Abstract:The Tell Atlas of Algeria has a huge potential for hydrothermal energy from over 240 thermal springs with temperatures up to $$98^\circ$$
98
∘
C in the Guelma area. The most exciting region is situated in the northeastern part which is known to have the hottest hydrothermal systems. In this work, we use a high-resolution gravity study to identify the location and origin of the hot water, and how it reaches the surfac… Show more
“…The third question is about mapping the structural lineaments (Ganguli and Pal; Sun et al) which is used widely in geological mapping (Altinoğlu, 2023;Ashraf and Filina, 2023;Bayou et al, 2023;Ibrahim et al, 2023;Lghoul et al, 2023;Mnasri et al, 2023;Qadir et al, 2023). Such applications are based on the qualitative interpretation of gravity anomalies in which the edge detection filters are usually applied to enhance the lineament.…”
Editorial on the Research Topic Applications of gravity anomalies in geophysicsWith the progress of cheap, lightweight, and efficient gravimeters (Carbone et al., 2020;Stray et al., 2022;Kim and Choi, 2023), gravity anomalies are expected to receive wider attention in the future, opening up new perspectives for increasing the capability of gravimetry to Earth sciences. Since the knowledge of the crustal density of a planet is important in determining its interior structure, gravity anomaly is widely used in Solid Earth and exploration geophysics, and also extended to the moon and Mars. In addition to the routine applications focusing on the crustal density structure, contributing to the characterization and definition of underground structures at various scales, time-varying gravity, microgravity survey, and gravity admittance are widely applied in order to supply unique information on the dynamics of underground processes. The goal of this Research Topic is to highlight the various extracted information from gravity anomalies in applications, toward an understanding of choosing appropriate methods dealing with gravity anomalies in varying study cases.There are ten accepted papers on this Research Topic focusing on the following four research questions.The first question is about the equivalent-layer technique (Oliveira Junior et al.) which present a comprehensive review of the computation aspects concerning the equivalent-layer technique. The equivalent-layer technique is used widely in processing gravity and magnetic anomalies, e.g., the downward continuation and the reduction to the pole at low latitudes. While such method is very inefficient for dealing with massive data sets, lots of computationally efficient methods have been proposed to reduce its computational cost. The authors from Observatório Nacional and Universidade do Estado do Rio de Janeiro (Brazil) present a comprehensive review of diverse strategies to solve the linear system of the equivalent layer in which the advantages and disadvantages for the existing strategies are described in detail.The second question is about the time-varying gravity (Zhu et al.) which is used in monitoring the subsurface mass variation. Zhu et al., from China Earthquake Administration, have conducted numerous applications focusing on the time-varying gravity in earthquake research in the Chinese Mainland. The gravity changes before
“…The third question is about mapping the structural lineaments (Ganguli and Pal; Sun et al) which is used widely in geological mapping (Altinoğlu, 2023;Ashraf and Filina, 2023;Bayou et al, 2023;Ibrahim et al, 2023;Lghoul et al, 2023;Mnasri et al, 2023;Qadir et al, 2023). Such applications are based on the qualitative interpretation of gravity anomalies in which the edge detection filters are usually applied to enhance the lineament.…”
Editorial on the Research Topic Applications of gravity anomalies in geophysicsWith the progress of cheap, lightweight, and efficient gravimeters (Carbone et al., 2020;Stray et al., 2022;Kim and Choi, 2023), gravity anomalies are expected to receive wider attention in the future, opening up new perspectives for increasing the capability of gravimetry to Earth sciences. Since the knowledge of the crustal density of a planet is important in determining its interior structure, gravity anomaly is widely used in Solid Earth and exploration geophysics, and also extended to the moon and Mars. In addition to the routine applications focusing on the crustal density structure, contributing to the characterization and definition of underground structures at various scales, time-varying gravity, microgravity survey, and gravity admittance are widely applied in order to supply unique information on the dynamics of underground processes. The goal of this Research Topic is to highlight the various extracted information from gravity anomalies in applications, toward an understanding of choosing appropriate methods dealing with gravity anomalies in varying study cases.There are ten accepted papers on this Research Topic focusing on the following four research questions.The first question is about the equivalent-layer technique (Oliveira Junior et al.) which present a comprehensive review of the computation aspects concerning the equivalent-layer technique. The equivalent-layer technique is used widely in processing gravity and magnetic anomalies, e.g., the downward continuation and the reduction to the pole at low latitudes. While such method is very inefficient for dealing with massive data sets, lots of computationally efficient methods have been proposed to reduce its computational cost. The authors from Observatório Nacional and Universidade do Estado do Rio de Janeiro (Brazil) present a comprehensive review of diverse strategies to solve the linear system of the equivalent layer in which the advantages and disadvantages for the existing strategies are described in detail.The second question is about the time-varying gravity (Zhu et al.) which is used in monitoring the subsurface mass variation. Zhu et al., from China Earthquake Administration, have conducted numerous applications focusing on the time-varying gravity in earthquake research in the Chinese Mainland. The gravity changes before
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