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Effect of tectonic-climatic controllers on the transition of Endorheic to Exorheic Basins in the Zagros mountain range

引用

Journal of Mountain Science 2023年第12期20卷 3500-3524页

作者： gholam hassan jafari Peyman MOHAMMADI-AHMADMAHMOUDI Mohsen EHTESHAMI-MOINABADI Department of Geomorphology University of ZanjanZanjan ***Iran Department of Physical Geography Faculty of Earth SciencesShahid Beheshti UniversityTehran ***Iran Department of Sedimentary Basins and Petroleum Faculty of Earth SciencesShahid Beheshti UniversityTehran ***Iran

Endorheic basins(ENBs) are inland drainage basins allowing no outflow to *** basins in the active mountain chains of the convergence zones are under the influence of compressional tectonic activity and climate *** Zagros Mountains of Iran is one of the youngest convergence zones in which continental-continental collision has *** this paper we hypothesize the formation of ENBs among the Zagros range after the epeirogenic stage in the Late Paleogene-Early *** to tectonic activity and Quaternary climatic conditions,the ENBs pass the transition stage to exorheic,and still,some tectonic depressions are not linked to the evolutionary process of exorheic drainage of *** geometry of the drainage network of Kul and Mond basins in Fars arch shows that 67% of their water gaps are located along the thrusts and transverse basement faults in the east and west of the Fars ***,the Kul and Mond basins form triangles with their sides matching with the edges of the Arabian Plate where the major inherited faults of Arabian plate controls the shape of the Zagros basin and a low strain zone along the Razak fault with lower salt tectonic activity,where the wind gaps are *** ENBs are located in the rainshadow slopes,but the Kul and Mond basins are located in the upwind slopes of rain *** factor and the heavy rains of the basin lead to increase of the erosion potential,destruction of depressions,and floods and consequently,the funnel-shaped gaps have a significant impact on the flood flow.

关键词： Transition of landforms Controllers of lakes Basement faults Sedimentary basins Zagros

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