Scholarlink

Abstract <p>This paper presents the results of a study of sublimates (mineral deposits from volcanic gases) that have been collected in silica tubes placed at high-temperature vents in the Eastern Fumarolic Field of Avachinsky Volcano, Kamchatka in 2013–2023. The ICP-MS and ICP-AES methods were used to obtain the concentration distributions for 62 elements throughout the tube lengths, i.e., along the temperature gradient. A total of 35 sublimate phases corresponding to naturally occurring minerals have been identified, in addition to 7 sublimate phases for which there are no naturally occurring analogues, or they are still unknown. The overall mineral sequence with decreasing temperature is as follows: Na and K halogenides; Na, K, and Ca sulphates; sulfides; As–S amorphous glass, and Tl, Pb, and Bi halogenides. The most abundant phases are As–S glass, SiO<sub>2</sub> (cristobalite), NaCl, KCl, Na<sub>2</sub>SO<sub>4</sub>‒K<sub>2</sub>SO<sub>4</sub>; rare phases: KCdCl<sub>3</sub>, K<sub>2</sub>Pb(SO<sub>4</sub>)<sub>2</sub>, Tl(I, Cl, Br), Pb<sub>2</sub>Tl(Cl, I, Br)<sub>5</sub>, PbTl<sub>3</sub>(Cl, I, Br)<sub>5</sub>, Pb(Cl, I, Br)<sub>2</sub>, Tl<sub>3</sub>BiI<sub>6</sub>, ReS<sub>2</sub>, the sulfides of Pb–Zn–Cd–In and AgI.</p>

错误：搜索内容不能为空，请输入英文关键词
错误：关键词超出字数限制，请精简
高级检索

The Chemical and Phase Composition of High Temperature Sublimates: Avachinsky Volcano, Kamchatka

  • 期刊论文

  • 发表日期：

    2025年8月19日

查看全文
  • E. Yu. Plutakhina,
  • N. A. Malik,
  • I. Yu. Nikolaeva

摘要

Abstract

This paper presents the results of a study of sublimates (mineral deposits from volcanic gases) that have been collected in silica tubes placed at high-temperature vents in the Eastern Fumarolic Field of Avachinsky Volcano, Kamchatka in 2013–2023. The ICP-MS and ICP-AES methods were used to obtain the concentration distributions for 62 elements throughout the tube lengths, i.e., along the temperature gradient. A total of 35 sublimate phases corresponding to naturally occurring minerals have been identified, in addition to 7 sublimate phases for which there are no naturally occurring analogues, or they are still unknown. The overall mineral sequence with decreasing temperature is as follows: Na and K halogenides; Na, K, and Ca sulphates; sulfides; As–S amorphous glass, and Tl, Pb, and Bi halogenides. The most abundant phases are As–S glass, SiO2 (cristobalite), NaCl, KCl, Na2SO4‒K2SO4; rare phases: KCdCl3, K2Pb(SO4)2, Tl(I, Cl, Br), Pb2Tl(Cl, I, Br)5, PbTl3(Cl, I, Br)5, Pb(Cl, I, Br)2, Tl3BiI6, ReS2, the sulfides of Pb–Zn–Cd–In and AgI.