Based on data of gravity survey, seismic exploration, aerial magnetical survey and surface geology, the central fault belt was identified in the Qaidam Basin.
重力、航磁、地震、遥感、地表地质等资料的研究结果表明，柴达木盆地基底存在着中央断裂带。
High Density Resistivity is widely used in engineering geology exploration because of such advantages as its abundant data, low cost, good anti-jamming and et al.
高密度电法以其数据量丰富、成本低、受场地干扰小等优点而广泛应用于工程地质勘察中。
Magnetic anomaly data are very valuable in the field of resource exploration, deep subsurface geology and geophysics research.
磁异常资料在地质矿产资源勘查以及深部地质方面有着十分重要的作用。
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