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Geophysical gravity survey is a method to acquire subsurface information of a target area. Usually this method is a preliminary survey to distinguish the prospect of an area. G r a vity survey measures the gravity variation of an area to obtain the density <br /> <br /> variation or to l...

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Main Author: LESMANA (NIM : 124 03 008), WENY
Format: Final Project
Language:Indonesia
Online Access:https://digilib.itb.ac.id/gdl/view/24689
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Institution: Institut Teknologi Bandung
Language: Indonesia
id id-itb.:24689
spelling id-itb.:246892017-01-24T15:34:38Z#TITLE_ALTERNATIVE# LESMANA (NIM : 124 03 008), WENY Indonesia Final Project INSTITUT TEKNOLOGI BANDUNG https://digilib.itb.ac.id/gdl/view/24689 Geophysical gravity survey is a method to acquire subsurface information of a target area. Usually this method is a preliminary survey to distinguish the prospect of an area. G r a vity survey measures the gravity variation of an area to obtain the density <br /> <br /> variation or to locate density anomaly. With this information we can acquire and study what is under the survey area. <br /> <br /> G ravity data acquisition involves variables such as coordinates (x, y, z) and relative gravity value of each measurement locations. To attain gravity anomaly data which is ready to be process, further correction procedures are required. If done manually it consumes a lot of time and there is a possibility of mistakes. While existing software are quite expensive. <br /> <br /> T h erefore the programming and use of my software to calculate gravity reduction value will accelerate and ease the processing of gravity acquisition data. This software calculates from diurnal correction to residual regional anomaly separation using trend surface analysis (TSA). 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 Geophysical gravity survey is a method to acquire subsurface information of a target area. Usually this method is a preliminary survey to distinguish the prospect of an area. G r a vity survey measures the gravity variation of an area to obtain the density <br /> <br /> variation or to locate density anomaly. With this information we can acquire and study what is under the survey area. <br /> <br /> G ravity data acquisition involves variables such as coordinates (x, y, z) and relative gravity value of each measurement locations. To attain gravity anomaly data which is ready to be process, further correction procedures are required. If done manually it consumes a lot of time and there is a possibility of mistakes. While existing software are quite expensive. <br /> <br /> T h erefore the programming and use of my software to calculate gravity reduction value will accelerate and ease the processing of gravity acquisition data. This software calculates from diurnal correction to residual regional anomaly separation using trend surface analysis (TSA).
format Final Project
author LESMANA (NIM : 124 03 008), WENY
spellingShingle LESMANA (NIM : 124 03 008), WENY
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author_facet LESMANA (NIM : 124 03 008), WENY
author_sort LESMANA (NIM : 124 03 008), WENY
title #TITLE_ALTERNATIVE#
title_short #TITLE_ALTERNATIVE#
title_full #TITLE_ALTERNATIVE#
title_fullStr #TITLE_ALTERNATIVE#
title_full_unstemmed #TITLE_ALTERNATIVE#
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url https://digilib.itb.ac.id/gdl/view/24689
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