In order to biostratigraphy of the Garau Formation in the centeral Lurestan, one subsurface section (Naft well) in Naft anticline, south Kermanshah was selected and studied. The drilled thickness of the Garau Formation in this section is up to 485 meters and lithologically composed of argillaceous limestones and dark gray marls. In this research 1150 thin sections of subsurface Naft well section were studied. In biostratigraphic studies of the Garau Formation in study section 61 species belong to 17 genera of planktonic foraminifera were recognized and 9 biozones were identified. Based on distribution of fossils and biozones identificated, the age of the Garau Formation in drilled part of the subsurface Naft well section is Early Aptian to ...
2508-2523The formation consists of marl with intercalation of limy marl with two formal members of L...
For biostratigraphy of the Eocene sediments in Iran, we studied Maroosk(398.2 m thickness) and Somea...
Gurpi Formation is one of the important formations in the Zagros Mountain which belongs to Cretaceou...
In order to study biostratigraphy of the Pabdeh Formation in southwest of Ilam, Marbera section was ...
In order to determine stratigraphy and the introduction of biozonationes in the Pabdeh Formation bas...
Micropalaeontological and biostratigraphic studies of the Gurpi Formation were carried out at the Ku...
The present study is an attempt to biostratigraphically classify the rocks of Gurpi Formation at Sam...
Copyright © 2013 Mohammad Anvar Moheghy et al. This is an open access article distributed under the ...
The Khami group within the petroliferous Zagros Basin of Iran includes the Surmeh, Hith, Fahliyan, G...
The foraminiferal content of two stratigraphic sections, located in eastern Iran within the Sahlabad...
The Fahliyan Formation of the Khami Group is the most important oil and gas reservoir in southwester...
AbstractThe Khami group within the petroliferous Zagros Basin of Iran includes the Surmeh, Hith, Fah...
Detailed investigation of Lower Cretaceous of the Banish area, Southwest Iran, has been made possibl...
International audienceThe Paleogene carbonate deposits of Pabdeh and Jahrum formations are widesprea...
The study of planktonic foraminifera of the Gurpi formations at Lar area (Kuh-e-kurdeh section) enab...
2508-2523The formation consists of marl with intercalation of limy marl with two formal members of L...
For biostratigraphy of the Eocene sediments in Iran, we studied Maroosk(398.2 m thickness) and Somea...
Gurpi Formation is one of the important formations in the Zagros Mountain which belongs to Cretaceou...
In order to study biostratigraphy of the Pabdeh Formation in southwest of Ilam, Marbera section was ...
In order to determine stratigraphy and the introduction of biozonationes in the Pabdeh Formation bas...
Micropalaeontological and biostratigraphic studies of the Gurpi Formation were carried out at the Ku...
The present study is an attempt to biostratigraphically classify the rocks of Gurpi Formation at Sam...
Copyright © 2013 Mohammad Anvar Moheghy et al. This is an open access article distributed under the ...
The Khami group within the petroliferous Zagros Basin of Iran includes the Surmeh, Hith, Fahliyan, G...
The foraminiferal content of two stratigraphic sections, located in eastern Iran within the Sahlabad...
The Fahliyan Formation of the Khami Group is the most important oil and gas reservoir in southwester...
AbstractThe Khami group within the petroliferous Zagros Basin of Iran includes the Surmeh, Hith, Fah...
Detailed investigation of Lower Cretaceous of the Banish area, Southwest Iran, has been made possibl...
International audienceThe Paleogene carbonate deposits of Pabdeh and Jahrum formations are widesprea...
The study of planktonic foraminifera of the Gurpi formations at Lar area (Kuh-e-kurdeh section) enab...
2508-2523The formation consists of marl with intercalation of limy marl with two formal members of L...
For biostratigraphy of the Eocene sediments in Iran, we studied Maroosk(398.2 m thickness) and Somea...
Gurpi Formation is one of the important formations in the Zagros Mountain which belongs to Cretaceou...