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为了查明海底活动断裂的几何形态和运动特征,许多方法被广泛地用于这一目的。地震资料通常是研究海底活动断层的最重要方法之一,然而地震剖面一般反映活动断裂有关的褶皱构造,并非反映断裂面本身。多波束水深测量用于探测活动断裂构造和生长历史,因为海底地形是活动断裂的最直接证据。深潜器和深拖可以直接观察海底全形过程。上述方法被广泛用于西相模湾活动断裂的综合研究。
Many methods have been widely used for this purpose in order to ascertain the geometry and movement characteristics of the submarine active faults. Seismic data are often one of the most important methods of studying submarine faulting. Seismic profiles, however, generally reflect fold structures associated with active faults and do not reflect the fracture surface itself. Multibeam water depth measurements are used to detect active fault structures and growth history as the seabed terrain is the most direct evidence of active faults. Deep submersibles and deep trailers can directly observe the entire seafloor process. The above method is widely used in the comprehensive study of active faults in the West Sagam Bay.