摩洛哥 Bou-Izourane 地区锌铅矿区的地质特征

IF 0.9 4区 地球科学 Q3 GEOLOGY Geological Quarterly Pub Date : 2024-04-25 DOI:10.7306/gq.1739
Jamal Achmani, Ilham Chraibi, Said Courba, Soufiane Boudrif
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引用次数: 0

摘要

位于摩洛哥高阿特拉斯山脉的 Bou-Izourane 地区的锌铅矿储量估计为 40 200 吨,平均品位为 20% 的锌和 3.5% 的铅。该矿床发育于切割 Liassic 碳酸盐泥灰岩矿床的 N-S 至 NNW-SSE 走向断层上。准成因矿物序列包括方铅矿、闪锌矿和晚期方解石。在 Bou-Izourane 矿石中,方铅矿氧化成铈矿和闪锌矿氧化成铁闪锌矿的现象很常见,这与流星水的渗入和这些硫化物的氧化有关。锌铅矿化与与塔马泽格特火成岩相关的萤石矿脉平行,但这两种矿化(即锌铅矿化和萤石矿化)之间没有岩相学或实地关系。在 Bou-Izourane 的锌铅矿化中,稀土元素和钇(REY)的分布与摩洛哥中部高阿特拉斯的密西西比河谷型(MVT)矿化有着显著的相似性,尽管其浓度更接近与塔马泽格特岩浆热液活动有关的萤石中的稀土元素和钇(REY)浓度。不过,对它们在后萤石方解石和后锌铅方解石中的分布进行的分析表明,这两种方解石具有很强的一致性,表明这两种方解石与同一阶段有关,并且具有共同的起源。Bou-Izourane 的锌铅矿远景区的分类仍存在争议,在 MVT 型矿化(与摩洛哥高阿特拉斯中部的大多数锌铅矿化类似)和与 Tamazeght 的岩浆热液活动有关的矿化(可提供热量和成矿物质)之间摇摆不定。对 Bou-Izourane 的锌铅矿进行定性,对今后在摩洛哥高阿特拉斯地区勘探锌铅矿床至关重要,并可推动该地区锌铅矿开采的发展,从手工开采发展到专业开采。
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Geological features of the Zn-Pb prospect in the Bou-Izourane district (Morocco)

The Zn-Pb mineralization in the Bou-Izourane district, located in the High Atlas Mountains of Morocco, contains estimated reserves of 40 200 tons of ore with an average grade of 20% Zn and 3.5% Pb. It is developed on N–S to NNW–SSE-trending faults that cut Liassic carbonate marl deposits. The paragenetic mineral sequence consists of galena, sphalerite and late-stage calcite. Oxidation phases of galena into cerussite and sphalerite into smithsonite are common in the Bou-Izourane ore, linked to the infiltration of meteoric waters and the oxidation of these sulphides. The Zn-Pb mineralization runs parallel to the fluorite veins associated with the igneous rocks of Tamazeght, but no petrographic or field relationship has been demonstrated between these two mineralizations (i.e., Zn-Pb and fluorite). The distribution of rare earth elements and yttrium (REY) in the Zn-Pb mineralization of Bou-Izourane shows a notable similarity with the Mississippi Valley Type (MVT) mineralization of the Central High Atlas of Morocco, although the concentrations more closely resemble those of REY in fluorite linked to the magmatic-hydrothermal activity of Tamazeght. However, the analysis of their distribution in post-fluorite calcite and post-Zn-Pb calcite reveals a strong concordance, suggesting that these two calcites are associated with the same phase and have a common origin. The classification of the Zn-Pb prospect in Bou-Izourane remains controversial, fluctuating between an MVT-type mineralization, similar to most Zn-Pb mineralizations in the Central High Atlas of Morocco, and a mineralization linked to the magmatic-hydrothermal activity of Tamazeght, which could provide heat and metallogenic material. Characterizing the Zn-Pb ore of Bou-Izourane is crucial for the future exploration of zinc and lead deposits in the High Atlas of Morocco and could advance the development of Zn-Pb mining in the region, from artisanal exploitation to professional mining

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来源期刊
Geological Quarterly
Geological Quarterly 地学-地质学
CiteScore
2.20
自引率
0.00%
发文量
19
审稿时长
>12 weeks
期刊介绍: The policy of the Geological Quarterly is to publish significant contributions of information and geological insight relevant to an international readership. The journal has been issued since 1957 at the Polish Geological Institute - National Research Institute and, at present, is the leading Earth sciences journal in Poland. All aspects of Earth and related sciences, and universal and broad regional rather than locally oriented topics are covered. The journal is intended to be an international forum for the exchange of information and ideas, particularly on important geological topics of Central Europe.
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