Collected Item: “Fluid inclusion study in quartz of the Rudnik Pb-Zn-Cu-Ag skarn deposit, Serbia”
Врста публикације
Рад у зборнику
Верзија документа
објављена
Језик
енглески
Аутор/и (Милан Марковић, Никола Николић)
Stefan Petrović, Ronald J. Bakker, Vladica Cvetković, Rade Jelenković
Наслов рада (Наслов - поднаслов)
Fluid inclusion study in quartz of the Rudnik Pb-Zn-Cu-Ag skarn deposit, Serbia
Назив конференције (зборника), место и датум одржавања
Mineral Resources in a Changing World-17th SGA Biennial Meeting, Zurich, between 28th August and 1st September 2023
Издавач (Београд : Просвета)
Genéve: Society for Geology Applied to Mineral Deposits
Година издавања
2023
Сажетак рада на енглеском језику
Abstract. Six types of fluid inclusions were identified in
three growth zones of hydrothermal quartz from the
Rudnik skarn deposit. In the core zone, primary two-phase
fluid inclusions of high (type 1) and moderate salinity (type
2) homogenized to liquid between 350-430 °C and 340-
420 °C, respectively. Raman analysis revealed that the
vapour phases are a CO2-CH4 gas mixture, with a
predominance of CO2. The core contains and dispersed
vapour-rich fluid inclusions of low salinity (type 3)
composed of CO2-CH4-H2S gas mixture with significant
amounts of H2S, as well as liquid-rich fluid inclusions (type
4) predominantly composed of pure water and small
vapour phase with lower homogenization temperatures
between 174-284 °C. In the transition zone, primary fluid
inclusions arranged perpendicular to the growth zone
(type 5) homogenize over a wide range of temperatures
between 235-401 °C. The vapour phase is a CO2-CH4 gas
mixture additionally enriched in CH4 compared to the other
types. Fluid inclusions in paths of the rim zone of the
quartz (type 6) have a homogenization temperature
between 259-385 °C. The vapour phase is a CO2-CH4
mixture with reduced CH4 content, while the liquid phase
has a low salinity.
three growth zones of hydrothermal quartz from the
Rudnik skarn deposit. In the core zone, primary two-phase
fluid inclusions of high (type 1) and moderate salinity (type
2) homogenized to liquid between 350-430 °C and 340-
420 °C, respectively. Raman analysis revealed that the
vapour phases are a CO2-CH4 gas mixture, with a
predominance of CO2. The core contains and dispersed
vapour-rich fluid inclusions of low salinity (type 3)
composed of CO2-CH4-H2S gas mixture with significant
amounts of H2S, as well as liquid-rich fluid inclusions (type
4) predominantly composed of pure water and small
vapour phase with lower homogenization temperatures
between 174-284 °C. In the transition zone, primary fluid
inclusions arranged perpendicular to the growth zone
(type 5) homogenize over a wide range of temperatures
between 235-401 °C. The vapour phase is a CO2-CH4 gas
mixture additionally enriched in CH4 compared to the other
types. Fluid inclusions in paths of the rim zone of the
quartz (type 6) have a homogenization temperature
between 259-385 °C. The vapour phase is a CO2-CH4
mixture with reduced CH4 content, while the liquid phase
has a low salinity.
Почетна страна рада
98
Завршна страна рада
100
Линк
https://sga2023.ch/wp-content/uploads/2023/08/SGA2023_session-1a.pdf
Шира категорија рада према правилнику МПНТ
М30
Ужа категорија рада према правилнику МПНТ
М33
Пројект у склопу кога је настао рад
176019
Ниво приступа
Отворени приступ
Лиценца
Creative Commons – Attribution-No Derivative Works 4.0 International
Формат датотеке
.pdf