Zobrazeno 1 - 10
of 26
pro vyhledávání: '"Saeed Khodabakhsh"'
Publikováno v:
Journal of Stratigraphy and Sedimentology Researches, Vol 38, Iss 4, Pp 53-76 (2023)
Abstract Qazvin alluvial fan is the largest alluvial fan in the northern margin of the Qazvin Plain. This research focuses on describing and interpreting the origin of the sediments and facies model of this alluvial fan using 24 sediment samples from
Externí odkaz:
https://doaj.org/article/a6fb89cee1874dd3966030ced2b9f4f6
Publikováno v:
Journal of Stratigraphy and Sedimentology Researches, Vol 38, Iss 3, Pp 35-58 (2022)
Abstract This study was done to describe and interpret the facies, the provenance of sediments, pedogenesis processes, and the model of the Abyek alluvial fan in the northern margin of Qazvin Plain, using 45 sediment samples in the form of nine profi
Externí odkaz:
https://doaj.org/article/5a5c98164d9b42968c73573e9a2930fd
Publikováno v:
Journal of Stratigraphy and Sedimentology Researches, Vol 34, Iss 4, Pp 57-82 (2018)
Abstract The Pabdeh Formation (Paleocene–Oligocene) is located in the Zagros foreland basin. This formation was well appreciated as a source rock and somehow a potential reservoir particularly in the Dezful Embayment. Although it has been less appr
Externí odkaz:
https://doaj.org/article/d757998738cc466ca15025ca4a4ec37d
Publikováno v:
Ultrasonics Sonochemistry
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=r3c4b2081b22::486ca340d07ff336c386a0ffbece98f6
Autor:
Saeed Khodabakhsh, Reinhard Hesse
Publikováno v:
Marine Geology. 393:67-92
Heinrich layers (H-layers) are distinct, decimetre to centimetre thick layers of ice-rafted debris (IRD) that were deposited in the North Atlantic during the Late and middle Pleistocene. H-layers (H-layers) are characterized by high detrital carbonat
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a3461d20b3b21908a89fb704dffd4e02
https://doi.org/10.1016/j.margeo.2017.08.020
https://doi.org/10.1016/j.margeo.2017.08.020
Autor:
Reinhard Hesse, Saeed Khodabakhsh
Publikováno v:
Marine Geology (0025-3227) (Elsevier Science Bv), 2016-10, Vol. 380, P. 44-66
Heinrich layers (H-layers) are distinct, decimetre to centimetre thick layers of ice-rafted debris (IRD) that were deposited in the North Atlantic during the Late and middle Pleistocene. H-layers (H-layers) are characterized by high detrital carbonat
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::fe44c6a59283e8cf312b2c96d7b8fd6a
https://doi.org/10.1016/j.margeo.2016.05.019
https://doi.org/10.1016/j.margeo.2016.05.019
Autor:
Naser Bahiraei, Zahra HosseiniAsgarabadi, Mohammadreza Gharibreza, Saeed Khodabakhsh, Mehri Maleki, Effat Paseban
Publikováno v:
Arabian Journal of Geosciences. 11
The most important depositional processes in continental sedimentary basins occur in fluvial systems. In this study, sedimentology of Shahrud River and its eastern tributary (Alamutrud River, N Iran) was studied for the first time. The study area is
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ee48e80150b9d267d9994c5fcb041746
https://doi.org/10.1007/s12517-018-4077-2
https://doi.org/10.1007/s12517-018-4077-2
Publikováno v:
Rock Mechanics and Rock Engineering. 46:1091-1101
To study the relationship between engineering properties and petrographic characteristics, 20 rock samples were collected from Jurassic sandstones in the Hamedan region, western Iran. The specimens were tested to determine uniaxial compressive streng
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1270d77a565f5bf4aea047a9cfd06f67
https://doi.org/10.1007/s00603-012-0333-z
https://doi.org/10.1007/s00603-012-0333-z
Publikováno v:
Neues Jahrbuch für Geologie und Paläontologie - Abhandlungen. 262:59-77
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::804e76a22cc9310aabd02f2c4ca624a5
https://doi.org/10.1127/0077-7749/2011/0185
https://doi.org/10.1127/0077-7749/2011/0185
Publikováno v:
Geo-Marine Letters. 28:31-41
Eight seismic profiles from the southwestern Caspian Sea were analyzed to establish the sedimentary environments and depositional history in the South Caspian Basin since Pliocene times. Based on reflection terminations, nine sequence boundaries (S1
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fc10e229893aa21281c116a434c4a9cb
https://doi.org/10.1007/s00367-007-0087-x
https://doi.org/10.1007/s00367-007-0087-x