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Palaeoworld, 2020
The well-exposed outcrops of the Bujan, northern Abadeh, and Varkan stratigraphic sections of the Qom Formation in the Iranian part of the ”northeastern margin” of the Tethyan Seaway were characterized by abundant biogenic components dominated by ...
E. Mohammadi
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The well-exposed outcrops of the Bujan, northern Abadeh, and Varkan stratigraphic sections of the Qom Formation in the Iranian part of the ”northeastern margin” of the Tethyan Seaway were characterized by abundant biogenic components dominated by ...
E. Mohammadi
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Journal of Paleontology, 2020
. The Oligocene strata of the Qom Formation from the Tajar-Kuh section, Central Iran, are rich in various Larger Benthic Foraminifera (LBF). Morphometric studies of the internal features of the LBF tests were carried out based on matrix-free specimens ...
Narges Akbar-Baskalayeh +4 more
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. The Oligocene strata of the Qom Formation from the Tajar-Kuh section, Central Iran, are rich in various Larger Benthic Foraminifera (LBF). Morphometric studies of the internal features of the LBF tests were carried out based on matrix-free specimens ...
Narges Akbar-Baskalayeh +4 more
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Periódico Tchê Química, 2020
Marine deposits of the Qom Formation, which is an important gas reservoir in Central Iran with the age of Early Oligocene to Early Miocene, is studied to determine facies, sedimentary paleoenvironment, and depositional sequences.
S. Hassanzadeh +4 more
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Marine deposits of the Qom Formation, which is an important gas reservoir in Central Iran with the age of Early Oligocene to Early Miocene, is studied to determine facies, sedimentary paleoenvironment, and depositional sequences.
S. Hassanzadeh +4 more
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Russian Geology and Geophysics, 2019
This research attempted to reconstruct the sedimentary environment and depositional sequences of the Qom Formation in Central Iran, using biofacies and taphofacies analyses.
M. Mahyad +3 more
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This research attempted to reconstruct the sedimentary environment and depositional sequences of the Qom Formation in Central Iran, using biofacies and taphofacies analyses.
M. Mahyad +3 more
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Miogypsinid biostratigraphy in lower Miocene Qom Formation, Central Iran
Micropaleontology, 2019The Qom Formation of Central Iran consists of carbonates, evaporates and clastics in several depositional cycles, divided into nine members in the type area around Qom city, as best exemplified in the Dobaradar section. Each cycle starts with carbonates,
J. Daneshian, L. Dana
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