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RISJurassic Biostratigraphy in the Persian Gulf, South of Iran
-tions consist of grey shales, dolomite, limestone and anhydrite. The Neyriz and Hith formations are barren of fossils and the age of NeyrizFormation is Early Jurassic and the age of Hith Formation is Late Jurassic (Tithonian) based on stratigraphy. In the Surmeh...
Microfacies analysis and paleoenvironment interpretation of Upper Jurassic carbonates of Jajarm area, N-NE Iran
This research is focused on the Upper Jurassic (Oxfordian-Kimmeridgian) carbonates in Jajarm area, north-northeast Iran. These deposits have very good and wide exposure in this area. Five stratigraphic sections that are studied in Jajarm area...
Facies analysis and depositional sequences of the Upper Jurassic Mozduran Formation, a carbonate reservoir in the Kopet Dagh Basin, NE Iran
Upper Jurassic carbonates of the Mozduran Formation constitute the principal reservoir intervals
at the giant Khangiran and Gonbadli gasfields in the Kopet Dagh Basin, NE Iran. These carbonates
were investigated using detailed field...
Stratigraghy and Identifying Boundaries of Mozduran Formation with Magnetite Method in East Kopet-Dagh Basin
made out of 52 samples. According to the findings of the thin section study, 18 genera and nine species of foraminifera and algae were identified. Based on the index fossils, the age of the Mozduran Formation was identified as Upper Jurassic...
Petrographical and geochemical evidences for paragenetic sequence interpretation of diagenesis in mixed siliciclastic–carbonate sediments: Mozduran Formation (Upper Jurassic), south of Agh-Darband, NE Iran
The Upper Jurassic Mozduran Formation with a thickness of 420 m at the type locality is the most important gas-bearing reservoir in NE Iran. It is mainly composed of limestone, dolostone with shale and gypsum interbeds that grade into coarser...
Carbonate Diagenesis of the Upper Jurassic Successions in the West of Binalud - Eastern Alborz (NE Iran)
The upper Jurassic carbonate settings in Iran are widely exposed in north and northeastern parts. Five
stratigraphic columns were selected in the north eastern Iran. Their thickness ranges from 330 to 500 m. The various diagenetic processes...
PALAEOENVIRONMENT AND BASIN ARCHITECTURE OF THE LOWER JURASSIC AB-HAJI FORMATION, EAST-CENTRAL IRAN
The Lower Jurassic Ab-Haji Formation of the Kalmard, Tabas and Lut blocks, east-central Iran, has been
studied using an integrated stratigraphic-sedimentologic approach. The Ab-Haji Formation is mostly composed of greenish sandstones...
The survey of Middle- Late Jurassic rocks in the west of Binalud Range Zone based on Macrofossils
A thick succession of marly limestones, marl and limestone with ammonites as the most important macrofossils in the west of Binalud Range has been studied.
The geodynamic history of east-central Iran during the Early Jurassic from the sedimentary records in the aftermath of the main Cimmerian orogeny
of the main Cimmerian event (Triassic
Jurassic boundary to Liassic). We measured and studied seven well-exposed outcrop sections
in order to identify lithofacies and facies associations and to interpret the palaeoenvironment.
Six facies...