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斑岩

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It was proved that deformation modulus, compression strength, tensile strength, shear strength and Poisson ratio of lamprophyre could not meet the design requirements after high pressure cement grouting, so chemical grouting was proposed to treat the lamprophyre. High permeable epoxy resin was employed to grout the weathered lamprophyre.

因仅靠单纯的高压水泥灌浆无法使岩体的变形模量、抗压、抗拉、抗剪强度以及泊松比等物理力学指标达到设计要求,应有针对性地采用化学灌浆方法对煌斑岩脉进行加固处理。

Lamprophyric veins, which mainly spread parallel to gold ore veins, might have provided some ore-forming materials and volatiles for gold mineralization.

斑岩脉空间上与金矿脉关系密切,形成时间与金成矿作用接近,岩脉的Au、Ag和挥发分的含量较高。

They are mica, lithium beryllium tantalum and gem bearing peg matite, marine volcanic massive sulfide, magmatic copper nickel, metasedimentary iron, gold bearing low grade metamorphosed carbon clastic rocks and gold bearing ductile shear zone. A great progress has been made in recent exploration of porphyry copper.

已知矿床的主要类型有伟晶岩型矿床、与海相火山岩有关的块状硫化物矿床、岩浆铜镍硫化物型矿床、沉积变质型铁矿、浅变质含碳细碎屑岩型金矿和韧性剪切带型金矿床,近年来在斑岩型铜矿床的找矿工作有了新进展。

Maoming City is rich in mineral resources with nearly hundreds of minerals and 27 proved reserves. Of them, oil shale and kaolin boast the most reserves in the country; quality and reserves of rare earth and orthophyre tin ore also play an important role in the country; jade mine, which called "the jade in the South", is one of the three biggest jade mines in our country.

茂名市矿藏丰富,各种矿物近百种,已探明储量的有27种,油母叶岩、高岭土储量名列全国之冠;稀土、斑岩型锡矿的质量和储量也在全国占有一席之地;有&南方碧玉&之称的玉石矿是我国三大玉矿之一。

Veined,stockwork and alteration-sheathed gold ores have been found in the area,belonging to four genetic types:the volcanic hydrothermal ores related to early—middle Carboniferous volcanism; subvolcanic hydrothermal ores related to intermediate—acidic porphyry intrusions; hydrothermal ores to the granitic intrusion and dynamo- hydrothermal ores related to regional dynamic metamorphism along the faults.

矿石类型有含金石英大脉型、石英网脉型和蚀变岩型。矿床成因类型有4种:一为火山热液型,其成因与区内早—中石炭世火山作用有关;二为潜火山热液型,与中酸性斑岩体侵位有关;三为岩浆热液型,与花岗质岩浆的侵位有关;四为动力变质热液型,沿断裂带分布于蚀变玄武岩中,系区域动力变质作用的产物。

From the point of the ΣREE,δEu, geochemical parameters and standard REE distribution patterns, lead-zinc mineralization altered rocks in the Shengmikeng deposit have close genetic relationship with the potassic trachyte porphyry with SHRIMP zircon age of 138.3±1.4 Ma.

从∑REE总量值、δEu值、地球化学参数及标准稀土元素配分模式图上看,生米坑铅锌矿化蚀变岩与钾质粗面斑岩具有密切的成因联系。

Pb-Sr-Nd isotope tracing shows that the source of magma in the island-arc belt of Zhongdian area belongs to crust-mantle mixed type. The proportion of mantle material is 59.5% crust's is 40.5%. Similarly, for the Cenozoic alkaline-enriched porphyries, the source of magma is crust-mantle mixed type, but the proportion of mantle material is increased to 54.3%.

通过Pb-Sr-Nd同位素示踪,发现中甸地区岛弧带岩浆物质来源为壳幔混合型,印支期的地幔物质的比例m平均值为59.5%,地壳物质的为40.5%;剑川、北衙等地的新生代富碱斑岩的m值平均54.3%,也表现为壳幔混合型,但与印支期火山-侵入杂岩相比,其地壳物质的比例增高。

A systematic study on S and/or Pb isotopic compositions of the copper-bearing porphyries, ore minerals and andesite of the deposit shows that S isotopic compositions of ore minerals are similar to those of porphyries.

矿石矿物(208Pb/204Pb=37.917~38.230,平均值38.075;207Pb/204Pb=15.528~15.614,平均值15.571;206Pb/204Pb=17.929~18.082,平均值17.981)与矿化斑岩(208Pb/204Pb=37.832、37.883,207Pb/204Pb=15.529、15.538,206Pb/204Pb=17.906、17.910)以及安山岩(208Pb/204Pb=37.816~37.884,207Pb/204Pb=15.549~15.562,206Pb/204Pb=17.845~17.919)的初始铅组成基本一致,变化范围较小,表明三者具有相同的来源;在铅构造模式图上,所有样品铅同位素均位于造山带演化线上或附近,在铅同位素源区判别图中,均落入造山带和下地壳区域,这表明Pb主要来源于壳幔混合。

The fluid geochemistry research bears out the ratio of W/R becomes more few from epithermal to porphyry.

成矿流体地球化学研究表明,大气降水在成矿系列中起到了重要的作用,水/岩比值由浅成低温热液低硫型→浅成低温热液高硫型→斑岩型有变小的趋势。

Their distribution districts contain both world-class porphyry copper gold as well as hot-spring gold deposits.

埃达克岩的分布区与世界级斑岩铜-金矿和浅成热泉金矿成矿带分布一致。

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然而,正如其名字所指出的那样,CD盘不能写,也不能用任何方式改变其内容。

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