Zobrazeno 1 - 10
of 15
pro vyhledávání: '"A. R. Galamay"'
Autor:
Xiaolong Yuan, Fanwei Meng, Xiying Zhang, Jinchang Sheng, A. R. Galamay, Huaide Cheng, Yongshou Li, Weiliang Miao, Wenxia Li, Qiliang Tang, Jun Li, Yongsheng Du
Publikováno v:
Frontiers in Earth Science, Vol 9 (2021)
Polyhalite occurrence in the Kunteyi Playa in the Qaidam Basin has been known for many years. However, the genetic mechanism of this deposit remains unclear. In this study, a typical section in the playa depocenter is selected to study the polyhalite
Externí odkaz:
https://doaj.org/article/27ca7645d4734e8b93b7ea68a9b8c0b5
Autor:
Anatoliy R. Galamay, Muazzez Çelik Karakaya, Krzysztof Bukowski, Necati Karakaya, Yaroslava Yaremchuk
Publikováno v:
Minerals
Volume 13
Issue 2
Pages: 171
Volume 13
Issue 2
Pages: 171
The halogenesis of the Messinian Tuz Gölü Basin corresponds to the sulfate type and the magnesium sulfate subtype. Compared to the Messinian Sea brines, they have a slightly higher [Na+] concentration, which is 96.6–116.4 g/L, and a much lower [K
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::e3088e1508527e4077e8b1f7e0e694fd
Publikováno v:
Minerals
Volume 11
Issue 8
Minerals, Vol 11, Iss 831, p 831 (2021)
Volume 11
Issue 8
Minerals, Vol 11, Iss 831, p 831 (2021)
Currently, fluid inclusions in halite have been frequently studied for the purpose of paleoclimate reconstruction. For example, to determine the air temperature in the Middle Miocene (Badenian), we examine single-phase primary fluid inclusions of the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::1d80124abe94878f5dca1c0298959351
Publikováno v:
Geology and Geochemistry of Combustible Minerals. 4:78-95
The fluid inclusions in the marine Middle Ordovician halite of the Majiagou Salt Formation of the Ordos Basin (China) have been investigated. In addition to the primary inclusions the secondary ones of several generations were also detected. The flui
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::95e8dc9999d997826889164bbce76894
https://doi.org/10.15407/ggcm2019.04.078
https://doi.org/10.15407/ggcm2019.04.078
Publikováno v:
Minerals, Vol 10, Iss 1113, p 1113 (2020)
Minerals
Volume 10
Issue 12
Minerals
Volume 10
Issue 12
The geochemical data and the study of fluid inclusions in primary halite are invaluable sources of saline basin information. Most of the previous analyses of salt from the Carpathian area have been obtained by studying the halite samples collected fr
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::9f77cf503cd1d5c4a003210c1478782a
https://www.mdpi.com/2075-163X/10/12/1113
https://www.mdpi.com/2075-163X/10/12/1113
Publikováno v:
Minerals, Vol 10, Iss 823, p 823 (2020)
Minerals
Volume 10
Issue 9
Minerals
Volume 10
Issue 9
Fluid inclusions in halite are widely used in research to determine the conditions of sedimentation in salt basins and reconstruct the chemical composition of seawater during a specific geological period. However, previous preliminary studies of the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::94045508f3ae808eb60a994c041ea58a
https://www.mdpi.com/2075-163X/10/9/823
https://www.mdpi.com/2075-163X/10/9/823
Publikováno v:
Geochemistry International. 56:719-734
Organic component in the Lower Permian salt sequence in the southern part of the Yakshinskoe deposit of the Upper Pechora potassium basin is represented by dispersed organic matter, liquid hydrocarbons in fluid inclusions in halite, as well as inclus
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::14149759e9d8ea422b3395d3e450a008
https://doi.org/10.1134/s0016702918070108
https://doi.org/10.1134/s0016702918070108
Autor:
Aleksandr Lyubchak, Pei Ni, Krzysztof Bukowski, Аnatolіy R. Galamay, Fanwei Meng, Yongsheng Zhang
Publikováno v:
Geological Quarterly.
During the Middle Ordovician, the salt deposits of the Majiagou Formation of the Ordos Basin in North China formed, the halite including various genetic types of fluid inclusion. In this study, fit-testing of primary inclusions was performed to recon
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c17ea83d9c2e07b0db470763c646d72e
https://doi.org/10.7306/gq.1490
https://doi.org/10.7306/gq.1490
Publikováno v:
Marine and Petroleum Geology. 122:104644
Abundant continental salt deposits were formed in salt basins in eastern China around the Cretaceous–Tertiary periods. However, whether these evaporites had a marine or non-marine origin remains controversial. The Jintan Basin is located between So
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::cba8b0303d1f086366845cae66f55d18
https://doi.org/10.1016/j.marpetgeo.2020.104644
https://doi.org/10.1016/j.marpetgeo.2020.104644
Autor:
Fanwei MENG, Yongsheng ZHANG, Anatoliy R. GALAMAY, Krzysztof BUKOWSKI, Pei NI, Enyuan XING, Limin JI
Publikováno v:
Geological Quarterly. 62
Fluid inclusions in halite can directly record the major composition of evaporated seawater; however, Ordovician halite is very rare. The Ordovician is a key time during the evolution history because profound changes occurred in the planet’s ecosys
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e1f11f864ec9ee9a50e6eb0b3d398a89
https://doi.org/10.7306/gq.1409
https://doi.org/10.7306/gq.1409