Geological mapping of kimberlite magmatism as an assessment of diamond-bearing objects in Western Yakutia

N. Shakhurdina
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Abstract

Тhe results of generalization and GIS integration of the results of the study of all known indigenous deposits and manifestations of diamonds located in the distributed and undistributed fund of the subsoil of the Russian Federation are presented. The work takes into account the results of prospecting, exploration and exploitation works, minutes of meetings of regional (TKZ) and federal (RKZ and GKZ) commissions on mineral reserves and published data. As a result, a GIS-integrated database was created containing 1,319 objects, for each of which key parameters were determined: coordinates, shape, size, age, average diamond content, forecast resources, and diamond reserves. It was established that the indigenous diamond deposits are concentrated in the Central Siberian subprovincia and account for 2.3 % of all known kimberlite bodies, diamond-bearing kimberlite bodies in the Yakut diamond-bearing province – 282, the predominant body shape is a pipe (59 %). There is no correlation between the size of kimberlite bodies and their diamond content, small pipes, as well as large diatremes, can be industrially diamondiferous, the prevailing absolute age of industrially diamondiferous kimberlites is 329-382 million years.
绘制金伯利岩岩浆地质图,评估西雅库特含钻石物体
介绍了对俄罗斯联邦底土分布式和非分布式基金中所有已知本地矿藏和钻石表现的研究成果进行归纳和地理信息系统整合的结果。这项工作考虑到了探矿、勘探和开采工作的结果、地区(TKZ)和联邦(RKZ 和 GKZ)矿产储量委员会的会议记录以及公布的数据。因此,建立了一个包含 1 319 个对象的地理信息系统集成数据库,并确定了每个对象的关键参数:坐标、形状、大小、年龄、平均钻石含量、预测资源量和钻石储量。结果表明,本土金刚石矿藏集中在中西伯利亚次大陆,占所有已知金伯利岩体的 2.3%,雅库特金刚石矿产省的含钻金伯利岩体为 282 个,主要岩体形状为管状(59%)。金伯利岩体的大小与其金刚石含量之间没有相关性,小的管状金伯利岩体和大的二矽管状金伯利岩体都可能含有工业金刚石,含有工业金刚石的金伯利岩体的普遍绝对年龄为 3.29-3.82 亿年。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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