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iranian journal of earth sciences
سال:2018 - دوره:10 - شماره:1
geochemical evolution and petrogenesis of the eocene kashmar granitoid rocks, ne iran: implications for fractional crystallization and crustal contamination processes
- صفحه:68-77
geothermal conditions of hydrocarbon formation in the south caspian basin
- صفحه:78-89
influence of front row burden on fragmentation, muckpile shape, excavator cycle time, and back break in surface limestone mines
- صفحه:1-10
mineral chemistry and thermobarometry of eocene alkaline volcanic rocks in sw germi, nw iran
- صفحه:39-51
role of supra-subduction zone ophiolites in the tectonic evolution of the southeastern zagros orogenic belt, iran
- صفحه:31-38
tectonic evolution of the khoy ophiolitic complex, nw iran
- صفحه:20-30
using the results of cptu to identify the subsurface sediment layers in urmia lake bridge site, nw iran
- صفحه:52-67
variation of lithosphere-asthenosphere boundary beneath iran by using s receiver function
- صفحه:11-19
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