NUMERICAL INTERPRETATION OF 3D GRAVITY WITH TIKHONOV REGULARIZATION APPROACHIMATION

Gravity method is one of passive geophysical methods by using Earths gravity natural source. In this method, distribution of rocks under the subsurface greatly affects the gravity value in the measurement point, is is caused by variation of any rocks density. In the modeling of subsurface, measureme...

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Main Author: IDRIS NURUL ULUM (NIM 10213078), AHMAD
Format: Final Project
Language:Indonesia
Online Access:https://digilib.itb.ac.id/gdl/view/20844
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Institution: Institut Teknologi Bandung
Language: Indonesia
id id-itb.:20844
spelling id-itb.:208442017-11-08T09:44:10ZNUMERICAL INTERPRETATION OF 3D GRAVITY WITH TIKHONOV REGULARIZATION APPROACHIMATION IDRIS NURUL ULUM (NIM 10213078), AHMAD Indonesia Final Project INSTITUT TEKNOLOGI BANDUNG https://digilib.itb.ac.id/gdl/view/20844 Gravity method is one of passive geophysical methods by using Earths gravity natural source. In this method, distribution of rocks under the subsurface greatly affects the gravity value in the measurement point, is is caused by variation of any rocks density. In the modeling of subsurface, measurement data must be corrected to get Bouguer anomaly. The corrections are tidal correction, drift, latitude, free air, bourguer and terrain correction around the measurement. In this study, subsurface modeling is constucted by using 3D forward modeling and also inverse modeling. Inverse modeling is contructed by Tikhonov regularization approximation. Regularization parameter used in this study is 1.2 , 0.5 for alpha value, and 1.1 for beta value. Based on these modeling, we get the inversion result is closed to forward modeling. text
institution Institut Teknologi Bandung
building Institut Teknologi Bandung Library
continent Asia
country Indonesia
Indonesia
content_provider Institut Teknologi Bandung
collection Digital ITB
language Indonesia
description Gravity method is one of passive geophysical methods by using Earths gravity natural source. In this method, distribution of rocks under the subsurface greatly affects the gravity value in the measurement point, is is caused by variation of any rocks density. In the modeling of subsurface, measurement data must be corrected to get Bouguer anomaly. The corrections are tidal correction, drift, latitude, free air, bourguer and terrain correction around the measurement. In this study, subsurface modeling is constucted by using 3D forward modeling and also inverse modeling. Inverse modeling is contructed by Tikhonov regularization approximation. Regularization parameter used in this study is 1.2 , 0.5 for alpha value, and 1.1 for beta value. Based on these modeling, we get the inversion result is closed to forward modeling.
format Final Project
author IDRIS NURUL ULUM (NIM 10213078), AHMAD
spellingShingle IDRIS NURUL ULUM (NIM 10213078), AHMAD
NUMERICAL INTERPRETATION OF 3D GRAVITY WITH TIKHONOV REGULARIZATION APPROACHIMATION
author_facet IDRIS NURUL ULUM (NIM 10213078), AHMAD
author_sort IDRIS NURUL ULUM (NIM 10213078), AHMAD
title NUMERICAL INTERPRETATION OF 3D GRAVITY WITH TIKHONOV REGULARIZATION APPROACHIMATION
title_short NUMERICAL INTERPRETATION OF 3D GRAVITY WITH TIKHONOV REGULARIZATION APPROACHIMATION
title_full NUMERICAL INTERPRETATION OF 3D GRAVITY WITH TIKHONOV REGULARIZATION APPROACHIMATION
title_fullStr NUMERICAL INTERPRETATION OF 3D GRAVITY WITH TIKHONOV REGULARIZATION APPROACHIMATION
title_full_unstemmed NUMERICAL INTERPRETATION OF 3D GRAVITY WITH TIKHONOV REGULARIZATION APPROACHIMATION
title_sort numerical interpretation of 3d gravity with tikhonov regularization approachimation
url https://digilib.itb.ac.id/gdl/view/20844
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