Fluid Evolution of the Magmatic Hydrothermal Porphyry Copper Deposit Based on Fluid Inclusion and Stable Isotope Studies at Darrehzar, Iran

<table>(a) Geological map of Iran (7 and 20) showing Sahand-Bazman belt: calc-alkaline volcanic and quartz-monzonite and quartz diorite intrusions, hosting Cu-Mo-porphyry-type mineralization and (b) detailed geological map of the Darrehzar area showing the distribution of different sites.</table>

International Scholarly Research Notices

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Figure 1: Fluid Evolution of the Magmatic Hydrothermal Porphyry Copper Deposit Based on Fluid Inclusion and Stable Isotope Studies at Darrehzar, Iran 

Figure 1 | Fluid Evolution of the Magmatic Hydrothermal Porphyry Copper Deposit Based on Fluid Inclusion and Stable Isotope Studies at Darrehzar, Iran 