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绿辉石

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These fine quality natural kunzite crystals have very nice light lavender , pale or deep pink, or white, gray, yellow, pink to violet, green and very rarely light blue or color zone with various colors(100% natural color) From Nooristan Afghanistan,and Minas Gerais, Brazil.

天然紫锂辉石晶体标本,一般有淡淡的似熏衣草紫色、粉红,也呈无色、灰、绿、黄,较少蓝色,以及几种颜色相伴形成的色带等,颜色百分百天然,著名产地为阿富汗 Nooristan 和巴西 Minas Gerais 。

The adsorption behavior of metal ions on the silicate minerals such as quartz, beryl, spodumene, lepidolite, garnet, and the flotability of such minerals activated by the metal ions were studied.

研究了石英、绿柱石、锂辉石、锂云母、石榴子石等硅酸盐矿物对金属离子的吸附规律及矿物经金属离子活化后的浮游性,并结合矿物晶体化学特性对实验结果进行了分

Viridis, apple green, snow gray, tender and delicate lavender, is the pyroxene class typical luster.

翠绿色、苹果绿、雪花白、娇嫩的淡紫色,都是辉石类的典型色泽。

Basalt core was unchanged, and feldspar and pyroxene partly steatited in its rind.

玄武岩的核心区矿物基本无变化,外环的长石及辉石发生了皂石化,部分基质绿泥石化。

The mixed collectors studied were as following: benzyl arsonic acid-sodium butyl xanthate for walframite flotation, salicylohydroxamic acid-F〓, salicylohydroxamic acid-cupferron, salicylohydroxamic acid-TBP , F〓-TBP, cupferron-benzohydroxamic acid etc. for cassiterite flotation and mixed aliphatic acid or aliphatic amine for beryl or spodumene flotation.

研究过程中,本文选用了如下具体实例:苄基胂酸与丁基黄药浮选黑钨矿,水杨羟肟酸与F〓、水杨羟肟酸与铜铁灵、水杨羟肟酸与磷酸三丁酯、F〓与磷酸三丁酯、铜铁灵与苯异羟肟酸两两结合浮选锡石,混合脂肪胺与混合脂肪酸浮选锂辉石与绿柱石。

Is around ore shoots to be distribute with symmetry, that show the block and brecciated ores of the Tongmugou zinc deposit are fluid metasomatic reformed deposit.

后生流体交代岩(主要由透闪石、绿帘石、透辉石、黑云母、石英、绿泥石等矿物组成)显著受层间断层控制,它是流体交代原热水沉积层和热水沉积闪锌矿纹层而形成的,该矿床为热水沉积-流体交代改造矿床。

We also report the exsolution texture of Crspinel in orthopyroxene in the studied harzburgite, and suggest that it is the result of a metamorphic reaction induced by the drastic increase of oxygen fugacity during the rapid emplacement of Darbut ophiolite.

方辉橄榄岩中的斜方辉石发育铬尖晶石出溶结构,出溶棒的成分特点表明,该结构是达拉布特蛇绿岩在快速就位过程中环境氧逸度突然升高诱发变质反应的结果。

We also report the exsolution texture of Cr-spinel in orthopyroxene in the studied harzburgite, and suggest that it is the result of a metamorphic reaction induced by the drastic increase of oxygen fugacity during the rapid emplacement of Darbut ophiolite.

方辉橄榄岩中的斜方辉石发育铬尖晶石出溶结构,出溶棒的成分特点表明,该结构是达拉布特蛇绿岩在快速就位过程中环境氧逸度突然升高诱发变质反应的结果。

The ophitic and subophitic textures, elongated apatite crystals, low Al(superscript Ⅵ)/Al(superscript Ⅳ) ratios (0.00-0.28, 0.12 on average) in clinopyroxene, and low Cao content in olivine (0.04%~0.24%, average 0.12%) indicate that the gabbrowas crystallized at a low pressure.

辉长岩所具有的辉绿辉长结构、大量细长针状磷灰石、单斜辉石中较低的Al/Al值(0.00~0.28,平均为0.12)及橄榄石中较低的CaO含量(0.04%~0.24%,平均为0.12%),均体现出浅成侵入岩的特点。

The ophitic and subophitic textures, elongated apatite crystals, low AlⅥ/AlⅣ ratios (0.00 ~0.28, 0.12 on average) in clinopyroxene, and low CaO content in olivine (0.04%~0.24%, average 0.12%) indicate that the gabbro was crystallized at a low pressure.

辉长岩所具有的辉绿辉长结构、大量细长针状磷灰石、单斜辉石中较低的AlⅥ/AlⅣ(0.00 ~0.28,平均为0.12)及橄榄石中较低的CaO含量(0.04%~0.24%,平均为0.12%),均体现出浅成侵入岩的特点。

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