biostratigraphy of the kazhdumi formation tang-e-maghar section, nw of behbahan based on planktonic foraminifera
Authors
abstract
in order to study of biostratigraphy and age dating of kazhdumi formation, based on planktonic foraminifera and correlation of identified biozones with global standard biozones, this formation at tang-e-maghar have been studied. in this study 73 samples of kazhdumi formation, with 270 meter thickness, have been collected. the main lithological units at the studied section consist of the black bituminous shale and marl with interbedded limestone. study of planktonic foraminifera assemblages led to identification of 33 species belonging to 8 genera of index foraminifera of the tethyan realm at studied section. in this study, 7 biozones including globigerinelloides blowi interval zone, leupoldina cabri taxon range zone, globigerinelloides ferreolensis partial range zone, hedbergella trocoidea partial range zone, paraticinella bejaouensis interval zone, muricohedbergella planispira interval zone and ticinella primula interval zone have been identified, which show late early aptian – middle albian ages and all of identified biozones can be correlated with premoli silva and verga 2004 biozones.
similar resources
Biostratigraphy of the Gurpi Formation in Sepidan section, Interior Fars basin based on planktonic foraminifera
In this study biostratigraphy of the Upper Cretaceous deposits (Gurpi Formation) in Sepidan section located in the Interior Fars basin (SW Iran) was studied. The Gurpi Formation in this section consists of 360 m lime shale, argillaceous limestone and shale laid continuously on the Ilam Formation and with a paraconformity under the Pabdeh Formation. Nine genera and 27 species of planktonic foram...
full textbiostratigraphy of the gurpi formation in sepidan section, interior fars basin based on planktonic foraminifera
in this study biostratigraphy of the upper cretaceous deposits (gurpi formation) in sepidan section located in the interior fars basin (sw iran) was studied. the gurpi formation in this section consists of 360 m lime shale, argillaceous limestone and shale laid continuously on the ilam formation and with a paraconformity under the pabdeh formation. nine genera and 27 species of planktonic foram...
full textInvestigating the paleoecological characteristics of Abtalkh Formation at Bahadorkhan Section (Central Kopet-Dagh) based on planktonic and benthic foraminifera
Study of a late Late Santonian to Late Campanian hemipelagic succession from Abtalkh Formation at the Bahadorkhan section (Central Kopet-Dagh) enabled us to verify paleoecology changes based on planktonic and benthic foraminifera assemblage. Bahadorkhan section is consisted of calcareous shale, lime marl, marl, and a few dispersed chalky limestone beds. Upper and lower boundaries of Abtalkh For...
full textbiostratigraphy and study of the role of morphotype groups of planktonic foraminifera in palaeobathymetry of the gurpi formation in lar area (kuh - e - kurdeh section)
0
full textBiostratigraphy of the Gurpi Formation based on Calcareous nannofossil in the Kouh-e sefid anticline section, Izeh structural zone
The Gurpi Formation with a thickness of 190 m at the Kouh-e sefid anticline is investigated with regard to the calcareous nannofossils. In this section, Gurpi Formation is mainly consists of shale, marls and argillaceous limestones. As a result of this study, 21 genera and 41 species of calcareous nannofossil have been recognized. Based on distribution of index species calcareous nannofossils...
full textpaleoecology of abtalkh formation based on planktonic and benthic foraminifera in padeha section, kopet-dagh basin
abtalkh formation is a part of late cretaceous sedimentary unit in the kopet- dagh basin, ne iran. this study deals with the study of this formation in the eastern parts of the basin in padeha village. it thickness is about 991m, and lithologically consists of grey, greyish to blue shale and marl. the lower contact with abderaz formation is conformable and transitional, but the upper boundary w...
full textMy Resources
Save resource for easier access later
Journal title:
دیرینه شناسیجلد ۲، شماره ۱، صفحات ۶۲-۰
Hosted on Doprax cloud platform doprax.com
copyright © 2015-2023