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科拉超深钻的钻进和探测首次提供了以前无法达到的深度的有关古老大陆地壳成分和构造的直接资料。岩石密度和它们弹性的各向异性已成为当今地表地质正式描述形式和参考剖面的主要参数。所给出的完整模型的证据是基于科拉超深钻的探测及辅助的地表地质研究。模型认为贝辰加矿区是一个幔源火山岩－侵入岩中心式成矿系统的水平部分。本文还对铜－镍硫化物矿床产出条件给予了新的解释，并有助于理解贝辰加矿区在贝辰加—依曼德—瓦尔朱格缝合带中的位置
For the first time ever, drilling and probing of Cora ultra-deep drilling provided direct information on the composition and tectonics of the ancient continental crust to a depth previously unachievable. Rock density and their anisotropy of elasticity have become the main parameters of the formal description and reference profiles of today’s surface geology. The evidence given for the complete model is based on the exploration of Coora ultradeep drilling and on the aid of surface geology studies. The model suggests that the Beichencao mining area is a horizontal part of a mantle-derived volcanic-intrusive central metallogenic system. This paper also gives a new interpretation of the copper-nickel sulfide deposit output conditions and helps to understand the location of the Beichen mining area in the Beichena-Ehime-Valdauge suture