Geothermal reconnaissance of the area between Marsa Alam and Ras Banas, northern Red Sea, Egypt, using aeromagnetic data
Aeromagnetic data of the area between Marsa Alam and Ras Banas were interpreted to estimate the Curie point isotherm, investigate the geothermal gradient and to determine its surface heat flow. Appling spectral analysis and 2-D inverse modeling techniques to aeromagnetic anomalies has provided equit...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Saada, Saada A. [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2016transfer abstract |
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| Schlagwörter: |
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| Umfang: |
8 |
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| Übergeordnetes Werk: |
Enthalten in: Moving beyond the employee: The role of the organizational context in leader workplace aggression - Sharma, Payal Nangia ELSEVIER, 2017, Amsterdam [u.a.] |
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| Übergeordnetes Werk: |
volume:118 ; year:2016 ; pages:45-52 ; extent:8 |
| Links: |
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| DOI / URN: |
10.1016/j.jafrearsci.2016.02.014 |
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ELV024176036 |
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| 245 | 1 | 0 | |a Geothermal reconnaissance of the area between Marsa Alam and Ras Banas, northern Red Sea, Egypt, using aeromagnetic data |
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| 520 | |a Aeromagnetic data of the area between Marsa Alam and Ras Banas were interpreted to estimate the Curie point isotherm, investigate the geothermal gradient and to determine its surface heat flow. Appling spectral analysis and 2-D inverse modeling techniques to aeromagnetic anomalies has provided equitable promising geological results, useful to further geothermal exploration. Spectral analysis indicates that, the area is underlined by an average Curie-point depth of about 10.58 km. This implies an average thermal heat flow (137 mW/m2) greater than the average heat flow of the Red Sea margins (116 mW/m2). The investigated area was divided into three subregions and the average depth to centroid was estimated for each subregion. 2-D inverse modeling technique indicated that the magnetic sources can be interpreted by a set of dykes dipping to the NE and SW. The integration of radially power spectrum and 2-D inverse modeling was used to estimating the depths to the bottom of these magnetic bodies (equivalent to the Curie-point depth). It indicated a general decrease from 24 to 10 km from west to east toward the Red Sea rifting zone. The calculated surface heat flow increases from 55 mW/m2 to >150 mW/m2 in the same direction. Consequently, the offshore area between Ras Banas and Marsa Alam is a promising area for further exploration of geothermal resources. | ||
| 520 | |a Aeromagnetic data of the area between Marsa Alam and Ras Banas were interpreted to estimate the Curie point isotherm, investigate the geothermal gradient and to determine its surface heat flow. Appling spectral analysis and 2-D inverse modeling techniques to aeromagnetic anomalies has provided equitable promising geological results, useful to further geothermal exploration. Spectral analysis indicates that, the area is underlined by an average Curie-point depth of about 10.58 km. This implies an average thermal heat flow (137 mW/m2) greater than the average heat flow of the Red Sea margins (116 mW/m2). The investigated area was divided into three subregions and the average depth to centroid was estimated for each subregion. 2-D inverse modeling technique indicated that the magnetic sources can be interpreted by a set of dykes dipping to the NE and SW. The integration of radially power spectrum and 2-D inverse modeling was used to estimating the depths to the bottom of these magnetic bodies (equivalent to the Curie-point depth). It indicated a general decrease from 24 to 10 km from west to east toward the Red Sea rifting zone. The calculated surface heat flow increases from 55 mW/m2 to >150 mW/m2 in the same direction. Consequently, the offshore area between Ras Banas and Marsa Alam is a promising area for further exploration of geothermal resources. | ||
| 650 | 7 | |a Curie-point |2 Elsevier | |
| 650 | 7 | |a Geothermal gradient |2 Elsevier | |
| 650 | 7 | |a Magnetic |2 Elsevier | |
| 650 | 7 | |a Surface heat flow |2 Elsevier | |
| 650 | 7 | |a 2-D inverse modeling |2 Elsevier | |
| 650 | 7 | |a Power spectrum |2 Elsevier | |
| 773 | 0 | 8 | |i Enthalten in |n Elsevier Science |a Sharma, Payal Nangia ELSEVIER |t Moving beyond the employee: The role of the organizational context in leader workplace aggression |d 2017 |g Amsterdam [u.a.] |w (DE-627)ELV002200333 |
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10.1016/j.jafrearsci.2016.02.014 doi GBVA2016003000006.pica (DE-627)ELV024176036 (ELSEVIER)S1464-343X(16)30069-3 DE-627 ger DE-627 rakwb eng 550 550 DE-600 300 330 360 VZ 85.05 bkl 85.06 bkl 89.52 bkl Saada, Saada A. verfasserin aut Geothermal reconnaissance of the area between Marsa Alam and Ras Banas, northern Red Sea, Egypt, using aeromagnetic data 2016transfer abstract 8 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Aeromagnetic data of the area between Marsa Alam and Ras Banas were interpreted to estimate the Curie point isotherm, investigate the geothermal gradient and to determine its surface heat flow. Appling spectral analysis and 2-D inverse modeling techniques to aeromagnetic anomalies has provided equitable promising geological results, useful to further geothermal exploration. Spectral analysis indicates that, the area is underlined by an average Curie-point depth of about 10.58 km. This implies an average thermal heat flow (137 mW/m2) greater than the average heat flow of the Red Sea margins (116 mW/m2). The investigated area was divided into three subregions and the average depth to centroid was estimated for each subregion. 2-D inverse modeling technique indicated that the magnetic sources can be interpreted by a set of dykes dipping to the NE and SW. The integration of radially power spectrum and 2-D inverse modeling was used to estimating the depths to the bottom of these magnetic bodies (equivalent to the Curie-point depth). It indicated a general decrease from 24 to 10 km from west to east toward the Red Sea rifting zone. The calculated surface heat flow increases from 55 mW/m2 to >150 mW/m2 in the same direction. Consequently, the offshore area between Ras Banas and Marsa Alam is a promising area for further exploration of geothermal resources. Aeromagnetic data of the area between Marsa Alam and Ras Banas were interpreted to estimate the Curie point isotherm, investigate the geothermal gradient and to determine its surface heat flow. Appling spectral analysis and 2-D inverse modeling techniques to aeromagnetic anomalies has provided equitable promising geological results, useful to further geothermal exploration. Spectral analysis indicates that, the area is underlined by an average Curie-point depth of about 10.58 km. This implies an average thermal heat flow (137 mW/m2) greater than the average heat flow of the Red Sea margins (116 mW/m2). The investigated area was divided into three subregions and the average depth to centroid was estimated for each subregion. 2-D inverse modeling technique indicated that the magnetic sources can be interpreted by a set of dykes dipping to the NE and SW. The integration of radially power spectrum and 2-D inverse modeling was used to estimating the depths to the bottom of these magnetic bodies (equivalent to the Curie-point depth). It indicated a general decrease from 24 to 10 km from west to east toward the Red Sea rifting zone. The calculated surface heat flow increases from 55 mW/m2 to >150 mW/m2 in the same direction. Consequently, the offshore area between Ras Banas and Marsa Alam is a promising area for further exploration of geothermal resources. Curie-point Elsevier Geothermal gradient Elsevier Magnetic Elsevier Surface heat flow Elsevier 2-D inverse modeling Elsevier Power spectrum Elsevier Enthalten in Elsevier Science Sharma, Payal Nangia ELSEVIER Moving beyond the employee: The role of the organizational context in leader workplace aggression 2017 Amsterdam [u.a.] (DE-627)ELV002200333 volume:118 year:2016 pages:45-52 extent:8 https://doi.org/10.1016/j.jafrearsci.2016.02.014 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U 85.05 Betriebssoziologie Betriebspsychologie VZ 85.06 Unternehmensführung VZ 89.52 Politische Psychologie Politische Soziologie VZ AR 118 2016 45-52 8 045F 550 |
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10.1016/j.jafrearsci.2016.02.014 doi GBVA2016003000006.pica (DE-627)ELV024176036 (ELSEVIER)S1464-343X(16)30069-3 DE-627 ger DE-627 rakwb eng 550 550 DE-600 300 330 360 VZ 85.05 bkl 85.06 bkl 89.52 bkl Saada, Saada A. verfasserin aut Geothermal reconnaissance of the area between Marsa Alam and Ras Banas, northern Red Sea, Egypt, using aeromagnetic data 2016transfer abstract 8 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Aeromagnetic data of the area between Marsa Alam and Ras Banas were interpreted to estimate the Curie point isotherm, investigate the geothermal gradient and to determine its surface heat flow. Appling spectral analysis and 2-D inverse modeling techniques to aeromagnetic anomalies has provided equitable promising geological results, useful to further geothermal exploration. Spectral analysis indicates that, the area is underlined by an average Curie-point depth of about 10.58 km. This implies an average thermal heat flow (137 mW/m2) greater than the average heat flow of the Red Sea margins (116 mW/m2). The investigated area was divided into three subregions and the average depth to centroid was estimated for each subregion. 2-D inverse modeling technique indicated that the magnetic sources can be interpreted by a set of dykes dipping to the NE and SW. The integration of radially power spectrum and 2-D inverse modeling was used to estimating the depths to the bottom of these magnetic bodies (equivalent to the Curie-point depth). It indicated a general decrease from 24 to 10 km from west to east toward the Red Sea rifting zone. The calculated surface heat flow increases from 55 mW/m2 to >150 mW/m2 in the same direction. Consequently, the offshore area between Ras Banas and Marsa Alam is a promising area for further exploration of geothermal resources. Aeromagnetic data of the area between Marsa Alam and Ras Banas were interpreted to estimate the Curie point isotherm, investigate the geothermal gradient and to determine its surface heat flow. Appling spectral analysis and 2-D inverse modeling techniques to aeromagnetic anomalies has provided equitable promising geological results, useful to further geothermal exploration. Spectral analysis indicates that, the area is underlined by an average Curie-point depth of about 10.58 km. This implies an average thermal heat flow (137 mW/m2) greater than the average heat flow of the Red Sea margins (116 mW/m2). The investigated area was divided into three subregions and the average depth to centroid was estimated for each subregion. 2-D inverse modeling technique indicated that the magnetic sources can be interpreted by a set of dykes dipping to the NE and SW. The integration of radially power spectrum and 2-D inverse modeling was used to estimating the depths to the bottom of these magnetic bodies (equivalent to the Curie-point depth). It indicated a general decrease from 24 to 10 km from west to east toward the Red Sea rifting zone. The calculated surface heat flow increases from 55 mW/m2 to >150 mW/m2 in the same direction. Consequently, the offshore area between Ras Banas and Marsa Alam is a promising area for further exploration of geothermal resources. Curie-point Elsevier Geothermal gradient Elsevier Magnetic Elsevier Surface heat flow Elsevier 2-D inverse modeling Elsevier Power spectrum Elsevier Enthalten in Elsevier Science Sharma, Payal Nangia ELSEVIER Moving beyond the employee: The role of the organizational context in leader workplace aggression 2017 Amsterdam [u.a.] (DE-627)ELV002200333 volume:118 year:2016 pages:45-52 extent:8 https://doi.org/10.1016/j.jafrearsci.2016.02.014 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U 85.05 Betriebssoziologie Betriebspsychologie VZ 85.06 Unternehmensführung VZ 89.52 Politische Psychologie Politische Soziologie VZ AR 118 2016 45-52 8 045F 550 |
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10.1016/j.jafrearsci.2016.02.014 doi GBVA2016003000006.pica (DE-627)ELV024176036 (ELSEVIER)S1464-343X(16)30069-3 DE-627 ger DE-627 rakwb eng 550 550 DE-600 300 330 360 VZ 85.05 bkl 85.06 bkl 89.52 bkl Saada, Saada A. verfasserin aut Geothermal reconnaissance of the area between Marsa Alam and Ras Banas, northern Red Sea, Egypt, using aeromagnetic data 2016transfer abstract 8 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Aeromagnetic data of the area between Marsa Alam and Ras Banas were interpreted to estimate the Curie point isotherm, investigate the geothermal gradient and to determine its surface heat flow. Appling spectral analysis and 2-D inverse modeling techniques to aeromagnetic anomalies has provided equitable promising geological results, useful to further geothermal exploration. Spectral analysis indicates that, the area is underlined by an average Curie-point depth of about 10.58 km. This implies an average thermal heat flow (137 mW/m2) greater than the average heat flow of the Red Sea margins (116 mW/m2). The investigated area was divided into three subregions and the average depth to centroid was estimated for each subregion. 2-D inverse modeling technique indicated that the magnetic sources can be interpreted by a set of dykes dipping to the NE and SW. The integration of radially power spectrum and 2-D inverse modeling was used to estimating the depths to the bottom of these magnetic bodies (equivalent to the Curie-point depth). It indicated a general decrease from 24 to 10 km from west to east toward the Red Sea rifting zone. The calculated surface heat flow increases from 55 mW/m2 to >150 mW/m2 in the same direction. Consequently, the offshore area between Ras Banas and Marsa Alam is a promising area for further exploration of geothermal resources. Aeromagnetic data of the area between Marsa Alam and Ras Banas were interpreted to estimate the Curie point isotherm, investigate the geothermal gradient and to determine its surface heat flow. Appling spectral analysis and 2-D inverse modeling techniques to aeromagnetic anomalies has provided equitable promising geological results, useful to further geothermal exploration. Spectral analysis indicates that, the area is underlined by an average Curie-point depth of about 10.58 km. This implies an average thermal heat flow (137 mW/m2) greater than the average heat flow of the Red Sea margins (116 mW/m2). The investigated area was divided into three subregions and the average depth to centroid was estimated for each subregion. 2-D inverse modeling technique indicated that the magnetic sources can be interpreted by a set of dykes dipping to the NE and SW. The integration of radially power spectrum and 2-D inverse modeling was used to estimating the depths to the bottom of these magnetic bodies (equivalent to the Curie-point depth). It indicated a general decrease from 24 to 10 km from west to east toward the Red Sea rifting zone. The calculated surface heat flow increases from 55 mW/m2 to >150 mW/m2 in the same direction. Consequently, the offshore area between Ras Banas and Marsa Alam is a promising area for further exploration of geothermal resources. Curie-point Elsevier Geothermal gradient Elsevier Magnetic Elsevier Surface heat flow Elsevier 2-D inverse modeling Elsevier Power spectrum Elsevier Enthalten in Elsevier Science Sharma, Payal Nangia ELSEVIER Moving beyond the employee: The role of the organizational context in leader workplace aggression 2017 Amsterdam [u.a.] (DE-627)ELV002200333 volume:118 year:2016 pages:45-52 extent:8 https://doi.org/10.1016/j.jafrearsci.2016.02.014 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U 85.05 Betriebssoziologie Betriebspsychologie VZ 85.06 Unternehmensführung VZ 89.52 Politische Psychologie Politische Soziologie VZ AR 118 2016 45-52 8 045F 550 |
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10.1016/j.jafrearsci.2016.02.014 doi GBVA2016003000006.pica (DE-627)ELV024176036 (ELSEVIER)S1464-343X(16)30069-3 DE-627 ger DE-627 rakwb eng 550 550 DE-600 300 330 360 VZ 85.05 bkl 85.06 bkl 89.52 bkl Saada, Saada A. verfasserin aut Geothermal reconnaissance of the area between Marsa Alam and Ras Banas, northern Red Sea, Egypt, using aeromagnetic data 2016transfer abstract 8 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Aeromagnetic data of the area between Marsa Alam and Ras Banas were interpreted to estimate the Curie point isotherm, investigate the geothermal gradient and to determine its surface heat flow. Appling spectral analysis and 2-D inverse modeling techniques to aeromagnetic anomalies has provided equitable promising geological results, useful to further geothermal exploration. Spectral analysis indicates that, the area is underlined by an average Curie-point depth of about 10.58 km. This implies an average thermal heat flow (137 mW/m2) greater than the average heat flow of the Red Sea margins (116 mW/m2). The investigated area was divided into three subregions and the average depth to centroid was estimated for each subregion. 2-D inverse modeling technique indicated that the magnetic sources can be interpreted by a set of dykes dipping to the NE and SW. The integration of radially power spectrum and 2-D inverse modeling was used to estimating the depths to the bottom of these magnetic bodies (equivalent to the Curie-point depth). It indicated a general decrease from 24 to 10 km from west to east toward the Red Sea rifting zone. The calculated surface heat flow increases from 55 mW/m2 to >150 mW/m2 in the same direction. Consequently, the offshore area between Ras Banas and Marsa Alam is a promising area for further exploration of geothermal resources. Aeromagnetic data of the area between Marsa Alam and Ras Banas were interpreted to estimate the Curie point isotherm, investigate the geothermal gradient and to determine its surface heat flow. Appling spectral analysis and 2-D inverse modeling techniques to aeromagnetic anomalies has provided equitable promising geological results, useful to further geothermal exploration. Spectral analysis indicates that, the area is underlined by an average Curie-point depth of about 10.58 km. This implies an average thermal heat flow (137 mW/m2) greater than the average heat flow of the Red Sea margins (116 mW/m2). The investigated area was divided into three subregions and the average depth to centroid was estimated for each subregion. 2-D inverse modeling technique indicated that the magnetic sources can be interpreted by a set of dykes dipping to the NE and SW. The integration of radially power spectrum and 2-D inverse modeling was used to estimating the depths to the bottom of these magnetic bodies (equivalent to the Curie-point depth). It indicated a general decrease from 24 to 10 km from west to east toward the Red Sea rifting zone. The calculated surface heat flow increases from 55 mW/m2 to >150 mW/m2 in the same direction. Consequently, the offshore area between Ras Banas and Marsa Alam is a promising area for further exploration of geothermal resources. Curie-point Elsevier Geothermal gradient Elsevier Magnetic Elsevier Surface heat flow Elsevier 2-D inverse modeling Elsevier Power spectrum Elsevier Enthalten in Elsevier Science Sharma, Payal Nangia ELSEVIER Moving beyond the employee: The role of the organizational context in leader workplace aggression 2017 Amsterdam [u.a.] (DE-627)ELV002200333 volume:118 year:2016 pages:45-52 extent:8 https://doi.org/10.1016/j.jafrearsci.2016.02.014 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U 85.05 Betriebssoziologie Betriebspsychologie VZ 85.06 Unternehmensführung VZ 89.52 Politische Psychologie Politische Soziologie VZ AR 118 2016 45-52 8 045F 550 |
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10.1016/j.jafrearsci.2016.02.014 doi GBVA2016003000006.pica (DE-627)ELV024176036 (ELSEVIER)S1464-343X(16)30069-3 DE-627 ger DE-627 rakwb eng 550 550 DE-600 300 330 360 VZ 85.05 bkl 85.06 bkl 89.52 bkl Saada, Saada A. verfasserin aut Geothermal reconnaissance of the area between Marsa Alam and Ras Banas, northern Red Sea, Egypt, using aeromagnetic data 2016transfer abstract 8 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Aeromagnetic data of the area between Marsa Alam and Ras Banas were interpreted to estimate the Curie point isotherm, investigate the geothermal gradient and to determine its surface heat flow. Appling spectral analysis and 2-D inverse modeling techniques to aeromagnetic anomalies has provided equitable promising geological results, useful to further geothermal exploration. Spectral analysis indicates that, the area is underlined by an average Curie-point depth of about 10.58 km. This implies an average thermal heat flow (137 mW/m2) greater than the average heat flow of the Red Sea margins (116 mW/m2). The investigated area was divided into three subregions and the average depth to centroid was estimated for each subregion. 2-D inverse modeling technique indicated that the magnetic sources can be interpreted by a set of dykes dipping to the NE and SW. The integration of radially power spectrum and 2-D inverse modeling was used to estimating the depths to the bottom of these magnetic bodies (equivalent to the Curie-point depth). It indicated a general decrease from 24 to 10 km from west to east toward the Red Sea rifting zone. The calculated surface heat flow increases from 55 mW/m2 to >150 mW/m2 in the same direction. Consequently, the offshore area between Ras Banas and Marsa Alam is a promising area for further exploration of geothermal resources. Aeromagnetic data of the area between Marsa Alam and Ras Banas were interpreted to estimate the Curie point isotherm, investigate the geothermal gradient and to determine its surface heat flow. Appling spectral analysis and 2-D inverse modeling techniques to aeromagnetic anomalies has provided equitable promising geological results, useful to further geothermal exploration. Spectral analysis indicates that, the area is underlined by an average Curie-point depth of about 10.58 km. This implies an average thermal heat flow (137 mW/m2) greater than the average heat flow of the Red Sea margins (116 mW/m2). The investigated area was divided into three subregions and the average depth to centroid was estimated for each subregion. 2-D inverse modeling technique indicated that the magnetic sources can be interpreted by a set of dykes dipping to the NE and SW. The integration of radially power spectrum and 2-D inverse modeling was used to estimating the depths to the bottom of these magnetic bodies (equivalent to the Curie-point depth). It indicated a general decrease from 24 to 10 km from west to east toward the Red Sea rifting zone. The calculated surface heat flow increases from 55 mW/m2 to >150 mW/m2 in the same direction. Consequently, the offshore area between Ras Banas and Marsa Alam is a promising area for further exploration of geothermal resources. Curie-point Elsevier Geothermal gradient Elsevier Magnetic Elsevier Surface heat flow Elsevier 2-D inverse modeling Elsevier Power spectrum Elsevier Enthalten in Elsevier Science Sharma, Payal Nangia ELSEVIER Moving beyond the employee: The role of the organizational context in leader workplace aggression 2017 Amsterdam [u.a.] (DE-627)ELV002200333 volume:118 year:2016 pages:45-52 extent:8 https://doi.org/10.1016/j.jafrearsci.2016.02.014 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U 85.05 Betriebssoziologie Betriebspsychologie VZ 85.06 Unternehmensführung VZ 89.52 Politische Psychologie Politische Soziologie VZ AR 118 2016 45-52 8 045F 550 |
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Geothermal reconnaissance of the area between Marsa Alam and Ras Banas, northern Red Sea, Egypt, using aeromagnetic data |
| abstract |
Aeromagnetic data of the area between Marsa Alam and Ras Banas were interpreted to estimate the Curie point isotherm, investigate the geothermal gradient and to determine its surface heat flow. Appling spectral analysis and 2-D inverse modeling techniques to aeromagnetic anomalies has provided equitable promising geological results, useful to further geothermal exploration. Spectral analysis indicates that, the area is underlined by an average Curie-point depth of about 10.58 km. This implies an average thermal heat flow (137 mW/m2) greater than the average heat flow of the Red Sea margins (116 mW/m2). The investigated area was divided into three subregions and the average depth to centroid was estimated for each subregion. 2-D inverse modeling technique indicated that the magnetic sources can be interpreted by a set of dykes dipping to the NE and SW. The integration of radially power spectrum and 2-D inverse modeling was used to estimating the depths to the bottom of these magnetic bodies (equivalent to the Curie-point depth). It indicated a general decrease from 24 to 10 km from west to east toward the Red Sea rifting zone. The calculated surface heat flow increases from 55 mW/m2 to >150 mW/m2 in the same direction. Consequently, the offshore area between Ras Banas and Marsa Alam is a promising area for further exploration of geothermal resources. |
| abstractGer |
Aeromagnetic data of the area between Marsa Alam and Ras Banas were interpreted to estimate the Curie point isotherm, investigate the geothermal gradient and to determine its surface heat flow. Appling spectral analysis and 2-D inverse modeling techniques to aeromagnetic anomalies has provided equitable promising geological results, useful to further geothermal exploration. Spectral analysis indicates that, the area is underlined by an average Curie-point depth of about 10.58 km. This implies an average thermal heat flow (137 mW/m2) greater than the average heat flow of the Red Sea margins (116 mW/m2). The investigated area was divided into three subregions and the average depth to centroid was estimated for each subregion. 2-D inverse modeling technique indicated that the magnetic sources can be interpreted by a set of dykes dipping to the NE and SW. The integration of radially power spectrum and 2-D inverse modeling was used to estimating the depths to the bottom of these magnetic bodies (equivalent to the Curie-point depth). It indicated a general decrease from 24 to 10 km from west to east toward the Red Sea rifting zone. The calculated surface heat flow increases from 55 mW/m2 to >150 mW/m2 in the same direction. Consequently, the offshore area between Ras Banas and Marsa Alam is a promising area for further exploration of geothermal resources. |
| abstract_unstemmed |
Aeromagnetic data of the area between Marsa Alam and Ras Banas were interpreted to estimate the Curie point isotherm, investigate the geothermal gradient and to determine its surface heat flow. Appling spectral analysis and 2-D inverse modeling techniques to aeromagnetic anomalies has provided equitable promising geological results, useful to further geothermal exploration. Spectral analysis indicates that, the area is underlined by an average Curie-point depth of about 10.58 km. This implies an average thermal heat flow (137 mW/m2) greater than the average heat flow of the Red Sea margins (116 mW/m2). The investigated area was divided into three subregions and the average depth to centroid was estimated for each subregion. 2-D inverse modeling technique indicated that the magnetic sources can be interpreted by a set of dykes dipping to the NE and SW. The integration of radially power spectrum and 2-D inverse modeling was used to estimating the depths to the bottom of these magnetic bodies (equivalent to the Curie-point depth). It indicated a general decrease from 24 to 10 km from west to east toward the Red Sea rifting zone. The calculated surface heat flow increases from 55 mW/m2 to >150 mW/m2 in the same direction. Consequently, the offshore area between Ras Banas and Marsa Alam is a promising area for further exploration of geothermal resources. |
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