Seismic Geomorphology: Subsurface Analyses, Data Integration and Palaeoenvironment Reconstructions – an introduction

A. M. W. Newton, K. J. Andresen, K. J. Blacker, R. Harding, E. Lebas
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Abstract

Since the last Special Publication on Seismic Geomorphology, the application of seismic data has grown substantially, revolutionising our understanding of basin evolution in the process. The papers presented here provide an insight into the direction of travel for seismic geomorphological analyses and how the science has evolved since 2007. New methods of data collection, new methods of processing and visualisation, and the integration of new types of complementary data, all have played a role in maximising the potential palaeo-environmental insights that can be derived from such studies. The submissions range across different geological settings, consisting of glacial, fluvial, volcanic, deltaic, and slope settings. Many of these studies integrate different methods, showing what can be achieved by combining multiple datasets to understand the subsurface. As more legacy datasets become available, the observed acceleration in seismic data availability and the associated publications will likely continue. Newer methods and the greater understanding of the subsurface are yielding a greater understanding on not just the palaeo-environments, but also what generates seismic reflectivity in the subsurface. The study of seismic geomorphology remains in its infancy, and much exciting research potential is yet to be realised.
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地震地貌学:地表下分析、数据整合与古环境重建--简介
自上次地震地貌学特别出版物以来,地震数据的应用已经大大增加,彻底改变了我们对盆地演化过程的理解。这里提出的论文提供了对地震地貌学分析的发展方向以及自2007年以来该科学如何发展的见解。新的数据收集方法,新的处理和可视化方法,以及新型互补数据的整合,都在最大限度地提高此类研究可能产生的古环境见解方面发挥了作用。提交的作品涵盖了不同的地质环境,包括冰川、河流、火山、三角洲和斜坡环境。其中许多研究整合了不同的方法,展示了通过结合多个数据集来了解地下的效果。随着越来越多的传统数据集的可用性,地震数据的可用性和相关出版物可能会继续加速。更新的方法和对地下的更深入的了解不仅使人们对古环境有了更深入的了解,而且还使人们对地下地震反射率的产生有了更深入的了解。地震地貌学的研究仍处于起步阶段,许多令人兴奋的研究潜力尚未实现。
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