Biostratigraphy and Sequence Stratigraphy of the Gurpi Formation at Deh Dasht Area, Zagros Basin, SW Iran [PDF]
A rich assemblage of planktonic foraminifera has been studied from an outcrop of the Gurpi Formation, the hydrocarbon source rock in the southwest Iran, Deh Dasht area (Kuh-e Siah anticline). Based on the distribution of the planktonic foraminifera, eight biozones have been recognized that included: Dicarinella concavata Interval Zone (Earliest ...
Mahboobeh FEREYDOONPOUR +2 more
core +7 more sources
Biostratigraphy of Foraminifera at The Upper Cretaceous and Lower Paleogene Strata in The Kuh-E Genu, Bandar Abbas City, Northwestern Persian Gulf, Southern Iran [PDF]
The study area is located in Tang-e Bagh at Kuh-e Genu, approximately 69 km, northern Persian Gulf. The age relationships of Sarvak, Gurpi, and Pabdeh formations were unclear in the study area because of the low-resolution biostratigraphy. Therefore, 152
Nadia Farsi +3 more
doaj +3 more sources
Study of Echinoids of Gurpi formation, Iran
AbstractIn order to detailed study of Echinoids, some samples are collected from Brown limestone member of Seimare from Gurpi Formation with 213 meter thickness which located in the vicinity of Ilam province; settling over Ilam Formation continuously. Paleontological results indicated Campanian - maastrichtian age at this section.
Behnaz Balmaki, Masoud Asgharian Rostami
exaly +5 more sources
Biostratigraphy of the Pabdeh Formation based on planktonic foraminifera in the Tang-e-Chogan section in Interior Fars, Zagros Basin [PDF]
The biostratigraphy of the marly-limestone Pabdeh Formation has been studied in a section located in the Interior Fars (folded Zagros). Five assemblage biozones of plankton foraminifera with Early Eocene to Late Eocene age were identified in the studied ...
Zahra Khaloasgari +2 more
doaj +3 more sources
Sequence stratigraphy of the Late Cretaceous–Paleocene Gurpi Formation in southwest Iran [PDF]
ABSTRACT Facies associations, microplanktonic diversity, palynofacies variations, geochemical data, and natural gamma-ray logs were analyzed from the Danial and Gurpi sections of the Campanian–Selandian Gurpi Formation in the Zagros Mountains, southwest Iran.
Bijan Beiranvand +3 more
openaire +3 more sources
Analysis of Microfacies , Sedimentary Environments and Sequence Stratigraphy of Pabdeh Formation, in type section, Zagros [PDF]
Type section of Pabdeh Formation (Late Paleocene- Early Oligocene) is located in the Gurpi anticline, Zagros, Khouzestan Province. Lithologically Pabdeh Formation consists of purple and white to yellowish marl, marly limestone and thin- to thick- bedded ...
Somaiyeh Saravani +3 more
doaj +3 more sources
Evaluation of Pabdeh/Asmari boundary based on calcareous nannofossil biostratigraphy at north eastern limb of Gurpi anticline, Khuzestan Province [PDF]
Introduction One of the most extensive Tertiary deposits is the marine strata of Pabdeh and Asmari Formations in Zagros, which was studied based on paleontology studies. Type section of Pabdeh Formation is located in Tang-e Pabdeh, North of Lali oilfield
Saeedeh Senemari
doaj +3 more sources
Impact of the Paleocene–Eocene Thermal Maximum (PETM) on organic petrographic characteristics of the basal Pabdeh Formation at Kuh-e-Gurpi Anticline, SW Iran [PDF]
This study investigates the impact of the Paleocene–Eocene Thermal Maximum (PETM) event on the organic petrographic characteristics of the base Pabdeh Formation in the Tang-e-Hati section, located at the Kuh-e-Gurpi Anticline, SW Iran.
Sasan Bakhtiary Nejad +2 more
doaj +3 more sources
Biostratigraphy of the Gurpi Formation (Zagros Basin, western Iran) based on planktonic foraminifera [PDF]
Micropalaeontological and biostratigraphic studies of the Gurpi Formation were carried out at the Kuhe-Surgah section (Zagros Basin, Iran). In this research, 62 species of planktonic foraminifera, belonging to 23 genera, were recognized and used to describe the following zones: 1) Contusotruncana plummerae Interval Zone; 2) Radotruncana calcarata Total
Atusa Honarmand +3 more
openaire +1 more source
Abstract Hormuz salt formation is considered the origin of the evaporated salt deposits in the Zagros and its ductile behavior has been known as the reason for the inhomogeneous deformation in the Zagros. However, our knowledge about this formation has been limited to the salt domes on the surface.
H. Kianimehr +3 more
wiley +1 more source

