Sultan Shihab Al-Hadiedi, A. (2010). Biostratigraphy of Planktic Foraminifera of Serikagni Formation (Lower Miocene) in Sfaya well No.16/North Western Iraq. , 15(3), 265-272.
Abdullah Sultan Shihab Al-Hadiedi. "Biostratigraphy of Planktic Foraminifera of Serikagni Formation (Lower Miocene) in Sfaya well No.16/North Western Iraq". , 15, 3, 2010, 265-272.
Sultan Shihab Al-Hadiedi, A. (2010). 'Biostratigraphy of Planktic Foraminifera of Serikagni Formation (Lower Miocene) in Sfaya well No.16/North Western Iraq', , 15(3), pp. 265-272.
Sultan Shihab Al-Hadiedi, A. Biostratigraphy of Planktic Foraminifera of Serikagni Formation (Lower Miocene) in Sfaya well No.16/North Western Iraq. , 2010; 15(3): 265-272.

Biostratigraphy of Planktic Foraminifera of Serikagni Formation (Lower Miocene) in Sfaya well No.16/North Western Iraq

Tikrit Journal of Pure Science
Article 1, Volume 15, Issue 3, 2010, Pages 265-272
Author
Abdullah Sultan Shihab Al-Hadiedi
Abstract
Planktonic Formaninifera is studied from Serikagui Formation in Sfaya well No.16 between the depth interval (630-780)m. Four Biostratigraphic Zones recognized in these stratigraphy succession. These are : form top to bottom .
1. Globigerinoides trilobus – Globigerinoides sicanus Partial Range Zone
2. Catapsydrax stainforthi – Catapsydrax unicavus Concurrent Range Zone.
3.Globoquadrina dehiscens praedehiscens – Globoquadrina dehiscens dehiscens Partial Range Zone.
4. Globigerinoides quadrilobatus primerdius – Globorotalia (Turborotalia) kugleri Concurrent Range Zone.
These Biostratigraphic Zones are correlated with other Zonal schemes inside and outside Iraq . The age of Serikagni Formation is Lower Miocene.
Statistics
Article View: 13
PDF Download: 2


Journal Management System. Powered by iJournalPro.com