GMT-Based Geological Mapping and Assessment of the Bathymetric Variations of the Kuril-Kamchatka Trench, Pacific Ocean

Polina Lemenkova
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引用次数: 14

Abstract

This manuscript summarizes the results of the geospatial analysis undertaken by means of Generic Mapping Tools (GMT). The comparative assessment of the bathymetry of the Kuril-Kamchatka hadal trench was performed for southern and northern segments separated by the Bussol Strait. The formation of the hadal trench is affected by the impacts of local geological and geophysical settings varying along the trench. The methodological approach is as follows. The profiling was undertaken using GMT modules ‘grdimage’, ‘grdtrack’ and ‘psxy’. The modelling consists of the collected data of 10706 observation samples from 52 profiles in southern part and 12726 from 62 profiles in the northern segment. The GMT modules ‘psrose’ and ‘pshistograms’ were used to plot histograms and rose diagrams visualizing bathymetric variables of depths. The geology was mapped using GMT modules ‘pscoast’, ‘grdcut’, ‘grdcontour’ and ‘psxy’ to plot lineaments and geological objects (ophiolites, faults, earthquakes, trench, magnetic anomalies, tectonic slabs, fracture zones and volcanoes). The base map is based on the ETOPO Global Relief Model. The comparison of the bathymetry shown variations in the northern and southern segments: southern part reaches -8,200 m maximal depths while northern has -7,800 m. This is influenced by the geological settings: earthquakes magnitude and seismisity are higher in the south-west. The submarine terraces and floodplains were observed at -4000 m depth forming landforms located southwards off the Bussol Strait. This geospatial analysis contributes to the development of the geological mapping with an example of the Kamchatka area, a region with high seismisity and repeated earthquakes.
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基于gmt的太平洋千岛-堪察加海沟水深变化地质填图与评价
本文总结了通过通用测绘工具(GMT)进行的地理空间分析的结果。对由布索尔海峡分隔的南段和北段千岛-堪察加海沟的水深进行了比较评估。海沟的形成受到沿海沟变化的当地地质和地球物理环境的影响。方法方法如下。使用GMT模块“grimage”、“grdtrack”和“psxy”进行分析。该模型由南部52条剖面的10706个观测样本和北部62条剖面的12726个观测样本组成。GMT模块“prose”和“pshistograms”用于绘制直方图和玫瑰图,以可视化深度的水深变量。地质图使用GMT模块“pscoast”、“grdcut”、“grdcontour”和“psxy”来绘制轮廓和地质对象(蛇绿岩、断层、地震、海沟、磁异常、构造板块、断裂带和火山)。底图基于ETOPO全球地形模型。水深对比显示南北段存在差异,南部最大深度为- 8200 m,北部最大深度为- 7800 m。这是受地质环境的影响:地震震级和地震活动性在西南部较高。海底梯田和洪泛平原在-4000米深度处被观测到,形成了布索尔海峡以南的地貌。这种地理空间分析有助于以堪察加地区为例进行地质制图的发展,堪察加地区是一个高地震活动和多次地震的地区。
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