Audio-Magnetotelluric Modeling for 2D Characterization of Shallow Sedimentary Basins and Groundwater System in Central Zagros, Iran
Author:
Funder
Iran Office of Vice-presidency for Science and Technology, Office of Drought, Erosion and Environmental Affairs
Publisher
Springer Science and Business Media LLC
Subject
Geochemistry and Petrology,Geophysics
Link
https://link.springer.com/content/pdf/10.1007/s00024-022-03181-y.pdf
Reference49 articles.
1. Ahmadhadi, F., Lacombe, O., & Marc Daniel, J. (2007). Early Reactivation of Basement Faults in Central Zagros (SW Iran), Evidence from Pre-Folding Fracture Populations in Asmari Formation and Lower Tertiary Paleogeography. In: Lacombe, O., Lave, J., Roure, F., Verges, J. (Eds), Thrust Belts and Foreland Basins (pp. 205–228). Springer. http://dx.doi.org/https://doi.org/10.1007/978-3-540-69426-7_11.
2. Asaue, H., Kubo, T., Yoshinaga, T., & Koike, K. (2012). Application of magnetotelluric (MT) resistivity to imaging of regional three-dimensional geologic structures and groundwater systems. Natural Resources Research, 21(3), 383–393. https://doi.org/10.1007/s11053-012-9184-2
3. Beamish, D., & Travassos, J. M. (1992). The use of the D+ solution in magnetotelluric interpretation. Journal of Applied Geophysics, 29, 1–19.
4. Bense, V. F., Gleeson, T., Loveless, S. E., Bour, O., & Scibek, J. (2013). Fault Zone Hydrogeology. Earth Sciences Review, 127, 171–192.
5. Berberian, M. (1995). Master blind thrust faults hidden under the Zagros folds: Active basement tectonics and surface morphotectonics. Tectonophysics, 241, 193–224.
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