Spatial and temporal changes of b-value, fractal analysis and stress tensor inversion in the Sistan and Makran zones, Eastern and Southeastern Iran

Author:

Sabahi MahnazORCID,Mahdi Khatib Mohammad,Djamour Yahya

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geology

Reference88 articles.

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2. Maximum likelihood estimate of b in the formula logN= a-bM and its confidence limits;Aki;Bull. Earthquake Res. Inst. Univ. Tokyo,1965

3. Angelier, J. (1991). Inversion directe et recherche 4-D: comparaison physique et mathématique de deux modes de détermination des tenseurs des paléocontraintes en tectonique de failles. Comptes rendus de l'Académie des sciences. Série 2, Mécanique, Physique, Chimie, Sciences de l'univers, Sciences de la Terre, 312(10), 1213-1218.

4. Insights on deep, accretionary subduction processes from the Sistan ophiolitic “mélange”(Eastern Iran);Angiboust;Lithos,2013

5. Active accommodation of plate convergence in Southern Iran: Earthquake locations, triggered aseismic slip, and regional strain rates;Barnhart;Journal of Geophysical Research: Solid Earth,2013

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