[HTML][HTML] Late Cretaceous biostratigraphy planktonic foraminifera of the Farokhi Formation, Iran

M Allameh, RRY Nejad - Open Journal of Geology, 2017 - scirp.org
The Farokhi Formation is one of the informal Central Iran formations, which is located in the
NW Tabas township. The Tabas area is a part of the Central Iran sedimentary basin which is …

Two echinoid species from the early Aptian (Early Cretaceous) of the Kopet-Dagh Basin, NE Iran.

N Schlüter, M Taherpour-Khalil-Abad, M Majidifard… - Zootaxa, 2019 - europepmc.org
Two echinoid species from the early Aptian (Early Cretaceous) of the Kopet-Dagh Basin, NE
Iran. - Abstract - Europe PMC Sign in | Create an account https://orcid.org Europe PMC Menu …

Palynofacies and paleoenvironment of marl segment in Farokhi formation (Central Iran)

M Allameh, B Torabian - Scientific Quarterly Journal of Geosciences, 2016 - gsjournal.ir
Farrokhi Formation is a Cretaceous rock unit in Central Iran that lithologically contains lime,
marl and marly lime accompanied by layers of fossiliferous limestones. This formation lays …

Calcareous nannofossil biostratigraphy of the marly part of Farrokhi formation in the Farrokhi stratigraphic section (Central Iran, West Tabas)

M Notghi Moghaddam, F Jalili… - Advanced Applied Geology, 2023 - aag.scu.ac.ir
In the present study, biostratigraphy of calcareous nannofossils from the marl part of Farrokhi
formation in the Central Iran basin, stratigraphic section of Farrokhi village, are investigated …

Late Cretaceous Echinoids from the Seymareh member (Lopha Limestone member), KabirKuh Anticline, Southwest of Iran

H Kamyabi Shadan, H Dashtban… - Geopersia, 2019 - geopersia.ut.ac.ir
In the present study, Kabir kuh Section, related to the Seymareh or Lopha Limestone
member (Gurpi Formation) have been Selected. The member has yielded a rich echinoid …

مطالعه محیط دیرینه بخش مارنی سازند فرخی بر پایه استراکدا (ایران مرکزی)

علامه, محسن - فصلنامه علمی علوم زمین, 2018‎ - gsjournal.ir
سازند فرخی جوان‌ترین واحد رسوبی کرتاسه بالایی است که در منطقه خور و بیابانک جای گرفته‌
است. ترکیب سنگی آن شامل 250 متر آهک، مارن و آهک مارنی با میان‌لایه‌هایی از سنگ‌آهک فسیل‌دار …

Paleoenvironmental study of the marly beds of the Farrokhi Formation (Central Iran) based on their ostracods content

M Allameh - Scientific Quarterly Journal of Geosciences, 2018 - gsjournal.ir
The Farrokhi Formation is the youngest sedimentary unit in Upper Cretaceous of Khur and
Biabanak area. Its lithology is mainly consists of limestone, marl, marly limestone with …

[引用][C] پالینوفاسیس و محیط دیرینه بخش مارنی سازند فرخی (ایران مرکزی)

علامه, محسن, ترابیان - فصلنامه علمی علوم زمین, 2016‎ - سازمان زمین شناسی و اکتشافات معدنی …