INTERPRETATION OF GRAVITY ANOMALY IN GEOTHERMAL FIELD ‘Z’

Gravity method is one of geophysical method that used variety of density contrast from subsurface. In general, the stages of geophysical method are acquisition, data processing, and interpretation. After data acquisition is done with gravimeter, gravity data is corrected by tidal, drift, latitude, a...

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Bibliographic Details
Main Author: HILMI AUFA (NIM : 10212057), MUHAMAD
Format: Final Project
Language:Indonesia
Online Access:https://digilib.itb.ac.id/gdl/view/23167
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Institution: Institut Teknologi Bandung
Language: Indonesia

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