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نمایش تعداد 1-10 از 13
Lithostratigraphy and carbonate microfacies across the Permian–Triassic boundary near Julfa (NW Iran) and in the Baghuk Mountains (Central Iran)
) the ‘Boundary Clay’, and (3) the earliest Triassic Elikah Formation with the conodont P–Tr boundary at its base. The carbonate microfacies reveals a facies change, in the sections near Julfa, within the Paratirolites Limestone with an increasing number...
Carbonate microfacies and δ13C and δ15N systematics across the Permian-Triassic boundary near Julfa (NW Iran)
water masses. The continuation of the main negative δ13C after the end of the δ15N excursion may indicate the mixing of the water column after the anoxic period. Data of carbonate microfacies as well as stable isotopes show that the P-Tr event started...
Microfacies analysis and paleoenvironment interpretation of Upper Jurassic carbonates of Jajarm area, N-NE Iran
of these formations. Based on five measured stratigraphic sections, field observations, detailed petrographic considerations on more than 500 thin sections, microfacies are analyzed and depositional environment are interpreted.
Microfacies petrographically...
Lithostratigraphy and carbonate microfacies across the Permian-Triassic boundary near Julfa (NW Iran) and Abadeh (Central Iran)
‘calcite fan’ layers, of probably inorganic origin. The earliest Triassic carbonate Elikah and Shahreza formations comprise thin-bedded yellow and grey limestone beds; the microfacies succession comprises bellerophontid and gastropod wackestone...
Lithostratigraphic and facies analyses of the Sarcheshmeh Formation (Lower Cretaceous) in the eastern Kopet Dagh Basin, NE Iran
The Kopet Dagh Basin is located in north-east Iran where sedimentation continued throughout the Jurassic–Tertiary. The area studied is in the easternmost part of the basin. Two stratigraphic sections representing mainly ...
Depositional environment, diagenesis, and geochemistry of Devonian Bahram formation carbonates, Eastern Iran
environment, diagenesis, and geochemistry
of major and minor elements. Petrographic and microfacies pattern studies led to the recognition of five
microfacies groups including shore face, tidal flat, lagoonal, shoal and open-marine facies...
Larger foraminiferal biostratigraphy and microfacies analysis from the Ypresian (Ilerdian-Cuisian) limestones in the Sistan Suture Zone (eastern Iran)
with the standard shallow benthic zonation, placing considerable emphasis on biostratigraphic and microfacies analysis implications. Four shallow benthic zones -SBZ8 and SBZ10–12- have been designated in LBF horizons comprising index zonal markers such as Alveolina...
Microfaices and sedimentary environments Asmari Formation in one of the Marun oil field wells
of microfacies and sedimentary environment of Asmari Formation in the mentioned well, 150 thin sections (mainly drilling cores) have been studied and 10 microfacies, 4 facies were recognized. Based on identified facies, the Asmari formation in a carbonate...
Sequence stratigraphy and microfacies analysis of Sarvak Formation in southwest of Firozabad area
چینه نگاری سکانسی و میکروفاسیس سازند سروک در جنوب غرب فیروزآباد
به منظور شناسایی رخسارههای سازند سروک در منطقه فیروزآباد، 137 نمونه با در نظر گرفتن تغییرات رخسارهای و خصوصیات سنگ شناختی برداشت و مورد بررسی قرار گرفت. شناسایی 13 رخساره و 3 سکانس رسوبی محدود شده توسط ناپیوستگیهای نوع ...
Microfacies analysis and environmental interpretation of the Qom Formation in Chenar area (northwest of Kashan)
بررسي ريز رخساره ها و تفسير محيط رسوبي سازند قم در منطقه چنار (شمال غرب کاشان)
نهشته های سازند قم در ناحیه چنار، در 50 کیلومتری شمال غرب کاشان با ضخامت 147 متر شامل سنگ آهک ماسهای، سنگ آهک نازک لایه تا ضخیم لایه، تودهای و شیل است که با ناپیوستگی آذرین پی بر روی سنگهای آتشفشانی ائوسن قرار دارند ...