Zobrazeno 1 - 5
of 5
pro vyhledávání: '"Reza Aharipour"'
Publikováno v:
Journal of Economic Geology, Vol 8, Iss 1, Pp 117-128 (2016)
Introduction Maceral is a term to introduce organic components visible under a microscope (Stopes, 1935). The physical and chemical characteristics of macerals such as elemental composition, moisture content, hardness, density and petrographic chara
Externí odkaz:
https://doaj.org/article/b869bb6f4226490f9b8a9660af0e8193
Publikováno v:
Journal of Asian Earth Sciences. 225:105046
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::354d38d2ba7a9e70914cd378e542907c
https://doi.org/10.1016/j.jseaes.2021.105046
https://doi.org/10.1016/j.jseaes.2021.105046
Autor:
Suzanne Y. O'Reilly, Hadi Shafaii Moghadam, Reza Aharipour, William L. Griffin, Robert J. Stern, Xian-Hua Li, Tonny B. Thomsen, Guido Meinhold
Publikováno v:
Lithos. :87-101
In this study we use detrital zircons to probe the Early Paleozoic history of NE Iran and evaluate the link between sediment sources and Gondwanan pre-Cadomian, Cadomian and younger events. U–Pb zircon ages and Hf isotopic compositions are reported
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d53570d4b3f8e1ec323f06113c3cf698
https://doi.org/10.1016/j.lithos.2016.09.008
https://doi.org/10.1016/j.lithos.2016.09.008
Autor:
Reza Aharipour, Amin Navidtalab, Stefan Huck, Mahboobeh Omidvar, Alireza Shakeri, Ulrich Heimhofer, Hossain Rahimpour-Bonab
Publikováno v:
Palaeogeography, Palaeoclimatology, Palaeoecology. 533:109255
A Neo-Tethyan upper Albian–Turonian (hemi-)pelagic carbonate succession (Sarvak Formation), accessible in outcrop in the Zagros, SW Iran, was investigated using sedimentology, microfacies analysis, planktonic foraminifera biostratigraphy, and carbo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8eead17c591f1f45427944dcd171f4c4
https://doi.org/10.1016/j.palaeo.2019.109255
https://doi.org/10.1016/j.palaeo.2019.109255
Publikováno v:
Facies. 56:279-294
The Padeha Formation in the Eastern-Alborz Mountains (northeast Iran) is an Early to Middle Devonian syn-rift succession. Siliciclastic rocks (conglomerates, sandstones, mudstones, and red paleosols) to non-marine carbonates (yellowish calcretes, dol
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fe40932bab746a6fa6c9e92dfa032e36
https://doi.org/10.1007/s10347-009-0200-x
https://doi.org/10.1007/s10347-009-0200-x