Modern Minerals Formation Genesis in Kavalerovsky Tin–Ore District Technogenic System (Primorsky Krai)
Parameters and conditions of crystallization for the majority of hypergenic and technogenic minerals have not yet been studied, as their determination is often difficult due to their imperfect crystalline structure (X-ray amorphous) and formation in polymineral compounds. The article discusses the f...
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doaj-622887f6420a46da8e553d8d50e19ecf2020-11-25T02:05:44ZengMDPI AGMinerals2075-163X2020-01-011029110.3390/min10020091min10020091Modern Minerals Formation Genesis in Kavalerovsky Tin–Ore District Technogenic System (Primorsky Krai)Valentina Zvereva0Anastasiya Lysenko1Konstantin Frolov2Laboratory of Hypergene Processes Geochemistry, Far East Geological Institute, Far Eastern Branch, Russian Academy of Sciences, 159 Prospekt 100-letiya, 690022 Vladivostok, RussiaLaboratory of Hypergene Processes Geochemistry, Far East Geological Institute, Far Eastern Branch, Russian Academy of Sciences, 159 Prospekt 100-letiya, 690022 Vladivostok, RussiaDepartment of Chemical and Resource-saving Technologies, School of Natural Sciences, Far Eastern Federal University, 8 Sukhanova St., 690090 Vladivostok, RussiaParameters and conditions of crystallization for the majority of hypergenic and technogenic minerals have not yet been studied, as their determination is often difficult due to their imperfect crystalline structure (X-ray amorphous) and formation in polymineral compounds. The article discusses the formation conditions of 20 hypergenic and technogenic minerals from technogenic waters in the mining industrial system of the Kavalerovsky district tin−sulfide deposits (Primorsky krai) in Russia. For various ratios of hypogenic minerals−host rocks in ore and in tailings in a wide temperature range (from −25 to 45 °C), the Eh-pH parameters and the minerals paragenesis were established. All hypergenic and technogenic minerals formed during modeling were found and diagnosed in the Kavalerovsky tin−ore district mining industrial technogenic system.https://www.mdpi.com/2075-163X/10/2/91physicochemical modelinghypergenesistechnogenesishypergenic and technogenic mineralsassociation or paragenesisenrichment tailingstechnogenic waters (minesludge and drainage) |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Valentina Zvereva Anastasiya Lysenko Konstantin Frolov |
spellingShingle |
Valentina Zvereva Anastasiya Lysenko Konstantin Frolov Modern Minerals Formation Genesis in Kavalerovsky Tin–Ore District Technogenic System (Primorsky Krai) Minerals physicochemical modeling hypergenesis technogenesis hypergenic and technogenic minerals association or paragenesis enrichment tailings technogenic waters (mine sludge and drainage) |
author_facet |
Valentina Zvereva Anastasiya Lysenko Konstantin Frolov |
author_sort |
Valentina Zvereva |
title |
Modern Minerals Formation Genesis in Kavalerovsky Tin–Ore District Technogenic System (Primorsky Krai) |
title_short |
Modern Minerals Formation Genesis in Kavalerovsky Tin–Ore District Technogenic System (Primorsky Krai) |
title_full |
Modern Minerals Formation Genesis in Kavalerovsky Tin–Ore District Technogenic System (Primorsky Krai) |
title_fullStr |
Modern Minerals Formation Genesis in Kavalerovsky Tin–Ore District Technogenic System (Primorsky Krai) |
title_full_unstemmed |
Modern Minerals Formation Genesis in Kavalerovsky Tin–Ore District Technogenic System (Primorsky Krai) |
title_sort |
modern minerals formation genesis in kavalerovsky tin–ore district technogenic system (primorsky krai) |
publisher |
MDPI AG |
series |
Minerals |
issn |
2075-163X |
publishDate |
2020-01-01 |
description |
Parameters and conditions of crystallization for the majority of hypergenic and technogenic minerals have not yet been studied, as their determination is often difficult due to their imperfect crystalline structure (X-ray amorphous) and formation in polymineral compounds. The article discusses the formation conditions of 20 hypergenic and technogenic minerals from technogenic waters in the mining industrial system of the Kavalerovsky district tin−sulfide deposits (Primorsky krai) in Russia. For various ratios of hypogenic minerals−host rocks in ore and in tailings in a wide temperature range (from −25 to 45 °C), the Eh-pH parameters and the minerals paragenesis were established. All hypergenic and technogenic minerals formed during modeling were found and diagnosed in the Kavalerovsky tin−ore district mining industrial technogenic system. |
topic |
physicochemical modeling hypergenesis technogenesis hypergenic and technogenic minerals association or paragenesis enrichment tailings technogenic waters (mine sludge and drainage) |
url |
https://www.mdpi.com/2075-163X/10/2/91 |
work_keys_str_mv |
AT valentinazvereva modernmineralsformationgenesisinkavalerovskytinoredistricttechnogenicsystemprimorskykrai AT anastasiyalysenko modernmineralsformationgenesisinkavalerovskytinoredistricttechnogenicsystemprimorskykrai AT konstantinfrolov modernmineralsformationgenesisinkavalerovskytinoredistricttechnogenicsystemprimorskykrai |
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