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第三次国际金伯利岩会议于1982年9月8日至11日在法国克勒蒙菲朗召开。会议由法国国家科学研究中心、国际火山学与地球内部化学协会、欧洲地质科学联合会、法国地质学会、法国矿物学与结晶学协会和克勒蒙第二大学等单位主办。会议广泛涉及金伯利岩岩石学、地球化学和构造学,以及由金伯利岩推导的上地幔性质,其讨论范围已扩大到玄武岩岩浆起源与下部地壳之间关系。会议还分别组织了玄武岩岩浆作用动力学地质旅行(简称火山岩地质旅行)和上地幔二辉橄榄岩与大陆地壳底部麻粒岩过渡带性质的地质旅行(简称莫霍面地质旅行)。
The Third International Kabul Rock Conference was held in Kleenex, France from September 8 to 11, 1982. The conference was sponsored by the French National Center for Scientific Research, the International Association of Volcanology and Intra-Earth Chemistry, the European Association of Geological Sciences, the French Geological Society, the French Association of Mineralogy and Crystallography and the Second University of Kölmont. The conference covered a wide range of kimberlite petrology, geochemistry and tectonics, and the nature of the upper mantle derived from kimberlite. The scope of the discussion has broadened to include the relationship between basaltic magma origin and the lower crust. The conference also separately organized the geological travel of basalt magmatic kinetic geologic travel (referred to as the volcanic geologic travel) and the geological travel of the transition zone between the upper mantle lherzolites and the bottom of the continental crust (referred to as the Moho Geological Travel).