在毛主席的无产阶级革命路线指引下,1970年在我们工作的地区发现了601含钴硫化镍矿床.现将近年来矿区的物化探工作情况简要介绍如下.一、矿床地质和物化探異常特点矿床产于某地带北缘的蚀变超基性岩体中.岩体侵入下古生界变质岩中.主岩体走向近东西,向南倾,呈似岩墙状,以深蚀变的镁质超基性岩为主.主要岩性是滑石菱镁岩、 Under the guidance of Chairman Mao’s proletarian revolutionary line, the cobalt-bearing nickel sulphide ore bearing 601 was found in the area where we worked in 1970. The geophysical and geochemical exploration work in the mining areas in recent years is briefly described as follows: 1. Geological and Geochemical Prospecting Characteristics of the Deposits Deposits It is produced in altered ultramafic rocks in the northern margin of a certain zone, and intrusion into the Lower Paleozoic metamorphic rocks.The main rocks move towards east-west and southward, Mainly composed of ultrabasic rocks.The main lithologies are talc magnesite,