斯洛伐克Pezinok锑矿床热液演化的锑同位素变化

IF 4.4 2区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS Mineralium Deposita Pub Date : 2023-10-20 DOI:10.1007/s00126-023-01222-7
Andreas B. Kaufmann, Marina Lazarov, Stefan Weyer, Martin Števko, Stefan Kiefer, Juraj Majzlan
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引用次数: 0

摘要

在这项工作中,我们研究了来自斯洛伐克Pezinok附近矿床两个亚阶段的锑(Sb)矿物的原位同位素组成。原生Sb矿物的δ123Sb值在−0.4 ~ +0.8‰之间,沿降水序列逐渐增大。在第二阶段,各剖面δ123Sb值最低的是早期形成的辉锑矿(FeSb2S4), δ123Sb值最高的是辉锑矿(Sb2S3)和华菱锑矿(Sb2O3)。第三次阶段也有类似的趋势,从最初形成的辉锑矿开始,接着是角砾石(Sb2S2O)、华氏褐铁矿、硅辉锑矿(均为Sb2O3)和沙氏锑矿(FeSb2O4)。采用瑞利分馏模型,流体δ123Sb初始值为+0.3‰,对所有矿物采用相同的矿物-流体分馏因子,可以合理地解释这一演化过程。因此,结构上观察到的矿化顺序可以通过微量元素含量的减少和连续结晶的锑矿物中较重的δ123Sb值来证实。第三阶段的锑可能来自于第二阶段早期形成的辉锑矿的氧化溶解。数据解释虽然受到缺乏可靠的矿物-流体分馏因素的限制,但表明每个子阶段的Sb沉淀来自于偶发性金属沉淀,可能与流体和所有被研究的Sb矿物之间类似的Sb同位素分馏有关。随着温度的下降,流体的沉淀引起的大的同位素变化可能是破译热液矿床中金属来源的障碍。然而,Sb同位素似乎是一种很好的工具,可以增强我们对热液系统如何运作的理解。
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Changes in antimony isotopic composition as a tracer of hydrothermal fluid evolution at the Sb deposits in Pezinok (Slovakia)

In this work, we investigated in situ isotopic compositions of antimony (Sb) minerals from two substages of the ore deposits near Pezinok (Slovakia). The δ123Sb values of the primary Sb minerals range from −0.4 and +0.8‰ and increase progressively along the precipitation sequence. In the substage II, the early-formed gudmundite (FeSbS) shows in all sections the lowest δ123Sb values, followed by berthierite (FeSb2S4), stibnite (Sb2S3), and valentinite (Sb2O3) with the heaviest δ123Sb values. A similar trend was observed for the substage III, from the initially-formed stibnite, followed by kermesite (Sb2S2O), valentinite, senarmontite (both Sb2O3), and schafarzikite (FeSb2O4). The evolution can be rationalized by a Rayleigh fractionation model with a starting δ123Sb value in the fluid of +0.3‰, applying the same mineral-fluid fractionation factor to all minerals. Thus, the texturally observed order of mineralization is confirmed by diminishing trace element contents and heavier δ123Sb values in successively crystallized Sb minerals. Antimony in substage III was likely supplied from the oxidative dissolution of stibnite that formed earlier during substage II. The data interpretation, although limited by the lack of reliable mineral-fluid fractionation factors, implies that Sb precipitation within each substage occurred from an episodic metal precipitation, likely associated with a similar Sb isotope fractionation between fluid and all investigated Sb minerals. Large isotopic variations, induced by precipitation from a fluid as a response to temperature decrease, may be an obstacle in deciphering the metal source in hydrothermal ore deposits. However, Sb isotopes appear to be an excellent instrument to enhance our understanding on how hydrothermal systems operate.

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来源期刊
Mineralium Deposita
Mineralium Deposita 地学-地球化学与地球物理
CiteScore
11.00
自引率
6.20%
发文量
61
审稿时长
6 months
期刊介绍: The journal Mineralium Deposita introduces new observations, principles, and interpretations from the field of economic geology, including nonmetallic mineral deposits, experimental and applied geochemistry, with emphasis on mineral deposits. It offers short and comprehensive articles, review papers, brief original papers, scientific discussions and news, as well as reports on meetings of importance to mineral research. The emphasis is on high-quality content and form for all articles and on international coverage of subject matter.
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