| Autor: |
Aboulela, Hamdy, Bantan, Rashad, Aboud, Essam, Almalki, Khalid A. |
| Předmět: |
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| Zdroj: |
Acta Geophysica; Aug2024, Vol. 72 Issue 4, p2391-2403, 13p |
| Abstrakt: |
The Red Sea had inimitable geological ancient times and is considered a new ocean basin model. It has many islands of numerous sizes in the southern sector and a widespread group of shoals, such as Farasan (Saudi Arabia) and Dahlak (Eretria), due to its geological setting differences. In this work, a group of applications was used to provide a wider vision of the potential field, as well as to image the thermal and subsurface structures of the study area (Farasan and Dahlak Islands) using available marine potential field datasets (marine gravity and magnetic) and topographic and bathymetric datasets. These datasets were downloaded from the GEOSOFT server (Data sources: http://dap.geosoft.com/). We applied different filters of the marine potential field datasets data (e.g., horizontal gradient filter) to create a subsurface structure image. The horizontal gradient technique was used to locate density edges/boundaries from gravity data. The basement depth was displayed, as it was required during the Curie depth estimation by means of mathematical formulas. The profile ~ 500 km in length was selected to cross the study area and its surroundings so as to perform the joint 2D inversion modeling process. The results showed that the Farasan Islands have a shallower Curie point depth and basement relief than Dahlak Islands, indicating that both island groups were not isolated from each other but molded and formed independently. The results revealed that the islands' different thermal systems were based on heat flow values calculated for each group. [ABSTRACT FROM AUTHOR] |
| Databáze: |
Complementary Index |
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