2016
DOI: 10.1088/1755-1315/42/1/012009
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Geological, isothermal, and isobaric 3-D model construction in early stage of geothermal exploration

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Cited by 4 publications
(3 citation statements)
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“…The surrounding boundary is defined as boundaries 1 and 2, which are set to be impermeable layers. The numerical simulation result has been confirmed to be reaching its natural state by comparing the subsurface temperature from the simulation result to subsurface temperature estimation using an approach from Saputra [35] at the corresponding depth. The calculation result shows the estimated temperature beneath the Gedongsongo fumarole is 176 o C at elevation 115 mbsl and compared with the temperature at the same position and depth in the model, which temperature is 168 o C has an 8 o C deviation.…”
Section: Figure 2 Numerical Model Of the Ungaran Prospective Producti...mentioning
confidence: 72%
“…The surrounding boundary is defined as boundaries 1 and 2, which are set to be impermeable layers. The numerical simulation result has been confirmed to be reaching its natural state by comparing the subsurface temperature from the simulation result to subsurface temperature estimation using an approach from Saputra [35] at the corresponding depth. The calculation result shows the estimated temperature beneath the Gedongsongo fumarole is 176 o C at elevation 115 mbsl and compared with the temperature at the same position and depth in the model, which temperature is 168 o C has an 8 o C deviation.…”
Section: Figure 2 Numerical Model Of the Ungaran Prospective Producti...mentioning
confidence: 72%
“…There are about 70 lithology units on this map, but this unit will be simplified by coloring based on rock sources to aid modeling. Subsurface temperature distribution, other than based on the well data, is obtained from the results of temperature estimation given by Saputra (2006) [1]. By this method, the subsurface temperature of the conductive layers can be determined.…”
Section: Methodsmentioning
confidence: 99%
“…However, this 2D model has limited information, especially regarding the geometry of the geothermal system. Therefore, the delineation of geothermal systems in 3D models is a way to better understand geothermal systems [1].…”
Section: Introductionmentioning
confidence: 99%