Zobrazeno 1 - 10
of 10
pro vyhledávání: '"Hadi Amin-Rasouli"'
Publikováno v:
Journal of Economic Geology, Vol 13, Iss 4, Pp 789-815 (2021)
Introduction The lenticular Shahneshin barite deposit (N: 35°39'36'' and E: 46°36'11'') is located 80 km northeast of Marivan, Kurdistan Province; north Sanandaj-Sirjan Zone (Stöcklin, 1968). The deposit consists of stratiform ore and stringer zo
Externí odkaz:
https://doaj.org/article/c27026fe9290459d8c861ae15a60fb70
Karaftu Cave in the northwest of Divandareh includes four floors plus an underground area. The bat hall and its underground area are covered with guano deposits. 14C dating indicates the onset of guano deposition is about 14260±50 BP years, and its
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2bf19546d71c5037d2c0c9665bce30c3
https://doi.org/10.21203/rs.3.rs-2811114/v1
https://doi.org/10.21203/rs.3.rs-2811114/v1
Autor:
Hadi Amin-Rasouli, Hossein Azizi, Yoshihiro Asahara, John S. Armstrong-Altrin, Shahla Mahmodyan
Publikováno v:
Arabian Journal of Geosciences. 15
Autor:
Yaghoob Lasemi, Hadi Amin-Rasouli
Publikováno v:
The Sedimentary Record. 19
Autor:
Hadi Amin Rasouli
Publikováno v:
Journal of Zankoy Sulaimani - Part A. :249-265
Autor:
Hadi Amin Rasouli
Publikováno v:
Journal of Zankoy Sulaimani - Part A. :81-109
Publikováno v:
Carbonates and Evaporites. 23:21-38
The Lower Triassic Sorkh Shale Formation is a dominantly red colored marginal marine succession deposited in the north-south trending Tabas Basin of east central Iran. It is correlated with the unconformity-bounded lower limestone member of the Elika
Autor:
Hadi Amin-Rasouli, Yaghoob Lasemi
Publikováno v:
Sedimentary Geology. 201:302-320
Meter-scale buildups constructed exclusively by archaeocyaths have been recognized within the uppermost Lower Cambrian siliciclastic succession of Eastern Alborz in northern Iran. They are the only known Toyonian reefs in Iran and adjacent countries
Publikováno v:
Principles of Tidal Sedimentology ISBN: 9789400701229
Carbonate tidalites are sediments deposited in supratidal, intertidal and the adjacent shallow subtidal environments by tidal, biogenic, chemical and diagenetic processes and are among the most common deposits in ancient carbonate platform succession
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f01c754b4781d2751a41989e437f5f5f
https://doi.org/10.1007/978-94-007-0123-6_21
https://doi.org/10.1007/978-94-007-0123-6_21