俾路支省库兹达尔地区Bela蛇绿岩宝石分布研究

Salman Khan, Abdul Ghaffar, Inayat Ullah, Fida Murad, Jalil Ahmed, Muhammad Ishaq Kakar
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引用次数: 0

摘要

贝拉蛇绿岩和缝合带在下部和上覆岩石中含有几种类型的宝石,如石榴石(榴石和铝榴石)、石英、水辉石、孔雀石、黄铜矿、蓝铜矿、方解石、钠辉石、绿燧石、碧玉、蛇纹石、玛瑙、绿帘石、奥辉石和原辉石。然而,在蛇纹岩等蚀变橄榄岩中发现了一些稀有宝石,如菱形石榴石,呈十二面体绿色晶体。水辉石在贝拉蛇绿岩超镁质岩中呈盆状分布,与瓦德地区巴兰湖和阿莫尔扎伊地区铬铁矿伴生在寄主岩灰岩中。在与橄榄岩蛇纹石化后形成的蚀变超镁铁质岩相关的几个地点发现了蛇纹岩。此外,由于热液侵入石灰岩等沉积岩,形成了石油和金刚石石英等稀有宝石之一;方解石也以狗齿晶体的形式存在于石灰岩中。而蓝铜矿、孔雀石和黄铜矿则形成于毗邻玄武岩的Manjawi、Nal和Sonaro铜和硫化物矿氧化带的次生矿床。绿柱石以绿色晶体形式存在于寄主岩体花岗岩中,呈斑状结构。玛瑙、碧玉、绿燧石和其他几种类型的燧石被发现与msamuange和gossan的玄武岩燧石单元有关。此外,钠辉石主要在哈扎尔甘吉镇的Nal蛇绿岩中发现,以纤维状和圆柱形晶体的形式与白云岩岩脉的裂缝和孔洞伴生。在索纳罗地区贝拉蛇绿岩的变质底岩中,大理岩和石英岩与蛇绿岩演化时期形成的绿片岩、角闪岩等变质岩相相结合。伟晶岩辉长岩中,在Ornach交叉区附近的寄主岩辉长岩中发现了长条形、棱柱状的黑色辉长岩晶体,在Ornach地区的玄武岩与辉长岩过渡带中发现了前辉长岩宝石。
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A Case Study on Distribution of Gemstone in Bela Ophiolite, District Khuzdar, Balochistan
Bela Ophiolite and suture zone host several types of gemstones in the underlain and overlain rocks such as garnet (demantoid and almandine), quartz, brucite, malachite, chrysocolla, azurite, calcite, natrolite, green chert, jasper, serpentine, agate, epidote, augite and prehnite. However, the rare gemstones including demantoid garnet are found as dodecahedron green crystals associated with the altered peridotite rocks such as serpentinite. Brucite is found in the botryoidal habit in the ultramafic rocks of Bela Ophiolite associated with the chromite mines in the Baran Lak and Amorzai area of Wadh in the host rock dunite. The serpentine is found in several locations associated with the altered ultramafic rocks formed after the serpentinization of peridotite. Furthermore, one of the rare gemstones such as petroleum and diamond quartz is formed due to the hydrothermal intrusion in the sedimentary rocks such as limestone; calcite also occurs in limestone as dogtooth crystals. While azurite, malachite and chrysocolla are formed as secondary deposits in the oxidized zone of copper and sulphide mines in the Manjawi, Nal and Sonaro associated adjacent to basalt. Moreover, epidote is found as green crystals having porphyritic texture in the host rock granite mainly in the Bakhalo area, Wadh. Agate, jasper, green chert and several other kinds of chert are found associated with the basalt chert unit in the mélange and gossan. In addition to that natrolite is found in the Nal ophiolite mainly in the Hazarghanji town found associated with the cracks and vugs of dolerite dykes as fibrous and cylindrical crystals. In metamorphic sole rocks of Bela Ophiolite in the Sonaro area, marble and quartzite are associated with the metamorphic rocks such as greenschist and amphibolite facies that are formed during the e volution period of the ophiolite. In pegmatite gabbro, the elongated and prismatic black crystals of augite are found in the host rock gabbro near the Ornach cross area, and the prehnite gemstone is found associated with the basalt and gabbroic rocks transition zone in the Ornach area.
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