极地乌拉尔地区Nyrdvomenshor矿床软玉组成及形成条件

E. Kislov, M. P. Popov, F. M. Nurmukhametov, V. F. Posokhov, V. V. Vanteev
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摘要

研究课题。研究了极地乌拉尔地区Nyrdvomenshor矿床中的软玉及其相关岩石。涅尔德门肖尔矿床位于Rai-Iz超镁铁地块的外接触层,受乌拉尔主断裂的限制。矿床是在地质勘查过程中发育的;已经为一部分押金签发了许可证。的目标。对该矿床冲积物中的软玉及相关岩石进行了研究,建立了其成因模型。方法。用双目显微镜和专用手电筒目测定性特征。用x射线荧光法测定化学成分。用ICP-MS法测定了样品中微量元素的含量。采用能量色散显微分析系统,在扫描电子显微镜下对矿物组成进行了研究。对氧的同位素组成进行了测量。结果。除维苏岩岩外,该矿床还常见水榴石岩。所研究的软玉不合格。软玉中以透闪石为主,透辉石形成残粒。玉云母分布广泛,形成两种自形晶粒,有时为鞘状,少数为伸长异形,并取代铬铁矿。辉长石上长满了铬铁矿和无辉云母的颗粒。在水石组中发现了铁优势矿物的颗粒。结论。软玉是由变质作用和交代作用共同形成的。蛇纹岩被透辉石取代,透辉石又被软玉取代。变质作用增强了蛇纹岩混杂岩的交代作用,形成了软玉的隐晶缠结纤维结构。变质和交代作用使软玉形成辉石,并使软玉开裂,使其质量下降。随着这些过程的进行,地壳流体的贡献增加,这一点得到了软玉和矿床其他岩石氧同位素组成研究结果的证实。
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Composition and formation conditions of nephrite, Nyrdvomenshor deposit, Polar Urals
   Research subject. Nephrite and related rocks from the Nyrdvomenshor deposit in the Polar Urals were studied. The Nyrdvomenshor deposit is located in the exocontact of the Rai-Iz ultramafic massif, confined to the Main Ural Fault. The deposit was developed in the process of geological exploration; a license has been issued for a part of the deposit.   Aim. To study the nephrite and related rocks from alluvial of the deposit, to formulate a model of its origin.   Methods. Qualitative characteristics were assessed visually using a binocular microscope and a special flashlight. The chemical composition was determined by the X-ray fluorescence method. The contents of trace elements were determined by ICP-MS analysis. The mineral composition was studied on a scanning electron microscope with an energy dispersive microanalysis system. Measurements of the isotopic composition of oxygen were carried out.   Results. In addition to vesuvianite rodingite, hydrogarnet rodingite was found to be common at the deposit. The studied nephrite is substandard. Tremolite predominates in nephrite, diopside forms relic grains. Uvarovite is widespread, forming both idiomorphic grains, sometimes sheath, less often elongated xenomorphic, and replacing chromite. Omphacite overgrows grains of chromite and uvarovite. Grains of the Fe-dominant mineral of the shuiskite group are noted.   Conclusions. Nephrite was formed through both metamorphic and metasomatic processes. Serpentinite was replaced by diopside, which was then replaced by nephrite. Metamorphism enhanced the metasomatism of the serpentinite melange and provided the cryptocrystalline tangled fibrous structure of the nephrite. Then metamorphism and metasomatism led to the formation of omphacite and cracking of the nephrite, which reduced its quality. As these processes progressed, the contribution of the crustal fluid increased, which is confirmed by the results of studying the oxygen isotopic composition of nephrite and other rocks of the deposit.
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