The thermal structure of the crust at Ikogosi Warm Spring area is examined using Curie Point Depth (CPD) estimates from spectral analysis of aeromagnetic data. The CPD values from 22 slid… Altro …
The thermal structure of the crust at Ikogosi Warm Spring area is examined using Curie Point Depth (CPD) estimates from spectral analysis of aeromagnetic data. The CPD values from 22 sliding overlapping blocks, 55 x 55 km in size, are estimated from the data. The slope of the longest wavelength part of the radially averaged log power spectrum divided by the radial frequency produced the depth to the centroid (zo) for the deepest crustal block. The depth to the top (zt) is obtained by the slope of the second longest wavelength part of the spectrum. From these depths, the CPD is calculated by using zb = 2zo - zt. The average CPD estimates for the Ikogosi Warm Spring area is 5.8 km. Corresponding heat-flow and thermal gradient values are calculated from the CPD estimates. The shallow CPD observed at the warm spring area explains the thermal source of the Ikogosi Warm Spring. Interpretation of aeromagnetic data indicates that the warm spring source is structurally controlled. Generally, the results indicate that the area is promising for further geothermal explorations. Bücher / Naturwissenschaften, Medizin, Informatik & Technik / Geowissenschaften<
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Paperback, [PU: LAP LAMBERT Academic Publishing], The thermal structure of the crust at Ikogosi Warm Spring area is examined using Curie Point Depth (CPD) estimates from spectral analysis… Altro …
Paperback, [PU: LAP LAMBERT Academic Publishing], The thermal structure of the crust at Ikogosi Warm Spring area is examined using Curie Point Depth (CPD) estimates from spectral analysis of aeromagnetic data. The CPD values from 22 sliding overlapping blocks, 55 x 55 km in size, are estimated from the data. The slope of the longest wavelength part of the radially averaged log power spectrum divided by the radial frequency produced the depth to the centroid (zo) for the deepest crustal block. The depth to the top (zt) is obtained by the slope of the second longest wavelength part of the spectrum. From these depths, the CPD is calculated by using zb = 2zo - zt. The average CPD estimates for the Ikogosi Warm Spring area is 5.8 km. Corresponding heat-flow and thermal gradient values are calculated from the CPD estimates. The shallow CPD observed at the warm spring area explains the thermal source of the Ikogosi Warm Spring. Interpretation of aeromagnetic data indicates that the warm spring source is structurally controlled. Generally, the results indicate that the area is promising for further geothermal explorations., Earth Sciences<
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The thermal structure of the crust at Ikogosi Warm Spring area is examined using Curie Point Depth (CPD) estimates from spectral analysis of aeromagnetic data. The CPD values from 22 slid… Altro …
The thermal structure of the crust at Ikogosi Warm Spring area is examined using Curie Point Depth (CPD) estimates from spectral analysis of aeromagnetic data. The CPD values from 22 sliding overlapping blocks, 55 x 55 km in size, are estimated from the data. The slope of the longest wavelength part of the radially averaged log power spectrum divided by the radial frequency produced the depth to the centroid (zo) for the deepest crustal block. The depth to the top (zt) is obtained by the slope of the second longest wavelength part of the spectrum. From these depths, the CPD is calculated by using zb = 2zo - zt. The average CPD estimates for the Ikogosi Warm Spring area is 5.8 km. Corresponding heat-flow and thermal gradient values are calculated from the CPD estimates. The shallow CPD observed at the warm spring area explains the thermal source of the Ikogosi Warm Spring. Interpretation of aeromagnetic data indicates that the warm spring source is structurally controlled. Generally, the results indicate that the area is promising for further geothermal explorations. Bücher / Naturwissenschaften, Medizin, Informatik & Technik / Geowissenschaften<
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Abraham, Ema: Interpretation of Aeromagnetic Data for Geothermal Energy Investigation of Ikogosi Warm Spring Area, Ekiti State, Southwestern Nigeria - nuovo libro
Abraham, Ema: Interpretation of Aeromagnetic Data for Geothermal Energy Investigation of Ikogosi Warm Spring Area, Ekiti State, Southwestern Nigeria - nuovo libro
The thermal structure of the crust at Ikogosi Warm Spring area is examined using Curie Point Depth (CPD) estimates from spectral analysis of aeromagnetic data. The CPD values from 22 slid… Altro …
The thermal structure of the crust at Ikogosi Warm Spring area is examined using Curie Point Depth (CPD) estimates from spectral analysis of aeromagnetic data. The CPD values from 22 sliding overlapping blocks, 55 x 55 km in size, are estimated from the data. The slope of the longest wavelength part of the radially averaged log power spectrum divided by the radial frequency produced the depth to the centroid (zo) for the deepest crustal block. The depth to the top (zt) is obtained by the slope of the second longest wavelength part of the spectrum. From these depths, the CPD is calculated by using zb = 2zo - zt. The average CPD estimates for the Ikogosi Warm Spring area is 5.8 km. Corresponding heat-flow and thermal gradient values are calculated from the CPD estimates. The shallow CPD observed at the warm spring area explains the thermal source of the Ikogosi Warm Spring. Interpretation of aeromagnetic data indicates that the warm spring source is structurally controlled. Generally, the results indicate that the area is promising for further geothermal explorations. Bücher / Naturwissenschaften, Medizin, Informatik & Technik / Geowissenschaften<
- Nr. 57dab0f2c38b050912b53bcc Costi di spedizione:Versandkosten: 0.0 EUR, Lieferzeit: 6 Tage, DE. (EUR 0.00)
Paperback, [PU: LAP LAMBERT Academic Publishing], The thermal structure of the crust at Ikogosi Warm Spring area is examined using Curie Point Depth (CPD) estimates from spectral analysis… Altro …
Paperback, [PU: LAP LAMBERT Academic Publishing], The thermal structure of the crust at Ikogosi Warm Spring area is examined using Curie Point Depth (CPD) estimates from spectral analysis of aeromagnetic data. The CPD values from 22 sliding overlapping blocks, 55 x 55 km in size, are estimated from the data. The slope of the longest wavelength part of the radially averaged log power spectrum divided by the radial frequency produced the depth to the centroid (zo) for the deepest crustal block. The depth to the top (zt) is obtained by the slope of the second longest wavelength part of the spectrum. From these depths, the CPD is calculated by using zb = 2zo - zt. The average CPD estimates for the Ikogosi Warm Spring area is 5.8 km. Corresponding heat-flow and thermal gradient values are calculated from the CPD estimates. The shallow CPD observed at the warm spring area explains the thermal source of the Ikogosi Warm Spring. Interpretation of aeromagnetic data indicates that the warm spring source is structurally controlled. Generally, the results indicate that the area is promising for further geothermal explorations., Earth Sciences<
The thermal structure of the crust at Ikogosi Warm Spring area is examined using Curie Point Depth (CPD) estimates from spectral analysis of aeromagnetic data. The CPD values from 22 slid… Altro …
The thermal structure of the crust at Ikogosi Warm Spring area is examined using Curie Point Depth (CPD) estimates from spectral analysis of aeromagnetic data. The CPD values from 22 sliding overlapping blocks, 55 x 55 km in size, are estimated from the data. The slope of the longest wavelength part of the radially averaged log power spectrum divided by the radial frequency produced the depth to the centroid (zo) for the deepest crustal block. The depth to the top (zt) is obtained by the slope of the second longest wavelength part of the spectrum. From these depths, the CPD is calculated by using zb = 2zo - zt. The average CPD estimates for the Ikogosi Warm Spring area is 5.8 km. Corresponding heat-flow and thermal gradient values are calculated from the CPD estimates. The shallow CPD observed at the warm spring area explains the thermal source of the Ikogosi Warm Spring. Interpretation of aeromagnetic data indicates that the warm spring source is structurally controlled. Generally, the results indicate that the area is promising for further geothermal explorations. Bücher / Naturwissenschaften, Medizin, Informatik & Technik / Geowissenschaften<
- Nr. 7CC12F06TNN. Costi di spedizione:Versandkosten: 0 EUR, 11, zzgl. Versandkosten. (EUR 0.00)
Abraham, Ema: Interpretation of Aeromagnetic Data for Geothermal Energy Investigation of Ikogosi Warm Spring Area, Ekiti State, Southwestern Nigeria - nuovo libro
Abraham, Ema: Interpretation of Aeromagnetic Data for Geothermal Energy Investigation of Ikogosi Warm Spring Area, Ekiti State, Southwestern Nigeria - nuovo libro
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Informazioni dettagliate del libro - Interpretation of Aeromagnetic Data for Geothermal Energy
EAN (ISBN-13): 9783659281204 ISBN (ISBN-10): 3659281204 Copertina flessibile Anno di pubblicazione: 2012 Editore: AV Akademikerverlag GmbH & Co. KG.
Libro nella banca dati dal 2014-10-10T09:29:14+02:00 (Zurich) Pagina di dettaglio ultima modifica in 2023-11-11T16:19:34+01:00 (Zurich) ISBN/EAN: 9783659281204
ISBN - Stili di scrittura alternativi: 3-659-28120-4, 978-3-659-28120-4 Stili di scrittura alternativi e concetti di ricerca simili: Autore del libro : abraham Titolo del libro: ekiti, spring, area
