INTERPRETATION OF GRAVITY ANOMALY IN GEOTHERMAL FIELD ̉̉Z̉̉
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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| 格式: | Final Project |
| 語言: | Indonesia |
| 在線閱讀: | https://digilib.itb.ac.id/gdl/view/23167 |
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| 機構: | Institut Teknologi Bandung |
| 語言: | Indonesia |