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在火山岩产物发育区开展大比例尺地质测量工作的最主要任务之一,就是划分出旨在发现金属矿床的远景地段。如果广泛地应用研究裂隙构造的遥感方法,上述问题是不难解决的.鄂霍次克-楚科奇火山带矿床成因论研究者认为,构造因素,首先是线性断裂和火山构造成因构造在内生金属矿床形成及分布中起着主导性作用。在火山-构造成因构造中,矿体通常富集在边缘部分和中心部分,且受与火山-构造成因构造相切的断裂以及弧状断裂与长期活动的正交和斜交系统断裂交叉带所控制.
One of the most important tasks in carrying out large-scale geological surveys in volcanic product development areas is to identify the long-term prospects for the discovery of metal deposits. The above problems are not difficult to solve if the remote sensing method for studying fissure structure is widely used.The researchers of the genesis of the Okhotsk-Chukotka volcano belt suggest that the structural factors are firstly the formation of linear faults and volcanic tectonics The formation and distribution of raw metal deposits play a leading role. In the volcano-tectonic causation, ore bodies are usually enriched in the marginal and central parts and are controlled by fractures that are tangent to the volcano-tectonic causality and to the intersection of the normal and oblique systems of arcuate and long-term activities .