The importance of gravity data for estimating and identifying the sediment thickness of subsurface structure around Majene Sulawesi Barat

Gravity method is one of the geophysical methods based on a gravity anomaly that arises due to a mass tight variation of the earth’s subsurface material constituents. Research with power spectral analysis of gravity anomaly data has been widely done for sediment thickness estimation. When the Mw 6.2...

Ausführliche Beschreibung

Bibliographische Detailangaben

Hauptverfasser:	Dewanto, Bondan G., Margiono, Relly, Segoro, Yan A., Pramesthi, Elisabet, Maimuna, Afra K.
Format:	Tagungsbericht
Sprache:	eng
Schlagworte:	Density distribution Domains Earthquake damage Estimation Fourier transforms Geophysical methods Gravity anomalies Sediments Seismic waves Spectrum analysis Thickness Three dimensional models
Online-Zugang:	Volltext
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