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江西银山矿田伴生金银综合回收利用研究 总被引:2,自引:0,他引:2
叙述了银山铜铅锌多金属矿田铅锌成矿系列和铜硫成矿系列6个成矿带中伴生金银的赋存状态、富集特征和成矿规律,并进行伴生金银相关性分析。认为伴生金银是以独立矿物存在为主,主要载体矿物有黄铜矿,含砷铜矿物、黄铁矿、方铅矿和闪锌矿。Au、Ag与Pb、Zn、Cu、S密切相关。同时分析了金银生产中存在的具体问题,提出综合回收金银的措施和建议。 相似文献
275.
本文介绍了作者运用地质力学方法、原理并借鉴国际研究动态,涉足侵入接触构造研究获取的部分成果。基本要点包括:(1)侵入接触构造自成系统;(2)可分3种基本型式;(3)是岩体侵位动力和区域构造应力双重作用的结果;(4)控矿构造的多期活动与水压破裂相关;(5)一般所谓外接触带构造,实质为热动力变质构造. 相似文献
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Large national budgets are required for flood damage reduction projects, making it critical to ensure that public money used
therein be spent efficiently. Accordingly, reliable assessment of flood damage is a critical issue in analysis of the economic
aspects of flood damage reduction projects. To this end, this study aims to provide a GIS (geographical information system)-based
technique for distributed flood damage assessment. We consider two aspects of flood damage assessment from an engineering
and economic perspective, i.e. flood inundation analysis and multi-dimensional flood damage analysis (MD-FDA). To perform
this assessment, we used a GIS-based framework and data processing method to assess damages. The proposed methodology was
applied to flood control channel projects for flood disaster prevention in the Anyang Stream Basin in Korea and presents detailed
GIS data processing and assessment results. Findings from this study may contribute to the improvement of usability of MD-FDA
and may provide research directions for integrating economic and engineering factors. This distributed technique will also
assist in the decision-making process when evaluating the economic feasibility of flood damage reduction projects for structural
and non-structural measures. 相似文献
278.
混酸溶解矿石样品,在酒石酸介质中,用电感耦合等离子体发生光谱法(ICP-AES)测定溶液中的铌钽。该方法ρ(Nb2O5)和ρ(Ta2O5)在0~20 μg/mL时,铌钽原子发射光谱强度与浓度呈良好的直线关系,Nb、Ta标准曲线相关系数尺分别为0.999 9和0.999 7。检出限分别为0.023 μg/mL和0.072 μg/mL。本方法测定标准样品,测定值与认定值相符。对实际样品分析,Nh、Ta的相对标准偏差(n=6)分别为0.42%~2.3%和1.8%~3.3%,加标回收率均为97%~103%,适合地质找矿、选冶等领域的样品测试。 相似文献
279.
Zhou Taofa Wu Mingan Fan Yu Duan Chao Yuan Feng Zhang Lejun Liu Jun Qian Bing Franco Pirajno David R. Cooke 《Ore Geology Reviews》2011,43(1):154-169
The Middle-Lower Yangtze (Changjiang) River Valley metallogenic belt is located on the northern margin of the Yangtze Craton of eastern China. Most polymetallic deposits in the Changjiang metallogenic belt are clustered in seven districts where magmatism of Mesozoic age (Yanshanian tectono-thermal event) is particularly extensive. From west to east these districts are: E-dong, Jiu-Rui, Anqing-Guichi, Lu-Zong, Tong-Ling, Ning-Wu and Ning-Zhen. World-class iron ore deposits occur in the Lu-Zong and Ning-Wu ore clusters, which are mainly located in continental fault-bound volcanic-sedimentary basins. One of these deposits is the Longqiao iron deposit, discovered in the northern part of the Lu-Zong Basin in 1985. This deposit consists of a single stratabound and stratiform orebody, hosted in sedimentary carbonate rocks of the Triassic Dongma'anshan Formation. A syenite pluton (Longqiao intrusion) is situated below the deposit. The iron ore is massive and disseminated and the ore minerals are mainly magnetite and minor pyrite. Wall rock alteration mostly consists of skarn minerals, such as diopside, garnet, potassic feldspar, quartz, chlorite, phlogopite and anhydrite. Thin sedimentary siderite beds of Triassic age occur as relict laminated ore at the top and the margin of the magnetite orebody. These sideritic laminae are part of Triassic evaporite-bearing carbonate deposits (Dongma'anshan Formation).Sulfur isotopic compositions show that the sulfur in the deposit was derived from a mixture of magmatic hydrothermal fluids and carbonate–evaporite host rocks. Similarly, the C and O isotopic compositions of limestones from the Dongma'anshan Formation indicate that these rocks interacted with magmatic hydrothermal fluids. The O isotopic compositions of the syenitic rocks and minerals from the deposit show that the hydrothermal magnetite and skarn minerals were formed from magmatic fluids. The Pb isotopic compositions of sulfides are similar to those of the Longqiao syenite. Phlogopite coexisting with magnetite in the magnetite ores yielded a plateau age of 130.5 ± 1.1 Ma (2σ), whereas the LA-ICP MS age of the syenite intrusion is 131.1 ± 1.5 Ma, which is slightly older than the age of phlogopite.The Longqiao syenite intrusion may have crystallized from a parental alkaline magma, generated by partial melting of lithospheric mantle, during extensional tectonics. The ore fluids were probably first derived from magma at depth, later emplaced in the sedimentary rocks of the Dongma'anshan Formation, where it interacted with siderite and evaporite-bearing carbonate strata, resulting in the formation of magnetite and skarn minerals. The Longqiao iron deposit is a skarn-type stratabound and stratiform mineral system, genetically and temporally related to the Longqiao syenite intrusion. The Longqiao syenite is part of the widespread Mesozoic intracontinental magmatism (Yanshanian event) in eastern China, which has been linked to lithospheric delamination and asthenospheric upwelling. 相似文献
280.
酒泉盆地青西凹陷下沟组湖相热水沉积岩锶同位素地球化学特征 总被引:10,自引:0,他引:10
以地质背景、物质组分和岩石组构分析为基础,对酒泉盆地青西凹陷下沟组湖相热水沉积钠长石—铁白云石岩进行了Sr同位素地球化学研究。结果表明,热水沉积岩87Sr/86Sr比值变化范围为0.712 25~0.717 81,平均值0.715 61,远高于同期海水和下沟组玄武岩,略高于代表早白垩世湖水锶同位素组成的藻灰岩,但低于基底壳源硅铝质岩,反映热流体不可能为单纯的湖水或幔源岩浆水;其中直接化学结晶沉淀的纹层状泥微晶热水沉积岩锶同位素比值变化范围较小,可代表均一化的热卤水池流体锶同位素组成特征;指示不同喷流口位置的“水爆角砾岩”锶同位素组成变化较大,但同一位置的热水角砾与胶结物锶同位素组成基本一致,说明两者应属于具相同成因意义的同期热水喷流沉积产物;综合青西凹陷下沟组湖相热水沉积岩锶同位素地球化学特征,初步推测早白垩世湖底热流体可能为富集硅铝质基底岩石高放射成因Sr的深循环下渗湖水与少量上升幔源岩浆水构成的混合热流体,可为青西凹陷早白垩世湖底热流体性质的确定以及热流体循环动力学模型和热水沉积模式的建立奠定基础。 相似文献