Zobrazeno 1 - 10
of 13
pro vyhledávání: '"Hamideh Noroozpour"'
Autor:
Hamideh Noroozpour
Publikováno v:
Journal of Stratigraphy and Sedimentology Researches, Vol 36, Iss 3, Pp 55-76 (2020)
Abstract The Permian deposits (Doroud Formation) are exposed in a wide area of central Alborz. A stratigraphic section of Permian deposits in the Eram section (South Neka) has been selected for the study of facies, depositional environments, sequence
Externí odkaz:
https://doaj.org/article/01d4cf283d7e4e2186836bdc77f7e624
Publikováno v:
Geological Journal. 56:3460-3471
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6cc3a51e529abf3e6e94cb9a8ee442f5
https://doi.org/10.1002/gj.4111
https://doi.org/10.1002/gj.4111
Autor:
Hamideh Noroozpour
Publikováno v:
Carbonates and Evaporites. 36
The Posht Darband stratigraphic section of the Qom Formation is considered to undertake paleontological study in the northwest of Sanandaj–Sirjan Zone, Western Iran. Field observations demonstrate that the Qom Formation is composed of medium to thi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::da432a0512675614e136c58b08da3557
https://doi.org/10.1007/s13146-021-00710-z
https://doi.org/10.1007/s13146-021-00710-z
Publikováno v:
International Journal of Geography and Geology. 6:8-17
Using palynoflora findings, the present study was conducted to determine paleoecology of Permo-Triassic boundary in Shourjestan Region in north of Fars Province. Permo-Triassic boundary in this region is gradational (transitional) and continuous. Fou
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ba6bb4b28e0d2d6258bacc5c9c1b990e
https://doi.org/10.18488/journal.10/2017.6.1/10.1.8.17
https://doi.org/10.18488/journal.10/2017.6.1/10.1.8.17
Publikováno v:
Open Journal of Geology. :281-290
The major Quaternary faults in the Tehran-Semnan region can be classified based on their strikes into three sets: northeast-southwest, northwest-southeast and east-west. In this paper, we use a model to evaluate fault movement potential (FMP). Their
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b035cb9b5821e52140c7bbabfdc1a477
https://doi.org/10.4236/ojg.2015.55025
https://doi.org/10.4236/ojg.2015.55025
Autor:
Mehran Arian, Hamideh Noroozpour
Publikováno v:
Open Journal of Geology. :291-299
Kareh Bas is one the transverse fault systems in Zagros fold-thrust belt. Kareh Bas Transcurrent Fault System with a total length of 200 Km is situated about 80 Km east of the Borazjan segment (a part of Kazerun fault zone) and 40 Km west of Shiraz.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::78071019ff4a56fcefefc4efa5bab6a7
https://doi.org/10.4236/ojg.2015.55026
https://doi.org/10.4236/ojg.2015.55026
Publikováno v:
Open Journal of Geology. :383-386
In this research, a review was done on Permo-Triassic deposits in Central Iran including Abadeh, Hambast, and Elika formations. Following an overview about the circumstances of Central Iran Basin during Permotriassic time interval, the respective for
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f4b0edb8c4f876c03be8706398243888
https://doi.org/10.4236/ojg.2015.56035
https://doi.org/10.4236/ojg.2015.56035
Autor:
Mehran Arian, Hamideh Noroozpour
Publikováno v:
Open Journal of Geology. :55-60
One of the most interesting salt structures is salt-tongue canopy. The Central Iran basin has a few salt provinces and in this paper, morphotectonic concept of the salt-tongue canopy on the west of Garmsar city has been investigated. In this study, f
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::aa8b346a86dcda41bfadff60884e69d3
https://doi.org/10.4236/ojg.2015.52005
https://doi.org/10.4236/ojg.2015.52005
Publikováno v:
Open Journal of Geology. :399-404
In the present paper, Talezang Formation, located in southwest of Khoramabad, is studied. Ghalebi section (200 m thickness) contains gray limestones with cherty nodules and sandy limestone isoclinally overlies Amiran Formation (gray shale and limesto
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::cdc2f0c6594ce4f886e373f824589a7b
https://doi.org/10.4236/ojg.2015.56038
https://doi.org/10.4236/ojg.2015.56038