| dc.creator |
Afşin, Mustafa |
|
| dc.creator |
Davraz, Ayşen |
|
| dc.creator |
Maden, Nafız |
|
| dc.creator |
Aksever, Fatma |
|
| dc.date |
2019-12-31T21:00:00Z |
|
| dc.date.accessioned |
2020-10-06T11:50:02Z |
|
| dc.date.available |
2020-10-06T11:50:02Z |
|
| dc.identifier |
ed95141e-ac95-469a-bc07-62b885ec80b7 |
|
| dc.identifier |
https://avesis.sdu.edu.tr/publication/details/ed95141e-ac95-469a-bc07-62b885ec80b7/oai |
|
| dc.identifier.uri |
http://acikerisim.sdu.edu.tr/xmlui/handle/123456789/75506 |
|
| dc.description |
<p>significant geothermal energy source field. The analysis of power spectrum,</p><p>conventional heat flow and silica heat flow methods were implemented to</p><p>identify the geothermal waters circulation depth, depth to Curie point and surface</p><p>heat flow rate in the Hüdai-Sandıklı geothermal field. Hydrogeochemical facies of</p><p>geothermal immature ancient waters having deep circulation in lower hydraulic</p><p>conductive aquifers are Na–Ca–HCO3–SO4 and Na–Ca–SO4–HCO3, which is</p><p>represented very high ion content because of extensive contact with rocks. The heat</p><p>conduction law is employed to specify the rate of heat flow using the geothermal</p><p>gradient value. The numerical results determined from silica geothermometer</p><p>method, the mean heat flow density and Curie temperature depth are obtained as</p><p>103:69mWm2 and 11.81 km, respectively. The study region was represented by a</p><p>mean geothermal gradient of 49.18 °C km−1 yielding average reservoir depths of</p><p>0.90 km. The estimated Curie temperature, heat flow, reservoir temperature values</p><p>demonstrated that the region indicates significant geothermal energy potential</p><p>because of the partial melting of lithospheric crust.</p> |
|
| dc.language |
eng |
|
| dc.rights |
info:eu-repo/semantics/closedAccess |
|
| dc.title |
Advances in Modeling and Interpretation in Near Surface Geophysics |
|
| dc.type |
info:eu-repo/semantics/bookPart |
|