以地表地质和勘探地震资料为基础，对洛阳盆地的负反转构造进行了研究。

The negative inverted structure in Luoyang basin is studied on the basis of geological data and prospecting seismic data.

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通过野外地表地质调查，建立了浙江省宁波市大榭岛地下储油罐区地表构造模型；

After the surface geology investigation, the surface tectonic model of the site is set up in the paper.

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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。

Based on data of gravity survey, seismic exploration, aerial magnetical survey and surface geology, the central fault belt was identified in the Qaidam Basin.

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