1887
PDF

Abstract

Summary

Understanding fault and damage zone network is of upmost importance in geothermal exploration projects. While doing basin scale analysis of the discontinuity screening, it is important to focus on the faults that can be heat/fluid pathways for the geothermal purposes. This research paper describes approaches of tilt derivative interpretation of bandpass-filtered Complete Bouguer anomaly data of Ukrainian Carpathian Foredeep. The purpose of such analysis is to identify faults in the reservoir section that are potential pathways for geothermal systems. Further analysis of fault permeability is required and will be performed for the purpose of understanding geothermal potential of Ukrainian Carpathian Foredeep

Loading

Article metrics loading...

/content/papers/10.3997/2214-4609.2025510168
2025-04-14
2026-02-08
Loading full text...

Full text loading...

/deliver/fulltext/2214-4609/2025/monitoring_2025/Mon25-168.html?itemId=/content/papers/10.3997/2214-4609.2025510168&mimeType=html&fmt=ahah

References

  1. Akın, U. & Şerifoğlu, B. & Duru, M. (2011). The use of tilt angle in gravity and magnetic methods. Mineral Res. Expl. Bull. 143. 1–12
    [Google Scholar]
  2. Al-Banna, A. & Daim, F & Al-Zubaidi, A. (2017). The Deep Faults in Kut-Hai and Surrounding Area Inferred From Gravity and Magnetic Data Iraqi Journal of Science.
    [Google Scholar]
  3. Handayani, L. (2019). Active Fault Zones of The 2006 Yogyakarta Earthquake Inferred from Tilt Derivative Analysis of Gravity Anomalies. RISET Geologi dan Pertambangan. 29. 1. 10.14203/risetgeotam2019.v29.1018.
    https://doi.org/10.14203/risetgeotam2019.v29.1018 [Google Scholar]
  4. Hursky, D.S., Kalinin, V.I. (2007). Geological Map Pre-Cenozoic Formations of Ukraine, State Geological Service.
    [Google Scholar]
  5. Nasuti, A., Pascal, C, Ebbing, J. (2012). Onshore-offshore potential field analysis of the Møre-Trøndelag Fault Complex and adjacent structures of Mid Norway. Tectonophysics 518–521, 17–28. DOI:10.1016/j.tecto.2011.11.003
    https://doi.org/10.1016/j.tecto.2011.11.003 [Google Scholar]
  6. PetrokushynR., BezrodnyiD. (2024). Edge Detection Methods For Fault Delineation Using Potential Field Data. XIV Ukrainian Young Researchers Conference “Modern Problems of the Earth Sciences”
    [Google Scholar]
  7. Saad, A. H. (2006). Understanding gravity gradients—a tutorial. Lead. Edge25, 942–949. DOI:10.1190/1.2335167
    https://doi.org/10.1190/1.2335167 [Google Scholar]
  8. Syamsu, R., ClaudiyaA. (2020). Tilt angle analysis of gravity data to identify geothermal heat source in Mt. Lawu field. AIP Conf. Proc.2296 (1): 020036.
    [Google Scholar]
  9. Verduzco, B., Fairhead, J. D., MacKenzie, C. (2004). New insights into magnetic derivatives for structural mapping. Lead.Edge23, 116–119
    [Google Scholar]
  10. Zucchi, M. (2020). Faults controlling geothermal fluid flow in low permeability rock volumes: An example from the exhumed geothermal system of eastern Elba Island (northern Tyrrhenian Sea, Italy). Geothermics, ISSN 0375-6505, https://doi.org/10.1016/j.geothermics.2019.101765
    [Google Scholar]
/content/papers/10.3997/2214-4609.2025510168
Loading
/content/papers/10.3997/2214-4609.2025510168
Loading

Data & Media loading...

This is a required field
Please enter a valid email address
Approval was a Success
Invalid data
An Error Occurred
Approval was partially successful, following selected items could not be processed due to error