Coupled hydro-mechanical analysis of underground gas storage at Sarajeh field, Qom formation, Iran
Production or injection of fluids from/in an underground storage site causes variations of pore pressure and stress states. These fluctuations significantly affect implications for hydraulic fracturing, wellbore integrity, top surface subsidence and ...
Mohsen Bakhtiari +3 more
semanticscholar +3 more sources
Application of elemental data in reconstruction of paleoredox conditions of the Qom Formation at Khani Abad section, southeast of Kashan [PDF]
Introduction The abundances of minor-elements in carbonate rocks depend on the noncarbonate materials, including detrital minerals, accessory authigenic precipitates, noncarbonate skeletal material, organic matter, phases formed during diagenesis and the
Elham Asadi Mehmandosti +2 more
doaj +3 more sources
Zooxanthellate corals are Iran's most abundant macrofossils in the Oligocene-early Miocene Qom Formation deposits in the NE margin of the Tethyan Seaway.
Ebrahim Mohammadi, Mehdi Ghaedi
semanticscholar +2 more sources
Paleoecology and biostratigraphic data of the large benthic foraminifera in the Oligocene-Miocene Qom Formation in Kahak area, in the Urumieh-Dokhtar province in Iran [PDF]
The Oligocene-Miocene Qom Formation was deposited in different thickness in the Central Iran, Urumiehh–Dokhtar magmatic arc and Sanandaj–Sirjan provinces in Iran.
mahnaz amirshahkarami, mona naimi
doaj +1 more source
Identification of the Oligocene-Miocene boundary in the Central Iran Basin (Qom Formation): calcareous nannofossil evidences [PDF]
A diverse Late Oligocene to Early Miocene calcareous nannofossil assemblage was examined from the Qom Formation in the Central Iran Basin, and the Oligocene-Miocene boundary was identified based on the quantitative analysis of the assemblages in 303 ...
M. Parandavar, F. Hadavi
semanticscholar +2 more sources
SIRENIA FOSSILS FROM QOM FORMATION (BURDIGALIAN) OF THE KABUDAR AHANG AREA, NORTHWEST IRAN
Fossil remains of sirenians (Mammalia; Dugongidae) are reported from the late early Miocene (Burdigalian) Qom Formation near the town of Shirin Su, northwest Kabudar Ahang region, west of Tehran, Iran. The fossils consist of partial postcranial skeletons
NASROLLAH ABBASSI +3 more
doaj +2 more sources
Microfacies, sedimentary environment and sequence stratigraphy of the Qom Formation in Yort e Shah no-1 well and Morreh Kuh surface section (South of Tehran) [PDF]
Introduction: The drilled wells in central Iran basin representing the Oligo-Miocene Qom Formation could be considered as a hydrocarbon system wherever the complete successions of these marine sediments are deposited (Baghbani 1998).
Mahmoud jalali +2 more
doaj +1 more source
Biostratigraphy and Microfacies of Qom Formation in Urumieh – Dokhtar Zone, Iran [PDF]
Qom Formation is well developed in Urumieh–Dokhtar Zone, Iran. Three different measured sections were studied in this area in order to interpret the biostratigraphy and microfacies of QomFormation.
Zohreh Holakouee +3 more
semanticscholar +2 more sources

