Zobrazeno 1 - 10
of 14
pro vyhledávání: '"Freshteh Sajjadi"'
Publikováno v:
Journal of Stratigraphy and Sedimentology Researches, Vol 34, Iss 1, Pp 91-108 (2018)
Introduction The Dalichai Formation is represented by greenish-grey color shales, calcareous shales, marls, and richly ammonitiferous limestones (Steiger, 1966), being widely distributed in the Alborz Mountain, northern Iran. It disconformably overli
Externí odkaz:
https://doaj.org/article/ff1f1dc2e48c412c8ec130963feb9945
Publikováno v:
Journal of Stratigraphy and Sedimentology Researches, Vol 33, Iss 2, Pp 41-64 (2017)
The Dalichai Formation at the Guydagh stratigraphic section in the southeast of Maragheh, (Western Alborz), with measured thicknesses of 198 meters (consisting of limestone, Calcareous shale, shale limestone, shale and marl) contain terrestrial (spor
Externí odkaz:
https://doaj.org/article/e5513deadcc14c2f9e7af701dceb8f1d
Autor:
Freshteh Sajjadi, Seyede Sepideh Mirrabie, Seyed Mohammad Zamanzadeh, Houshang Mehrabi, Behzad Soltani, Vahid Tavakoli, Abdolhossein Amini
Publikováno v:
Acta Geochimica. 40:787-805
In the present study, the Lower-Middle Pliocene Cheleken Formation in the south of Ghaemshahr city was studied to determine the provenance of the comprising sediments, paleoclimatic conditions, and tectonic setting of the rocks. Petrographic and geoc
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::79bc02e99b88ad66ab6ced7ee54fa7b5
https://doi.org/10.1007/s11631-021-00480-4
https://doi.org/10.1007/s11631-021-00480-4
Publikováno v:
Palaeobiodiversity and Palaeoenvironments. 99:379-399
We performed a palynological study on Jurassic successions of the Hojedk Formation, Central Iran. The sampled material was recovered from well no. 233, South Kuchak-Ali area belonging to the Tabas Block. The lithology comprises 475.80 m of green–gr
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4d2f9d48b125e26460099e1532bac703
https://doi.org/10.1007/s12549-018-0361-0
https://doi.org/10.1007/s12549-018-0361-0
Publikováno v:
Journal of Asian Earth Sciences. 111:553-567
Reasonably diverse and moderately preserved palynofloras of exclusively terrestrial derivation occur in surface samples of the Nayband Formation, Kamar Macheh Kuh, southeastern Tabas, east-central Iran. No marine palynomorphs encountered in the sampl
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3d6c9e6fe428d4d1821cd37c0fc3edc9
https://doi.org/10.1016/j.jseaes.2015.05.030
https://doi.org/10.1016/j.jseaes.2015.05.030
Publikováno v:
REVISTA BRASILEIRA DE PALEONTOLOGIA. 18:251-260
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::42d5efbb6e4e0a6bb5814457653a0652
https://doi.org/10.4072/rbp.2015.2.06
https://doi.org/10.4072/rbp.2015.2.06
Publikováno v:
Science China Earth Sciences. 56:2107-2115
Palynological data are used to draw paleoecological inferences for the Dalichai Formation, northeast of Semnan, northeastern Iran. All samples examined yield well-preserved, diverse palynofloras consisting predominantly of miospores; dinoflagellate c
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a340f1cdabc5a4000c44fe34aadf800b
https://doi.org/10.1007/s11430-013-4697-z
https://doi.org/10.1007/s11430-013-4697-z
Publikováno v:
Micropaleontology. 53:391-408
Diverse and moderately well-preserved palynofloras occur in Middle Jurassic sediments of the Kashafrud Formation at the Senjedak section, southeast of Mashhad, northeastern Iran. Trilete and monolete spores and pollen dominate the assemblages, wherea
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::785d4483fe3f92eda8989608c41efa92
https://doi.org/10.2113/gsmicropal.53.5.391
https://doi.org/10.2113/gsmicropal.53.5.391
Autor:
Freshteh Sajjadi, Geoffrey Playford
Publikováno v:
Palaeontographica Abteilung B. 261:99-165
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6bdc5cd53da8dda943853ea3dae8b764
https://doi.org/10.1127/palb/261/2002/99
https://doi.org/10.1127/palb/261/2002/99