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Synthesis, characterization, and hydrogen bonding analysis of copper complexes with acetate bridging: insights into interactions in crystal networks. [PDF]
Mirtamizdoust B +4 more
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Enhanced sulfadiazine degradation through synergistic visible light assisted peroxymonosulfate activation using a magnetic Fe₃O₄-ZnIn₂S₄ catalyst. [PDF]
Aali R +9 more
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Paleontological Research, 2021
. The Qom Formation deposits, located at 12 km southeast of Salafchegan (N: 34° 21′ 26″ and E: 50° 32′ 14″), have a thickness of 110 m. The formation includes thin, and medium-to-thick bedded limestone, as well as shale, overlying the Lower Red Formation
Amrollah Safari
exaly +2 more sources
. The Qom Formation deposits, located at 12 km southeast of Salafchegan (N: 34° 21′ 26″ and E: 50° 32′ 14″), have a thickness of 110 m. The formation includes thin, and medium-to-thick bedded limestone, as well as shale, overlying the Lower Red Formation
Amrollah Safari
exaly +2 more sources
Sedimentology and Reservoir Characterization of the Qom Formation, Central Iran Basin
The Qom Formation has been considered as a significant reservoir succession in Central Iran forming various hydrocarbon fields. The geological data from four wells from the two hydrocarbon fields (I and II) have been investigated for a reconstruction ...
Seyed Behzad Mirzadeh Vaghefi +4 more
semanticscholar +2 more sources
The Qom Formation is deposited along more than 1800 km of the NE margin of the Tethyan Seaway in the Oligocene-Early Miocene during the final sea transgression on the Iranian Plate.
Ebrahim Mohammadi, H. Ameri
semanticscholar +2 more sources
Microfacies and depositional environments of the Qom Formation in Barzok area, SW Kashan, Iran
Carbonates and Evaporites, 2018Hossein Vaziri-Moghaddam +2 more
exaly +2 more sources

