Zobrazeno 1 - 8
of 8
pro vyhledávání: '"Balandeh Aminzadeh"'
Publikováno v:
Journal of Economic Geology, Vol 14, Iss 3, Pp 95-121 (2022)
The Kal-Baneh Mn deposit is located 56 km northwest of Jiroft city in the southeast of the Sanandaj-Sirjan Zone. The ore mineralization occurs as layered, banded, massive, and disseminated textures within radiolarian cherts of the upper parts of the
Externí odkaz:
https://doaj.org/article/9d27a72fd7614eefb5e6ffc34caf1b4e
Autor:
Balandeh Aminzadeh
Publikováno v:
Journal of Economic Geology, Vol 11, Iss 3, Pp 387-401 (2019)
Introduction More than 300 sediment-hosted Zn–Pb deposits and occurrences have been recognized in Iran (Rajabi et al., 2013). Most of these deposits are concentrated in the Central Alborz, Tabas-Posht-e-Badam, Malayer-Esfahan and Yazd-Anarak metal
Externí odkaz:
https://doaj.org/article/fb243cc9b2c04ff79b173e7713c583bc
Autor:
Marzieh Alimolaei, Balandeh Aminzadeh
Publikováno v:
Journal of Economic Geology, Vol 11, Iss 2, Pp 321-337 (2019)
Introduction The rare earth elements (REEs) are classified into light (La, Ce, Pr, Nd, and Sm), medium (Eu, Gd, Tb, Dy, and Y), and heavy (Ho, Er, Tm, Yb, and Lu) groups (Seredin and Dai, 2012). Goldschmidt (1933) was the first to study the REEs in
Externí odkaz:
https://doaj.org/article/ed66eb7f13244e7cac743b2a32ec17d8
Publikováno v:
Journal of Economic Geology, Vol 2, Iss 2, Pp 191-197 (2011)
Molybdenite occurs in five forms in the Sar Cheshmeh porphyry copper deposit, namely, (1)-veinlets with quartz-molybdenite, (2)-veinlets with quartz-molydenite that were filled with pyrite, (3)-veinlets with quartz-molybdenite-pyrite–chalcopyrite,
Externí odkaz:
https://doaj.org/article/c9b34fad456140cbb424fe44d24e5f47
Autor:
Balandeh Aminzadeh
Publikováno v:
Arabian Journal of Geosciences. 14
The Tarz Zn–Pb deposit is located in the Tabas block of the Central Iranian Microcontinent and consists of stratabound orebodies hosted by dolomitic limestone of the Middle Triassic Shotori Formation. Two stages of sphalerite were identified in the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7c495efd394bc7d8dcdad92ca3edc0d5
https://doi.org/10.1007/s12517-021-08404-5
https://doi.org/10.1007/s12517-021-08404-5
Autor:
Yaser Rahimpour, Balandeh Aminzadeh
Publikováno v:
Geochemistry. 81:125827
The Godar Sabz Mn deposit is located in the Nain-Baft ophiolitic belt in the northeast margin of the Sanandaj-Sirjan zone, Iran. The Nain-Baft back-arc extensional basin resulted from the subduction of the oceanic crust of Neo-Tethys under the southe
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::118c26897623d754b81af025eb1b8b7b
https://doi.org/10.1016/j.chemer.2021.125827
https://doi.org/10.1016/j.chemer.2021.125827
Publikováno v:
Ore Geology Reviews. 81:369-395
The Ravar Copper Belt (RCB) is located in the north of Kerman in the Central Iran. This belt is a part of the Tabas Block which is 450 km long and 50 km wide. It is bounded by Kuhbanan- Kalmard Fault in the west and Nayband Fault in the east. The mai
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2e41fb23334082ddf531619ecba0d78d
https://doi.org/10.1016/j.oregeorev.2016.09.035
https://doi.org/10.1016/j.oregeorev.2016.09.035
Publikováno v:
Resource Geology. 61:290-295
This paper presents the results of a study on the variation of Re in the Sar Cheshmeh porphyry copper-molybdenum deposit in Iran. The Re content was determined in monomineralic molybdenite separates from veinlets and from molybdenum milled floatation
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::cdbe4ba5aa5468a9569033c787f6d637
https://doi.org/10.1111/j.1751-3928.2011.00165.x
https://doi.org/10.1111/j.1751-3928.2011.00165.x