波兰苏台德东部Karkonosze花岗质岩体中的银化合物矿物

IF 1.1 4区 地球科学 Q3 GEOLOGY
A. KozŁowski
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引用次数: 1

摘要

:Kozłowski,A.和Matyszczak,W.2022。波兰苏台德东部Karkonosze花岗质岩体中的银化合物矿物。波兰地质学报,72(4),443–468。Warszawa。在Varisan Karkonosze花岗质岩体的13个位置发现了20种硫化物、砷化物、硒化物、碲化物、硫盐和氯化物银矿物。以前,该地区只知道其中一种矿物。这些发现包括在出版物中被描述为罕见或异常罕见的物种,例如绿柱石和黑柱石。它们出现在伟晶岩和石英脉中;描述了它们的副基因。研究包括化学成分的测定、公式计算和XRD图谱的记录。共生石英中的包裹体研究表明,它们是从低温热液中结晶出来的,具有常见但低组分的CO2。结果表明,Karkonosze花岗质岩石中微量元素(含银)形成的矿物是由于寄主花岗质岩石的局部再结晶程度。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Silver compounds as minerals in the eastern Karkonosze granitoid pluton, Sudetes, Poland
: Kozłowski, A. and Matyszczak, W. 2022. Silver compounds as minerals in the eastern Karkonosze granitoid pluton, Sudetes, Poland. Acta Geologica Polonica , 72 (4), 443–468. Warszawa. Twenty silver minerals of the sulphide, arsenide, selenide, telluride, sulphosalt and chloride groups were found in 13 locations in the Variscan Karkonosze granitoid pluton. Previously only one of these minerals was known from this area. The findings include species characterized in publications as rare or exceptionally rare, e.g., muthmannite and tsnigriite. They occur in pegmatites and quartz veins; their parageneses are described. The studies include determination of chemical compositions, formulae calculations and recording of XRD patterns. Inclusion studies in paragenetic quartz indicate that they crystallized from epithermal fluids with a common but low component of CO 2 . The results suggest that the minerals formed from trace elements (Ag included) in the Karkonosze granitoid due to very local degrees of recrystallization of the host granitoid.
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来源期刊
Acta Geologica Polonica
Acta Geologica Polonica 地学-地质学
CiteScore
1.70
自引率
18.20%
发文量
0
审稿时长
>12 weeks
期刊介绍: Acta Geologica Polonica publishes original and review papers on all aspects of basic geology, with particular focus on sedimentology, stratigraphy, palaeontology, regional geology, structural geology, and regional petrography. All papers are published in English.
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