GRAVITY PROCESSING AND INTERPRETATION OF WAE SANO GEOTHERMAL FIELD
Western part of Flores Island has run into rapid progress in tourism industry for past few years. Electricity demand is increasing due to this matter. In order to meet demands, exploration of geothermal energy is conducted in Wae Sano. Wae Sano geothermal field is expected to have potention of 26...
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id-itb.:518432020-10-01T09:55:45ZGRAVITY PROCESSING AND INTERPRETATION OF WAE SANO GEOTHERMAL FIELD Ababil Akram, Muhamad Indonesia Final Project gravity method, geothermal, first horizontal derivative, second vertical derivative, Wae Sano INSTITUT TEKNOLOGI BANDUNG https://digilib.itb.ac.id/gdl/view/51843 Western part of Flores Island has run into rapid progress in tourism industry for past few years. Electricity demand is increasing due to this matter. In order to meet demands, exploration of geothermal energy is conducted in Wae Sano. Wae Sano geothermal field is expected to have potention of 26 Mwe. The purpose of this study was to investigate the geothermal system of Wae Sano geothermal field based on the interpretation of gravity data. This research was conducted by analyzing the gravity method that starts from processing the gravity measurement data conducted by PSDMBP in 2015 to obtain a complete Bouguer anomaly. The complete Bouguer anomaly range is 60 - 116 mGal. Then anomalous separation is performed to obtain residual Bouguer anomalies by using the moving average method which produces anomalies of -20-14 mGal. To assist in forwarding the 2.5D modeling, a qualitative analysis was performed with the First Horizontal Derivative method which has an anomaly range of -0.06 to 0.04 mGal and the Second Vertical Derivative method which has an anomaly range of -11 - 8 mGal. The results of the modelling with a base density of 2.65 gr / cm3 show that there is an intrusion of diorite (?? = +0,15 gr/cm3) , dasit - rhyolite lava and pyroclastic product around the crater of Sano Nggoang (?? = -0,25 – 0,47 gr/cm3) which breaks through the Poco Dedeng volcanic unit (?? = +0,00 gr/cm3). The bedrock in this area is interpreted as a tertiary age sedimentary rock unit (?? = +0,05 gr/cm3). There is also a fault structure pattern in the study area in accordance with previous geological research. There is a fault structure pattern in the study area in accordance with previous geological research. Based on the results, the upflow zone is estimated to be in the Wae Sano hot spring manifestation area. While the outflow zone is estimated to be in the area of manifestation of Namparmancing warm water and Bobok warm water. text |
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Western part of Flores Island has run into rapid progress in tourism industry for
past few years. Electricity demand is increasing due to this matter. In order to meet
demands, exploration of geothermal energy is conducted in Wae Sano. Wae Sano
geothermal field is expected to have potention of 26 Mwe. The purpose of this study
was to investigate the geothermal system of Wae Sano geothermal field based on the
interpretation of gravity data. This research was conducted by analyzing the gravity
method that starts from processing the gravity measurement data conducted by
PSDMBP in 2015 to obtain a complete Bouguer anomaly. The complete Bouguer
anomaly range is 60 - 116 mGal. Then anomalous separation is performed to obtain
residual Bouguer anomalies by using the moving average method which produces
anomalies of -20-14 mGal. To assist in forwarding the 2.5D modeling, a qualitative
analysis was performed with the First Horizontal Derivative method which has an
anomaly range of -0.06 to 0.04 mGal and the Second Vertical Derivative method
which has an anomaly range of -11 - 8 mGal. The results of the modelling with a
base density of 2.65 gr / cm3 show that there is an intrusion of diorite (?? = +0,15
gr/cm3) , dasit - rhyolite lava and pyroclastic product around the crater of Sano
Nggoang (?? = -0,25 – 0,47 gr/cm3) which breaks through the Poco Dedeng
volcanic unit (?? = +0,00 gr/cm3). The bedrock in this area is interpreted as a
tertiary age sedimentary rock unit (?? = +0,05 gr/cm3). There is also a fault
structure pattern in the study area in accordance with previous geological research.
There is a fault structure pattern in the study area in accordance with previous
geological research. Based on the results, the upflow zone is estimated to be in the
Wae Sano hot spring manifestation area. While the outflow zone is estimated to be
in the area of manifestation of Namparmancing warm water and Bobok warm water. |
format |
Final Project |
author |
Ababil Akram, Muhamad |
spellingShingle |
Ababil Akram, Muhamad GRAVITY PROCESSING AND INTERPRETATION OF WAE SANO GEOTHERMAL FIELD |
author_facet |
Ababil Akram, Muhamad |
author_sort |
Ababil Akram, Muhamad |
title |
GRAVITY PROCESSING AND INTERPRETATION OF WAE SANO GEOTHERMAL FIELD |
title_short |
GRAVITY PROCESSING AND INTERPRETATION OF WAE SANO GEOTHERMAL FIELD |
title_full |
GRAVITY PROCESSING AND INTERPRETATION OF WAE SANO GEOTHERMAL FIELD |
title_fullStr |
GRAVITY PROCESSING AND INTERPRETATION OF WAE SANO GEOTHERMAL FIELD |
title_full_unstemmed |
GRAVITY PROCESSING AND INTERPRETATION OF WAE SANO GEOTHERMAL FIELD |
title_sort |
gravity processing and interpretation of wae sano geothermal field |
url |
https://digilib.itb.ac.id/gdl/view/51843 |
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1822928863340003328 |