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Seismic Investigation and 3D Tomography in the Ross Sea (Antarctica) for Western Ice Sheet Evolution Studies

机译:西部冰板进化研究中罗斯海(南极洲)的地震调查与3D层析

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Recent studies based on multichannel seismic surveys carried out in Ross Sea (Eastern Basin, Antarctica) detected an important erosion surface in the Lower Pliocene, called RSU2. The RSU2 horizon determines a sharp change both in the margin geometry and in the depositional sequences, which may be interpreted as a major increase of the glacial influence. In this work, we present the preliminar results obtained from the processing and the tomographic inversion of the multichannel seismic data collected by the OGS_Explora vessel during the last Antarctic cruise. This study, mainly based on the reflection seismic method, provides new information about the erosion process that produced the RSU2 horizon, and about the nature of adjacent sediments.
机译:基于罗斯海(东部盆地,南极洲)进行的多通道地震调查的最近研究检测到叫做RSU2的下部全茂的重要侵蚀表面。 RSU2 Horizo​​ n确定边缘几何形状和沉积序列中的急剧性变化,其可以被解释为冰川影响的主要增加。在这项工作中,我们介绍了在最后一个南极巡航期间由OGS_EXPLORA船收集的多通道地震数据的处理和断层反转获得的预先参见。本研究主要基于反射地震方法,提供了有关产生RSU2地平线的侵蚀过程的新信息,以及关于相邻沉积物的性质。

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