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There are also large scale gypsum and celestite deposit,middle scale sulfur iron ore within 10 km~2.,besides lead-zinc deposit.Some basic geological problems are still ambiguous,and ore deposit genesis are controversial.

除铅锌矿外,在矿区不到10km~2的范围内尚有大型石膏矿和天青石矿,以及中型硫铁矿等,成矿地质条件相当复杂。

Main ore-forming fluid is oil-field brine in celestite mineralization system. Ore-forming fluid is dominated by meteoric water, mixed with formation water.

锶矿成矿系统中成矿流体主要为油田水,成矿流体以大气降水为主,加上盆地压实释放水,通过深大断裂循环加热、水-岩相互作用和湖盆蒸发作用等一系列演化过程,同时,还有来自深部的地质流体的混入而形成。

Ore source of celestite mineralization system is complex in this area. Weathering and erosion of the floor of the basin and the mountain around the basin, evaporite sediment in the earlier, deep water, Mesozoic and Cenozoic volcanism can provide the strontium. In particular, serving as initial ore source, oil-field brine supplies the majority of strontium.

该区矿源场分析表明,锶的来源有基底和周边山系风化剥蚀来源、老含盐地层补给、深部水和中、新生代火山活动补给;其中,盆地基底和周边老山风化以及深部水补给为主要来源,特别是油田水作为矿源层为锶矿床的形成提供了大量锶源。

The study of fluid inclusions in sphalerites and associated gangue minerals (quartz, celestite, calcite and gypsum) shows that homogenization temperatures cluster around 110-150℃, with salinities of 1.6-18.0 wt% NaCl equivalent. The fluid temperature increased with the decrease in salinities during the main ore stages, and there is also a systematic westward decrease in temperature and increase in salinity in the Jinding ore district.

闪锌矿及相关脉石矿物(石英、天青石、方解石、石膏)中流体包裹体观测的均一温度主体在110~150℃,盐度在1.6%~18.0% NaCl;在时间上,大规模成矿主要阶段伴随着流体温度的不断升高和盐度的逐渐降低;在空间上,金顶矿区空间上从东到西,成矿流体温度明显降低,盐度系统性升高。

The Product Is Suitable for separating the granularity is 0.3-0.02mm of the iron ore,limonite,chromites,trotline,zirconium,retiles,monazite,centimes,wolfram ore,Stan nary,tantalum minerals,niobium minerals and other non feerous metal,rare metal and non metal.

本设备适用于分选粒度0.3--0.02毫米细料的铁矿、钛铁矿、铬铁矿、硫铁矿、锆英石、金红石、独居石、磷乙矿、钨矿、锡矿、钽矿、铌矿以及具有比重差异的其他有色金属、稀有金属和非金属矿物体。

Based on the detailed contrast between the chondrite normalized REE pattern s and REE geochemical evolution law, this paper proves that the ore bearing fluid for the Carlin type gold deposits in the area mainly originates from the upper mantle differentiation, and that the crust matter partly contaminates the plutonic ore bearing fluid during moving from mantle to crust.

通过稀土元素配分模式的详细对比和地球化学演化规律的研究,论证了滇黔桂地区金矿的成矿物质主要来源于上地幔分异,但深部成矿流体在运移至地壳的成矿过程中不可避免地混染了部分地壳物质,从而在一定程度上掩盖了成矿物质的实质来

Based on the detailed contrast between the chondrite normalized REE patterns and REE geochemical evolution law, this paper proves that the ore bearing fluid for the Carlin type gold deposits in the area mainly originates from the upper mantle differentiation , and that the crust matter partly contaminates the plutonic ore bearing fluid during moving from mantle to crust.

通过稀土元素配分模式的详细对比和地球化学演化规律的研究,论证了滇黔桂地区金矿的成矿物质主要来源于上地幔分异,但深部成矿流体在运移至地壳的成矿过程中不可避免地混染了部分地壳物质,从而在一定程度上掩盖了成矿物质的实质来

We want to buy Manganese Ore, Iron Ore, Molybdenum, Chromite, Non-Metallic Mineral Products

我们要采购锰矿石,矿砂,锄,铬铁矿,非金属的矿物产品

Based on the above results, a new ore-forming process of sand-type uranium ore associated coal measures was proposed.

基于上述结果,提出了亲煤型砂岩铀矿的成矿过程,为揭示煤与铀矿共伴生关系提供了基础数据。

The process by which cyanide solution, added to ore, dissolves and removes gold from the ore into the solution.

加到矿石上的氰化物溶液把黄金从矿石中溶解出来使之进入溶液中。

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听,指出并且检查你的答案。

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