Ore bodies are jointly controlled by both strata and structures, and usually they are distributed in folded layers' fissures, structural fissures and joints or in the broken belts of fold flanks.
矿体受地层和构造联合控制，一般产在褶皱的层间剥离裂隙、构造裂隙及节理中，或产于褶皱翼部的断裂破碎带内。
The results show that the upper crustal structure is relatively well-distributed laterally and obviously by layers vertically.
结果显示上部地壳结构总体上横向比较均匀，纵向分层明显。
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