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海南岛西部的戈枕断裂带处于东南地洼区儋县地穹的西南缘。由于该区地壳经历了前地槽、地槽、地台、地洼等四个发展阶段，致使该区经受区域变质、混合岩化、岩浆侵入和动力变质等多种地质作用，为戈枕断裂带多阶段成矿创造了良好的地质构造条件，并使受戈枕断裂控制的金矿床在矿体形态、产状、矿化特点、围岩蚀变、矿石类型、成矿阶段、金矿成矿物质来源、成矿的地质、地球化学特征等许多方面，具有多因复成金矿成矿特点。构造控金模拟实验结果为戈枕断裂带构造变形及构造作用使金活化迁移、富集提供实验依据。
The Gezhen fault zone in the western part of Hainan Island lies in the southwestern margin of the Qiongxian Earth Dome in the southeastern depression area. Because of the developmental stages of the former crust, the trough, the platform and the diwa, the crust in the area has undergone various geological processes such as metamorphism, migmatization, magmatic intrusion and dynamic metamorphism, The multi-stage mineralization has created good geological conditions and controlled the gold deposits controlled by the Gezhen fault in terms of ore body morphology, occurrence, mineralization characteristics, wall rock alteration, ore type, metallogenic stage, Mineral resources, mineralization geology, geochemical characteristics and many other aspects, with many due to complex gold mineralization characteristics. The structure control experiment results show that the geotectonic deformation and tectonic function of the Gezhen fault zone make the activation and migration of gold and enrich the experimental data.