Fault type assessment based on vertical gravity gradient anomalies – advantages and limitations
Објеката
- Тип
- Рад у зборнику
- Верзија рада
- објављена
- Језик
- енглески
- Креатор
- Ivana Vasiljević, Snežana Ignjatović, Branislav Sretković
- Извор
- Vth Congress of the Geologists of the Republic of North Macedonia, Ohrid, Republic of North Macedonia, September 27-28, 2024
- Уредник
- Serafimovski, T., Boev, B.
- Издавач
- Macedonian Geological Society
- Датум издавања
- 2024
- Сажетак
- The type of dip-slip faults can be assessed based on the analysis of vertical gravity gradients. Theoretically, just a simple comparation of the gradient extreme values can give us an answer whether the fault is normal or reverse (thrust). Practical application of this method is far more complicated and the results depend on a number of parameters, such as a complexity of geological setting, the quality of gravity data, dip angle and displacement of the fault, density contrast, etc. Both the advantages and the limitations of the method based on using vertical gravity gradients for fault type determination are presented in the paper through the application on synthetic models and field example.
- почетак странице
- 86
- крај странице
- 90
- Subject
- dip-slip faults, vertical gravity gradients, field data analysis
- Шира категорија рада
- М30
- Ужа категорија рада
- М33
- Је дио
- Ministarstvo nauke, tehnološkog razvoja i inovacija Republike Srbije, ugovor br. 451-03-65/2024-03/200126
- Права
- Затворени приступ
- Лиценца
- All rights reserved
- Формат
Ivana Vasiljević, Snežana Ignjatović, Branislav Sretković. "Fault type assessment based on vertical gravity gradient anomalies – advantages and limitations" in Vth Congress of the Geologists of the Republic of North Macedonia, Ohrid, Republic of North Macedonia, September 27-28, 2024, Macedonian Geological Society (2024)
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