A technique for extracting gravity anomalies originating from sediments deposited on folded oceanic crust
Negative gravity anomalies observed over sediments accumulated on folded oceanic crust are usually caused by two negative density contrasts. The first is the contrast between low-density sediments lying on folded high density oceanic crust and the second is the contrast between low-density oceanic...
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| Asıl Yazarlar: | , , |
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| Materyal Türü: | Artigo |
| Dil: | Inglês |
| Baskı/Yayın Bilgisi: |
National Science Foundation of Sri Lanka
2026-01-01
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| Seri Bilgileri: | Journal of the National Science Foundation of Sri Lanka |
| Konular: | |
| Online Erişim: | https://account.jnsfsl.sljol.info/index.php/sljo-j-jnsfsl/article/view/12668 |
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