The First Results of a Study of Large Diamonds from Industrial Deposits of Yakutia

IF 0.8 4区 地球科学 Q3 GEOLOGY
L. D. Bardukhinov, E. M. Sedykh, A. A. Evstratov, K. V. Garanin, N. N. Zinchuk
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Abstract

A representative amount of diamonds larger than 10.8 carats extracted from deposits of Yakutia during separate ore processing of each kimberlite pipe has been studied for the first time. It is shown that, according to the diamond typomorphic characteristics of habit, nitrogen content, and aggregation, as well as hydrogen concentration in diamond, it is possible to carry out a preliminary evaluation of the deposit to predict the presence of large and giant diamonds. It has been established that large diamonds from the deposits of the Daldyn-Alakitsky area have wide variations of nitrogen impurity and its aggregations in comparison with diamonds from the Malobotuobinsky and Srednemarkhinsky areas. It is determined that the content of large diamonds in the pipes of Yakutia is inversely proportional to the number of rounded dodecahedroids. The most promising deposits for finding large diamonds are those in which the majority of diamonds belong to one population—average nitrogen low-aggregated diamonds that were formed at a temperature of ~1100°C. According to the study of geological collections of diamonds, it is shown that, in kimberlite pipes with an increased nitrogen content in diamonds, an increase in the proportion of large diamonds in the deposit is noted. On the contrary, according to the aggregation of nitrogen in diamonds, as a parameter of postgrowth history, there is a negative correlation with the content of large diamonds. An increased value of the concentrations of hydrogen in diamonds not only negatively affect the total diamond content of the deposit, but also generally control the decrease in the content of large diamonds.

Abstract Image

雅库特工业矿藏大型钻石研究的初步成果
摘要 首次研究了在雅库特矿床对每个金伯利岩管进行单独矿石加工时提取的大于 10.8 克拉的代表性金刚石。研究表明,根据金刚石的习性、含氮量、聚集度以及金刚石中氢浓度等金刚石类型学特征,可以对矿床进行初步评估,以预测大型和巨型金刚石的存在。已经确定,与马洛博图奥宾斯基和斯列德纳马克金斯基地区的钻石相比,达尔丁-阿拉基茨基地区矿藏中的大钻石在氮杂质及其聚集方面有很大差异。据测定,雅库特管道中大型钻石的含量与圆形十二面体的数量成反比。最有希望发现大型金刚石的矿藏是那些大部分金刚石属于一个群体--平均氮低聚集金刚石,在约 1100°C 的温度下形成的矿藏。对钻石地质藏品的研究表明,在金伯利岩管中,如果钻石的含氮量增加,矿床中大钻石的比例也会增加。相反,根据金刚石中氮的聚集情况,作为生长后历史的参数,与大粒金刚石的含量呈负相关。金刚石中氢浓度值的增加不仅会对矿床的总钻石含量产生负面影响,而且一般会控制大钻石含量的减少。
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来源期刊
Geology of Ore Deposits
Geology of Ore Deposits 地学-地质学
CiteScore
1.10
自引率
14.30%
发文量
24
审稿时长
6-12 weeks
期刊介绍: Geology of Ore Deposits is a periodical covering the topic of metallic and nonmetallic mineral deposits, their formation conditions, and spatial and temporal distribution. The journal publishes original scientific articles and reviews on a wide range of problems in theoretical and applied geology. The journal focuses on the following problems: deep geological structure and geodynamic environment of ore formation; distribution pattern of metallogenic zones and mineral deposits; geology and formation environment of large and unique metallic and nonmetallic deposits; mineralogy of metallic and nonmetallic deposits; physicochemical and isotopic characteristics and geochemical environment of ore deposition; evolution of ore-forming systems; radiogeology and radioecology, economic problems in exploring, developing, and mining of ore commodities.
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