the equation of Δg_h=Δg_0-2πGρ(H-h), where Δg_0(mgal) is...
| Main Authors: | , |
|---|---|
| Format: | Article |
| Language: | English |
| Published: |
National Institute of Polar Research
1978-03-01
|
| Series: | Antarctic Record |
| Online Access: | https://doi.org/10.15094/00007981 |