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… Más…
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<
Dodax.de
Nr. 57dab0f2c38b050912b53bcc Gastos de envío:Versandkosten: 0.0 EUR, Lieferzeit: 6 Tage, DE. (EUR 0.00) Details...
(*) Libro agotado significa que este título no está disponible por el momento en alguna de las plataformas asociadas que buscamos.
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… Más…
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<
BookDepository.com
Gastos de envío:Versandkostenfrei. (EUR 0.00) Details...
(*) Libro agotado significa que este título no está disponible por el momento en alguna de las plataformas asociadas que buscamos.
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… Más…
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<
Dodax.de
Nr. 7CC12F06TNN. Gastos de envío:Versandkosten: 0 EUR, 11, zzgl. Versandkosten. (EUR 0.00) Details...
(*) Libro agotado significa que este título no está disponible por el momento en alguna de las plataformas asociadas que buscamos.
Abraham, Ema: Interpretation of Aeromagnetic Data for Geothermal Energy Investigation of Ikogosi Warm Spring Area, Ekiti State, Southwestern Nigeria - libro nuevo
Abraham, Ema: Interpretation of Aeromagnetic Data for Geothermal Energy Investigation of Ikogosi Warm Spring Area, Ekiti State, Southwestern Nigeria - libro nuevo
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… Más…
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 Gastos de envío: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… Más…
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… Más…
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. Gastos de envío: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 - libro nuevo
Abraham, Ema: Interpretation of Aeromagnetic Data for Geothermal Energy Investigation of Ikogosi Warm Spring Area, Ekiti State, Southwestern Nigeria - libro nuevo
1Dado que algunas plataformas no nos comunican las condiciones de envío y éstas pueden depender del país de entrega, del precio de compra, del peso y tamaño del artículo, de una posible membresía a la plataforma, de una entrega directa por parte de la plataforma o a través de un tercero (Marketplace), etc., es posible que los gastos de envío indicados por eurolibro/terralibro no concuerden con los de la plataforma ofertante.
Detalles del libro - Interpretation of Aeromagnetic Data for Geothermal Energy
EAN (ISBN-13): 9783659281204 ISBN (ISBN-10): 3659281204 Tapa blanda Año de publicación: 2012 Editorial: AV Akademikerverlag GmbH & Co. KG.
Libro en la base de datos desde 2014-10-10T02:29:14-05:00 (Mexico City) Página de detalles modificada por última vez el 2023-11-11T09:19:34-06:00 (Mexico City) ISBN/EAN: 9783659281204
ISBN - escritura alterna: 3-659-28120-4, 978-3-659-28120-4 Mode alterno de escritura y términos de búsqueda relacionados: Autor del libro: abraham Título del libro: ekiti, spring, area
