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Sedimentology and Reservoir Characterization of the Qom Formation, Central Iran Basin
Journal Of The Geological Society Of IndiaABSTRACT 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 of sedimentary and diagenetic environments as well as reservoir quality of the ...
Seyed Behzad Mirzadeh Vaghefi +4 more
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Journal of the Geological Society of India
Abstract 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. We present (foraminiferal-based) biostratigraphic data from three exposed sections near the northwestern Jazmurian Lake, as the southeasternmost ...
Ebrahim Mohammadi, Hamed Ameri
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Abstract 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. We present (foraminiferal-based) biostratigraphic data from three exposed sections near the northwestern Jazmurian Lake, as the southeasternmost ...
Ebrahim Mohammadi, Hamed Ameri
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An early Rupelian origin of Titanoderma pustulatum recorded in the Qom Formation, Iran
2019The Rupelian Uromieh section of the Qom Formation consists of Nummulites-bearing limestones that overlay thick polymictic conglomerates and are overlaid by marlstones rich in planktonic foraminifera. The section was analyzed with the aim to provide a first description of its still unknown coralline algal assemblages, and for depicting its benthic ...
Basso, D +3 more
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The Early Miocene Qom Formation depositional setting; Northwest of Central Iran Basin
2021An outcrop of the Qom Formation (Fm.) is considered to determine the depositional setting model in the northwest of Central Iran. Field observations show that the Qom Fm. is composed of thin to thick-beds limestone along with alternation of green marl and argillaceous limestone.
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2009
Sediments of the Qom Formation in the Jazeh area, south of Kashan, are Ropelian - Chatian in age and have a thickness of 299 meters. It consists of medium to thick bedded and massive limestone, shale and marl. They overlie on the Eocene volcanic rocks with unconformity and its upper boundary is covered by alluvium.
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Sediments of the Qom Formation in the Jazeh area, south of Kashan, are Ropelian - Chatian in age and have a thickness of 299 meters. It consists of medium to thick bedded and massive limestone, shale and marl. They overlie on the Eocene volcanic rocks with unconformity and its upper boundary is covered by alluvium.
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The Qom Formation was deposited in the Central Basin of Iran, representing the northern part of the Tethyan Seaway during the Burdigalian (Lower Miocene). This study focuses on the deep marine marls of member e of the Qom succession in the Dochah section.
Masoud Sharifi-Yazdi +3 more
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Masoud Sharifi-Yazdi +3 more
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Zeitschrift der Deutschen Gesellschaft für Geowissenschaften, 2020
Amrollah Safari +3 more
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Amrollah Safari +3 more
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2014
Echinoids fauna are common and distributed in the Lower Miocene deposits of the Bagher Abad area, northeast Isfahan, Central Iran.There are six Echinoid taxa belonging to the Echinoidea Class that can be described as: Clypeaster intermedius, Prinocidaris sp. andspines related to: Eucidaris zaemays, Stylocidaris Polyacantha, Spatangoid sp.
Nouradini, Maryam +2 more
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Echinoids fauna are common and distributed in the Lower Miocene deposits of the Bagher Abad area, northeast Isfahan, Central Iran.There are six Echinoid taxa belonging to the Echinoidea Class that can be described as: Clypeaster intermedius, Prinocidaris sp. andspines related to: Eucidaris zaemays, Stylocidaris Polyacantha, Spatangoid sp.
Nouradini, Maryam +2 more
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Sedimentary geochemistry of the sedimentary facies of the Qom Formation in the southwest of Saveh
2023openaire +1 more source