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遵照伟大领袖毛主席关于“教育必须为无产阶级政治服务,必须同生产劳动相结合”,的教导,一九七五年五至八月,我们协同冶金地质九三四队进行了野外地质调查,发现石碌地区构造形迹的形成及其结构面的力学性质,都与南北方向挤压作用有关.因此,根据石碌群地层形变特征,运用地质力学的原理,分析石碌岭复式向斜构造形迹的力学性质,构造应力场活动方式,推求石碌岭——金波岭复式大向斜的存在,从构造控矿方面阐明石碌铁矿的形成,提出继续寻找石碌式铁矿,扩大外围远景的意见。由于工作时间不长,对前人的成果来不及深入的研究,我们的意
In accordance with the guidance of Chairman Mao, the great leader, that “education must serve proletarian politics and must be integrated with productive labor.” From May to August 1975, we collaborated with the 934th Team of the Metallurgical Geology in conducting field geology surveys, It is found that the formation of Shiku area structural features and the mechanical properties of the structural plane are all related to the extrusion in the north and south directions.Therefore, according to the deformation characteristics of Shilu formation and using the principle of geomechanics, the mechanics of Shiluling double syncline structural features The structure of stress field activity, the existence of the Shiluling - Jinboling double synclinal syncline, and the formation of Shilu iron ore from the aspects of structural control of ore deposit, and the suggestion of continuing to find Shilu iron ore and expanding its peripheral vision . As the working time is not long, the achievements of the predecessors too late to study, our intention