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Copper and gold mineralization in the Maher-Abad deposit, eastern Iran, is closely related to the multiple emplacement episodes of Upper Eocene granodiorite porphyries within andesitic volcaniclastic and coeval quartz monzonite stocks. The magmatic hydrothermal fluids thereafter hydrofracturing provided appropriate conduits, formed a stockwork of quartz and quartz–sulfide veinlets within the porphyritic host rocks which were extensively altered into potassic, propylitic, phyllic, and argillic assemblages.

The Masjed Daghi mineralization is located 30 km southeast of Jolfa city at the bank of Araxes River, northwest Iran. This area is situated in the AlborzAzarbaijan structural zone of Iran. The most widespread rocks in the mineralization area are andesite and trachyandesite, while there are rock units of latite tuff, andesitic agglomerate, and hornblende porphyry basalt in eastern hills and Eocene flysch in the southern part of the area. Several intrusive bodies are present in the study area, from which the dominant intrusive rock hosting the mineralization is diorite porphyry.

The Sari Gunay epithermal gold deposit is located within a mildly alkaline latitic to trachytic volcanic complex in central-northwest Iran. Intrusive and volcanic rocks that host the deposit have been dated at between 11.7 and 11.0 Ma (with one younger sample at 8.0 Ma; 40Ar/39Ar dating of igneous biotite and hornblende), whereas sericitic alteration associated with an early stage of hydrothermal activity occurred between ~10.8 and ~10.3 Ma (the best age estimate is 10.7 Ma obtained by 40Ar/39Ar dating of sericite).

Обобщая геологоструктурные особенности двух участков (Веди-Ехегнадзор и Хой-Аваджик) можно заключить:
Исходя из сравнения стратиграфических данных участков Веди-Ехегнадзор и Хой-Аваджик можно предположить, что, по всей вероятности, до открытия северного Неотетиса в раннем мезозое эти единицы принадлежали Г'ондване.
Происхождение основных складчатых строений обусловлено обдукцией офиолитов на Южно Армянско-Хойском Микрконтиненте (ЮАХМ) и коллизией евразийской плиты в эпоху палеоцена- нижний эоцена далее коллизией Арабской и Евразийских плит, в эпоху верхнего эоцена-нижнего олигоцена которые вместе с более мелкими тектоническими сдвигами, а также с другими экзогенными (эрозия, крупномасштабные склоновые процессы и т. д.) процессами образовали современную сложную структуру изучаемых участков.

1. The Jurassic Badamu Formation in the Kerman Region with Remarks on the Jurassic Stratigraphy of Iran
2. Eocene Fish Remains from the Pabdeh Formation North of Ham
3. Upper Permian Corals from Julfa