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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Główni autorzy:	D. A. Tantrigoda, M. M. P. M. Fernando, S.A. Samaranayake
Format:	Artigo
Język:	Inglês
Wydane:	National Science Foundation of Sri Lanka 2026-01-01
Seria:	Journal of the National Science Foundation of Sri Lanka
Hasła przedmiotowe:	Fourier transform gravity anomaly, oceanic crust upper mantle sediments inverse method
Dostęp online:	https://account.jnsfsl.sljol.info/index.php/sljo-j-jnsfsl/article/view/12668
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