缅甸纳莫原生翡翠矿体特征与成因研究
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P619.28+ 1; P611.1

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Characteristics and genesis of the primary jadeite jade orebody in Nammaw, Myanmar
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    摘要:

    缅甸纳莫翡翠原生矿体呈透镜状侵入于蛇纹石化超基性岩中,矿体中分布有团块状围岩捕虏体。矿物结晶顺序为:具帚状结构的粗晶柱状硬玉→具柱状交织结构的细晶柱状硬玉→具流动构造的微晶柱状硬玉与粒状方沸石组成的绿色翡翠细脉→粒状方沸石脉→钠长石与石英组成的脉。绿色翡翠细脉沿矿体构造裂隙呈条带状、脉状产出,主要由微晶柱状硬玉组成,其长度为0.06~0.08mm,宽为0.01~0.015mm。矿体主要由具柱状交织结构的细晶柱状硬玉组成,是超基性岩浆结晶分异演化的产物。

    Abstract:

    The primary jadeite jade orebody in the lenticular form intruded into the serpentinous ultrabasic rocks. Trapped massive bodies with composition of country rocks are distributed in the jadeite jade orebody. The order of crystallization in the orebody is coarse-prismatic jadeite with broom-like texture→fine-prismatic jadeite with interlocking texture→veins of macro-prismatic jadeite with flowage structure and granulous analcite→veins of analcite→veins of albite and quartz. The green jadeite jade, 0.06~0.08 mm in length and 0.01~0.015 mm in width, consists mainly of macro-prismatic jadeite with flowage structure. The orebody consists mainly of fine-prismatic jadeite with interlocking texture. It is held that the jadeite jade orebody was formed bythe evolution of ultrabasic magma during crystallization.

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张良钜, 2004. 缅甸纳莫原生翡翠矿体特征与成因研究[J]. 岩石矿物学杂志, 23(1):49~53.
ZHANG Liang-ju, 2004. Characteristics and genesis of the primary jadeite jade orebody in Nammaw, Myanmar[J]. Acta Petrologica et Mineralogica, 23(1): 49~53.

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