航空热高光谱成像的熔岩湖断层地质带图

R. Witkosky, P. Adams, S. Akciz, K. Buckland, Janet Harvey, P. Johnson, D. Lynch, Frank Sousa, J. Stock, D. Tratt
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引用次数: 3

摘要

1999年Lavic湖断层上的Hector Mine地震产生了约5 m的最大右侧位移,但长期累积偏移仍未解决。为了确定被断层偏移的基岩,我们利用航空高光谱图像制作了一张带状图。高空间和光谱分辨率,加上缺乏重要的植被覆盖,有助于我们区分岩性单元,并创建具有监督和非监督分类的地质图。在一个小的测试点上进行监督分类的总体精度为71±1%,并且在我们的非监督分类中,单元之间的一些边界与先前发布的覆盖同一区域的地质图中的岩性边界具有良好的相关性。我们的地质断层带图将有助于解决沿Lavic湖断层基岩的总构造偏移。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Geologic swath map of the lavic lake fault from airborne thermal hyperspectral imagery
The 1999 Hector Mine earthquake on the Lavic Lake fault produced a maximum right-lateral displacement of ∼5 m, but the long-term cumulative offset remains unresolved. To identify bedrock that has been offset by the fault, we produced a swath map from airborne hyperspectral imagery. High spatial and spectral resolution, along with a lack of significant vegetation cover helped us differentiate lithologic units and create a geologic map with supervised and unsupervised classifications. Supervised classifications over a small test site had an overall accuracy of 71 ± 1%, and some of the boundaries between units in our unsupervised classification correlate well with lithologic boundaries from a previously published geologic map that covers the same area. Our geologic fault swath map will help to resolve the total tectonic offset of bedrock along the Lavic Lake fault.
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