Curie Point Depth, Geothermal Gradient and Heat-Flow Estimation and Geothermal Anomaly Exploration from Integrated Analysis of Aeromagnetic and Gravity Data on the Sabalan Area, NW Iran

Author:

Afshar A.,Norouzi G. H.,Moradzadeh A.,Riahi M. A.,Porkhial S.

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Reference74 articles.

1. Aboud, E., Salem, A., & Mekkawi, M. (2011). Curie depth map for Sinai Peninsula, Egypt deduced from the analysis of magnetic data. Tectonophysics, 506(1), 46–54.

2. Alavi, M. (1994). Tectonics of the Zagros orogenic belt of Iran: New data and interpretations. Tectonophysics, 229(3), 211–238.

3. Amini. (1998). Meshkin Shahr geological map in scale of 1/100000. GSI, Iran.

4. Amirpour-asl, A., Ghods, A., Rezaeian, M., & Bahroudi, A. (2010). Depth of Curie temperature isotherm from aeromagnetic spectra in Iran: Tectonic implication, Tectonic crossroads: Evolving Orogens of Eurasia–Africa–Arabia, Ankara, Turkey.

5. Aydin, I., & Oksum, E. (2010). Exponential approach to estimate the Curie-temperature depth. Journal of Geophysics and Engineering, 7, 113–125.

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