Zobrazeno 1 - 10
of 23
pro vyhledávání: '"Azam Mahanipour"'
Autor:
Azam Gholami Fard, Anoshirvan Lotfali Kani, Azam Mahanipour, Amir mohammad Jamali, fariba foroughi
Publikováno v:
Journal of Stratigraphy and Sedimentology Researches, Vol 35, Iss 3, Pp 99-114 (2019)
Abstract In the current study, a succession from the middle part of the Sarcheshmeh Formation was investigated to record the early Aptian oceanic anoxic event 1a (OAE1a) at the Qaleh-Zoo section in the central part of the Kopet-dagh Basin. The OAE1a
Externí odkaz:
https://doaj.org/article/9f0caf3ffd3e4cfab644999eef6fed99
Publikováno v:
Journal of Stratigraphy and Sedimentology Researches, Vol 34, Iss 2, Pp 23-42 (2018)
Introduction The Zagros mountain belt extends over 1800 km from Kurdistan in N Iraq to the Strait of Hormuz in Iran (Lacombe and Mouthereau 2006). Zagros Mountain belt is one of the richest oil provinces in the world (Emmami 2008) and is important to
Externí odkaz:
https://doaj.org/article/ef33df7164d4427db40bcfd01433c158
Publikováno v:
Journal of Stratigraphy and Sedimentology Researches, Vol 33, Iss 1, Pp 69-84 (2017)
1- Introduction Kopet Dagh Basin is located on the northeast of Iran, extending over Iran, Turkmenistan and Afghanistan with a west-northwest to east-southeast trend. The Iranian part of the basin is located between 61°14ˊ and 54°00ˊE and 38°15
Externí odkaz:
https://doaj.org/article/384e0890b2e04c0ab55a28bca3a1508b
Publikováno v:
Journal of Stratigraphy and Sedimentology Researches, Vol 31, Iss 1, Pp 57-66 (2015)
Abstract The Kopet-Dagh Basin is located in the north and north east of Iran, within the border triangle of Iran, Turkmenistan and Afghanistan. Sediments of Cretaceous age are well exposed in this basin. Sarcheshmeh and Sanganeh formations belong to
Externí odkaz:
https://doaj.org/article/c4b0b57d8fc44dc399751545e44b7a38
Publikováno v:
Journal of Stratigraphy and Sedimentology Researches, Vol 31, Iss 1, Pp 57-66 (2015)
Abstract The Kopet-Dagh Basin is located in the north and north east of Iran, within the border triangle of Iran, Turkmenistan and Afghanistan. Sediments of Cretaceous age are well exposed in this basin. Sarcheshmeh and Sanganeh formations belong to
Externí odkaz:
https://doaj.org/article/6b1c36b889b2443fb478f829fd82e5da
Publikováno v:
Iraqi Geological Journal, Vol 53, Iss 2C, Pp 68-86 (2020)
Calcareous nannofossils, mineralogical and geochemical investigations are carried out on the Cenomanian-Turonian boundary of the Gulneri Formation in the Azmir, Dokan and Degala sections, northern Iraq. Regarding the calcareous nannofossil data CC11
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::b196a4d6316bf3d99af1666f1dcd66db
https://doi.org/10.46717/igj.53.2c.6rs-2020-09/06
https://doi.org/10.46717/igj.53.2c.6rs-2020-09/06
Publikováno v:
Marine Micropaleontology. 149:64-74
Calcareous nannofossils and stable isotope data (δ13Ccarb) from a pelagic section of the Zagros Basin (west Iran) were used for an integrated oceanographic analysis of the Barremian – Aptian interval. The study aims at analyzing various oceanograp
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c5931a9dac2cf4d5425cabf7f020b5c8
https://doi.org/10.1016/j.marmicro.2019.04.003
https://doi.org/10.1016/j.marmicro.2019.04.003
Publikováno v:
Stratigraphy and Geological Correlation. 26:783-797
The calcareous nannofossils from the upper part of Garau Formation were studied in the NW Zagros Basin, western Iran (Kabir-Kuh section). The ca. 510 m thick studied interval is mainly composed of interlayered marls, marly limestones, marly shales, l
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fc4bbe56b81f9456f46e32429822c6dd
https://doi.org/10.1134/s0869593818070031
https://doi.org/10.1134/s0869593818070031
Autor:
Azam Mahanipour, Jörg Mutterlose
The Early–mid Cretaceous Garau and Kazhdumi Formations of the Zagros Basin (western and southwestern Iran) have been studied for calcareous nannofossils and their assemblage composition. The 722 m thick Garau Formation was investigated in the Kabir
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9f20c7944b0bc5767bb9998ef106bc3a
https://doi.org/10.1016/bs.sats.2021.09.005
https://doi.org/10.1016/bs.sats.2021.09.005
