Zobrazeno 1 - 10
of 17
pro vyhledávání: '"Farhang Aliyari"'
Autor:
Farhang Aliyari
Publikováno v:
Journal of Economic Geology, Vol 11, Iss 1, Pp 169-189 (2019)
Introduction The Agh Ziarat (Au±Cu±Mo) Polymetallic deposit is located at 75 north of Urmia, northwestern part of the Sanandaj-Sirjan Zone. Several studies have been carried out on chemical composition, geochemistry, petrology, and petrogenesis of
Externí odkaz:
https://doaj.org/article/5df83589b11f48218250ffce74a6726a
Publikováno v:
Journal of African Earth Sciences. 200:104865
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6fb49a59ace522a2a7f81b360249494d
https://doi.org/10.1016/j.jafrearsci.2023.104865
https://doi.org/10.1016/j.jafrearsci.2023.104865
Mineralogy and fluid inclusion investigations in the Zarshuran gold deposit, north of Takab, NW Iran
Publikováno v:
Iranian Journal of Crystallography and Mineralogy. 27:537-550
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::468a85ec20925fb401de100f40343258
https://doi.org/10.29252/ijcm.27.3.537
https://doi.org/10.29252/ijcm.27.3.537
Publikováno v:
Journal of Geochemical Exploration. 231:106864
The Zarshuran gold deposit as sediment-hosted Carlin-type has a total reserve of 120 million metric tonnes and an average grade of 3.5 g/t Au. The dominant hydrothermal alterations associated with gold mineralization are argillic and silicic as well
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fdba6c62c32e9e98903ef1ff1c80b271
https://doi.org/10.1016/j.gexplo.2021.106864
https://doi.org/10.1016/j.gexplo.2021.106864
Publikováno v:
Journal of African Earth Sciences. 134:308-319
The aim of this study is to determine a relationship between zinc mineralization and a major fault in the Behabad area, central Iran, using the Concentration-Distance to Major Fault (C-DMF), Area of Mineralized Zone-Distance to Major Fault (AMZ-DMF),
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::19a9ceb5874538db0a5bdaaa4d37a678
https://doi.org/10.1016/j.jafrearsci.2017.06.025
https://doi.org/10.1016/j.jafrearsci.2017.06.025
Publikováno v:
Ore Geology Reviews. 127:103835
The Guijeh Qaleh iron deposit, located in the Takab district of northwestern Iran contains ca. 0.3 million metric tons (Mt) of ore at 48 wt. % Fe. The host rocks are Eocene to Oligocene volcano-sedimentary sequences consisting of andesite, trachy-and
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3575713341e376a53a9272bebb90fedd
https://doi.org/10.1016/j.oregeorev.2020.103835
https://doi.org/10.1016/j.oregeorev.2020.103835
Publikováno v:
Applied Geochemistry. 121:104694
Main aim of this study is to propose a developed zonality index for Cu-Mo porphyry deposits based on staged factor analysis with Number-Size (N-S) fractal model. This method was used in an Iranian porphyry system as named Serenu (SE Iran). The develo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::53aff20818c168d618f14bcb9c113c82
https://doi.org/10.1016/j.apgeochem.2020.104694
https://doi.org/10.1016/j.apgeochem.2020.104694
Publikováno v:
Arabian Journal of Geosciences. 11
The Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) and the Landsat-8 data were integrated with geological data to map lithologic units, lineament features, hydrothermal alteration zones, and distribution of Fe3+-bearing minera
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9e8d07d2af023779f1860f6f0c80388b
https://doi.org/10.1007/s12517-018-3822-x
https://doi.org/10.1007/s12517-018-3822-x
Publikováno v:
Ore Geology Reviews. 116:103238
The Kahang Cu-Mo porphyry deposit is located in the middle part of the Urumieh-Dokhtar Magmatic Arc, Central Iran, and is hosted by middle to late Miocene (~14 Ma) porphyritic quartz-diorite and granodiorite stocks intruded into the Eocene tuff, basa
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d36d17edfc5a4661ef4c57b6cdfe1e43
https://doi.org/10.1016/j.oregeorev.2019.103238
https://doi.org/10.1016/j.oregeorev.2019.103238
Publikováno v:
Journal of Geochemical Exploration. 140:111-125
The Qolqoleh orogenic gold deposit in the northern part of the Sanandaj–Sirjan metamorphic belt in northwestern Iran is hosted by a steeply dipping sequence of greenschist facies Cretaceous volcano–sedimentary rocks, including mafic to intermedia
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::eae8e36d04e99d039c2587144fe538ec
https://doi.org/10.1016/j.gexplo.2014.01.007
https://doi.org/10.1016/j.gexplo.2014.01.007