Zobrazeno 1 - 10
of 29
pro vyhledávání: '"I. V. Talovina"'
Publikováno v:
Геодинамика и тектонофизика, Vol 15, Iss 3 (2024)
The western margin of Central Iran – the Nain area – is composed of the Mesozoic ophiolitic mélanges deposited during the Late Cretaceous. The Nain and Darrech Deh faults whose trace indicators can be seen in the study area are among the larges
Externí odkaz:
https://doaj.org/article/9302e60efec84896b95bcf65df04b511
Publikováno v:
Геодинамика и тектонофизика, Vol 14, Iss 2 (2023)
Within the Urumieh-Dokhtar Magmatic Arc in the central part of Iran, the formation of which is associated with the Neotethys closure, there are many porphyry copper deposits and ore occurrences. One of them is the Astaneh porphyry copper ore deposit,
Externí odkaz:
https://doaj.org/article/58a57eac1b0a4b8db6fbdae0f5ae2d86
Publikováno v:
Известия высших учебных заведений: Геология и разведка, Vol 63, Iss 2, Pp 8-20 (2020)
Background. Large-scale geological structures, such as lineaments, are of great research interest due to their potential to mark the presence of ore fields.Aim. To determine the relationship between ore deposits, lineaments and large-scale faults in
Externí odkaz:
https://doaj.org/article/378bc4d1190744a3a2ebcb57cbeaa87c
Publikováno v:
Записки Горного института, Vol 236, Pp 142-142 (2019)
In the southern part of the Khur area, there is faults system with predominantly North-West strike. This network of tectonic disturbances is one of the most important fault systems in Central Iran which crosses Paleozoic metamorphic rocks, Cretaceous
Externí odkaz:
https://doaj.org/article/afcce09e9dc04b8e82bc1299d122dd78
Publikováno v:
Записки Горного института, Vol 232, Pp 341-341 (2018)
University museums are a group of educational museums of various specializations that are created to support the educational process, serve as a scientific research base for the academic teaching staff and students, and contribute to the knowledge de
Externí odkaz:
https://doaj.org/article/175a48e4586e437b9f08409e5fcac6a1
Autor:
I. V. Talovina, G. Khaide
Publikováno v:
Записки Горного института, Vol 221, Pp 629-629 (2016)
Data are presented on the results of X-Ray structural and thermal analyses, data from chemical and microscopic studies of serpentines of chrysotile Mg3Si2O5(OH)4 – pecoraite Ni3Si2O5(OH)4 series from the silicate nickel deposits in the Urals. Nomen
Externí odkaz:
https://doaj.org/article/69f16ee7da214b4eb78fdd7e67f9a59e
Publikováno v:
International Journal of Image and Data Fusion. 12:155-175
Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) satellite imagery was used to identify argillic, phyllic and propylitic alteration zones and mapping geological structural feat...
Publikováno v:
Mining Informational and analytical bulletin. 5:173-180
Publikováno v:
Minerals, Vol 10, Iss 2, p 129 (2020)
Minerals
Volume 10
Issue 2
Minerals
Volume 10
Issue 2
Profound knowledge of the structure and texture of rocks and ores as well as the behavior of the materials under external loads is essential to further improvements in size reduction processes, particularly in terms of liberation size. New analytical
Publikováno v:
E3S Web of Conferences, Vol 192, p 02023 (2020)
The complexity of deep processing of fine-grained and refractory mineral raw materials is determined by the difficulty of disclosing aggregates of ore components during disintegration and extracting them into commercial products of standard quality.